Plant Community Classification of the Pakowki Sandhills

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Plant Community Classification of the Pakowki Sandhills and Sand Plains Prepared for: Resource Data Branch Alberta Sustainable Resource Development Edmonton, Alberta Prepared by: Valerie Coenen Jerry Bentz Geowest Environmental Consultants Ltd. Suite 203, 4208 – 97 Street Edmonton, Alberta Canada T6E 5Z9 January, 2003

Transcript of Plant Community Classification of the Pakowki Sandhills

Plant Community Classification of the Pakowki Sandhills and Sand Plains

Prepared for:

Resource Data Branch

Alberta Sustainable Resource Development

Edmonton, Alberta

Prepared by:

Valerie Coenen

Jerry Bentz

Geowest Environmental Consultants Ltd.

Suite 203, 4208 – 97 Street

Edmonton, Alberta

Canada

T6E 5Z9

January, 2003

Plant Community Classification of the Pakowki Sandhills and Sand Plains

Executive Summary The Resource Data Division of Alberta Sustainable Resource Development contracted Geowest Environmental Consultants Ltd. to produce a classification of sand dune and sand plain plant community types within the Grassland Natural Region of Alberta. This initiative is in support of the Alberta Natural Heritage Information Centre (ANHIC). ANHIC collects, evaluates and makes available data on elements of natural biodiversity in Alberta, including flora, fauna and native plant communities. ANHIC develops tracking lists of elements that are considered of high priority because they are considered rare or special in some way. ANHIC’s long-term goal is to develop a list of plant community types that occur throughout the province and to attempt to identify community types that require conservation initiatives.

The primary objective of this project was to develop a plant community classification of sand dune and sand plain plant communities of the Grassland Natural Region based on field survey, correlations with other surveys and any available previously-collected data. Furthermore, each identified community type was evaluated and assigned a preliminary provincial rank, based on its rarity/endemism or threats to its condition. This was accomplished by developing a sampling protocol and subsequently collecting field data on plant communities of the sand dune and sand plain landscapes of the Pakowki Sandhills. Furthermore, a comparison of defined plant community types to similar types described in previously conducted field surveys in similar landscapes in Alberta and adjacent provinces and states was completed. A similarity rating based on a scale provided by Corns (1983) was also provided.

This classification will provide a better understanding of plant community biodiversity in Alberta and will contribute to the development of a Canadian National Vegetation Classification (CNVC), the Canadian component of the International Classification of Ecological Communities (ICEC). The ICEC system has been adopted by the United States and it is a national standard for vegetation classification known as the U.S. National Vegetation Classification (USNVC).

An exhaustive literature search was completed, to locate references relating to sand dune and sand plain plant communities in Alberta. Literature related to other jurisdictions was also obtained, primarily for Saskatchewan, Montana, Idaho, Wyoming, North and South Dakota and Nebraska.

Field sampling occurred between July 26th and 30th, 2002 following a review of the sampling strategy with Alberta Sustainable Resource Development staff. In total 40 sampling plots were established, distributed throughout a range of community types and topographic positions. Survey sites were selected based on an initial review of the survey area, using aerial photographs and vegetation trends observed in the field.

Cluster and ordination analyses were performed on the field data resulting in 17 community types based on the hierarchical guidelines documented in the International Classification of Ecological Communities: Terrestrial Vegetation of the United States: Volume 1 – The National Classification System: Development, Status and Application (Grossman et al. 1998).

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Each community type identified from the analysis of the plot data was compared against floristically similar community types described for Alberta and other jurisdictions. A summary of the findings are provided as correlation tables, which compare the Pakowki Sandhills community types against community types described in literature based on Alberta and other jurisdictions, respectively. A similarity rating between the community types, based on Corns (1983) and recently applied by Strong (2002), was also provided in the tables. A discussion of the community types and associated literature was also provided.

All proposed community types were assigned a preliminary provincial ranking. Knowledge gaps were identified and strategies to address these gaps were provided. The information in this report can be used to update the community-tracking list by including new community types. Finally, this report can also be used to decide which community types require further studies and to prioritize these studies.

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Acknowledgements We wish to thank Lorna Allen and Ksenija Vujnovic (Alberta Natural Heritage Information Centre – Alberta Community Development) and Keith Ainsley (Resource Data Division – Alberta Sustainable Resource Development) for assistance throughout this project. The services of Kathy Tannas are also greatly appreciated for identification and verification of plant species. We are also grateful to Erin Anderson for assistance with fieldwork, as well as Dennis O’Leary and Terry Lang (Geowest Environmental Consultants Ltd.) who contributed to the successful completion of this project.

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Table of Contents Executive Summary......................................................................................................................................... i Acknowledgements ....................................................................................................................................... iii Table of Contents ……………………………………………………………………………………………..v List of Tables................................................................................................................................................ vii List of Figures ............................................................................................................................................. viii List of Plates................................................................................................................................................ viii List of Appendices......................................................................................................................................... ix 1.0 Introduction........................................................................................................... 1 1.1 Project Purpose and Objectives .......................................................................................... 1 1.2 Study Area Description ...................................................................................................... 1

1.2.1 Climate, landforms and topography.................................................................................. 1 1.2.2 Disposition and Land-Use .................................................................................................. 2

2.0 Methods.................................................................................................................. 2 2.1 Literature Search ................................................................................................................ 2 2.2 Field Sampling ................................................................................................................... 2 2.3 Plant Identification Verification......................................................................................... 3 2.4 Vegetation Data Analysis and Classification ..................................................................... 3 2.5 Taxonomic Considerations................................................................................................. 5 2.6 Cross-referencing of Proposed Community Types to Literature........................................ 5 2.7 Community Classification System ..................................................................................... 6 2.8 Evaluation and Assignment of Preliminary Provincial Ranking........................................ 6 3.0 Results and Discussion.......................................................................................... 7 3.1 Vegetation Data Analysis and Classification ..................................................................... 7 3.2 Preliminary Classification of Community Types ............................................................. 11

3.2.1 Description of Community Types......................................................................................... 12 3.2.1.1 Populus deltoides / Glycyrrhiza lepidota - Juncus balticus Association ......................... 13 3.2.1.2 Rosa woodsii / Sporobolus cryptandrus Association ....................................................... 15 3.2.1.3 Salix amygdaloides – Rosa woodsii / Juncus balticus – Sporobolus cryptandrus

Association ...................................................................................................................... 17 3.2.1.4 Elaeagnus commutata / Glycyrrhiza lepidota Association .............................................. 19 3.2.1.5 Elaeagnus commutata / Artemisia ludoviciana - Calamovilfa longifolia Association..... 21 3.2.1.6 Prunus virginiana / Calamovilfa longifolia Association ................................................. 23 3.2.1.7 Eurotia lanata / Stipa comata - Calamovilfa longifolia Association ............................... 25 3.2.1.8 Salix exigua / Glycyrrhiza lepidota - Juncus balticus Association .................................. 27 3.2.1.9 Glycyrrhiza lepidota - Calamovilfa longifolia Association ............................................. 29 3.2.1.10 Glycyrrhiza lepidota – Artemisia spp. - Stipa comata Association.................................. 31 3.2.1.11 Rumex venosus Association ............................................................................................. 33 3.2.1.12 Oryzopsis hymenoides – Sporobolus cryptandrus Association........................................ 35 3.2.1.13 Stipa comata – Oryzopsis hymenoides Association ......................................................... 37 3.2.1.14 Artemisia spp. - Stipa comata – Calamovilfa longifolia Association .............................. 39 3.2.1.15 Stipa comata – Cyperus schweinitzii – Calamovilfa longifolia Association.................... 41 3.2.1.16 Sporobolus cryptandrus – Calamovilfa longifolia –Oryzopsis hymenoides Association. 43 3.2.1.17 Artemisia cana / Stipa comata Association ..................................................................... 45

3.3 Cross-Referencing of Proposed Community Types with Literature ................................ 47

3.3.1 Populus deltoides / Glycyrrhiza lepidota - Juncus balticus Association .............................. 47

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3.3.2 Rosa woodsii / Sporobolus cryptandrus Association............................................................ 49 3.3.3 Salix amygdaloides – Rosa woodsii / Juncus balticus – Sporobolus cryptandrus

Association…………………………………………………………………………………50 3.3.4 Elaeagnus commutata / Glycyrrhiza lepidota Association................................................... 50 3.3.5 Elaeagnus commutata / Artemisia ludoviciana - Calamovilfa longifolia Association ......... 51 3.3.6 Prunus virginiana / Calamovilfa longifolia Association ...................................................... 53 3.3.7 Eurotia lanata / Stipa comata – Calamovilfa longifolia Association ................................... 54 3.3.8 Salix exigua / Glycyrrhiza lepidota - Juncus balticus Association....................................... 54 3.3.9 Glycyrrhiza lepidota - Calamovilfa longifolia Association .................................................. 56 3.3.10 Glycyrrhiza lepidota – Artemisia spp. - Stipa comata Association ...................................... 56 3.3.11 Rumex venosus Association.................................................................................................. 56 3.3.12 Oryzopsis hymenoides – Sporobolus cryptandrus Association ............................................ 57 3.3.13 Stipa comata – Oryzopsis hymenoides Association.............................................................. 57 3.3.14 Artemisia spp. - Stipa comata – Calamovilfa longifolia Association ................................... 59 3.3.15 Stipa comata – Cyperus schweinitzii – Calamovilfa longifolia Association ........................ 59 3.3.16 Sporobolus cryptandrus – Calamovilfa longifolia – Oryzopsis hymenoides Association .... 60 3.3.17 Artemisia cana / Stipa comata Association .......................................................................... 62

3.4 Assignment of a Preliminary Provincial Ranking and Identification of Knowledge

Gaps……………….......................................................................................................... 63 3.4.1 Populus deltoides / Glycyrrhiza lepidota - Juncus balticus Association .............................. 63 3.4.2 Rosa woodsii / Sporobolus cryptandrus Association............................................................ 64 3.4.3 Salix amygdaloides – Rosa woodsii / Juncus balticus – Sporobolus cryptandrus

Association .......................................................................................................................... 64 3.4.4 Elaeagnus commutata / Glycyrrhiza lepidota Association................................................... 65 3.4.5 Elaeagnus commutata / Artemisia ludoviciana - Calamovilfa longifolia Association ......... 65 3.4.6 Prunus virginiana / Calamovilfa longifolia Association ...................................................... 66 3.4.7 Eurotia lanata / Stipa comata – Calamovilfa longifolia Association ................................... 66 3.4.8 Salix exigua / Glycyrrhiza lepidota - Juncus balticus Association....................................... 66 3.4.9 Glycyrrhiza lepidota - Calamovilfa longifolia Association .................................................. 67 3.4.10 Glycyrrhiza lepidota – Artemisia spp. - Stipa comata Association ...................................... 67 3.4.11 Rumex venosus Association.................................................................................................. 67 3.4.12 Oryzopsis hymenoides – Sporobolus cryptandrus Association ............................................ 68 3.4.13 Stipa comata – Oryzopsis hymenoides Association.............................................................. 68 3.4.14 Artemisia spp. - Stipa comata – Calamovilfa longifolia Association.................................... 69 3.4.15 Stipa comata – Cyperus schweinitzii – Calamovilfa longifolia Association ........................ 69 3.4.16 Sporobolus cryptandrus – Calamovilfa longifolia – Oryzopsis hymenoides Association .... 70 3.4.17 Artemisia cana / Stipa comata Association .......................................................................... 70

4.0 Conclusion ........................................................................................................... 71 5.0 Literature Cited .................................................................................................. 72

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List of Tables Table 1. Summary of climatic data for the Dry Mixedgrass Natural Subregion………………….………….2 Table 2. Synonymy of plant species for the Pakowki Sandhills……………………………………………...5 Table 3. Hierarchical levels and definitions for the ICEC terrestrial vegetation classification

system……….……………………………………………………………………………………6 Table 4. Provincial conservation ranks and definitions………………………………….…………………...7 Table 5. Plant community types (associations) found in the Pakowki Sandhills.…………………………..11 Table 6. Numeric codes used to define different vegetation structural strata………………………………12

Table 7. Summary statistics for the Populus deltoides / Glycyrrhiza lepidota – Juncus balticus community type (n=3)…...…………………………………………………………………………...……..14

Table 8. Summary of site data for the Populus deltoides / Glycyrrhiza lepidota – Juncus balticus community type……..…………………………...……………………………………...……..14

Table 9. Summary statistics for the Rosa woodsii / Sporobolus cryptandrus community type (n=4)………………………………………………………...………….………………………16

Table 10. Summary of site data for the Rosa woodsii / Sporobolus cryptandrus community type……………………….…..…………………………………..………….…………………16

Table 11. Summary statistics for the Salix amygdaloides – Rosa woodsii / Juncus balticus – Sporobolus cryptandrus community type (n=2)……………………...…………………………………….18

Table 12. Summary of site data for the Salix amygdaloides – Rosa woodsii / Juncus balticus – Sporobolus cryptandrus community type……..………………….………………………………………...18

Table 13. Summary statistics for the Elaeagnus commutata / Glycyrrhiza lepidota community type (n=2)……….…………………………………………………………………………………...20

Table 14. Summary of site data for the Elaeagnus commutata / Glycyrrhiza lepidota community type………….…..……………………………………………………………………………...20

Table 15. Summary statistics for the Elaeagnus commutata / Artemisia ludoviciana – Calamovilfa longifolia community type (n=1)………………………………………………………………21

Table 16. Summary of site data for the Elaeagnus commutata / Artemisia ludoviciana – Calamovilfa longifolia community type……..………………………………………………………………22

Table 17. Summary statistics for the Prunus virginiana / Calamovilfa longifolia community type (n=4)……….…………………………………………………………………………………...24

Table 18. Summary of site data for the Prunus virginiana / Calamovilfa longifolia community type……..……………………………………………………….……………………………...24

Table 19. Summary statistics for the Eurotia lanata / Stipa comata – Calamovilfa longifolia community type (n=1)………………………………………………………………………………………26

Table 20. Summary of site data for the Eurotia lanata / Stipa comata – Calamovilfa longifolia community type……………………………………………………………………………………………..26

Table 21. Summary statistics for the Salix exigua / Glycyrrhiza lepidota – Juncus balticus community type (n=2)……………………………………………………….…………………………………...28

Table 22. Summary of site data for the Salix exigua / Glycyrrhiza lepidota – Juncus balticus community type……………………………………………………………………………………………..28

Table 23. Summary statistics for the Glycyrrhiza lepidota – Calamovilfa longifolia community type (n=1)……………………………………………………………………………………………30

Table 24. Summary of site data for the Glycyrrhiza lepidota – Calamovilfa longifolia community type……..………………………………………………………………………………………30

Table 25. Summary statistics for the Glycyrrhiza lepidota – Artemisia spp. – Stipa comata community type (n=2)……………………………………………………………………………………………32

Table 26. Summary of site data for the Glycyrrhiza lepidota – Artemisia spp. – Stipa comata community type……..………………………………………………………………………………………32

Table 27. Summary statistics for the Rumex venosus community type (n=2)………………………………33 Table 28. Summary of site data for the Rumex venosus community type….……………………...………..34

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Table 29. Summary statistics for the Oryzopsis hymenoides – Sporobolus cryptandrus community type (n=5)…………………………………………………………………………………………....36

Table 30. Summary of site data for the Oryzopsis hymenoides – Sporobolus cryptandrus community type……..……………………………………………………….……………………………...36

Table 31. Summary statistics for the Stipa comata – Oryzopsis hymenoides community type (n=2)……………………………………………………………………………………………38

Table 32. Summary of site data for the Stipa comata – Oryzopsis hymenoides community type……..………………………………………………………………………………………38

Table 33. Summary statistics for the Artemisia spp. – Stipa comata – Calamovilfa longifolia community type (n=3)………………………………………………………………………………………40

Table 34. Summary of site data for the Artemisia spp. – Stipa comata – Calamovilfa longifolia community type……..………………………………………………………………………………………40

Table 35. Summary statistics for the Stipa comata – Cyperus schweinitzii – Calamovilfa longifolia community type (n=1)…………………………………………………………………………41

Table 36. Summary of site data for the Stipa comata – Cyperus schweinitzii – Calamovilfa longifolia community type……..…………………………………………………………………………42

Table 37. Summary statistics for the Sporobolus cryptandrus – Calamovilfa longifolia – Oryzopsis hymenoides community type (n=4)…………………………………………………………….44

Table 38. Summary of site data for the Sporobolus cryptandrus – Calamovilfa longifolia – Oryzopsis hymenoides community type…...………………………………………………………………44

Table 39. Summary statistics for the Artemisia cana / Stipa comata community type (n=1)……………………………………………………………………………………………45

Table 40. Summary of site data for the Artemisia cana / Stipa comata community type…………………………………………..…………………………………………………46

List of Figures Figure 1. Cluster analysis of 40 plots collected July 2002…………………………………………………...8

Figure 2. Ordination diagram based on Detrended Correspondence Analysis (DCA) of 40 plots collected in July 2002…………………...……………………………………………………………………9

Figure 3. Biplot based on Detrended Correspondence Analysis (DCA) of sample plots (40) and plant species (65) collected at the Pakowki Sandhills in July 2002………………………………....10

List of Plates Plate 1. Populus deltoides / Glycyrrhiza lepidota – Juncus balticus community type (Western cottonwood /

wild licorice – wire rush) Plot 17………………………………………………………………13 Plate 2. Rosa woodsii / Sporobolus cryptandrus community type (Common wild rose / sand dropseed) Plot

016……………………………………………………..………………………………………15 Plate 3. Salix amygdaloides – Rosa woodsii / Juncus balticus – Sporobolus cryptandrus (Peach-leaf willow

– common wild rose / wire rush – sand dropseed) Plot 27...…………………………………..17 Plate 4. Elaeagnus commutata / Glycyrrhiza lepidota community type (Silverberry / wild licorice) Plot

18………………………………………………………………………………………………19 Plate 5. Elaeagnus commutata / Artemisia ludoviciana – Calamovilfa longifolia (Silverberry / prairie

sagewort – sand grass) Plot 32…………………………………………………………………21 Plate 6. Prunus virginiana / Calamovilfa longifolia community type (Chokecherry / sand grass) Plot

14………………………………………………………………………………………………23 Plate 7. Eurotia lanata / Stipa comata – Calamovilfa longifolia community type (Winterfat / needle and

thread – sand grass). Plot 40…………………………………………………………………...25 Plate 8. Salix exigua / Glycyrrhiza lepidota – Juncus balticus community type (Sandbar willow / wild

licorice – wire rush). Plot 7…………………………………………………………………….27 Plate 9. Glycyrrhiza lepidota – Calamovilfa longifolia community type (Wild licorice – sand grass) Plot

36………………………………………………………………………………………………29

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Plate 10. Glycyrrhiza lepidota – Artemisia spp. – Stipa comata community type (Wild licorice – sage – needle and thread) Plot 19……………………………………………………………………..31

Plate 11. Rumex venosus community type (Wild begonia) Plot 006………………………………………..33 Plate 12. Oryzopsis hymenoides – Sporobolus cryptandrus community type (Indian rice grass – sand

dropseed) Plot 35………………………………………………………………………………35 Plate 13. Stipa comata – Oryzopsis hymenoides community type (Needle and thread – Indian rice grass)

Plot 8…………………………………………………………………………………………...37 Plate 14. Artemisia spp. – Stipa comata – Calamovilfa longifolia community type (Sage – needle and

thread – sand grass) Plot 39……………………………………………………………………39 Plate 15. Stipa comata – Cyperus schweinitzii – Calamovilfa longifolia community type (Needle and thread

– sand nut-grass – sand grass) Plot 33………………………………………………………....41 Plate 16. Sporobolus cryptandrus – Calamovilfa longifolia – Oryzopsis hymenoides (Sand dropseed – sand

grass – Indian rice grass) Plot 4…………………….………………………………………….43 Plate 17. Artemisia cana / Stipa comata community type (Silver sagebrush / needle and thread). Plot

24………………………………………………………………………………………………45

List of Appendices Appendix 1. Glossary of Scientific and Common Plant Species Names Appendix 2. PC-ORD output from Detrended Correspondence Analysis of Plot Data Appendix 3. Species Code Descriptions Appendix 4. Correlation table with literature from within Alberta Appendix 5. Correlation table with literature from outside Alberta

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1.0 Introduction

1.1 Project Purpose and Objectives The Resource Data Division of Alberta Sustainable Resource Development contracted Geowest Environmental Consultants Ltd. to produce a classification of sand dune and sand plain plant community types within the Grassland Natural Region of Alberta. This initiative is in support of the Alberta Natural Heritage Information Centre (ANHIC). ANHIC collects, evaluates and makes available data on elements of natural biodiversity in Alberta, including flora, fauna and native plant communities. ANHIC develops tracking lists of elements that are considered of high priority because they are rare or special in some way. ANHIC’s long-term goal is to develop a list of plant community types that occur throughout the province and to attempt to identify community types that require conservation initiatives.

The primary objective of this project was to develop a plant community classification of sand dune and sand plain plant communities of the Grassland Natural Region based on field survey, correlations with other surveys and any available previously-collected data. Furthermore, each identified community type was evaluated and assigned a preliminary provincial rank, based on its rarity/endemism or threats to its condition. This was accomplished by developing a sampling protocol and subsequently collecting field data on plant communities of the sand dune and sand plain landscapes of the Pakowki Sandhills. Furthermore, a comparison of defined plant community types to similar types described in previously conducted field surveys in similar landscapes in Alberta and adjacent provinces and states was completed. A similarity rating based on a scale provided by Corns (1983) was also provided.

This classification will provide a better understanding of plant community biodiversity in Alberta and will contribute to the development of a Canadian National Vegetation Classification (CNVC), the Canadian component of the International Classification of Ecological Communities (ICEC). The ICEC system has been adopted by the United States and it is a national standard for vegetation classification known as the U.S. National Vegetation Classification (USNVC).

1.2 Study Area Description

1.2.1 Climate, landforms and topography The Pakowki Sandhills study area (Pakowki Sandhills) is located in the Dry Mixedgrass Natural Subregion (Achuff 1994) and is representative of sand dune and sand plain ecosystems of this subregion. The climate of the Dry Mixedgrass Subregion is the warmest and driest in all of Alberta (Table 1). It has a characteristic continental climate with cold winters, warm summers and relatively low precipitation. Total annual precipitation is generally 260-280 mm, the lowest summer precipitation values compared to every other subregion in the province (Alberta Environmental Protection 1997). Winds are often quite high and chinooks are regular events during the winter months.

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Table 1. Summary of climatic data for the Dry Mixedgrass Natural Subregion.

Mean Annual Temperature 4 oC Mean Summer Temperature 16 oC Mean Winter Temperature -7 oC Total Annual Precipitation 260 – 280 mm

The topography of the Pakowki Sandhills is gently rolling with relatively shallow slopes. Dune fields are located in both the northern and southern blocks, comprising approximately 50% of the northern block and 30% of the southern block. Both parabolic and longitudinal dunes with blowouts are present in the area (Shetsen 1987). Dunes consist of fine to medium grained sand and silt and reach depths of up to 7 metres. Hummocky stagnation till and ridged end moraine are also prevalent in the study area, with localized fluvial deposits along Irrigation and Canal creeks.

Elevations range from approximately 860 m at the former Pakowki lakeshore in the southwestern portion of the northern block, to 900 m in the northeastern corner. Elevations in the southern block range from approximately 860 m in the east to 915 m in the southeast.

1.2.2 Disposition and Land-Use The study area consists of a northern block adjacent to and east of the north end of Pakowki Lake and a southern block directly east of the south end of the lake. The Pakowki Sandhills are Crown land in right of the Province of Alberta, administered by Alberta Sustainable Resource Development. Current land uses consist primarily of cattle grazing on native and non-native pasture with some cultivation on adjacent parcels of privately owned land. There are approximately 10 grazing leaseholders within the Pakowki Sandhills.

2.0 Methods

2.1 Literature Search An exhaustive literature search was completed to locate references relating to sand dune and sand plain plant communities in Alberta. Literature related to other jurisdictions was also obtained, primarily for Saskatchewan, Montana, Idaho, Wyoming, North and South Dakota and Nebraska. Lorna Allen, of Alberta Community Development, also provided many references.

2.2 Field Sampling Field sampling occurred between July 26th and 30th, 2002 following a review of the sampling strategy with Alberta Sustainable Resource Development staff. In total 40 sampling plots were established, distributed throughout a range of community types and topographic positions. All survey sites were accessed on foot. Survey sites were selected based on an initial review of the survey area, using aerial photographs and vegetation trends observed in the field. In most instances, a minimum of three plots were established

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in each observed community type. This was not possible for certain community types, as their distribution was quite limited.

Vegetation and site description forms (RDB 2002-3 and RDB 2002-1 respectively) were completed at each site. The forms were completed using definitions and guidelines from Alberta Environmental Protection (1994). Percent cover of vascular plant species was visually estimated in each plot, using the relevé method. All dominant, codominant and diagnostic species were recorded. Each grass species encountered was collected for expert identification. Furthermore, unknown species were also collected for identification.

Plots were documented with a 35mm photograph to characterize the structure and composition of the plant community. The location of each survey site was determined using a Trimble GeoExplorer III unit and the locations were recorded on the site description forms. Furthermore, the location of each plot was marked on the aerial photographs. Each plot was located with a pinprick and circled and annotated on the back of the aerial photograph.

2.3 Plant Identification Verification Each grass species encountered was collected, as were any unknown species. Kathy Tannas, of Eastern Slopes Rangeland Seeds, verified these specimens. The plot forms and digital database were updated, to reflect Ms. Tannas’ findings.

2.4 Vegetation Data Analysis and Classification Vegetation data were entered into an Excel spreadsheet, comprising a matrix of field plot versus plant species abundance. The plant species were identified by stratum, as plant community structure was considered to be important in defining community types. The final database contained 40 plots and 65 species columns. The species columns may include duplicate species names, in cases where one species was found in more than one stratum (e.g. Elaeagnus commutata as both a tall and short shrub). However, the different strata were designated by a numeric value following the species code to allow for differentiation. The field data spreadsheet was then imported into PC ORD version 4.20, for classification analysis.

Cluster Analysis The vegetation classification incorporated all stages of plant succession and was not restricted to potential or predicted climax associations, following Braun-Blanquet (1965). Cluster analysis was used to allow for a more objective classification of sand dune and sand plain communities based on species composition. An hierarchical, agglomerative clustering technique (Farthest Neighbour Analysis) was used to help identify plant community types. This clustering method progressively combines plots/samples from an individual based on their similarity until all samples are in one group (similarity analysis).

Several clustering options available in PC ORD v.4.20 were explored and the group linkage method with the lowest percent chaining (maximum information) was selected for analysis (Farthest Neighbor). The Bray-Curtis (Sorensen) and Relative Sorensen

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distance measures were investigated and in combination with the Farthest Neighbor group linkage method, provided the lowest percent chaining values. Other distance measures were explored (Euclidean, Relative Euclidean), however, these measures had higher percent chaining values and seemed to introduce confusion into the clustering results.

Detrended Correspondence Analysis Detrended correspondence analysis was also investigated to help identify plant community types. Detrended correspondence analysis (DCA) is an indirect gradient analysis/ordination technique that ordinates both species and samples (plots) concurrently (Hill and Gauch 1980). Indirect gradient analysis/ordination obtains axes characterizing major trends of environmental and community variation from calculations based on the sample data (Whittaker 1978). Conversely, direct gradient analysis (DGA) relates species directly to measured environmental factors. DCA therefore does not include analysis of environmental factors (indirect analysis), however, this data is used to help interpret and explain the results.

DCA is based on reciprocal averaging (RA) or correspondence analysis (CA). Its main advantage is that through the detrending process, an ‘arch’ effect is eliminated that commonly distorts the results of RA and CA. PC-ORD offers several options prior to running the ordination:

��Down-weighting rare species and

��Rescaling of axes.

By down-weighting rare species in DCA, the abundances of species rarer than

Fmax/5

(where Fmax is the frequency of the most common species)

are down weighted in a relative amount to their frequency. Species that are more common than Fmax/5 are not down weighted (McCune and Mefford 1999). This option was selected for the analysis to capture the influence of less prevalent species in the sandhills plant community composition without overly distorting the results.

Another option presented in DCA is the rescaling of axes. Another drawback to CA (aside from the arch effect) is that the axis extremes can be condensed. In particular the distances between samples along an axis may not reflect the actual variation in species composition. This compression of the ends of the gradients is corrected in DCA by non-linear rescaling. The non-linear rescaling is based on the average standard deviation of species turnover and follows the original version of DECORANA in multiplying the standard deviations by 100 and shifting the scales such that all scores are positive (McCune and Mefford 1999). This option was selected, using the default values in PCORD v.4.20 to eliminate the compression of species/samples at the extremes of axes.

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2.5 Taxonomic Considerations Plant scientific names used in this report correspond to Moss (1983) and Alberta Environmental Protection (1993). However, there is a discrepancy between these references and those used for the classification of ecological communities used by Natureserve, which follows A synonymized checklist and atlas with biological attributes for the vascular flora of the United States, Canada and Greenland (Kartesz 1999). A summary of the discrepancies is provided in Table 2.

Table 2. Synonymy of plant species for the Pakowki Sandhills. Alberta Environmental

Protection (1993) Kartesz (1999) / Natureserve (2002) Common Name

Agropyron dasystachyum Elymus lanceolatus spp. lanceolatus Northern wheatgrass Agropyron sibiricum Agropyron fragile Sibirian wheatgrass Agropyron smithii Pascopyrum smithii western wheatgrass Carex lanuginosa Carex pellita Wooly sedge Coryphantha vivipara Escobaria vivipara Cushion cactus Eurotia lanata Krascheninnikovia lanata Winter fat Franseria acanthicarpa Ambrosia acanthicarpa Bur ragweed Helianthus subrhomboideus Helianthus pauciflorus ssp. subrhomboideus Rhombic leaved sunflower Lactuca pulchella Lactuca tatarica var. pulchella Common blue lettuce Lygodesmia rostrata Shinnersoseris rostrata Annual skeletonweed Oryzopsis hymenoides Achnatherum hymenoides Indian rice grass Smilacina stellata Maianthemum stellata Star-flowered Solomon’s seal Stipa comata Hesperostipa comata Needle and thread

The primary concern regarding the use of synonymous species names, is when searching Natureserve for ecological communities, using scientific plant names other than those of Kartesz (1999) will yield false results. For example, searching for Oryzopsis hymenoides within ecological communities will return no similar plant community types. However, searching for Achnatherum hymenoides will return numerous related alliances and associations.

Furthermore, no attempt to standardize species and community names was made when referencing other literature. Many recent reports from the United States describe community types using Kartesz (1999) as the taxonomic reference. As such, community names described in this report may not be completely synonymous with those stated in the literature, although they are referring to the same species. A glossary relating scientific and common plant species names is provided in Appendix 1.

2.6 Cross-referencing of Proposed Community Types to Literature Based on the review of existing literature and the development of a preliminary classification of sandhill community types, two cross-reference tables were developed. The first table cross-referenced proposed community types with similar community types previously described for Alberta. The second table cross-referenced proposed community types with similar community types identified in other jurisdictions, including Saskatchewan, Montana, Idaho, Wyoming, North and South Dakota and Nebraska. In both tables, the proposed community types are also given a similarity rating to the previously identified community types, based on a scale provided by Corns (1983) and also recently used by Strong (2002). The tables facilitated the identification of similar types as well as the identification of information gaps.

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

2.7 Community Classification System Community classification for the Pakowki Sandhills followed the hierarchical guidelines documented in the International Classification of Ecological Communities: Terrestrial Vegetation of the United States: Volume 1 – The National Classification System: Development, Status and Application (Grossman et al. 1998). The classification system outlined in this publication organizes terrestrial vegetation into five physiognomic and two floristic levels, as shown in Table 3.

Table 3. Hierarchical levels and definitions for the ICEC terrestrial vegetation classification system, adapted from (Grossman et al. 1998).

Hierarchical Level Definition Levels or Examples

Formation Class Formation class is defined based on the vegetation structure of the dominant, uppermost life form

1. Forest/Woodland: Trees with crowns overlapping (25-99% cover) 2. Shrubland: Shrubs generally >0.5 m height forming >25% cover. 3. Dwarf-Shrubland: Shrubs <0.5 m height forming >25% cover.4. Herbaceous: Graminoids, ferns and forbs dominant. 5. Non-vascular: Bryophytes, lichens and algae dominant. 6. Sparse: Abiotic substrate dominant

Formation Subclass Subclass is based on the growth-form characteristics of the dominant life form, predominantly leaf phenology

Evergreen, deciduous, mixed-deciduous for Forest/Woodland, Shrubland and Dwarf-Shrubland Classes. Perennial and Annual for the Herbaceous class. Substrate characteristics (e.g. rock, sand, cobbles, etc.) are used for the Sparse vegetation class.

Formation Group Group is defined based on leaf characters, the presence of a woody stratum or topographic position.

Broad leaf or needle leaf used for Forest/Woodland, Shrubland and Dwarf-Shrubland classes. Presence of a woody stratum separates groups in Herbaceous and Non-vascular classes. Sparse vegetation communities are separated based on topographic position (e.g. shore, cliffs, dunes, etc).

Formation Subgroup

Subgroup is defined based on the level of anthropogenic disturbance.

All groups divide each community type into a Natural/Near Natural, Semi-Natural or Planted/Cultivated subgroup. Ph

ysio

gnom

ic L

evel

s

Formation Formations represent vegetation types that share a definite physiognomy or structure within broadly defined environmental factors, landscape positions or hydrological regimes.

e.g. Temperate or sub-polar deciduous shrubland

Alliance Alliance is a physiognomically uniform groups of plant associations sharing one or more diagnostic species, which as a rule are found in the uppermost stratum of the vegetation

e.g. Populus tremuloides – Picea glauca / Linnea borealis Forest Alliance e.g. Carex utriculata Herbaceous Alliance

Flor

istic

Lev

els

Association Association is the lowest level of the hierarchy and is defined as a plant community type of definite floristic composition, uniform habitat conditions and uniform physiognomy.

Nomenclature is based on the diagnostic species. Species occurring in the uppermost stratum are listed first (separated by a hyphen if in the same stratum or a slash if in a different strata) followed successively by those occurring in lower levels. Within the same stratum, the order of species names generally reflects decreasing levels of dominance or constancy.

2.8 Evaluation and Assignment of Preliminary Provincial Ranking Each community type was evaluated and assigned a preliminary provincial ranking. The ranking system used is based on The Nature Conservancy’s species ranking system (Grossman et al. 1994), as used by ANHIC (Allen 2002). The two primary criteria for

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

developing community ranks are the total number of occurrences and the total area of each community, range-wide. Measures of geographic range, trends in status and immediate threats to the community’s persistence are also considered in ranking. Preliminary ranks range from S1 (rare) to S5 (wide-spread) and are defined in Table 4.

Table 4. Provincial conservation ranks and definitions (adapted from Allen 2002). Preliminary

Rank* Criteria

G1(S1) Five or fewer occurrences or very few remaining hectares G2(S2) Six to 20 occurrences or few remaining hectares G3(S3) 21 to 100 occurrences. May be rare and local throughout its range or found locally,

even abundantly, in a restricted range (e.g. a single western province or physiographic region in the East)

G4(S4) Apparently secure globally (State / Province wide), though it may be quite rare in parts of its range, especially at the periphery.

G5(S5) Demonstrably secure globally (State / Province wide) thought it might be quite rare in parts of its range, especially at the periphery.

GU(SU) Status is uncertain GH(SH) Historic. Presumed eliminated in the province with little or no likelihood that it will be

rediscovered. There may be the potential for restoration. GX(SX) Believed to be eliminated throughout its range, with virtually no likelihood that it will

be rediscovered (e.g. American Chestnut Forest) GP(SP) Potentially exists. Further documentation needed. G?(S?) Element is not yet ranked.

MODIFIERS Q Can be added to any global rank to denote questionable taxonomy (e.g. G2Q= 6 to 20

known occurrences but questions exist concerning the classification of this type). ? Can be added to any rank to denote an inexact numeric rank (e.g. G1? = Believed to be

5 or less occurrences but some doubt still exists concerning status). *Ranks can be combined to indicate a range (e.g. G2G3 = May be between 6 to 100 occurrences throughout range but the exact status is uncertain). Combined ranks indicate a larger margin of error than ranks assigned a “?” qualifier.

Where information was available, plant communities from the Pakowki Sandhills were compared with any similar communities found within the subregion, in other regions of the province, or from other provinces or states.

3.0 Results and Discussion

3.1 Vegetation Data Analysis and Classification Results from the agglomerative clustering methods were examined to determine the ecological meaning of the clusters and interpret the community types (Figure 1). Examination of the resulting dendrogram revealed numerous small groups. Several community types were consistently clustered together, particularly:

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

��Plots with high Prunus virginiana cover (plots 10, 13, 14 and 34) ��Plots with high Rosa woodsii cover (and little grass cover) (plots 5, 16 and 26) ��Plots with high Salix amygdaloides - Rosa woodsii cover (plots 27 and 28) ��Plots with high Salix exigua / Glycyrrhiza lepidota cover (plots 2 and 7) ��Plots with high Elaeagnus commutata cover (plots 11, 18 and 32) ��Plots with high Rumex venosus cover (plots 6 and 30)

SAND DUNE COMMUNITIES

Distance (Objective Function)

Information Remaining (%)

5.4E-03

100

1.9E+00

75

3.8E+00

50

5.7E+00

25

7.6E+00

0

13537342329315261627288152125101413342719369171263011321820222438333940

Figure 1. Cluster analysis of 40 plots collected July 2002. Linkage method: Farthest Neighbour. Distance Measure: Bray-Curtis (Sorensen). Percent Chaining=2.82%.

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

However, other community types, particularly grass and forb-dominated communities could not be easily discerned based on the cluster analysis alone.

Detrended correspondence analysis (DCA) helped to group plots with similar species compositions and also confirmed some of the community types observed from the grouping of plots in the cluster analysis. Approximately 17 groups were recognized based on the ordination of plots and species, with several ‘groups’ comprising only one sample plot as shown in Figure 2 and Figure 3. Output from the PC-ORD DCA is provided in Appendix 2.

1

2

3

4

5

6

7

8

9

10

11

12

13

14

15

16

17

18

19

20

21

22

23

24

25

26

27

28

29

30

31

32

33

34

35

36

37

38

39

40

SAND DUNE COMMUNITIES

Axis 1

Axis

2

ë=0.786

ë=0.663

Community TypesCommunity Types

Artemisia cana / Stipa comataArtemisia cana / Stipa comata

Artemisia spp. - Stipa comata - Calamovilfa longifoliaArtemisia spp. - Stipa comata - Calamovilfa longifolia

Elaeagnus commutata / Artemisia ludoviciana - Calamovilfa longifoliaElaeagnus commutata / Artemisia ludoviciana - Calamovilfa longifolia

Elaeagnus commutata / Glycyrrhiza lepidotaElaeagnus commutata / Glycyrrhiza lepidota

Eurotia lanata / Stipa comataEurotia lanata / Stipa comata

Glycyrrhiza lepidota - Artemisia spp. - Stipa comataGlycyrrhiza lepidota - Artemisia spp. - Stipa comata

Glycyrrhiza lepidota - Calamovilfa longifoliaGlycyrrhiza lepidota - Calamovilfa longifolia

Populus deltoides / Glycyrrhiza lepidota - Juncus balticusPopulus deltoides / Glycyrrhiza lepidota - Juncus balticus

Rosa woodsii / Sporobolus cryptandrusRosa woodsii / Sporobolus cryptandrus

Salix amygdaloides - Rosa woodsii / Juncus balticus - Sporobolus cryptandrusSalix amygdaloides - Rosa woodsii / Juncus balticus - Sporobolus cryptandrus

Salix exigua / Glycyrrhiza lepidota - Juncus balticusSalix exigua / Glycyrrhiza lepidota - Juncus balticus

Sporobolus cryptandrus - Calamovilfa longifolia - Oryzopsis hymenoidesSporobolus cryptandrus - Calamovilfa longifolia - Oryzopsis hymenoides

Stipa comata - Cyperus schweinitziiStipa comata - Cyperus schweinitzii

Stipa comata - Oryzopsis hymenoidesStipa comata - Oryzopsis hymenoides

Rumex venosusRumex venosus

Oryzopsis hymenoides - Sporobolus cryptandrusOryzopsis hymenoides - Sporobolus cryptandrus

Prunus virginiana / Calamovilfa longifoliaPrunus virginiana / Calamovilfa longifolia Figure 2. Ordination diagram based on Detrended Correspondence Analysis (DCA) of 40 plots collected in July 2002. Total variance in the species data (inertia) = 6.2854. Eigenvector 1 = 0.786 or 12.5% of the total variance in the species data. Eigenvector 2 = 0.663 or 10.54% of the total variance in the species data.

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

1

2

3

4

5

6

7

8

9

10

11

12

13

14

15

16

17

18

19

20

21

22

23

24

25

26

27

28

29

30

31

3233

34

35

36

37

38

39

40

POPUDEL1

POPUDEL2

SALIAMY3

ELEACOM4

SALIAMY4

PRUNVIR4

SALIAMY5

ARTECAN5

PRUNVIR5

ELAECOM5

SALIEXI5

EUROLAN5

ROSAWOO5

ARTECAM6

ARTELUD6

ARTEFRI6

RUMEVEN6

GLYCLEP6

CYPESCH7

JUNCBAL7

STIPCOM7

ORYZHYM7

SPORCRY7

CALALON7

SAND DUNE COMMUNITIES

Axis 1

Axis

2

Community TypesCommunity Types

Artemisia cana / Stipa comataArtemisia cana / Stipa comata

Artemisia spp. - Stipa comata - Calamovilfa longifoliaArtemisia spp. - Stipa comata - Calamovilfa longifolia

Elaeagnus commutata / Artemisia ludoviciana - Calamovilfa longifoliaElaeagnus commutata / Artemisia ludoviciana - Calamovilfa longifolia

Elaeagnus commutata / Glycyrrhiza lepidotaElaeagnus commutata / Glycyrrhiza lepidota

Eurotia lanata / Stipa comataEurotia lanata / Stipa comata

Glycyrrhiza lepidota - Artemisia spp. - Stipa comataGlycyrrhiza lepidota - Artemisia spp. - Stipa comata

Glycyrrhiza lepidota - Calamovilfa longifoliaGlycyrrhiza lepidota - Calamovilfa longifolia

Populus deltoides / Glycyrrhiza lepidota - Juncus balticusPopulus deltoides / Glycyrrhiza lepidota - Juncus balticus

Rosa woodsii / Sporobolus cryptandrusRosa woodsii / Sporobolus cryptandrus

Salix amygdaloides - Rosa woodsii / Juncus balticus - Sporobolus cryptandrusSalix amygdaloides - Rosa woodsii / Juncus balticus - Sporobolus cryptandrus

Salix exigua / Glycyrrhiza lepidota - Juncus balticusSalix exigua / Glycyrrhiza lepidota - Juncus balticus

Sporobolus cryptandrus - Calamovilfa longifolia - Oryzopsis hymenoidesSporobolus cryptandrus - Calamovilfa longifolia - Oryzopsis hymenoides

Stipa comata - Cyperus schweinitziiStipa comata - Cyperus schweinitzii

Stipa comata - Oryzopsis hymenoidesStipa comata - Oryzopsis hymenoides

Rumex venosusRumex venosus

Oryzopsis hymenoides - Sporobolus cryptandrusOryzopsis hymenoides - Sporobolus cryptandrus

Prunus virginiana / Calamovilfa longifoliaPrunus virginiana / Calamovilfa longifolia

ë=0.786

ë=0.663

Figure 3. Biplot based on Detrended Correspondence Analysis (DCA) of sample plots (40) and plant species (65) collected at the Pakowki Sandhills in July 2002.

Data were summarized for the resulting community types, including mean percent cover of plant species and surface substrates, standard deviation and standard error and species prominence. This information is presented in section 3.2.1.

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

3.2 Preliminary Classification of Community Types A total of 17 plant communities (associations) were found to occur in the Pakowki Sandhills. The majority of communities were ranked SU or S2S3. Community types included all classes, except Non-Vascular and are presented in Table 5 by major physiognomic level.

Table 5. Plant community types (associations) found in the Pakowki Sandhills. Terrestrial Associations Forest/Woodland Deciduous Forest/Woodland

Cold Deciduous Forest/Woodland Natural / Near Natural

Temperate or subpolar cold deciduous forest/woodland

Populus deltoides Forest/Woodland Alliance Populus deltoides / Glycyrrhiza lepidota - Juncus balticus Shrubland Deciduous Shrubland

Cold Deciduous Shrubland Natural / Near Natural

Temperate cold deciduous shrubland Rosa woodsii Shrubland Alliance Rosa woodsii / Sporobolus cryptandrus Salix amygdaloides Shrubland Alliance Salix amygdaloides – Rosa woodsii / Juncus balticus –

Sporobolus cryptandrus Elaeagnus commutata Shrubland Alliance Elaeagnus commutata / Glycyrrhiza lepidota Elaeagnus commutata Shrubland Alliance Elaeagnus commutata / Artemisia ludoviciana - Calamovilfa

longifolia Prunus virginiana Shrubland Alliance Prunus virginiana / Calamovilfa longifolia

Dwarf shrubland Evergreen dwarf shrubland

Extremely xeromorphic evergreen dwarf shrubland Natural / Near Natural

Extremely xeromorphic evergreen subdesert dwarf-shrubland

Eurotia lanata Dwarf-Shrubland Alliance Eurotia lanata / Stipa comata – Calamovilfa longifolia Herbaceous Vegetation

Perennial forb vegetation Temperate or subpolar perennial forb

Natural / Near Natural Low temperate or subpolar perennial forb

Glycyrrhiza lepidota Herbaceous Alliance Salix exigua / Glycyrrhiza lepidota - Juncus balticus Glycyrrhiza lepidota Herbaceous Alliance Glycyrrhiza lepidota - Calamovilfa longifolia Glycyrrhiza lepidota – Artemisia spp. Herbaceous Alliance

Glycyrrhiza lepidota – Artemisia spp. - Stipa comata

Rumex venosus Herbaceous Alliance Rumex venosus Herbaceous Vegetation Perennial Graminoid Vegetation

Temperate or sub-polar grasslands Natural / Near Natural

Medium-tall bunch temperate or sub-polar grasslands

Oryzopsis hymenoides Herbaceous Alliance Oryzopsis hymenoides – Sporobolus cryptandrus Stipa comata Bunch Herbaceous Alliance Stipa comata - Oryzopsis hymenoides

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

Table 5 (cont.). Plant community types (associations) found in the Pakowki Sandhills. Terrestrial Associations Herbaceous Vegetation Perennial Graminoid Vegetation

Temperate or sub-polar grasslands Natural / Near Natural

Medium-tall sod temperate or sub-polar grasslands

Stipa comata Bunch Herbaceous Alliance Artemisia spp. - Stipa comata – Calamovilfa longifolia Herbaceous Vegetation Perennial Graminoid Vegetation

Temperate or sub-polar grasslands Natural / Near Natural

Tall sod temperate or sub-polar grasslands Calamovilfa longifolia Herbaceous Alliance Stipa comata – Calamovilfa longifolia – Cyperus schweinitzii

Herbaceous Vegetation Perennial graminoid vegetation

Temperate or subpolar grassland with a sparse shrub layer

Natural / Near Natural Medium-tall temperate or subpolar grassland Sporobolus cryptandrus Herbaceous Alliance Sporobolus cryptandrus – Calamovilfa longifolia – Oryzopsis

hymenoides Herbaceous Vegetation Perennial graminoid vegetation

Temperate or subpolar grassland with a sparse shrub layer

Natural / Near Natural Medium-tall temperate or subpolar grassland with a sparse needle-leaved or microphyllous evergreen shrub layer

Artemisia cana Shrub Herbaceous Alliance Artemisia cana / Stipa comata

3.2.1 Description of Community Types A summary of the 17 community types (associations) found in the Pakowki Sandhills is described below. Representative photos for each community type are provided as Plates 1 – 17. A full listing of species codes is provided in Appendix 3. Table 6 provides an explanation of strata codes, which follow the seven-letter species code.

Table 6. Numeric codes used to define different vegetation structural strata.

Code Stratum 1 Main Canopy Trees 2 Understorey Trees 3 Tall Shrubs 4 Medium Shrubs 5 Low Shrubs 6 Forbs / Herbs 7 Grasses

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3.2.1.1 Populus deltoides / Glycyrrhiza lepidota - Juncus balticus Association Western cottonwood / wild licorice – wire rush

Plate 1. Populus deltoides / Glycyrrhiza lepidota – Juncus balticus community type (Western cottonwood / wild licorice – wire rush) Plot 17.

This community was dominated by Populus deltoides, but occurred in association with Populus tremuloides or Salix amygdaloides, in tree form. Understorey shrubs such as Rosa woodsii, Salix exigua and Elaeagnus commutata were occasionally present, though they typically did not exceed more than 5 % cover. Glycyrrhiza lepidota was present at all sites and ranged in cover between 2 % and 20 % cover. Thermopsis rhombifolia, Chenopodium fremontii, C. pratericola, Artemisia ludoviciana and Solidago missouriensis were also typical forb species. Juncus balticus was the dominant graminoid species, although Poa pratensis and Bouteloua gracilis were also commonly present. Table 7 summarizes the species composition, mean percent cover, standard error and species prominence for this community type. Species prominence was calculated using the following formula:

mean % cover x % presence

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

Table 7. Summary statistics for the Populus deltoides / Glycyrrhiza lepidota - Juncus balticus community type (n = 3).

Species Mean %

Cover Standard

Error Presence Prominence

POPUDEL2 23.33 23.33 1 40.4 POPUDEL1 36.67 17.64 3 36.7 POPUTRE2 13.33 13.33 1 23.1 SALIAMY3 8.33 8.33 1 14.4 GLYCLEP6 12.33 5.36 3 12.3 JUNCBAL7 11.67 4.41 3 11.7 CHENPRA6 2.67 1.20 3 2.7 THERRHO6 2.00 1.53 2 2.4 POAPRA7 2.00 1.53 2 2.4 CHENFRE6 1.67 0.33 3 1.7 DESCSOP6 1.00 0.50 3 1.0 ROSAWOO5 0.67 0.33 2 0.8 SOLIMIS6 0.67 0.17 3 0.7 ARTELUD6 0.50 0.29 2 0.6 ELAECOM5 0.33 0.33 1 0.6 BOUTGRA7 0.33 0.33 1 0.6

Species Mean %

Cover Standard

Error Presence Prominence

TARAOFF6 0.33 0.17 2 0.4 CRYPFEN6 0.33 0.17 2 0.4 SALIEXI5 0.17 0.17 1 0.3 CLEOSER6 0.17 0.17 1 0.3 HELISUB6 0.17 0.17 1 0.3 EQUIHYE6 0.17 0.17 1 0.3 TRAGDUB6 0.17 0.17 1 0.3 CHENSUB6 0.17 0.17 1 0.3 SMILSTE6 0.17 0.17 1 0.3 SOLICAN6 0.17 0.17 1 0.3 HETEVIL6 0.17 0.17 1 0.3 ELYMCAN7 0.17 0.17 1 0.3

DECAY9 0.50 0.00 MINERAL9 11.67 4.41 ORG9 50.00 5.77

This community was found in localized depressions between dunes and in more open sand plain areas. Soils were sandy, but with some organic matter buildup on the soil surface. A summary of site data is provided in Table 8.

Table 8. Summary of site data for the Populus deltoides / Glycyrrhiza lepidota - Juncus balticus community type.

Plot Elevation Aspect Slope DrainageSite

Position Surface Shape

Moisture Regime

Nutrient Regime

9 870 n/a 0 Rapid Level Straight Submesic Mesotrophic 12 863 n/a 0 Rapid Level Straight Subxeric Submesotrophic

17 864 n/a 0 Rapid Level Straight Subxeric Submesotrophic

This community was typically well used by both livestock and wild ungulates, with many pellet groups observed.

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

3.2.1.2 Rosa woodsii / Sporobolus cryptandrus Association Common wild rose / sand dropseed

Plate 2. Rosa woodsii / Sporobolus cryptandrus community type (Common wild rose / sand dropseed) Plot 16.

This community was dominated by Rosa woodsii in the shrub layer, although other species such as Ribes oxyacanthoides and Salix exigua were also present. Glycyrrhiza lepidota was the dominant forb species with a cover ranging up to 30 %. Other typical forb species included Chenopodium pratericola, C. fremontii and Heterotheca villosa. Sporobolus cryptandrus was the dominant graminoid species, although Calamovilfa longifolia was quite common, while Oryzopsis hymenoides was occasionally present. Table 9 summarizes the species composition, mean percent cover, standard error and species prominence for this community type.

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

Table 9. Summary statistics for the Rosa woodsii / Sporobolus cryptandrus community type (n = 4).

Species Mean %

Cover Standard

Error Presence Prominence

ROSAWOO5 42.50 12.08 4 42.5 SPORCRY7 12.50 4.08 4 12.5 GLYCLEP6 7.75 7.01 3 8.9 RIBEOXY5 2.50 2.50 1 5.0 ARTELUD6 2.50 2.50 1 5.0 CALALON7 3.00 2.38 2 4.2 THERRHO6 0.50 0.50 1 1.0 CHENPRA6 0.75 0.35 4 0.8 SOLIMIS6 0.50 0.29 2 0.7 HELIANN6 0.38 0.24 2 0.5 ORYZHYM7 0.38 0.24 2 0.5 PRUNVIR5 0.25 0.25 1 0.5 AGRODAS7 0.25 0.25 1 0.5

Species Mean %

Cover Standard

Error Presence Prominence

AGROSIB7 0.25 0.25 1 0.5 CARELAN7 0.25 0.25 1 0.5 HETEVIL6 0.38 0.00 4 0.4 SALIEXI5 0.25 0.48 2 0.4 LYGOROS6 0.25 0.14 2 0.4 CHENFRE6 0.25 0.13 3 0.3 CORYVIV6 0.13 0.13 1 0.3 LATUPUL6 0.13 0.13 1 0.3 ELYMCAN7 0.13 0.13 1 0.3 CHENSUB6 0.13 0.14 2 0.2 RUMEVEN6 0.13 0.14 2 0.2 MINERAL9 17.50 5.95 ORG9 17.63 8.45

This community was typically found on the north to southeast, leeward slopes of partially stabilized dunes. Soils were sandy, with some organic matter buildup on the soil surface and some exposed sand. A summary of site data is provided in Table 10.

Table 10. Summary of site data for the Rosa woodsii / Sporobolus cryptandrus community type (n = 4).

Plot Elevation Aspect Slope Drainage Site PositionSurface Shape

Moisture Regime

Nutrient Regime

5 898 104 45 Rapid Upper Slope Straight Xeric Submesotrophic 16 866 5 18 Rapid Middle Slope Straight Subxeric Submesotrophic 23 886 158 10 Rapid Middle Slope Straight Xeric Submesotrophic 26 883 35 15 Rapid Upper Slope Straight Subxeric Submesotrophic

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

3.2.1.3 Salix amygdaloides – Rosa woodsii / Juncus balticus – Sporobolus cryptandrus Association Peach-leaf willow – common wild rose / wire rush – sand dropseed

Plate 3. Salix amygdaloides – Rosa woodsii / Juncus balticus – Sporobolus cryptandrus (Peach-leaf willow – common wild rose / wire rush – sand dropseed) Plot 27.

This community was co-dominated by Salix amygdaloides and Rosa woodsii in the shrub layer. Juncus balticus and Sporobolus cryptandrus were the dominant graminoids, although Glycyrrhiza lepidota and Thermopsis rhombifolia constituted a substantial forb cover at certain sites. Other typical species, though with low percent cover, included Prunus virginiana, Chenopodium pratericola and C. fremontii. Table 11 summarizes the species composition, mean percent cover, standard error and species prominence for this community type.

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

Table 11. Summary statistics for the Salix amygdaloides – Rosa woodsii / Juncus balticus – Sporobolus cryptandrus community type (n = 2).

Species Mean %

Cover Standard

Error Presence Prominence

SALIAMY4 40.00 10.00 2 40.0 ROSAWOO5 40.00 0.00 2 40.0 GLYCLEP6 22.50 22.50 1 31.8 SPORCRY7 25.00 0.00 2 25.0 THERRHO6 22.50 2.50 2 22.5 JUNCBAL7 15.00 0.00 2 15.0 PRUNVIR5 1.00 0.00 2 1.0 CHENPRA6 1.00 0.00 2 1.0 CHENFRE6 1.00 0.00 2 1.0

Species Mean %

Cover Standard

Error Presence Prominence

SOLIMIS6 0.50 0.50 1 0.7 AGROSIB7 0.50 0.50 1 0.7 POAPRA7 0.50 0.50 1 0.7 ELYMCAN7 0.50 0.50 1 0.7 DESCSOP6 0.50 0.00 2 0.5 TRAGDUB6 0.25 0.25 1 0.4 HETEVIL6 0.25 0.25 1 0.4 AGRODAS7 0.25 0.25 1 0.4

DECAY9 7.50 2.50 MINERAL9 12.50 2.50

This community was found in relatively level sand plain sites, with rapidly to well drained sandy soils. Organic matter buildup on the soil surface was commonly greater than 30% cover, though exposed sand was still at the soil surface. A summary of site data is provided in Table 12.

Table 12. Summary of site data for the Salix amygdaloides – Rosa woodsii / Juncus balticus – Sporobolus cryptandrus community type (n = 2).

Plot Elevation Aspect Slope Drainage Site PositionSurface Shape

Moisture Regime

Nutrient Regime

27 875 n/a 0 Well Level Straight Subxeric Submesotrophic 28 874 n/a 0 Rapid Level Straight Xeric Submesotrophic

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

3.2.1.4 Elaeagnus commutata / Glycyrrhiza lepidota Association Silverberry / wild licorice

Plate 4. Elaeagnus commutata / Glycyrrhiza lepidota community type (Silverberry / wild licorice) Plot 18.

This community was dominated by Elaeagnus commutata in the mid-shrub-layer. Glycyrrhiza lepidota was the dominant forb, averaging about 15% cover. Other typical forbs that may have a low percent cover included: Artemisia ludoviciana, Thermopsis rhombifolia, Cryptantha fendleri and Chenopodium pratericola. Juncus balticus was the dominant graminoid species, although other species such as Stipa comata, Koeleria macratha and Agropyron dasystachyum also occurred. Table 13 summarizes the species composition, mean percent cover, standard error and species prominence for this community type.

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

Table 13. Summary statistics for the Elaeagnus commutata / Glycyrrhiza lepidota community type (n = 2).

Species Mean %

Cover Standard

Error Presence Prominence

ELAECOM5 50.00 15.00 2 50.0 GLYCLEP6 15.00 10.00 2 15.0 SALIEXI5 10.00 10.00 1 14.1 JUNCBAL7 10.00 10.00 1 14.1 ELEACOM4 2.50 2.50 1 3.5 ARTELUD6 2.50 2.50 1 3.5 STIPCOM7 2.75 2.25 2 2.8 THERRHO6 1.50 1.50 1 2.1 POAPRA7 1.50 1.50 1 2.1 PRUNVIR5 1.00 1.00 1 1.4 SOLIMIS6 1.00 1.00 1 1.4 LYGOROS6 1.00 1.00 1 1.4 CYPESCH7 1.00 1.00 1 1.4

Species Mean %

Cover Standard

Error Presence Prominence

SPORCRY7 1.00 1.00 1 1.4 CALALON7 1.00 1.00 1 1.4 KOELMAC7 1.25 0.75 2 1.3 AGRODAS7 1.25 0.75 2 1.3 CRYPFEN6 0.75 0.25 2 0.8 HETEVIL6 0.75 0.25 2 0.8 ROSAWOO5 0.50 0.50 1 0.7 CHENPRA6 0.50 0.00 2 0.5 CHENFRE6 0.25 0.25 1 0.4 HELIANN6 0.25 0.25 1 0.4

DECAY9 0.25 0.25 MINERAL9 15.00 5.00 ORG9 20.00 10.00

This community types was found in depressional locations on the windward side of dunes, with well-drained soils. Surface organic matter ranged from 10 % to 30 %, with only 10 % to 20% exposed sand at the soil surface. A summary of site data is provided in Table 14.

Table 14. Summary of site data for the Elaeagnus commutata / Glycyrrhiza lepidota community type (n = 2).

Plot Elevation Aspect Slope Drainage Site PositionSurface Shape

Moisture Regime

Nutrient Regime

11 864 n/a 0 Well Depression Straight Subxeric Mesotrophic 18 863 n/a 0 Well Depression Concave Subxeric Submesotrophic

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

3.2.1.5 Elaeagnus commutata / Artemisia ludoviciana - Calamovilfa longifolia Association Silverberry / prairie sagewort – sand grass

Plate 5. Elaeagnus commutata / Artemisia ludoviciana – Calamovilfa longifolia (Silverberry / prairie sagewort – sand grass) Plot 32.

This community type was dominated by Elaeagnus commutata in the mid-shrub layer. Calamovilfa longifolia was the dominant graminoid, with a cover in this plot of 25 %. Other graminoid species included Stipa comata, Cyperus schweinitzii, Sporobolus cryptandrus, Koeleria macrantha and Agropyron dasystachyum generally with covers of less than 1%. Artemisia ludoviciana was the dominant forb with about 5 % cover, although other species also occur including Solidago missouriensis and Heterotheca villosa. Table 15 summarizes the species composition and percent cover for this community type

Table 15. Summary statistics for the Elaeagnus commutata / Artemisia ludoviciana / Calamovilfa longifolia community type (n = 1).

Species Percent Cover

ELAECOM5 40 CALALON7 25 ARTELUD6 5 STIPCOM7 5 PRUNVIR5 1 SOLIMIS6 1 HETEVIL6 1 CYPESCH7 1 SPORCRY7 1 CRYPFEN6 0.5

Species Percent Cover

CHENPRA6 0.5 CHENFRE6 0.5 LYGOROS6 0.5 OPUNPOL6 0.5 HELIANN6 0.5 KOELMAC7 0.5 AGRODAS7 0.5

DECAY9 0.5 MINERAL9 10 ORG9 5

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

This community type was found in a small downslope-trending depression or gully on the windward side of a dune. The dune appeared to be quite stabilized with a high vegetative cover. The soil was rapidly drained and the site had a concave surface shape. A summary of site data is provided in Table 16.

Table 16. Summary of site data for the Elaeagnus commutata / Artemisia ludoviciana - Calamovilfa longifolia community type (n = 1).

Plot Elevation Aspect Slope Drainage Site PositionSurface Shape

Moisture Regime

Nutrient Regime

32 879 281 10 Rapid Lower Slope Concave Subxeric Submesotrophic

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

3.2.1.6 Prunus virginiana / Calamovilfa longifolia Association Choke cherry / sand grass

Plate 6. Prunus virginiana / Calamovilfa longifolia community type (Chokecherry / sand grass) Plot 14.

This community type was dominated by Prunus virginiana in the mid- and low-shrub strata. Mean percent cover for this species was greater than 60% and it formed dense thickets that were impossible to walk through. Calamovilfa longifolia was the dominant graminoid species. Oryzopsis hymenoides was also present at every sample location although with a low percent cover. Sporobolus cryptandrus was also commonly found, although generally with a mean percent cover of less than 3 %. Total graminoid cover was typically between 5-10 %. Common forbs included Helianthus annuus, Lygodesmia rostrata, Heterotheca villosa and Cryptantha fendleri. Although these species were present at most sample plot locations, their total percent cover was relatively low. Table 17 summarizes the species composition, mean percent cover, standard error and species prominence for this community type.

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

Table 17. Summary statistics for the Prunus virginiana / Calamovilfa longifolia community type (n = 4).

Species Mean %

Cover Standard

Error Presence Prominence

PRUNVIR5 63.75 8.26 4 63.8 CALALON7 4.25 2.14 4 4.3 PRUNVIR4 2.00 1.22 2 2.8 SPORCRY7 2.25 1.60 3 2.6 HELIANN6 1.75 1.09 4 1.8 ORYZHYM7 1.75 0.48 4 1.8 RUMEVEN6 1.00 0.58 2 1.4 STIPCOM7 1.00 0.71 2 1.4 ARTELUD6 0.50 0.50 1 1.0 LYGOROS6 0.63 0.24 3 0.7 CHENPRA6 0.50 0.29 2 0.7 HETEVIL6 0.63 0.13 4 0.6 AGRODAS7 0.38 0.24 2 0.5 CHENFRE6 0.25 0.25 1 0.5

Species Mean %

CoverStandard

Error Presence Prominence

CRYPFEN6 0.38 0.13 3 0.4 ROSAWOO5 0.13 0.13 1 0.3 SOLIMIS6 0.13 0.13 1 0.3 ARTECAM 0.13 0.13 1 0.3 SALSKAL6 0.13 0.13 1 0.3 EQUIHYE6 0.13 0.13 1 0.3 CHENSUB6 0.13 0.13 1 0.3 DESCSOP6 0.13 0.13 1 0.3 ARTEFRI6 0.13 0.13 1 0.3 OPUNPOL6 0.13 0.13 1 0.3 FRANACA6 0.13 0.13 1 0.3 ELYMCAN7 0.13 0.13 1 0.3

DECAY9 3.88 3.71 MINERAL9 46.25 5.54 ORG9 6.00 2.31

This community was consistently found on upper slope or crest topographic positions on dunes, with very rapid to rapid drainage. Slopes were strong, ranging from a minimum of 25 % to 75 % and generally had a south to southwesterly aspect. Little organic matter was present on the soil surface, typically with up to 40 % exposed sand.

A summary of site data is provided in Table 18.

Table 18. Summary of site data for the Prunus virginiana / Calamovilfa longifolia community type (n = 4).

Plot Elevation Aspect Slope Drainage Site Position Surface ShapeMoisture Regime

Nutrient Regime

10 874 228 55 Very Rapid Crest Straight Xeric Submesotrophic 13 876 239 75 Very Rapid Upper Slope Straight Xeric Submesotrophic 14 876 6 25 Rapid Upper Slope Straight Xeric Submesotrophic 34 891 199 25 Rapid Crest Convex Xeric Submesotrophic

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

3.2.1.7 Eurotia lanata / Stipa comata - Calamovilfa longifolia Association Winter fat / needle and thread – sand grass

Plate 7. Eurotia lanata / Stipa comata – Calamovilfa longifolia community type (Winterfat / needle and thread – sand grass) Plot 40.

This community type was dominated by Stipa comata with a low shrub layer composed of Eurotia lanata and Rosa woodsii. Stipa comata constituted 60 % cover, with Eurotia lanata providing 20 % cover. Calamovilfa longifolia contributed approximately 15% cover. Forbs provided less than 10% cover and typical forbs included Opuntia polycantha, Chenopodium pratericola, Artemisia frigida and Heterotheca villosa. The community was extensive with localized dense clumps of Eurotia lanata scattered throughout the Stipa comata, which formed pure localized grasslands. Table 19 summarizes the species composition and mean percent cover for this community type.

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

Table 19. Summary statistics for the Eurotia lanata / Stipa comata community type (n = 1).

Species Percent Cover

STIPCOM7 60 EUROLAN5 20 CALALON7 15 ROSAWOO5 5 OPUNPOL6 2 CHENPRA6 1 ARTEFRI6 1 HETEVIL6 1 EQUIHYE6 0.5 ARTELUD6 0.5 CRYPFEN6 0.5 CHENSUB6 0.5

MINERAL9 10 ORG9 40

This community was found mid-slope on an elevated dune flank, which graded into a level plain to the east. The soils were rapidly drained with a straight surface shape. A summary of site data is provided in Table 20.

Table 20. Summary of site data for the Eurotia lanata / Stipa comata community type (n = 1).

Plot Elevation Aspect Slope Drainage Site PositionSurface Shape

Moisture Regime

Nutrient Regime

40 866 n/a 0 Rapid Level Straight Xeric Submesotrophic

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

3.2.1.8 Salix exigua / Glycyrrhiza lepidota - Juncus balticus Association Sandbar willow / wild licorice – wire rush

Plate 8. Salix exigua / Glycyrrhiza lepidota – Juncus balticus community type (Sandbar willow / wild licorice – wire rush) Plot 7.

This community type was co-dominated by Glycyrrhiza lepidota in the forb layer and Juncus balticus in the graminoid layer. Salix exigua was the dominant shrub, with a cover ranging from 7 to 20 %. Other prevalent species included Carex lanuginosa and Poa pratensis in the graminoid layer and Solidago missouriensis in the forb layer. However, these species each typically had a cover of less than 3 %. Table 21 summarizes the species composition, mean percent cover and standard error and species prominence for this community type.

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

Table 21. Summary statistics for the Salix exigua / Glycyrrhiza lepidota - Juncus balticus community type (n = 2).

Species Mean %

Cover Standard

Error Presence Prominence

GLYCLEP6 45.00 5.00 2 45.0 JUNCBAL7 42.50 17.50 2 42.5 SALIEXI5 13.50 6.50 2 13.5 ARTEFRI6 2.50 2.50 1 3.5 SOLIMIS6 1.50 0.50 2 1.5 SALIAMY5 1.00 1.00 1 1.4 CHENSUB6 1.00 1.00 1 1.4 HELIANN6 1.00 1.00 1 1.4 CARELAN7 0.75 0.25 2 0.8 POAPRA7 0.75 0.25 2 0.8 SOLICAN6 0.50 0.50 1 0.7 DESCSOP6 0.25 0.25 1 0.4

Species Mean %

Cover Standard

Error Presence Prominence

SMILSTE6 0.25 0.25 1 0.4 CHENFRE6 0.25 0.25 1 0.4 OENONUT6 0.25 0.25 1 0.4 HETEVIL6 0.25 0.25 1 0.4 ANTIMIC6 0.25 0.25 1 0.4 LATUPUL6 0.25 0.25 1 0.4 AGRODAS7 0.25 0.25 1 0.4 ELYMCAN7 0.25 0.25 1 0.4 SPORCRY7 0.25 0.25 1 0.4 CALALON7 0.25 0.25 1 0.4

MINERAL9 2.00 0.00

This community type was most commonly found in concave, well-drained depressions between sand dunes. The soil moisture regime ranged from subxeric to submesic. A summary of site data is provided in Table 22.

Table 22. Summary of site data for the Salix exigua / Glycyrrhiza lepidota - Juncus balticus community type (n = 2).

Plot Elevation Aspect Slope Drainage Site PositionSurface Shape

Moisture Regime

Nutrient Regime

2 879 n/a 0 Well Depression Concave Submesic Submesotrophic

7 862 n/a 0 Well Depression Concave Subxeric Mesotrophic

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

3.2.1.9 Glycyrrhiza lepidota - Calamovilfa longifolia Association Wild licorice – sand grass

Plate 9. Glycyrrhiza lepidota – Calamovilfa longifolia community type (Wild licorice – sand grass) Plot 36.

This community type was dominated by Glycyrrhiza lepidota in the forb stratum and Calamovilfa longifolia in the grass stratum. Where this community was surveyed, Glycyrrhiza lepidota had a cover 60 %. A sparse shrub layer was present, which included Prunus virginiana and Rosa woodsii with a cover of less than 10 %. Several forbs were present including Artemisia ludoviciana, A. frigida and Chenopodium pratericola, among others. Stipa comata, Juncus balticus and Agropyron dasystachyum were also present, but with a total cover of less than 10 %. Table 23 summarizes the species composition and percent cover for this community type.

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

Table 23. Summary statistics for the Glycyrrhiza lepidota - Calamovilfa longifolia community type (n = 1).

Species Percent Cover

GLYCLEP6 60 CALALON7 25 STIPCOM7 7 PRUNVIR5 5 ARTELUD6 2 ROSAWOO5 1 CHENPRA6 1 ARTEFRI6 1 HETEVIL6 1 JUNCBAL7 1

Species Percent Cover

CORYVIV6 0.5 EQUIHYE6 0.5 CRYPFEN6 0.5 CHENSUB6 0.5 DESCSOP6 0.5 CHENFRE6 0.5 OPUNPOL6 0.5 CERAARV6 0.5 AGRODAS7 0.5

MINERAL9 5 ORG9 10

This community type was found in a small inter-dune depression with well-drained soils. A summary of site data is provided in Table 24.

Table 24. Summary of site data for the Glycyrrhiza lepidota - Calamovilfa longifolia community type (n = 1).

Plot Elevation Aspect Slope Drainage Site PositionSurface Shape

Moisture Regime

Nutrient Regime

36 893 n/a 0 Well Depression Concave Subxeric Submesotrophic

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

3.2.1.10 Glycyrrhiza lepidota – Artemisia spp. - Stipa comata Association Wild licorice – sage – needle and thread

Plate 10. Glycyrrhiza lepidota – Artemisia spp. – Stipa comata community type (Wild licorice – sage – needle and thread) Plot 19.

This community type was co-dominated by Glycyrrhiza lepidota in the forb stratum and Stipa comata in the graminoid stratum. Several species of Artemisia were also common, including Artemisia ludoviciana and A. frigida. Other common species with lower percent covers included Heterotheca villosa, Chenopodium pratericola and Tragopogon dubius in the forb layer and Juncus balticus in the graminoid layer. Table 25 summarizes the species composition, mean percent cover, standard error and species prominence for this community type.

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

Table 25. Summary statistics for the Glycyrrhiza lepidota - Artemisia spp. - Stipa comata community type (n = 2).

Species Mean %

Cover Standard

Error Presence Prominence

GLYCLEP6 32.50 7.50 2 32.5 STIPCOM7 25.00 15.00 2 25.0 ARTELUD6 13.00 12.00 2 13.0 JUNCBAL7 5.00 5.00 1 7.1 HETEVIL6 2.50 2.50 1 3.5 ARTEFRI6 3.00 2.00 2 3.0 CHENPRA6 1.50 0.50 2 1.5 ROSAWOO5 1.00 1.00 1 1.4 TRAGDUB6 0.75 0.25 2 0.8 KOELMAC7 0.50 0.50 1 0.7

Species Mean %

Cover Standard

Error Presence Prominence

AGROSIB7 0.50 0.50 1 0.7 POAPRA7 0.50 0.50 1 0.7 ACHIMIL6 0.25 0.25 1 0.4 CRYPFEN6 0.25 0.25 1 0.4 CHENSUB6 0.25 0.25 1 0.4 DESCSOP6 0.25 0.25 1 0.4 HELIANN6 0.25 0.25 1 0.4 AGRODAS7 0.25 0.25 1 0.4

MINERAL9 12.50 2.50 ORG9 30.00 0.00

This plant community was typically found in level, very rapidly drained sand plain habitats. Organic matter accumulation at the soil surface averaged 30 % cover. A summary of site data is provided in Table 26.

Table 26. Summary of site data for the Glycyrrhiza lepidota - Artemisia spp. - Stipa comata community type (n = 2).

Plot Elevation Aspect Slope Drainage Site PositionSurface Shape

Moisture Regime

Nutrient Regime

19 866 n/a 0 Very Rapid Level Straight Xeric Submesotrophic

20 865 n/a 0 Very Rapid Level Straight Xeric Submesotrophic

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

3.2.1.11 Rumex venosus Association Wild begonia

Plate 11. Rumex venosus community type (Wild begonia) Plot 6.

This community type was dominated by Rumex venosus in the forb stratum. It was typically found on the leeward side of active sand dunes, where sand accumulation was occurring. There was little grass cover, although Sporobolus cryptandrus was found in both plots (under 2 % cover) and at one site, Oryzopsis hymenoides provided 5 % cover. Table 27 summarizes the species composition, mean percent cover, standard error and species prominence for this community type.

Table 27. Summary statistics for the Rumex venosus community type (n = 2).

Species Mean %

CoverStandard

Error Presence Prominence

RUMEVEN6 42.50 17.50 2 42.5 ORYZHYM7 2.50 2.50 1 3.5 FRANACA6 1.00 1.00 1 1.4 HELIANN6 1.00 1.00 1 1.4 SPORCRY7 1.25 0.75 2 1.3 THERRHO6 0.50 0.50 1 0.7 ROSAWOO5 0.25 0.25 1 0.4 HETEVIL6 0.25 0.25 1 0.4 ELYMCAN7 0.25 0.25 1 0.4 CALALON7 0.25 0.25 1 0.4

MINERAL9 55.00 15.00 ORG9 0.50 0.00

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

This community type was typically found on the leeward side of dunes with slopes ranging from 18 - 30 % and a north to northeast aspect. Sites were located on the mid to upper slopes of dunes and were very rapidly to rapidly drained. Exposed mineral soil comprised 40 to 70 % cover, with virtually no organic matter accumulation at the soil surface. A summary of site data is provided in Table 28.

Table 28. Summary of site data for the Rumex venosus community type (n = 2).

Plot Elevation Aspect Slope Drainage Site PositionSurface Shape

Moisture Regime

Nutrient Regime

6 863 37 18 Rapid Middle Slope Straight Xeric Submesotrophic 30 887 48 30 Very Rapid Upper Slope Straight Xeric Submesotrophic

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

3.2.1.12 Oryzopsis hymenoides – Sporobolus cryptandrus Association Indian rice grass – sand dropseed

Plate 12. Oryzopsis hymenoides – Sporobolus cryptandrus community type (Indian rice grass – sand dropseed) Plot 35.

This community was co-dominated by Oryzopsis hymenoides and Sporobolus cryptandrus in the graminoid stratum, however, total percent cover was generally less than 40 %. This community was typically found on dune sites, where sand movement was active. As such, only one shrub species (Elaeagnus commutata) was encountered with less than 1 % cover. Two forb species were common to all or most survey sites, including Helianthus annuus and Heterotheca villosa. Other forb and graminoid species were found at different survey sites, but few were common to all or most plots. Table 29 summarizes the species composition, mean percent cover and standard error and species prominence for this community type.

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

Table 29. Summary statistics for the Oryzopsis hymenoides – Sporobolus cryptandrus community type (n = 5).

Species Mean %

Cover Standard

Error Presence Prominence

SPORCRY7 17.20 5.69 5 17.2 ORYZHYM7 10.00 2.24 5 10.0 THERRHO6 4.40 3.92 2 7.0 HELIANN6 2.80 0.92 5 2.8 RUMEVEN6 1.30 0.94 3 1.7 HETEVIL6 0.70 0.20 4 0.8 CALALON7 0.30 0.20 2 0.5 SOLIMIS6 0.20 0.20 1 0.4 LYGOROS6 0.20 0.20 1 0.4 FRANACA6 0.20 0.20 1 0.4

Species Mean %

Cover Standard

Error Presence Prominence

GLYCLEP6 0.20 0.20 1 0.4 CYPESCH7 0.20 0.20 1 0.4 KOELMAC7 0.20 0.20 1 0.4 ELYMCAN7 0.20 0.20 1 0.4 CHENPRA6 0.20 0.12 2 0.3 ELAECOM5 0.10 0.10 1 0.2 AGRODAS7 0.10 0.10 1 0.2

DECAY9 2.00 2.00 MINERAL9 62.00 12.71 ORG9 3.80 2.81

This community type was commonly found on south to southwest facing slopes of active dunes. Sand movement was evident and in most sites the percentage of exposed sand at the soil surface exceeded 60 % (reaching up to 90 %). There was little organic matter accumulation at the soil surface and some decaying wood (shrub branches) was found at one survey site. A summary of site data is provided in Table 30.

Table 30. Summary of site data for the Oryzopsis hymenoides – Sporobolus cryptandrus community type (n = 5).

Plot Elevation Aspect Slope Drainage Site PositionSurface Shape

Moisture Regime

Nutrient Regime

21 862 168 15 Very Rapid Upper Slope Straight Very Xeric Oligotrophic 29 888 11 25 Very Rapid Middle Slope Straight Xeric Oligotrophic 31 894 284 25 Rapid Upper Slope Straight Xeric Submesotrophic 35 891 n/a 0 Rapid Upper Slope Concave Xeric Submesotrophic 37 886 207 10 Very Rapid Lower Slope Concave Very Xeric Oligotrophic

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

3.2.1.13 Stipa comata – Oryzopsis hymenoides Association Needle and thread – Indian rice grass

Plate 13. Stipa comata – Oryzopsis hymenoides community type (Needle and thread – Indian rice grass) Plot 8.

This community was co-dominated by Stipa comata and Oryzopsis hymenoides, although their combined cover was typically less than 20 %. This community was found on partially stabilized dunes. Shrub species, including Elaeagnus commutata, Rosa woodsii and Salix exigua were encountered though with very low percent covers (generally less than 2 %). Forb species that were relatively common (at low percent cover) included Helianthus annuus, Chenopodium pratericola, C. subglabrum and Lygodesmia rostrata. Table 31 summarizes the species composition, mean percent cover, standard error and species prominence for this community type.

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

Table 31. Summary statistics for the Stipa comata – Oryzopsis hymenoides community type (n = 2).

Species Mean %

Cover Standard

Error Presence Prominence

ORYZHYM7 6.50 3.50 2 6.5 STIPCOM7 5.00 0.00 2 5.0 CRYPFEN6 2.50 2.50 1 3.5 SPORCRY7 2.50 2.50 1 3.5 HELIANN6 2.50 0.50 2 2.5 THERRHO6 1.50 1.50 1 2.1 AGROSMI7 1.50 1.50 1 2.1 CHENSUB6 0.75 0.25 2 0.8 CHENPRA6 1.50 0.50 2 1.5 LYGOROS6 0.75 0.25 2 0.8

Species Mean %

Cover Standard

Error Presence Prominence

ROSAWOO5 0.50 0.50 1 0.7 HETEVIL6 0.50 0.50 1 0.7 GLYCLEP6 0.50 0.50 1 0.7 ELAECOM5 0.25 0.25 1 0.4 SALIEXI5 0.25 0.25 1 0.4 RUMEVEN6 0.25 0.25 1 0.4 KOELMAC7 0.25 0.25 1 0.4

MINERAL9 22.50 12.50 ORG9 7.50 2.50

This community was typically found on mid to upper slope positions of moderately inclined south to southeast facing slopes. Exposed sand at the soil surface ranged from 10 to 35 % and organic matter accumulation was typically less than 10 % cover. A summary of site data is provided in Table 32.

Table 32. Summary of site data for the Stipa comata – Oryzopsis hymenoides community type (n = 2).

Plot Elevation Aspect Slope Drainage Site PositionSurface Shape

Moisture Regime

Nutrient Regime

8 868 162 15 Rapid Upper Slope Straight Xeric Submesotrophic 25 885 149 20 Rapid Middle Slope Concave Xeric Submesotrophic

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Plant Community Classification of the Pakowki Sandhills and Sand Plains

3.2.1.14 Artemisia spp. - Stipa comata – Calamovilfa longifolia Association Sage – needle and thread – sand grass

Plate 14. Artemisia spp. – Stipa comata – Calamovilfa longifolia (Sage – needle and thread – sand grass) Plot 39.

This community was dominated by Stipa comata in the graminoid stratum and a variety of Artemisia species in the forb layer. Artemisia frigida was found at all sites, while A. ludoviciana was found at two sites and A. campestris was found at one site. Several other forbs were common in this community including Heterotheca villosa, Chenopodium pratericola and C. subglabrum, all with relatively low percent covers. Rosa woodsii was common to all survey sites, with a mean cover of less than 2 %. Several other grasses were common, including Calamovilfa longifolia, Koeleria macrantha and Sporobolus cryptandrus but with low percent covers. Table 33 summarizes the species composition, mean percent cover and standard error and species prominence for this community type.

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Table 33. Summary statistics for the Artemisia spp. - Stipa comata –Calamovilfa longifolia community type (n = 3).

Species Mean %

Cover Standard

Error Presence Prominence

STIPCOM7 40.00 5.77 3 40.0 ARTECAM 3.33 3.33 1 5.8 CALALON7 5.33 2.60 3 5.3 ARTEFRI6 2.67 1.20 3 2.7 ARTELUD6 2.00 1.53 2 2.4 HETEVIL6 2.00 0.58 3 2.0 OPUNPOL6 1.33 0.88 2 1.6 ROSAWOO5 1.50 0.76 3 1.5 SOLIMIS6 1.00 0.58 2 1.2 THERRHO6 0.83 0.60 2 1.0 KOELMAC7 1.00 0.00 3 1.0 CHENPRA6 0.83 0.17 3 0.8 SPORCRY7 1.00 0.58 3 1.0

Species Mean %

Cover Standard

Error Presence Prominence

LYGOROS6 0.33 0.33 1 0.6 AGRODAS7 0.33 0.33 1 0.6 CHENSUB6 0.50 0.00 3 0.5 LEPIDEN6 0.33 0.17 2 0.4 ACHIMIL6 0.33 0.17 2 0.4 PRUNVIR5 0.17 0.17 1 0.3 PLANPAT6 0.17 0.17 1 0.3 CRYPFEN6 0.17 0.17 1 0.3 DESCSOP6 0.17 0.17 1 0.3 GLYCLEP6 0.17 0.17 1 0.3 ORYZHYM7 0.17 0.17 1 0.3

MINERAL9 18.33 1.67 ORG9 16.83 8.66

This community type was found on level, sand plain habitats that were very rapidly to well drained. A summary of site data is provided in Table 34.

Table 34. Summary of site data for the Artemisia spp. - Stipa comata – Calamovilfa longifolia community type (n = 3).

Plot Elevation Aspect Slope Drainage Site PositionSurface Shape

Moisture Regime

Nutrient Regime

22 866 n/a 0 Very Rapid Level Straight Xeric Submesotrophic 38 883 n/a 0 Well Level Straight Xeric Submesotrophic 39 878 n/a 0 Rapid Level Straight Xeric Submesotrophic

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3.2.1.15 Stipa comata – Cyperus schweinitzii – Calamovilfa longifolia Association Needle and thread – sand nut-grass – sand grass

Plate 15. Stipa comata – Cyperus schweinitzii – Calamovilfa longifolia community type (Needle and thread – sand nut-grass – sand grass) Plot 33.

This community type was dominated by graminoids, with Stipa comata, Cyperus schweinitzii and Calamovilfa longifolia having the highest percent covers. Several forbs were typical, including Artemisia campestris, Lygodesmia rostrata, Opuntia polycantha and Heterotheca villosa. Rosa woodsii was also present, but with only a 1 % cover. Table 35 summarizes the species composition and mean percent cover for this community type.

Table 35. Summary statistics for the Stipa comata – Cyperus schweinitzii –Calamovilfa longifolia community type (n = 1).

Species Percent Cover

STIPCOM7 25 CYPESCH7 20 CALALON7 10 ROSAWOO5 1 ARTECAM 1 LYGOROS6 1 OPUNPOL6 1 HETEVIL6 1 CRYPFEN6 0.5 HELIANN6 0.5 SPORCRY7 0.5

MINERAL9 70 ORG9 2

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This site was located on a shallow, windward, south-facing dune slope. The site was very exposed to the wind and likely had active sand movement. The community had approximately 70% exposed sand at the soil surface and was very rapidly drained. A summary of site data is provided in Table 36.

Table 36. Summary of site data for the Stipa comata – Cyperus schweinitzii – Calamovilfa longifolia community type (n = 1).

Plot Elevation Aspect Slope Drainage Site PositionSurface Shape

Moisture Regime

Nutrient Regime

33 877 195 15 Very Rapid Upper Slope Straight Xeric Submesotrophic

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3.2.1.16 Sporobolus cryptandrus – Calamovilfa longifolia –Oryzopsis hymenoides Association Sand dropseed – sand grass – Indian rice grass

Plate 16. Sporobolus cryptandrus – Calamovilfa longifolia – Oryzopsis hymenoides community type (Sand dropseed – sand grass – Indian rice grass) Plot 4.

This community type occurred on dunes in the very early stages of stabilization, but that still have active sand movement. It was co-dominated by Sporobolus cryptandrus and Calamovilfa longifolia, with lesser amounts of Oryzopsis hymenoides. Low shrubs were present at some survey sites, however, the percent cover was quite low and included shrubs such as Eurotia lanata, Rosa woodsii and Elaeagnus commutata. A forb layer was typically present and included species such as Helianthus annuus, Lygodesmia rostrata and Heterotheca villosa. Table 37 summarizes the species composition, mean percent cover and standard error and species prominence for this community type.

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Table 37. Summary statistics for the Sporobolus cryptandrus – Calamovilfa longifolia –Oryzopsis hymenoides community type (n = 4).

Species Mean %

Cover Standard

Error Presence Prominence

SPORCRY7 13.00 4.36 4 13.0 STIPCOM7 2.50 2.50 1 5.0 CALALON7 4.25 0.75 4 4.3 HELIANN6 3.38 2.30 3 3.9 ORYZHYM7 3.25 1.03 4 3.3 EUROLAN5 2.00 1.68 2 2.8 ROSAWOO5 2.00 1.68 2 2.8 ELAECOM5 1.25 1.25 1 2.5 GLYCLEP6 0.88 0.72 2 1.2 LYGOROS6 0.75 0.43 3 0.9 CHENSUB6 0.38 0.24 2 0.5 CHENPRA6 0.38 0.24 2 0.5

Species Mean %

Cover Standard

Error Presence Prominence

LATUPUL6 0.25 0.25 1 0.5 HETEVIL6 0.38 0.13 3 0.4 CRYPFEN6 0.25 0.14 2 0.4 ELYMCAN7 0.25 0.14 2 0.4 CORYVIV6 0.13 0.13 1 0.3 SALSKAL6 0.13 0.13 1 0.3 ARTELUD6 0.13 0.13 1 0.3 ARTEFRI6 0.13 0.13 1 0.3 OPUNPOL6 0.13 0.13 1 0.3 CERAARV6 0.13 0.13 1 0.3 KOELMAC7 0.13 0.13 1 0.3

MINERAL9 55.00 2.89 ORG9 1.75 0.25

This community was typically found on gentle to moderate southeast to southwest facing dune slopes. The dunes were partially active, however vegetation growth was beginning to stabilize the dune. Typically, there was greater than 50 % exposed sand at the soil surface, with very little organic matter accumulation. A summary of site data is provided in Table 38.

Table 38. Summary of site data for the Sporobolus cryptandrus - Calamovilfa longifolia –Oryzopsis hymenoides community type (n = 4).

Plot Elevation Aspect Slope Drainage Site PositionSurface Shape

Moisture Regime

Nutrient Regime

1 883 221 16 Very Rapid Crest Straight Very Xeric Oligotrophic 3 885 300 27 Very Rapid Upper Slope Straight Very Xeric Oligotrophic 4 878 120 9 Very Rapid Upper Slope Straight Very Xeric Oligotrophic 15 872 152 5 Very Rapid Middle Slope Straight Very Xeric Submesotrophic

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3.2.1.17 Artemisia cana / Stipa comata Association Silver sagebrush / needle and thread

Plate 17. Artemisia cana / Stipa comata community type (Silver sagebrush / needle and thread) Plot 024.

This sand plain community type was dominated by Stipa comata in the grass layer with a sparse low shrub layer, dominated by Artemisia cana, although Koeleria macrantha and Agropyron dasystachyum were also present but with low covers. Other low shrub species were also present at low levels of abundance including Eurotia lanata and Rosa woodsii. Typical forbs included Erigeron caespitosus, Thermopsis rhombifolia, Artemisia frigida and Polycantha vivipara. Table 39 summarizes the species composition and mean percent cover for this community type.

Table 39. Summary statistics for the Artemisia cana / Stipa comata community type (n = 1).

Species Percent Cover

STIPCOM7 30 ARTECAN5 10 ERIGCAE6 2 THERRHO6 2 ARTEFRI6 2 KOELMAC7 2 EUROLAN5 1 ROSAWOO5 1 CORYVIV6 1 ANTEPAR6 1

Species Percent Cover

HETEVIL6 1 POTEPEN6 0.5 LEPIDEN6 0.5 CLEOSER6 0.5 ARTELUD6 0.5 CHENSUB6 0.5 AGRODAS7 0.5

MINERAL9 10 ORG9 0.5

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This community was found on a level sand plain and its distribution was quite limited. Soils generally had a higher silt content than any of the other soils encountered in the Pakowki Sandhills study area. There was approximately 10 % exposed mineral soil at the soil surface, with little organic matter accumulation. A summary of site data is provided in Table 40.

Table 40. Summary of site data for the Artemisia cana / Stipa comata community type (n = 1).

Plot Elevation Aspect Slope Drainage Site PositionSurface Shape

Moisture Regime

Nutrient Regime

24 883 n/a 0 Rapid Level Straight Very xeric Submesotrophic

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3.3 Cross-Referencing of Proposed Community Types with Literature Each community type identified from the analysis of the plot data was compared against floristically similar community types described for Alberta and other jurisdictions. A summary of the findings are provided in Appendices 4 and 5, which compare the Pakowki Sandhills community types against community types described in literature based in Alberta and other jurisdictions, respectively. A similarity rating between the community types, based on Corns (1983) and recently applied by Strong (2002), is also provided in the tables. A discussion of the community types and associated literature is provided below.

3.3.1 Populus deltoides / Glycyrrhiza lepidota - Juncus balticus Association Western cottonwood / wild licorice – wire rush

Community types, dominated by Populus deltoides have been described for Alberta, though with some variation, particularly in the associated habitat. A floristically similar community type was found occasionally in the Manyberries region, though it was located in moist coulees (Smoliak 1985). A P. deltoides association was also described for CFB-Suffield, where it was found on floodplains and alluvial terraces of the South Saskatchewan River (Adams et al. 1997). In a 1993 survey of the Pakowki Sandhills P. deltoides was found on sand dunes and plains although a community type was not described in detail. Isolated Populus deltoides were reported to occur in low areas, although aspen clones were reported to be more common (Komex 1993).

Outside Alberta, a floristically similar community type has been described occurring throughout the Great Plains in North America, including Saskatchewan, Montana, Idaho, Wyoming, South and North Dakota and Nebraska. Epp and Townley-Smith (1983) noted Populus deltoides and P. tremuloides community types in low areas in sand flats of the Great Sand Hills in Saskatchewan. The community type was reported in locations where soil salinity was low and they also noted that Glycyrrhiza lepidota was an understorey forb species in those locations.

A Populus deltoides – (Salix amygdaloides) / Salix exigua Woodland has been described for numerous locations within the Great Plains region of the United States. At Scotts Bluff National Monument (Nebraska), this community was found on level to gently sloping locations, at the base of low, north-facing slopes. The soils were described as silty rather than sandy and contained more eastern species such as Fraxinus pennsylvanica and Acer negundo (USGS 2002a). At Devil’s Tower National Monument (Wyoming) this community was found on river floodplains with sandy soils (USGS 2002b). At this location, the community was very small and had a high cover of invasive, exotic species. Faber-Langendoen (2001) also noted this association in the mid-western United States where it was typically found along the banks of streams and rivers and developed on newly deposited alluvium. This report noted that Glycyrrhiza lepidota was a common forb where site disturbance was low. At Agate Fossil Beds NM (Nebraska) this community was found on the floodplain of the Niobara River. The community type was typically located on level or sloping ground, on the banks or in old channels of the primary floodplain. Soils were described as fine sands and sandy loams that are

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somewhat poorly drained (USGS 2002c). At Badlands National Park, in South Dakota this community was found along river and creek floodplains, pond and reservoir margins, seeps and springs in mesic draws and seeps and springs that occur along the edge of sandhill complexes (USGS 2002d).

According to Natureserve (2002) “ This cottonwood - willow woodland is found widely in the central Great Plains of the United States. Stands occur on recently deposited alluvial material along rivers and streams. The soils are derived from alluvial sand, silt and clay and are poorly developed. The water table fluctuates with the level of the adjacent river or stream. Populus deltoides is the dominant species in this community, although Salix exigua and/or Salix interior is generally more dominant in the initial stage following a major flood event. Salix amygdaloides is rare to codominant. The shrub/sapling layer is conspicuous, especially near the stream bank and consists mainly of Salix exigua, Populus deltoides and Salix amygdaloides, or occasionally Salix lutea. In the more easterly parts of the range, Salix interior may replace Salix exigua. On the older margins of this community Fraxinus pennsylvanica is often found as a sapling or small canopy tree. The herbaceous stratum is variable. Graminoids typical of undisturbed sites include Carex emoryi, Carex pellita (= Carex lanuginosa), Pascopyrum smithii and Spartina pectinata. Equisetum arvense and Glycyrrhiza lepidota are common forbs in these sites. Widely distributed species that are adapted to these sites include Ambrosia psilostachya, Artemisia campestris ssp. caudata, Artemisia ludoviciana, Calamovilfa longifolia, Cenchrus longispinus, Chamaesyce serpyllifolia (= Euphorbia serpyllifolia), Euphorbia esula, Grindelia squarrosa, Helianthus petiolaris, Heterotheca villosa, Phyla lanceolata (= Lippia lanceolata), Opuntia macrorhiza, Poa pratensis and Sporobolus cryptandrus. These sites are prone to invasion by exotic grasses and forbs, the most widely established being Agrostis stolonifera, Bromus tectorum, Cirsium arvense, Bassia scoparia (= Kochia scoparia), Melilotus spp., Taraxacum officinale and Tragopogon dubius.” It was also noted that many sites were overgrazed and invaded by exotic woody and herbaceous species.

A Populus deltoides / Pascopyrum smithii woodland was found in Thunder Basin National Grassland (Wyoming) along the Cheyenne River (Jones 1998a). In this location, the community type forms linear groves of trees that run parallel to the stream course on alluvial materials. A Populus deltoides / Calamovilfa longifolia woodland was also described in Thunder Basin National Grassland, along Antelope Creek (Jones 1998b). A Populus deltoides / Symphoricarpos occidentalis Woodland was found in the Bitter Creek Badlands region of Montana, where it was found along rivers on unstabilized floodplains where it colonized alluvial deposits on meanders of streams and rivers (Cooper et al. 2001). In this location, the authors noted that a well-developed shrub layer was typically present. A Populus tremuloides / Symphoricarpos alba forest has been described from the Medicine Lake Sandhills in Montana (Heidel et al. 2000). There was no P. deltoides observed at this site and the community type did not have a native understorey.

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3.3.2 Rosa woodsii / Sporobolus cryptandrus Association Common wild rose / sand dropseed

Rosa woodsii was also found on dunes in the 1993 during a survey of the Pakowki Sandhills (Komex 1993). The species was reported to occur in low areas between dunes, often in association with wild licorice, although a full community description was not provided.

Outside Alberta, a shrubland, dominated by Elaeagnus commutata, Rosa woodsii, Symphoricarpos occidentalis or Prunus virginiana was noted for the Great Sandhills in Saskatchewan (Epp and Townley-Smith 1980). They noted that these species formed closed shrublands on stabilized slip faces that were typically north facing. The shrub composition varied from location to location and each shrub species could be dominant at specific sites, where at others the species were co-dominant. Furthermore, Epp and Townley-Smith (1980) noted a Rosa woodsii community that was dominant in areas “where sand has been whipped off dune by strong winds, creating areas of slow sand accumulation.” Coupland (1950) noted that a Rosa woodsii (Artemisia cana / Elaeagnus commutata) community type was found in undulating to gently rolling areas between stabilized dunes in the prairie provinces. He noted that the water table was typically within eight to twelve feet of the soil surface where this community was found. Thorpe and Godwin (1993) noted a grass and shrub / sand type in the Manito Sand Hills of Western Saskatchewan. While this community type was dominated by Symphoricarpos occidentalis, Rosa spp. and Prunus virginiana were also present in 50% of plots in this type. The community type was typically found on stabilized dunes, with rapidly drained, sandy soils. However, Sporobolus cryptandrus was not listed as a prevalent species.

Natureserve (2002) notes a Rosa woodsii Temporarily Flooded Shrubland Alliance. These shrublands were typically found in the foothills and plains of Montana and Idaho. Elevations for the community type ranged from 650-1700 m and typically occurred on floodplains and alluvial terraces along rivers and streams. This alliance was also located on hillsides below springs and in ravines and swales where overland flow from snowmelt and summer precipitation provided additional moisture. Sites were generally flat to moderately steep and had soils that ranged from sandy loams to silt loams. Although these sites are considered temporarily flooded, they were well drained and were not found to have a shallow water table.

Cooper et al. (1999) noted a Rosa woodsii Shrubland community type in Beaverhead Mountain region of Montana. Although it was listed as a community type for this area, it was not described in detail in the associated report. The Montana and Idaho natural heritage programs (MNHP 2002; Rust 1997) listed a Rosa woodsii Shrubland as a natural plant community for their states. However, detailed descriptions of the community and associated habitats were not provided.

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3.3.3 Salix amygdaloides – Rosa woodsii / Juncus balticus – Sporobolus cryptandrus Association Peach-leaf willow – common wild rose / wire rush – sand dropseed

Salix amygdaloides was reported on dunes during a 1993 survey of the Pakowki Sandhills (Komex 1993). It was typically found in low areas, in both a tree and shrub form. Unfortunately, a community description was not provided. A general Salix spp. / Stipa comata association was reported for CFB-Suffield, where it was found on floodplains and alluvial terraces of the South Saskatchewan River (Jaques 1977). No reports of a similar community could be found for other Canadian provinces.

A Salix amygdaloides Woodland type was reported by Natureserve (2002) and was found in the Northern Rocky Mountains and potentially into parts of the western Great Plains. Stands occurred in riparian areas and the vegetation was dominated by Salix amygdaloides. Specifically, the Salix amygdaloides Woodland was documented in the Black Hills of South Dakota at the confluence of two creeks where it formed a tall-shrub stratum with Salix bebbiana and Cornus sericea and was more a shrubland than a woodland (Faber-Langendoen 2001; Marriott and Faber-Langendoen 2000).

A Salix amygdaloides Woodland was listed as a natural plant community for Montana where it was ranked G3/S3 by the Montana Natural Heritage Program (2002).

A Salix amygdaloides / Salix exigua Woodland was also reported by Natureserve (2002) where the association occurred in riparian habitats on the Columbian Plateau in the interior Northwest and in northeastern Utah. The association was found at elevations ranging from 100-1600 m and was located in overflow channels of large rivers and on narrow floodplains of small creeks. Soil textures were reported to be quite variable, but did not include clay. This community has been reported to have a moderately open canopy dominated by the small tree Salix amygdaloides. Salix exigua dominated the tall-shrub layer. Other tree species reported for this community type included Populus fremontii, Acer negundo, Populus angustifolia, Populus deltoides and the introduced Elaeagnus angustifolia.

3.3.4 Elaeagnus commutata / Glycyrrhiza lepidota Association Silverberry / wild licorice

An Elaeagnus commutata Shrubland was identified during a 1993 survey of the Pakowki Sandhills (Komex 1993). This community was reported to occur as thickets on some north-facing slopes and at the base of some dunes. However, a detailed description of the community type was not provided. An Elaeagnus commutata community has been described for Alberta based on three reports in Central Parkland, at Dillberry Lake Provincial Park, near Rumsey and in Dry Island Buffalo Jump (Wheatley and Bentz 2002). This community occurred as low shrublands and shrubby meadows along the perimeter of saline lakes, adjacent to marshes and graminoid meadows. At Dillberry Lake Provincial Park, Elaeagnus commutata occurred as a shrubland primarily with Symphoricarpos occidentalis, Rosa acicularis, Calamovilfa longifolia, Agropyron trachycaulum and Carex spp.. As a meadow community, E. commutata was more common with Rosa woodsii, Glycyrrhiza lepidota, Juncus balticus and Calamovilfa

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longifolia. An Elaeagnus commutata / Symphoricarpos occidentalis – Rosa woodsii / Poa palustris community was also described from Central Parkland occurring near Wainwright on subxeric to submesic dune sites with good internal soil drainage. Currently, ANHIC lists an Elaeagnus commutata / Pascopyrum smithii Shrubland community for the Grassland Natural Region and it is ranked S3 (Allen 2002).

Epp and Townley-Smith (1980) reported an Elaeagnus commutata – Rosa woodsii – Symphoricarpos occidentalis – Prunus virginiana closed shrubland in the Great Sand Hills of Saskatchewan. The community was typically found on stabilized slip faces that were north facing. They noted that the shrub composition varied from location to location and that each shrub species could be dominant at specific sites, where at others they may be co-dominant. The authors also noted an Elaeagnus commutata shrubland that was often found inhabiting blowouts away from bare sand (Epp and Townley-Smith 1980). Coupland (1950) described a Rosa woodsii (Artemesia cana / Elaeagnus commutata) community type for the prairie provinces that was found in undulating to gently rolling areas between stabilized dunes. At these locations, the water table was typically within 8 to 12 feet of the soil surface.

Heidel et al. (2000) reported an Elaeagnus commutata Shrubland community for northern Montana, located east of the Continental divide. The community type was generally classified as temporarily flooded. At the Medicine Lake sandhills, sites typically had a shrub cover of 10% and grass cover of 70% and sites were not flooded but the water table was within the rooting zone.

An Elaeagnus commutata Shrubland Alliance was reported by Natureserve (2002) for the northern Great Plains in a mixedgrass prairie matrix. The alliance was dominated by mid to tall shrubs, particularly Elaeagnus commutata. Pascopyrum smithii was reported as the dominant species in the herbaceous layer and was typically accompanied by Koeleria macrantha, Schizachyrium scoparium and Hesperostipa comata. They also note that Elaeagnus commutata was most abundant on flat sandy sites in southern Saskatchewan.

Natureserve (2002) also reported an Elaeagnus commutata / Pascopyrum smithii Shrubland Association, within the shrubland alliance that typically occurred on a variety of glacial landforms including kames, eskers and areas of till and outwash. The association was most common on north-facing slopes and sites where moisture is more abundant, including river valley slopes.

An Elaeagnus commutata Shrubland was listed as a natural plant community for Montana and was ranked G2Q/S2? by the Montana Natural Heritage Program (2002). Unfortunately no description of the community type is given.

3.3.5 Elaeagnus commutata / Artemisia ludoviciana - Calamovilfa longifolia Association Silverberry / prairie sagewort – sand grass

An Elaeagnus commutata Shrubland was identified during a 1993 survey of the Pakowki Sandhills (Komex 1993). This community was reported to occur as thickets on some north-facing slopes and at the base of some dunes. However, a detailed description of the community type was not provided. An Elaeagnus commutata community has been

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described for Alberta based on three reports in Central Parkland, at Dillberry Lake Provincial Park, near Rumsey and in Dry Island Buffalo Jump (Wheatley and Bentz 2002). This community occurred as low shrublands and shrubby meadows along the perimeter of saline lakes, adjacent to marshes and graminoid meadows. At Dillberry Lake Provincial Park, Elaeagnus commutata occurred as a shrubland primarily with Symphoricarpos occidentalis, Rosa acicularis, Calamovilfa longifolia, Agropyron trachycaulum and Carex spp.. As a meadow community, E. commutata was more common with Rosa woodsii, Glycyrrhiza lepidota, Juncus balticus and Calamovilfa longifolia. An Elaeagnus commutata / Symphoricarpos occidentalis – Rosa woodsii / Poa palustris community was also described from Central Parkland occurring near Wainwright on subxeric to submesic dune sites with good internal soil drainage. Currently, ANHIC lists an Elaeagnus commutata / Pascopyrum smithii Shrubland community for the Grassland Natural Region and it is ranked S3 (Allen 2002).

Epp and Townley-Smith (1980) reported an Elaeagnus commutata – Rosa woodsii – Symphoricarpos occidentalis – Prunus virginiana closed shrubland in the Great Sand Hills of Saskatchewan. The community was typically found on stabilized slip faces that were north facing. They noted that the shrub composition varied from location to location and that each shrub species could be dominant at specific sites, where at others they may be co-dominant. The authors also noted an Elaeagnus commutata shrubland that was often found inhabiting blowouts away from bare sand (Epp and Townley-Smith 1980). Coupland (1950) described a Rosa woodsii (Artemesia cana / Elaeagnus commutata) community type for the prairie provinces that was found in undulating to gently rolling areas between stabilized dunes. At these locations, the water table was typically within 8 to 12 feet of the soil surface.

Heidel et al. (2000) reported an Elaeagnus commutata Shrubland community for northern Montana, located east of the Continental divide. The community type was generally classified as temporarily flooded. At the Medicine Lake sandhills, sites typically had a shrub cover of 10% and grass cover of 70% and sites were not flooded but the water table was within the rooting zone.

An Elaeagnus commutata Shrubland Alliance was reported by Natureserve (2002) for the northern Great Plains in a mixedgrass prairie matrix. The alliance was dominated by mid to tall shrubs, particularly Elaeagnus commutata. Pascopyrum smithii was reported as the dominant species in the herbaceous layer and was typically accompanied by Koeleria macrantha, Schizachyrium scoparium and Hesperostipa comata. They also note that Elaeagnus commutata was most abundant on flat sandy sites in southern Saskatchewan.

Natureserve (2002) also reports an Elaeagnus commutata / Pascopyrum smithii Shrubland Association, within the shrubland alliance that typically occurred on a variety of glacial landforms including kames, eskers and areas of till and outwash. The association was most common on north-facing slopes and sites where moisture is more abundant, including river valley slopes.

An Elaeagnus commutata Shrubland was listed as a natural plant community for Montana and was ranked G2Q/S2? by the Montana Natural Heritage Program (2002). Unfortunately no description of the community type is given.

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3.3.6 Prunus virginiana / Calamovilfa longifolia Association Choke cherry / sand grass

A 1993 survey of the Pakowki Sandhills reported a Prunus virginiana shrubland (Komex 1993). The authors of this survey noted that this community typically occurred along low dune ridges and slopes. A Prunus virginiana – Amelanchier alnifolia / Agropyron trachycaulum – Poa pratensis community was described for the Central Parkland (Wheatley and Bentz 2002). This community was found on a steep, south-facing slope in the Blackfoot Provincial Recreation Area.

Epp and Townley-Smith (1980) reported an Elaeagnus commutata – Rosa woodsii – Symphoricarpos occidentalis – Prunus virginiana closed shrubland in the Great Sand Hills of Saskatchewan. The community was typically found on stabilized slip faces that were north facing. They noted that the shrub composition varied from location to location and that each shrub species could be dominant at specific sites, where at others they may be co-dominant. Thorpe and Godwin (1993) reported a grass and shrub / sand type that was dominated by Symphoricarpos occidentalis, however, Rosa spp. and Prunus virginiana were present in 50% of plots. This community type was typically found on stabilized dunes, with rapidly drained, sandy soils and Calamovilfa longifolia was listed as a common graminoid species.

Heidel et al. (2000) and the Montana Natural Heritage Program (2002) both report a Prunus virginiana Shrubland in Montana. The Natural Heritage Program does not provide a description of the community but gives it a rank of G4Q/S4. Heidel et al. (2000) noted that the shrubland was small in area when it occurred in the Medicine Lake Sandhills. They noted that the community type typically had a high shrub cover and low understorey cover due to the density of shrubs, although Hesperostipa comata was a common understorey graminoid species. Prunus virginiana has a deep root system, allowing the shrubs to reach the water table in the Medicine Lake Sandhills. Elsewhere in Montana the community type was considered to be a riparian community (Heidel et al. 2000).

Cooper et al (1999) reported a Prunus virginiana – (Prunus americana) Shrubland community in Montana. It was found in the Bitter Creek Badlands, located at heads of coulees feeding into badlands. The community occurred as very small patches, often linear in shape and very dense. Very few other species were present because of the density of the Prunus.

Natureserve (2002) reported a Prunus virginiana Shrubland Alliance. The community was typically found along streams, rivers, lakes and ponds and on terraces, or in canyons or steep gullies where elevations range from 716 m to about 1600 m in Montana, Wyoming and Colorado and up to 2440 m in Nevada. In certain locations, the alliance occurred on side slopes, immediately below a seep or spring. Some examples of this alliance have been classified as having an intermittently or temporarily flooded hydrologic regime. Soils were typically well developed and well drained and were typically composed of shallow to deep alluvial deposits.

A Prunus virginiana – (Prunus americana) Shrubland was reported occurring in Badlands National Park, South Dakota (USGS 2002d). This community, however, was dominated by Prunus americana, with some P. virginiana. It was typically found in

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sloping to nearly level mesic draws and nearly level oxbows, although a few stands were also found at seep zones on the edge of sandhills (USGS 2002d).

3.3.7 Eurotia lanata / Stipa comata – Calamovilfa longifolia Association Winter fat / needle and thread – sand grass

Within Alberta, Smoliak (1985) reported a Stipa – Bouteloua – Agropyron type near Manyberries, in southern Alberta. The author noted that this type was typically found on upland prairie, with Eurotia lanata as a common shrub.

Looman (1980) recorded a Stipa comata Association for the prairie provinces in Canada. The author noted that this community was found to be common (with Bouteloua gracilis) on dry prairie. A variation of the community was also noted and included Calamovilfa longifolia, occurring on sandy loam or loamy sand soils. Eurotia lanata was not mentioned as occurring.

Natureserve (2002) reported a Krascheninnikovia lanata / Hesperostipa comata Dwarf-Shrubland Alliance. It was considered to be a minor alliance and included dwarf-shrublands scattered across the interior western U.S. Stands occur on plateaus, plains, mesas, hillslopes, alkaline flats around playas and along drainages. Some habitats were intermittently flooded wetlands. It was typically found on flat to gently sloping sites occurring on any aspect, but stands have also been reported from moderately steep slopes. Soils were commonly calcareous to moderately alkaline and are typically stony, sandy loam. The ground cover was mostly bare soil. The cover of Krascheninnikovia lanata and Hesperostipa comata varied from 5 to 60%. The vegetation was reported to be sparse in many of these stands and might be better classified in a sparsely vegetated alliance.

The Montana Natural Heritage Program (2002) reported a Krascheninnikovia lanata / Stipa comata Dwarf-Shrubland community for Montana and ranked it as G3/S3. A Eurotia lanata / Poa secunda extremely xeromorphic dwarf-shrubland was listed as a natural plant community type for Idaho (Rust 1997) 3. Unfortunately no descriptions were given for either of these communities.

Faber-Langendoen (2001) reported a Krascheninnikovia lanata / Bouteloua gracilis Dwarf Shrub Herbaceous community type for the mid-western United States. The vegetation contained open shrub and graminoid layers, where the short herbaceous layer was dominated by Bouteloua gracilis, Echinacea angustifolia and Liatris punctata. This community type was found in the southwestern Great Plains and semi-desert mountains, from Colorado south to New Mexico and Arizona and was also reported in Kansas.

3.3.8 Salix exigua / Glycyrrhiza lepidota - Juncus balticus Association Sandbar willow / wild licorice – wire rush

No community types with a similar plant species composition could be found for Alberta. However, many have been described for the Great Plains region in the United States.

Faber-Langendoen (2001) described a Salix exigua / Mesic Graminoids Shrubland for the Midwestern United States. For this community type, the vegetation was dominated by

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shrubs with a fairly dense (at least 30 %) ground cover of mesic graminoids and forbs. Juncus spp. was noted as a common herbaceous species. The community was most commonly found on sandbars, islands and shorelines of stream channels and braided rivers and soils are typically poorly developed. This community was predominantly found in the Great Plains but also in parts of Rocky Mountains and intermountain semi-desert regions, from Wyoming west to possibly Idaho, south to Utah and east to Oklahoma. The author also reported a Salix exigua Temporarily Flooded Shrubland community that was dominated by 2 – 4 m tall Salix exigua with a moderate to high stem density. This community was dominantly found on recently deposited or disturbed alluvial materials, composed primarily of sands. It was found at lower elevations throughout the northwestern US and Great Plains and into Manitoba.

Cooper et al. (1999) noted a Salix exigua Temporarily Flooded Shrubland community in the Beaverhead Mountains of Montana. At this location, the community was typically found on gravelly alluvial materials on floodplains and terraces in river bottoms. Understorey species were minimal due to the high disturbance rate, but the most common were reported to be Cirsium arvense, Mentha arvensis and Phalaris arundinacaea.

Several natural plant community types, dominated by Salix exigua, were reported by the Montana Natural Heritage Program (2002). They included a Salix exigua / Barren Shrubland, a Salix exigua / Mesic Graminoid Shrubland and a Salix exigua Temporarily Flooded Shrubland. Unfortunately no descriptions of the community types were provided but all were ranked as G5/S5.

Several natural plant community types dominated by Salix exigua were reported for the State of Idaho (Rust 1997) and are listed below:

��Salix exigua / Barren seasonally flooded cold-deciduous shrubland, ��Salix exigua / Equisetum arvense seasonally flooded cold-deciduous shrubland, ��Salix exigua / Mesic Forb seasonally flooded cold-deciduous shrubland, ��Salix exigua / Mesic Graminoid seasonally flooded cold-deciduous shrubland and ��Salix exigua / Rosa woodsii seasonally flooded cold-deciduous shrubland.

Unfortunately, no detailed descriptions were provided for these community types.

A Salix exigua Shrubland community, has been described from the margins of the North Platte River at Scotts Bluff National Monument in Nebraska (USGS 2002a) This community type was reported to occur on recently deposited alluvial sands where there was little soil development. The understorey species composition was quite different from that found at the Pakowki Sandhills and the occasional Populus deltoides was also noted to occur. A similar Salix exigua Shrubland [Provisional] community was found along the Niobara River, at the Agate Fossil Beds NM in Nebraska (USGS 2002c). At this location, the community was found along lower floodplain terraces, with sandy loam soils that were poorly to somewhat poorly drained. Juncus balticus was listed as an abundant species and the authors noted that species diversity was quite high.

A Salix exigua Temporarily Flooded Shrubland community has been described from Badlands National Park, in South Dakota (USGS 2002d) At this location, the community was found along banks of several creeks within the park. The authors noted that the sites for this plant community were nearly all level and that ground water was present.

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3.3.9 Glycyrrhiza lepidota - Calamovilfa longifolia Association Wild licorice – sand grass

A 1993 survey of the Pakowki Sandhills reported the occurrence of Glycyrrhiza lepidota with Calamovilfa longifolia and Artemesia ludoviciana (Komex 1993). Although a detailed description of the community type was not provided, the authors noted that wire rush (Juncus balticus) was also commonly found in Glycyrrhiza lepidota sites.

The only reported Glycyrrhiza lepidota community type from outside Alberta was found in Montana. The Montana Natural Heritage Program (2002) recorded a Glycyrrhiza lepidota Herbaceous Vegetation community for the state and it is currently ranked as S? . Unfortunately, no detailed description of the plant community was provided.

3.3.10 Glycyrrhiza lepidota – Artemisia spp. - Stipa comata Association Wild licorice – sage – needle and thread

A 1993 survey of the Pakowki Sandhills reported the occurrence of Glycyrrhiza lepidota with Calamovilfa longifolia and Artemesia ludoviciana (Komex 1993).

Looman (1980) recorded a Stipa comata Association for the prairie provinces in Canada. The author noted that this community was found to be common (with Bouteloua gracilis) on dry prairie. A variation of the community was also noted and includes Calamovilfa longifolia, occurring on sandy loam or loamy sand soils, although Glycyrrhiza lepidota was not noted to occur.

Hulett et al. (1966) recorded a Stipa comata – Artemesia frigida plant community that was dominant on stabilized dunes in Great Sand Hills of Saskatchewan Glycyrrhiza lepidota was not reported to be present in the community.

The only reported Glycyrrhiza lepidota community type from outside Alberta was found in Montana. The Montana Natural Heritage Program (2002) recorded a Glycyrrhiza lepidota Herbaceous Vegetation community for the state and it is currently ranked as S? . Unfortunately, no detailed description of the plant community was provided.

3.3.11 Rumex venosus Association Wild begonia

No community types with a similar plant species composition could be found for Alberta. However, several have been described for areas outside Alberta, but not in the United States.

Looman (1980) described a Rumex venosus Alliance that was dominant on highly mobile dunes, during early stages of development. Epp and Townley-Smith (1980) also noted that Rumex venosus occurred on active sand dune complexes, typically towards the edge of the deflation zone and on sides of dunes in their Active Sand Dune Complex. However, no Rumex venosus community type was described.

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3.3.12 Oryzopsis hymenoides – Sporobolus cryptandrus Association Indian rice grass – sand dropseed

Only one community type with a somewhat similar plant species composition could be found for Alberta. Fehr (1984) reported a Carex foenea – Calamovilfa longifolia – Elymus canadensis – Oryzopsis hymenoides community in the Wainwright sand dune area, on active blowouts. ANHIC reported an Oryzopsis hymenoides / Leymus canadensis sparsely vegetated plant community that they have ranked as S2 for the province (Allen 2002), but no detailed description was provided.

Outside Alberta, there are numerous reports of related community types. Looman (1980) reported an Oryzopsis hymenoides Order within the Calamovilfetea class for the Canadian prairie provinces, though no details were provided on its species composition or the associated habitat. Hulett et al. (1966) reported a Psoralea lanceolata – Oryzopsis hymenoides community that was a dominant association in the Great Sand Hills (Saskatchewan) on active sand dune complexes. Epp and Townley-Smith (1980) also reported a Psoralea lanceolata – Oryzopsis hymenoides community type from the Great Sand Hills where it formed a sparse cover located on the edge of deflation zones away from the active portions of the dune. The authors noted that the vegetative cover tended to increase as the distance from deflation zone increased.

In Montana, Heidel et al. (2000) reported an Oryzopsis hymenoides – Psoralidium lanceolatum community in the Medicine Lake Sandhills in Montana, that was restricted to slopes and crests of sand dunes recently disturbed by soil erosion. Sporobolus cryptandrus was also present and often formed up to 10% cover. The community type was most commonly found in blowouts and was thought to be the driest and earliest stage of succession.

An Oryzopsis hymenoides – Psoralidium lanceolatum Herbaceous vegetation association was reported to be a natural plant community for the state of Montana, where it was ranked G3Q/S? (MNHP 2002).

An Achnatherum hymenoides Herbaceous Alliance was reported by Natureserve (2002) where it occurred in two distinctively different habitats: sandy areas and shale barrens, in different geographic areas. Sandy areas included 'blowouts' in the Great Plains and in arid and semi-arid dune systems in the Chihuahua Desert, San Luis Valley, Colorado Plateau and Great Basin. Substrates were dominantly sand or shale. This alliance was characterized by a sparse to moderately dense herbaceous layer that was dominated by Achnatherum hymenoides (= Oryzopsis hymenoides). An Achnatherum hymenoides - Psoralidium lanceolatum Herbaceous Vegetation association and a Calamovilfa longifolia - Achnatherum hymenoides Herbaceous Vegetation association was also listed by Natureserve (2002) but no descriptions were given.

3.3.13 Stipa comata – Oryzopsis hymenoides Association Needle and thread – Indian rice grass

Only one community type with a somewhat similar plant species composition could be found for Alberta. Fehr (1984) reported a Carex foenea – Calamovilfa longifolia –

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Elymus canadensis – Oryzopsis hymenoides community in the Wainwright sand dune area, on active blowouts. However, Stipa comata was not listed as a component of this community.

Looman (1980) recorded a Stipa comata Association for the prairie provinces in Canada. The author noted that this community was found to be common (with Bouteloua gracilis) on dry prairie. A variation of the community was also noted and includes Calamovilfa longifolia, occurring on sandy loam or loamy sand soils although Achnatherum hymenoides was not noted to occur. Looman (1980) also reported an Oryzopsis hymenoides Order within the Calamovilfetea class for the Canadian prairie provinces, though no details are provided on its species composition or the associated habitat. Hulett et al.(1966) reported a Psoralea lanceolata – Stipa comata community that was a dominant association in Dundurn Sand Hills (Saskatchewan) on stabilized dune complexes. Hulett et al.(1966) reported a Psoralea lanceolata – Oryzopsis hymenoides community that was a dominant association in the Great Sand Hills (Saskatchewan) on active sand dune complexes. This same report also recorded a Stipa comata – Artemesia frigida plant community that was dominant on stabilized dunes in the Great Sand Hills of Saskatchewan.

Epp and Townley-Smith (1980) also reported a Psoralea lanceolata – Oryzopsis hymenoides community type from the Great Sand Hills where if formed a sparse cover located on the edges of deflation zones away from the active portions of the dune. The authors noted that the vegetative cover tended to increase as the distance from the deflation zone increased.

Heidel et al. (2000) reported a Stipa comata / Psoralidium lanceolatum Herbaceous Vegetation association from the Medicine Lake sand hills in Montana. This community was restricted to wind-blown sand deposits with undeveloped soils and was found on choppy dunes to rolling plains. It was thought to be a seral stage between the Oryzopsis hymenoides / Psoralidium lanceolatum and the Pascopyrum smithii - Stipa comata association. Grass cover was typically 20-40% and most was composed of Stipa comata. This community was most common on stabilized to partially stabilized sand dunes. An Oryzopsis hymenoides – Psoralidium lanceolatum Herbaceous vegetation association was reported to be a natural plant community for the state of Montana, where it is ranked G3Q/S? (MNHP 2002).

Natureserve (2002) reported an Hesperostipa comata - Achnatherum hymenoides Herbaceous Vegetation association. This grass type has been reported from the Great Divide Basin in south-central Wyoming. Hesperostipa comata and Achnatherum hymenoides co-dominated the graminoid stratum, while Pascopyrum smithii was a secondary species. Scattered shrubs were present, primarily Artemisia tridentata ssp. wyomingensis. This type apparently has not been described outside the Great Divide Basin of south-central Wyoming. Other basins in south-central and southwestern Wyoming and the northwestern quarter of Colorado are similar in climate and geology and this association may well extend over a wide area of the two states.

An Hesperostipa comata Bunch Herbaceous Alliance was also reported by Natureserve (2002). This grassland alliance was found on sandy soils in the Intermountain Steppe, Wyoming Basin, Colorado Plateau, Great Basin and Columbia Plateau. The community

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typically occurred on upland sites with coarse-textured soils such as sandstone outcrop ridges in the plains, dry-sandy sites in the Columbia Basin and on dissected alluvial fans below sandstone plateaus, but not on dunes.

3.3.14 Artemisia spp. - Stipa comata – Calamovilfa longifolia Association Sage – needle and thread – sand grass

Smoliak (1985) reported a Calamovilfa longifolia – Artemisia community on upland prairie with sandy soils in the Manyberries region of southern Alberta. However, no other description of the community type was provided.

Looman (1980) recorded a Stipa comata Association for the prairie provinces in Canada. The author noted that this community was found to be common (with Bouteloua gracilis) on dry prairie. A variation of the community was also noted and included Calamovilfa longifolia, occurring on sandy loam or loamy sand soils. However, no mention of Artemisia spp. being a component of this community was noted.

Hulett et al. (1966) recorded a Stipa comata – Artemesia frigida plant community that was dominant on stabilized dunes in the Great Sand Hills of Saskatchewan, but did not elaborate on its composition or distribution.

3.3.15 Stipa comata – Cyperus schweinitzii – Calamovilfa longifolia Association Needle and thread – sand nut-grass – sand grass

Adams et al. (1997) described a similar Calamovilfa longifolia – Hesperostipa comata community from CFB Suffield, in southeastern Alberta. Site conditions differed in that this community was described as occurring on fluvial slump features along the South Saskatchewan River, where a sand veneer was present. Soils were typically loamy sand and slopes ranged from 5 to 15 %, although some 60% slopes were reported. This community type was also found on glaciofluvial outwash plains, with minimal eolian action. Soil textures were loamy sand and slopes ranged from 0 to 5%. Smoliak (1985) reported two similar community types in the Manyberries area of southern Alberta. The author described a Calamovilfa longifolia – Artemesia plant community that was found on upland prairie with sandy soils and a Calamovilfa longifolia – Stipa comata community found on sandy soils, in coulee bottoms.

Looman (1980) recorded a Stipa comata Association for the prairie provinces in Canada. The author noted that this community was found to be common (with Bouteloua gracilis) on dry prairie. A variation of the community was also noted and includes Calamovilfa longifolia, occurring on sandy loam or loamy sand soils.

Hulett et al. (1966) recorded a Stipa comata – Artemesia frigida plant community that was dominant on stabilized dunes in the Great Sand Hills of Saskatchewan and noted that Calamovilfa longifolia was present. Hulett et al. (1966) also described a Psoralea lanceolata - Stipa comata plant community that was dominant at the Dundurn Sand Hills (Saskatchewan) on stabilized dunes. Calamovilfa longifolia was reported to be present in this community. Furthermore, the authors described a Stipa comata – Calamovilfa longifolia – Agropyron spp. community that was found in the Dundurn Sand Hills. The

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authors noted that this community was most common in dune depressions and appeared to be intermediate between stabilized blowouts and stabilized dunes.

Cooper et al. (2001) reported a Calamovilfa longifolia – Hesperostipa comata Herbaceous Vegetation association from the Rock Creek Canyon and a few sandy outcrops in the Bitter Creek Badlands area of Montana. This community was found to occur most abundantly where sandy substrates were dominant, on stabilized dunes, interdunal swales and colluvial sands. The authors reported that the community was found to be highly restricted in area and occurred mainly on colluvial sands.

Heidel et al. (2000) also reported a Calamovilfa longifolia – Stipa comata Herbaceous Vegetation association in the Medicine Lake Sandhills in Montana. The authors considered it to be a minor type. It did not appear to be a widespread community in the Medicine Lake Sandhills, occurring only in small patches on low ridges and in a mosaic pattern on gentle plains of Medicine Lake.

Jones (1998a; 1998b) noted Calamovilfa longifolia - Hesperostipa comata Grassland communities along several rivers and streams in northeastern Wyoming. The author described this community type on sandy soils at an intermediate height above the river channel and noted it was a major community type in the region. Other dominant species included Calamovilfa longifolia, Stipa comata and Psoralea lanceolata.

Faber-Langendoen (2001) and Natureserve (2002) reported a Calamovilfa longifolia – Hesperostipa comata Herbaceous Vegetation community from the mid-western United States. The vegetation had an open canopy dominated by Calamovilfa longifolia and Hesperostipa comata. This community was found to occur on stabilized sand dunes as well as in interdunal valleys or draws, colluvial sands and less commonly on silty terraces of intermittent streams. Soils were generally medium to fine sands, formed from either eolian or colluvial processes. The author noted that this community was found in the central and northern Great Plains, ranging from Colorado to Nebraska and north to Wyoming and South Dakota.

3.3.16 Sporobolus cryptandrus – Calamovilfa longifolia – Oryzopsis hymenoides Association Sand dropseed – sand grass – Indian rice grass

Wheatley and Bentz (2002) and Meijer and Karpuk (1999) described a Sporobolus cryptandrus – Calamovilfa longifolia – Koeleria macrantha – Carex obtusata community type from the Central Parkland of Alberta. This community type was found on active dunes and blowouts at Dillberry Lake Provincial Park where it was generally located on south to west-facing aspects and had a sparse vegetative cover. Heterotheca villosa was also reported to be present. In a 1993 survey of the Pakowki Sandhills, a Calamovilfa longifolia – Sporobolus cryptandrus sparsely vegetated active sand dune complex was reported (Komex 1993). Other reported species included Helianthus couplandii, Thermopsis rhombifolia and Heterotheca villosa.

ANHIC currently ranks Sporobolus cryptandrus sparsely vegetated active dune plant communities as S2 (Allen 2002).

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Looman (1980) described a Calamovilfa longifolia vegetation Class from the Canadian prairie provinces. This class was reported to be dominant in well-developed sandhill prairie and could include other characteristic species such as Elymus canadensis, Helianthus couplandii and Sporobolus cryptandrus.

Thorpe and Godwin (1993) described a Carex pennsylvanica – Sporobolus cryptandrus – Cyperus schwentzeii – Calamovilfa longifolia community on active sand in the Manito Sandhills of west-central Saskatchewan. This community type was found on sparsely vegetated, active east/west oriented sand dunes that were rapidly drained. The soils were coarse-textured and had little to no organic matter to retain moisture.

The Montana Natural Heritage Program (2002) listed a Sporobolus cryptandrus Shrub Herbaceous Vegetation association as a natural plant community for the state. The community was ranked G2/S2 for Montana, but unfortunately, no description of the community was provided.

The State of Idaho also listed several natural Sporobolus cryptandrus plant communities, including:

��Sporobolus cryptandrus – Poa secunda Medium-tall bunch temperate or sub-polar grassland,

��Sporobolus cryptandrus Medium-tall temperate or subpolar grassland with a needle-leaved or microphyllous evergreen shrub layer and

��Heterotheca villosa / Sporobolus cryptandrus Low temperate or subpolar forb vegetation.

Natureserve (2002) listed two Alliances and one Association with Sporobolus cryptandrus as the dominant species. A Sporobolus cryptandrus Herbaceous Alliance was described for the lower Salmon and Snake river canyons of Idaho, Oregon and Washington, the Columbia River in central Washington and the Green and Virgin rivers in Utah (Natureserve 2002). This alliance typically occurred on river terraces, lower slopes of benches and alluvial fans. The elevation ranges from 240 - 1460 m and sites are flat to gently sloping (up to 30%) and tend to occur on all aspects. The climate in the canyon bottoms was relatively hot and dry and soils were moderately deep and derived from loess and alluvium-colluvium. The soil texture varies from sandy loam to silt loam.

A Sporobolus cryptandrus - Poa secunda Herbaceous Vegetation association was described by Natureserve (2002) for the Columbia Basin and lower Snake River, where it occurred on gentle, lower slopes. It was also found on river terraces in the valleys of the Snake and Clearwater rivers. Sites were typically dominated by Sporobolus cryptandrus, although Poa secunda was common but varied in abundance. Aristida purpurea var. longiseta (= Aristida longiseta) and Hesperostipa comata (= Stipa comata) were also frequently present in low abundance.

A Sporobolus cryptandrus Shrub Herbaceous Alliance was described from Montana, Idaho and New Mexico (Natureserve 2002). In New Mexico, the alliance occurred in the northwestern part of the state on alluvial flats at an elevation of approximately 2140 m. The climate was semi-arid with most of the highly variable annual precipitation falling during the summer as high-intensity storms. Sites are nearly level, soils are calcareous, loamy and generally less than 25 cm deep.

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3.3.17 Artemisia cana / Stipa comata Association Silver sagebrush / needle and thread

A similar community type has been described in several sources for Alberta. Holcroft Weerstra (2001) describe an Artemisia cana / Stipa comata community that was found to occur along old river terraces, badlands, ravine side slopes and valley walls on a range of parent materials, but occurred most often on sandy glacial drift and alluvium. Adams et al. (1997) also described an Artemisia cana / Calamovilfa longifolia – Stipa comata from CFB-Suffield in southeastern Alberta. This community was typically found on glaciofluvial channel banks, with slopes greater than 15% and also on glaciofluvial terraces, with superimposed sand dunes. On both parent materials, the soil texture was sand to loamy sand. ANHIC currently lists an Artemisia cana / Stipa comata Shrub Herbaceous community and an Artemisia cana / Stipa comata – Calamovilfa longifolia Shrub Herbaceous community, both of which are currently ranked S2S3.

Coupland (1950) described a Rosa woodsii (Artemesia cana / Elaeagnus commutata) community type for the prairie provinces that was found in undulating to gently rolling areas between stabilized dunes. At these locations, the water table was typically within eight to twelve feet of the soil surface. However, the author did not describe the associated graminoid composition.

Cooper et al. (2001) described an Artemisia cana / Hesperostipa comata Shrub Herbaceous Vegetation association in the Bitter Creek / Frenchman Creek area in Montana. It was considered to be a minor type, due to limited distribution of coarse textured materials. At this location, the community type was found on benches to gently inclined slopes (30% maximum recorded) in the vicinity of breaklands. This community type was found to occur on a variety of parent materials but was located dominantly on well-drained, often sandy glacial drift and sandy alluvium. The Montana Natural Heritage Program (2002) lists an Artemisia cana / Stipa comata Shrub Herbaceous Vegetation natural plant community for Montana. It is currently ranked S3 for the state.

Faber-Langendoen (2001) described an Artemisia cana / Hesperostipa comata Shrub Herbaceous Vegetation from the Midwestern United States. The author considered this community to be a small patch type, with a narrow geographic distribution, though it may be expected to occur in Saskatchewan and North Dakota. The author considered habitats with the potential to support this type to be relatively abundant, but the type itself to be comparatively uncommon. The community was typically found on well-drained benches and gently inclined landforms in a primarily agricultural landscape and thus puts it at a moderate risk for agriculture conversion. Fortunately this landform also occurred in breakland and badland environments that are less attractive for agriculture, thus reducing the risk of this type being converted to agriculture.

Natureserve (2002) reported an Artemisia cana / Hesperostipa comata Shrub Herbaceous Vegetation community occurring in the northwestern Great Plains. This shrub prairie association generally occurred in small patches (less than 1 hectare). Sites occurred on various parent materials, but mostly well-drained, often sandy, glacial drift and sandy alluvium. Artemisia cana was the dominant shrub with canopy coverages to 50 %, but averaged around 25 %.

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3.4 Assignment of a Preliminary Provincial Ranking and Identification of Knowledge Gaps The amount (i.e. proposed plant communities with only one plot) and quality of available data used to describe the proposed sand dune and sand plain community types and assign provincial rankings differed from community to community. Furthermore, mapping of community types was not a component of this project. As such, there is no spatial context to provide an estimate of how much area each community type covers. Consequently, some community types were difficult to rank due to deficient or incomplete data and a lack of spatial context. For those communities that are ranked, more information is required to confirm the proposed rank. The recommended provincial ranks for each of the proposed community types is presented below, in association with an explanation of information gaps and recommended strategies to help address these gaps.

3.4.1 Populus deltoides / Glycyrrhiza lepidota - Juncus balticus Association Western cottonwood / Wild licorice – wire rush Preliminary Rank: S2S3

A review of floristically similar plant communities throughout the Great Plains region revealed that this community type had been documented only in fluvial zones within Alberta, but in a similar sand dune/plain habitat in the Great Sand Hills of Saskatchewan. A somewhat similar community has been reported in numerous states, although restricted primarily to a fluvial-dominated habitat. Populus deltoides is currently ranked S3 by the province and Natureserve ranks a somewhat similar community type as G3G4. A preliminary rank of S2S3 is suggested for Alberta, due to the limited number of reports of this community type in a non-fluvial environment and also due to the current ranking of P. deltoides as S3.

This community was found in localized depressions between sand dunes and in more open sand plain areas. It was observed in a number of locations in the Pakowki Sandhill area and in certain locales, it appeared to be co-dominated by Populus tremuloides. One plot indicated that Populus tremuloides was a co-dominant species, although it shared a high prominence of understorey species that were also found in the Populus deltoides dominated plots. With limited plot data, it was difficult to assign a new community type based solely on one plot. As such it was included with this community type, but may indeed represent a different community type. Additional surveys of the Pakowki and other mixedgrass sandhill areas would be advantageous to identify this potential type.

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3.4.2 Rosa woodsii / Sporobolus cryptandrus Association Common wild rose / sand dropseed Preliminary Rank: S3?

Despite Rosa woodsii being a widely distributed and often abundant species, little information could be found documenting Rosa woodsii dominated plant community types. A prior survey of the Pakowki Sandhills (Komex 1993) noted its presence and a survey of the Great Sand Dunes mentioned that Rosa woodsii dominated communities could be dominant in leeward areas where sand accumulation was occurring (Epp and Townley-Smith 1980). It was also listed as a community type in two locations for the state of Montana, where it is ranked G5/S5 and is a reported plant community type for Idaho. Unfortunately no floristic or habitat descriptions accompany these records.

Considering that Sporobolus cryptandrus is currently ranked S3 by the province of Alberta and its limited documentation as a mixedgrass or sand hill community in the literature, a preliminary rank of S3? is recommended until additional information regarding this potential community type becomes available.

3.4.3 Salix amygdaloides – Rosa woodsii / Juncus balticus – Sporobolus cryptandrus Association Peach-leaf willow – common wild rose / wire rush – sand dropseed Preliminary Rank: S3?

Little information could be found documenting Salix amygdaloides dominated plant community types within Alberta. A prior survey of the Pakowki Sandhills (Komex 1993) noted its presence as both a shrub and a tree, in low-lying areas and a survey of CFB – Suffield noted a general Salix spp. / Stipa comata association along the floodplains and terraces of the South Saskatchewan River (Jaques 1977). Macdonald (1996) noted that Salix amygdaloides was an infrequent component in these wetter habitat types. Documentation of Salix amygdaloides or Salix amygdaloides / Salix exigua Woodlands along riparian zones exists for a number of Great Plains and Northern Rocky Mountain states. However, the habitat of these communities differs somewhat, in that periodic flooding or soil saturation is considered to be a natural factor in the riparian-type Salix amygdaloides-dominated communities.

Considering that Salix amygdaloides and Sporobolus cryptandrus are currently ranked S3 by the province of Alberta and its limited documentation as a mixedgrass or sandhill community in the literature, a preliminary rank of S3? is recommended until additional information regarding this potential community type becomes available.

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3.4.4 Elaeagnus commutata / Glycyrrhiza lepidota Association Silverberry / wild licorice Preliminary Rank: S2

A survey of Dillberry Provincial Park reported a meadow Elaeagnus commutata community with Glycyrrhiza lepidota and Juncus balticus and Calamovilfa longifolia. Wheatley and Bentz (2002) suggested a preliminary ranking of S2 for this community type. An Elaeagnus commutata / Symphoricarpos occidentalis – Rosa woodsii / Poa palustris was also described from the Central Parkland occurring near Wainwright on subxeric to submesic dune sites with good internal soil drainage (Fehr 1984), which was ranked SU (Wheatley and Bentz 2002). Currently, ANHIC lists an Elaeagnus commutata / Pascopyrum smithii Shrubland community for the Grassland Natural Region and it is ranked S3 (Allen 2002).

A preliminary rank of S2 is suggested for this community type, as it shares a similar floristic composition as the community type reported for Dillberry Provincial Park. Although it was not found in the immediate vicinity of a lake, it was found in depressional, moisture-receiving locations between sand dunes.

3.4.5 Elaeagnus commutata / Artemisia ludoviciana - Calamovilfa longifolia Association Silverberry / Prairie sagewort – sand grass Preliminary Rank: S2?

A survey of Dillberry Provincial Park reported a meadow Elaeagnus commutata community with Glycyrrhiza lepidota and Juncus balticus and Calamovilfa longifolia. Wheatley and Bentz (2002) suggested a preliminary ranking of S2 for this community type. An Elaeagnus commutata / Symphoricarpos occidentalis – Rosa woodsii / Poa palustris community was also described from Central Parkland occurring near Wainwright on subxeric to submesic dune sites with good internal soil drainage (Fehr 1984), which was ranked SU (Wheatley and Bentz 2002). Currently, ANHIC lists an Elaeagnus commutata / Pascopyrum smithii Shrubland community for the Grassland Natural Region and it is ranked S3 (Allen 2002).

A preliminary rank of S2? is suggested for this community type, as there is only one sample plot from the Pakowki Sandhills area and it shares some floristic and environmental characteristics with the community type described above. Further sampling in the Pakowki Sandhills and other sandhill and sand plains areas could help to clarify the status of this community type.

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3.4.6 Prunus virginiana / Calamovilfa longifolia Association Choke cherry – sand grass

Preliminary Rank: S4

A prior survey of the Pakowki Sandhills (Komex 1993) noted dense Prunus virginiana thickets along low dune ridges and slopes, but did not provide a further description of this type. In Montana, a Prunus virginiana Shrubland was found as a small patch community within the Medicine Lake Sandhills (Heidel et al. 2000) although elsewhere in the state it is considered a riparian community. Montana and Natureserve (MNHP 2002; Natureserve 2002) currently rank this community type as G4Q/S4. In Alberta, Prunus virginiana is currently ranked as S5 while Calamovilfa longifolia is ranked S4. As such, a preliminary rank of S4 is recommended for the Prunus virginiana / Calamovilfa longifolia community type.

3.4.7 Eurotia lanata / Stipa comata – Calamovilfa longifolia Association Winter fat / needle and thread – sand grass Preliminary Rank: S4?

Little information could be found documenting Eurotia lanata dominated plant community types within Alberta or Saskatchewan. A prior survey of the Pakowki Sandhills (Komex 1993) noted its presence in association with Bouteloua gracilis – Stipa comata on relatively level sites. Looman (1980) also noted that is a component of a Stipa comata grassland association. Several descriptions of a Eurotia lanata dominated plant community type exist for the Great Plains and Midwestern regions of the United States. Both Montana (MNHP 2002) and Natureserve (2002) report a Krascheninnikovia lanata / Hesperostipa comata dwarf shrubland association, which is ranked as G3/S3. Currently ANHIC ranks Eurotia lanata and Calamovilfa longifolia as S4, while Stipa comata is ranked S5. Therefore, due to the lack of information regarding this community type in Alberta and the individual rankings for each of the component species, a preliminary rank of S4? is recommended for this community type.

3.4.8 Salix exigua / Glycyrrhiza lepidota - Juncus balticus Association Sandbar willow / wild licorice – wire rush Preliminary Rank: SU

No information related to a Salix exigua dominated shrubland could be found from within Canada. Several Salix exigua dominated community types from the Great Plains and Midwestern regions of the United States were found, but in most instances the community types were associated with riparian habitats and experienced seasonally or temporary flooding. ANHIC currently ranks Salix exigua and Juncus balticus as S5 while

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Glycyrrhiza lepidota is ranked as S4. Despite the relative widespread distribution of the dominant species, little is recorded relating this community type to sandhill and sand plain habitats. As such a preliminary rank of SU is recommended while further studies are conducted to clarify the status of this community type.

3.4.9 Glycyrrhiza lepidota - Calamovilfa longifolia Association Wild licorice – sand grass Preliminary Rank: SU

Very little information exists in either Canada or the United States regarding Glycyrrhiza lepidota dominated community types. A prior survey of the Pakowki Sandhills (Komex 1993) noted Glycyrrhiza lepidota occurring with Calamovilfa longifolia and Artemisia ludoviciana. The Montana Natural Heritage Program (2002) notes a Glycyrrhiza lepidota herbaceous vegetation association as a natural plant community for the state, but provides a ranking of S?. Consequently, a preliminary rank of SU is recommended while further studies are conducted to clarify the status of this community type.

3.4.10 Glycyrrhiza lepidota – Artemisia spp. - Stipa comata Association Wild licorice – sage – needle and thread Preliminary Rank: SU Very little information exists in either Canada or the United States regarding Glycyrrhiza lepidota dominated community types. A prior survey of the Pakowki Sandhills (Komex 1993) noted Glycyrrhiza lepidota occurring with Calamovilfa longifolia and Artemisia ludoviciana. The Montana Natural Heritage Program (2002) notes a Glycyrrhiza lepidota herbaceous vegetation association as a natural plant community for the state, but provides a ranking of S?. Consequently, a preliminary rank of SU is recommended while further studies are conducted to clarify the status of this community type.

3.4.11 Rumex venosus Association Wild begonia Preliminary Rank: SU

Very little information exists in either Canada or the United States regarding Rumex venosus dominated community types. No references to any community types could be found in Alberta, although Looman (1980) notes a Rumex venosus Alliance for the Canadian Prairie Provinces, where it tends to occur on highly mobile sand dunes. Epp and Townley-Smith (1980) also noted that Rumex venosus could be prominent on active sand dunes in Saskatchewan, though it is not described as a community type per-se. Consequently, a preliminary rank of SU is recommended while further studies are conducted to clarify the status of this community type.

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3.4.12 Oryzopsis hymenoides – Sporobolus cryptandrus Association Indian rice grass – sand dropseed Association Preliminary Rank: S3 Very little information exists in Alberta or other prairie provinces regarding Oryzopsis hymenoides – Sporobolus cryptandrus communities. One report exists of a Carex foenea – Calamovilfa longifolia – Elymus Canadensis – Oryzopsis hymenoides community from an active blowout in the Wainwright sand dune area. However, the species present in this dune community are rather different than those found in the Pakowki Sandhills. Several surveys from Saskatchewan report a Psoralea lanceolata – Oryzopsis hymenoides community type in active sand dunes, but not an Achnatherum hymenoides – Sporobolus cryptandrus community type. In the United States, the Oryzopsis hymenoides – Psoralidium lanceolata community type has been described for Montana (Heidel et al. 2000) and is ranked G3Q / S? by the Montana Natural Heritage Program (2002). Natureserve (2002) also reports an Achnatherum hymenoides Herbaceous Alliance that is found on active sand dunes throughout the Great Plains and upland plateaus, but alliances are not given conservation ratings.

ANHIC currently ranks Oryzopsis hymenoides as S3S4 and Sporobolus cryptandrus as S3. Therefore, due to the limited area in which this community type was found, limited reports of similar community types and the component species current rankings, a preliminary ranking of S3 is recommended for this community type.

3.4.13 Stipa comata – Oryzopsis hymenoides Association Needle and thread – Indian rice grass

Preliminary Rank: S2S3

Very little information exists in Alberta or other prairie provinces regarding Stipa comata – Oryzopsis hymenoides communities. One report exists of a Carex foenea – Calamovilfa longifolia – Elymus Canadensis – Oryzopsis hymenoides community from an active blowout in the Wainwright sand dune area. However, the species present in this dune community are rather different than those found in the Pakowki Sandhills. Several surveys in Saskatchewan report Stipa comata dominated communities on both upland prairie and sand dune habitats, but not in association with Oryzopsis hymenoides. Natureserve (2002) reports two potentially related community types. One is an Hesperostipa comata – Achnatherum hymenoides association that is ranked G2 but has not been found outside the Great Divide Basin in Wyoming. The other similar type listed is an Hesperostipa comata Bunch Herbaceous Vegetation Alliance, from the Wyoming Basin, Colorado Plateau, Great Basin and Columbia Plateau. However, this alliance is not rated and it is also noted to not occur on dunes.

ANHIC currently ranks Oryzopsis hymenoides as S3S4 and Stipa comata S5. However, based on its similarities with the similar reported association in Natureserve (2002) and

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the ANHIC ranking for Oryzopsis hymenoides, a preliminary ranking of S2S3 is suggested for this community type.

3.4.14 Artemisia spp. - Stipa comata – Calamovilfa longifolia Association Sage – needle and thread – sand grass Preliminary Rank: S3S4

Several similar community types have been reported for Alberta and Saskatchewan, although they vary somewhat in species composition and habitat. Smoliak (1984) reports two related community types, one on sandy upland prairie and the other on moist, coulee bottoms in the Manyberries region. Adams et al. (1997) reported a similar community type, though lacking the Artemisia spp. on coarse textured fluvial and glaciofluvial deposits in CFB-Suffield. Hulett et al. (1966) also report a community on partially stabilized dunes with a similar floristic composition.

Natureserve (2002) reports a related association, however this community type places Calamovilfa longifolia as the dominant grass. Furthermore, although Artemisia spp. are noted to be present in certain habitats, they are not considered to be a diagnostic species in the association. This association is ranked as G3. ANHIC ranks Hesperostipa comata as S5 and Calamovilfa longifolia as S4. Based on the documentation of this community type and similar reported types, a preliminary ranking of S3S4 is suggested for the Artemisia spp. - Hesperostipa comata – Calamovilfa longifolia community type.

3.4.15 Stipa comata – Cyperus schweinitzii – Calamovilfa longifolia Association Needle and thread – sand nut-grass – sand grass

Preliminary Rank: S2?

Several similar community types have been reported for Alberta and Saskatchewan, although they vary somewhat in species composition and habitat. Smoliak (1984) reports two related community types, one on sandy upland prairie and the other on moist, coulee bottoms in the Manyberries region. Adams et al. (1997) reported a similar community type, on coarse textured fluvial and glaciofluvial deposits in CFB-Suffield. Hulett et al. (1966) also report a community on partially stabilized dunes with a similar floristic composition.

Natureserve (2002) reports a related association, however this community type places Calamovilfa longifolia as the dominant grass and does not mention the presence of Cyperus schweinitzii. This association is ranked as G3. ANHIC ranks Stipa comata as S5, Cyperus schweinitzii as S2 and Calamovilfa longifolia as S4. Based on the documentation of this community type and similar reported types, a preliminary ranking of S2? is suggested for the Stipa comata – Cyperus schweinitzii – Calamovilfa longifolia community type.

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3.4.16 Sporobolus cryptandrus – Calamovilfa longifolia – Oryzopsis hymenoides Association Sand dropseed – sand grass – Indian rice grass Preliminary Rank: S2S3

Several similar community types have been reported for Alberta and Saskatchewan, although they vary somewhat in species composition and habitat. Wheatley and Bentz (2002) and Meijer and Karpuk (1999) report a related Sporobolus cryptandrus – Calamovilfa longifolia – Koeleria macrantha – Carex obtusata community type from the Central Parkland and it was assigned a preliminary rank of S3. Reports of similar community types by Looman (1980) and Thorpe and Godwin (1993) also exist from Saskatchewan. Natureserve (2002) also reports several related Sporobolus cryptandrus dominated Herbaceous Alliances, although the habitat varies somewhat. Unfortunately, the alliances are not provided with a conservation ranking.

Based on previous reported rankings for similar communities (ANHIC S2 for a Sporobolus cryptandrus active dune community) and ANHIC’s S3 ranking of Sporobolus cryptandrus, a preliminary ranking of S2S3 is suggested for the Sporobolus cryptandrus – Calamovilfa longifolia – Oryzopsis hymenoides community type.

3.4.17 Artemisia cana / Stipa comata Association Silver sagebrush / needle and thread Preliminary Rank: S2S3

This community is currently tracked by ANHIC for the Grassland Natural Region and is ranked S2S3. The distribution and area of the Artemisia cana / Stipa comata community in the Pakowki Sandhills was rather limited and thus does not justify altering the ranking based on an increase in reported area.

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4.0 Conclusion The preliminary classification of the Pakowki Sandhills communities based on the analysis of plot data and a comparison with community types described in existing literature, revealed 17 community types. Community types included all classes, except Non-Vascular and Sparse. All proposed community types were described and assigned a suggested preliminary ranking. Cross-reference tables were created to present similar communities described in the literature, rate their similarity with the Pakowki Sandhills communities and explain their relation to the proposed community types. Knowledge gaps were identified and strategies to address these gaps were provided where possible.

Several difficulties were encountered which should be noted. In the literature, community type descriptions vary from a single sentence to extremely detailed descriptions and in most instances, there is insufficient information to adequately describe community structure and assign a conservation rank (i.e. based on distribution and abundance). No quantification of area for community types could be found in the literature, aside from qualitative notes such as ‘widely distributed’ or ‘abundant.’ Furthermore, no quantification of the area of community types was required for this project. As such, determining the areal coverage of community types was done through observation and estimation. Mapping of community types at a relatively detailed scale would provide a greater confidence behind the estimation of conservation ranks for this project and provide a means to track impacts on community types in the future.

The information in this report can be used to update the community-tracking list by including new community types. Finally, this report can also be used to decide which community types require further studies and to prioritize these studies.

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5.0 Literature Cited Achuff, P.L. 1994. Natural regions, Subregions and Natural History Themes of Alberta. Prepared for Parks Service, Alberta Environmental Protection, Edmonton, Alberta. Adams, G.D., G.C.Trottier, W.L. Strong, I.D. MacDonald, S.J. Barry, P.G. Gregoire, G.W. Babish and G. Weiss. 1997. Vegetation Component Report: Canadian Forces Base Suffield National Wildlife Area Wildlife Inventory. Canadian Wildlife Service, Environment Canada, Prairie and Northern Region. Edmonton, Alberta. Alberta Environmental Protection. 1993. Alberta plants and fungi – master species list and species group checklists. Pub. No.: Ref. 75. Edmonton, Alberta. Alberta Environmental Protection. 1994. Ecological land survey site description manual. Unpubl. Rep. Edmonton, Alberta. 165pp. Alberta Environmental Protection 1997. The Grassland Natural Region of Alberta. Natural Resources Service, Recreation and Protected Areas Division, Natural Heritage Protection and Education Branch. Edmonton, Alberta. Allen, L. 2002. Alberta Natural Heritage Information Centre Preliminary Plant Community Tracking List, Alberta Community Development, Edmonton, Alberta. Barker, W.T. and W.C. Whitman. 1988. Vegetation of the Northern Great Plains. Rangelands 10(6) 266-272. Bowers, J.E. The plant ecology of inland dunes in western North America. Braun-Blanquet, J. 1965. Plant sociology : the study of plant communities. Authorized English translation of Pflanzensoziologie by J. Braun-Blanquet. Translated, rev. and ed. by George D. Fuller and Henry S. Conard.Hafner Publishing Co., Longon, England. 439 pp. Burgess, R.L. 1965. A study of plant succession in the sandhills of southeastern North Dakota. Proceedings of the North Dakota Academy of Science 19:62-80. Chadwick, H.W. and P.D. Dalke. 1965. Plant succession on dune sands in Fremont County, Idaho. Ecology 46(6): 765-780. Cooper, S.V., C. Jean and B.L. Heidel. 1999. Plant associations and Related Botanical Inventory of the Beaverhead Mountains Section, Montana. Unpublished report to the Bureau of Land Management. Montana Natural Heritage Program, Helena. 235 pp. Cooper, S.V., C. Jean and P. Hendricks. 2001. Biological Survey of a Prairie Landscape in Montana’s Glaciated Plains. Report to the Bureau of Land Management, Montana

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Natural Heritage Program, Helena Montana. 24pp. plus appendices. Corns, I.G.W. 1983. Forest community types of west-central Alberta in relation to selected environmental factors. Canadian Journal of Forest Research 13:995-1010. Coupland, R.T. 1950. Ecology of mixed prairie in Canada. Ecological Monographs 20:273-315. Coupland, R.T. 1960. A reconsideration of grassland classification in the northern great plains of North America. Journal of Ecology 49:135-167. Dowding, E.S. 1929. The vegetation of Alberta: III The sandhill areas of central Alberta, with particular reference to the ecology of Arceuthobium americanum. Journal of Ecology, Vol. 17: 82-105. Epp, H.T. and L. Townley-Smith. 1980. The great sand hills of Saskatchewan. Saskatchewan Deportment of the Environment, Policy, Planning and Research Branch. Regina, Saskatchewan. Faber-Langendoen, D. editor. 2001. Plant communities of the Midwest: Classification in an ecological context. Association for Biodiversity Information, Arlington, VA. 61 pp. + appendix (705 pp.). Fehr, A.W. 1984. Wainwright study area: A biophysical inventory. Natural Areas Program, Alberta Energy and Natural Resources. Natural Areas Technical Report No. 15. Edmonton, Alberta. Grossman, D.H., K.L. Goodin and C.L. Reuss, editors. 1994. Rare plant communities of the conterminous United States: an initial survey. The Nature Conservancy, Arlington, Virginia, USA. Grossman, D.H., D. Faber-Langendoen, A.S. Weakley, M. Anderson, P. Bourgeron, R. Crawford, K. Goodin, S. Laandal, K. Metzler, K.D. Patterson, M. Pyne, M. Reid and L. Sneddon. 1998. International classification of ecological communities: terrestrial vegetation of the United States, Volume 1. The National Vegetation Classification System: development, status and applications. The Nature Conservancy, Arlington, Virginia, USA. Hanson, H.C. and W.C. Whitman. 1938. Grassland types in Western North Dakota. Ecological Monographs 8(1): 58-114. Heidel, B, S.V. Cooper and C. Jean. 2000. Plant species of special concern and plant associations of Sheridan County, Montana. Report to U.S. Fish and Wildlife Service. Montana Natural Heritage Program, Helena, Montana. 22pp. plus appendices. Hill, M.O. and H.G. Gauch. 1980. Detrended correspondence analysis: an improved

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ordination technique. Vegetatio 42:47-58. Holcroft-Weerstra, A.C. 2001. Preliminary Classification of Silver Sagebrush (Artemesia cana) Community Types. Alberta Natural Heritage Information Centre, Edmonton, Alberta. Biota Consultants, Cochrane, Alberta. Hulett, G.K., R.T. Coupland, R.L. Dix. 1966. The vegetation of dun sand areas within the grassland region of Saskatchewan. Canadian Journal of Botany 44: 1307-1331. Jaques, D.R. 1977. The vegetation and effects of grazing on the eastern portion of the Suffield Military Reserve, Alberta. pp. D41-D190-. In Stelfox, J.G. ed. Effects of livestock grazing on mixed prairie range and wildlife in PFRA pastures. Suffield Military Reserve. Range–Wildlife Study Committee, Can. Wild. Ser. Rep. Edmonton, Alberta. Jones, G.P. 1998a. Ecological evaluation of the potential Cheyenne River Research Natural Area within the Thunder Basin National Grassland, Converse County, Wyoming. Prepared for Nebraska, National Forest, and USDA Forest Service. Laramie, Wyoming, USA. Jones, G.P. 1998b. Ecological evaluation of the potential Antelope Creek Research Natural Area within the Thunder Basin National Grassland, Converse County, Wyoming. Prepared for Nebraska, National Forest, and USDA Forest Service. Laramie, Wyoming, USA. Kartesz, JT. 1999. A synonymized checklist and atlas with biological attributes for the vascular flora of the United States, Canada and Greenland. First edition. In: Kartesz, JT and CA Meacham. Synthesis of the North American flora [computer program]. Version 1.0. North Carolina Botanical Garden: Chapel Hill, NC. Komex International Ltd. 1993. Preliminary report on biophysical inventory of the Pakowki Sandhills sensitive area. Land Information Services Division, Alberta Forestry Lands and Wildlife, Edmonton, Alberta. Looman, J. 1980. The vegetation of the Canadian Prairie Provinces II. The grasslands, Part I. Phytocoenologia 8(2) 153-190. Macdonald, I.D. 1996. Vascular Plant Flora of Canadian Forces Base Suffield, National Wildlife Area. Canadian Wildlife Service, Environment Canada, Prairie and Northern Region, Edmonton, Alberta. Marriott, H. J. and D. Faber-Langendoen. 2000. The Black Hills community inventory. Volume 2: Plant community descriptions. The Nature Conservancy, Midwest Conservation Science Center and Association for Biodiversity Information, Minneapolis, MN. 326 pp.

Meijer, M. and E. Karpuk. 1999. Dillberry Lake Provincial Park Biophysical Inventory. Natural Resources Service, Parkland Region, Alberta Environment, Edmonton, Alberta.

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Meclune, B. and M.J. Mefford. 1999. PC-ORD. Multivariate Analysis of Ecological Data, Version 4. MjM Software Design, Gleneden Beach, Oregon, USA.

Montana Natural Heritage Program. 2002. 2002 List of Ecological Communities for Montana. Montana Natural Heritage Program, Montana State Library, Helena, Montana. Moss, E.H. 1983. Flora of Alberta. 2nd Edition Revised by J.G. Packer. University of Toronto Press, Toronto, Ontario. Natureserve Explorer: An online encyclopedia of life [web application]. 2001. Version 1.6 . Arlington, Virginia, USA: Natureserve. Available: http://www.natureserve.org/explorer. (Accessed: November 12, 2002 ). Patriquin, D.L. and D. L. Skinner. 1992. Review and assessment of the vegetation, wildlife and habitat of CFB Suffield, Alberta. D.A. Westworth and Associates, Edmonton, Alberta. Rust, S.K. 1997. Natural Plant Communities of Idaho: A Working List for the Conservation of Biological Diversity. Conservation Data Centre, Idaho Department of Fish and Game. Schacht, W.H., J.D. Volesky, D. Bauer, A.J. Smart and E.M. Mousel. 2000. Plant community patterns on upland prairie in the eastern Nebraska sandhills. Prairie Naturalist 32(1):43-58. Jamestown, ND: Northern Prairie Wildlife Research Center Home Page. http://www.npwrc.usgs.ggov/resource/2001/plantcom/plantcom.htm (Version 20AUG2001). Shetsen, I. 1987. Quaternary geology, southern Alberta. Alberta Research Council, Edmonton. Map. Smoliak, S. 1985. Flora of the Manyberries research substation. Lethbridge Research Station Contribution, No. 6, Research Branch, Agriculture Canada. Lethbridge, Alberta. Strong, W.L. 2002. Lodgepole pine / Labrador tea community types of western Canada. Canadian Journal of Botany 80:151-165. Ter Braak, C.J.F. and I.C. Prentice. 1988. A theory of gradient analysis. Advances in Ecological Research 18:271-313. Thorpe, J. and R. Godwin. 1993. Vegetation Survey of the Manito San Hills. Applied Plant Ecology Section, Saskatchewan Research Council. SRC Publication No. E-2550-1-E-93. United States Geological Survey. 2002a. Scotts Bluff National Monument USGS-NPS Vegetation Mapping Program Products–Vegetation Description. http:/biology/usgs.gov/npsveg/scbl/index.html United States Geological Survey. 2002b. Devil’s Tower National Monument USGS-NPS

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Vegetation Mapping Program Products–Vegetation Description. http:/biology/usgs.gov/npsveg/deto/index.html United States Geological Survey. 2002c. Agate Fossil Beds National Monument USGS-NPS Vegetation Mapping Program Products–Vegetation Description. http:/biology/usgs.gov/npsveg/agfo/index.html United States Geological Survey. 2002d. Badlands National Park. USGS-NPS Vegetation Mapping Program Products–Vegetation Description. http:/biology/usgs.gov/npsveg/badl/index.html Wallis, C. and C. Wershler. 1988. Rare Wildlife and Plant Conservation Studies in Sandhill and Sand Plain Habitats of Southern Alberta. Alberta Forestry, Lands and Wildlife, Alberta Recreation and Parks. Edmonton, Alberta. Wanek, W.J. and R.L. Burgess. 1965. Floristic composition of the sand prairies of southeastern North Dakota. Proceedings of the North Dakota Academy of Science 19:26-40. Wheatley, M. and J. Bentz. 2002. A preliminary classification of plant communities in the Central Parkland Natural Subregion of Alberta. Alberta Sustainable Resource Development, Public Lands Division, Resource Data Branch, Edmonton, Alberta. Whittaker, R.H. 1978. Ordination of Plant Communities. Dr. W. Junk Publishers, The Hague, Boston.

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Appendix 1. Glossary of Scientific and Common Plant Species Names

Appendix 1. Glossary of Scientific and Common Plant Species Names

Scientific Name Common Name Acer negundo Manitoba maple Achillea millefolium common yarrow Achnatherum hymenoides Indian rice grass Agropyron dasystachyum northern wheat grass Agropyron fragile Siberian wheat grass Agropyron sibiricum Siberian wheat grass Agropyron smithii western wheat grass Agropyron trachycaulum slender wheat grass Agrostis stolonifera creeping bentgrass Ambrosia acanthicarpa bur ragweed Ambrosia psilostachya perennial ragweed Antennaria microphylla little-leaf pussytoes Antennaria parvifolia small-leave pussytoes Aristida purpurea var. longiseta Fendler threeawn Artemisia campestris field sagewort Artemisia cana silver sagebrush Artemisia frigida pasture sagewort Artemisia ludoviciana prairie sagewort Artemisia tridentata ssp. wyomingensis Wyoming big sagebrush Artemisia spp. sage Bouteloua gracilis blue grama Bromus tectorum cheatgrass Calamovilfa longifolia sand grass Carex emoryi Emory's sedge Carex foenea dryspike sedge Carex lanuginosa wooly sedge Carex obtusata blunt sedge Carex pellita wooly sedge Carex pensylvanica sunloving sedge Cenchrus longispinus mat sandbur Cerastium arvense field chickweed Chamaesyce serpyllifolia thymeleaf sandmat Chenopodium fremontii Fremont's goosefoot Chenopodium pratericola desert goosefoot Chenopodium subglabrum smooth narrow-leaved goosefoot Cirsium arvense Canada thistle Cleome serrulata bee plant Cornus sericea redosier dogwood Coryphantha vivipara cushion cactus Cryptantha fendleri Fendler's cryptanth Cyperus schweinitzii sand nut-grass Descurainia sophia flixweed Echinacea angustifolia blacksamson echinacea Elaeagnus angustifolia Russian olive Elaeagnus commutata silver-berry Elymus canadensis Canada wild rye Elymus lanceolatus ssp. lanceolatus northern wheat grass Equisetum arvense common horsetail Equisetum hyemale scouring rush Erigeron caespitosus tufted fleabane Escobaria vivipara cushion cactus Euphorbia esula leafy spurge Eurotia lanata winter fat

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Appendix 1. Glossary of Scientific and Common Plant Species Names

Scientific Name Common Name Franseria acanthicarpa bur ragweed Fraxinus pennsylvanica green ash Glycyrrhiza lepidota wild licorice Grindelia squarrosa curlycup gumweed Helianthus annuus common annual sunflower Helianthus couplandii annual sunflower Helianthus pauciflorus ssp. subrhomboideus rhombic-leaved sunflower Helianthus petiolaris prairie sunflower Helianthus subrhomboideus rhombic-leaved sunflower Hesperostipa comata needle-and-thread grass Heterotheca villosa golden aster Juncus balticus wire rush Kochia scoparia Mexican-fireweed Koeleria macrantha June grass Krascheninnikovia lanata winter fat Lactuca pulchella common blue lettuce Lactuca tartarica var. pulchella common blue lettuce Lepidium densiflorum common peppergrass Leymus canadensis Canada wild rye Liatris punctata dotted blazingstar Lygodesmia rostrata annual skeleton-weed Maianthemum stellata star-flowered Solomon's seal Melilotus spp. sweet-clover Mentha arvensis wild mint Oenothera nuttallii white evening primrose Opuntia macrorhiza twistspine pricklypear Opuntia polyacantha prickly pear Oryzopsis hymenoides Indian rice grass Pascopyrum smithii western wheat grass Phalaris arundinacaea reed canarygrass Phyla lanceolata lanceleaf fogfruit Plantago patagonica wooly plantain Poa palustris fowl bluegrass Poa pratensis Kentucky bluegrass Poa secunda Sandberg bluegrass Populus angustifolia narrow-leaf cottonwood Populus deltoides western cottonwood Populus fremontii Fremont cottonwood Populus tremuloides aspen Potentilla pensylvanica Pennsylvania cinquefoil Prunus americana American plum Prunus virginiana chokecherry Psoralea lanceolata lemon scurfpea Psoralidium lanceolatum lemon scurfpea Ribes oxyacanthoides wild gooseberry Rosa acicularis prickly rose Rosa woodsii common wild rose Rumex venosus wild begonia / veined dock Salix amygdaloides peachleaf willow Salix bebbiana Bebb's willow Salix exigua sandbar willow Salix interior sandbar willow Salix lutea yellow willow

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Appendix 1. Glossary of Scientific and Common Plant Species Names

Scientific Name Common Name Salix spp. willow Salsola kali Russian thistle Schizachyrium scoparium little bluestem Shinnersoseris rostrata annual skeleton-weed Smilacina stellata star-flowered Solomon's seal Solidago canadensis Canada goldenrod Solidago missouriensis Missouri goldenrod Spartina pectinata prairie cord grass Sporobolus cryptandrus sand dropseed Stipa comata needle-and thread grass Symphoricarpos occidentalis buckbrush Taraxacum officinale common dandelion Thermopsis rhombifolia golden bean Tragopogon dubius goat's beard

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Appendix 1. Glossary of Scientific and Common Plant Species Names

Common Name Scientific Name American plum Prunus americana annual skeleton-weed Lygodesmia rostrata annual skeleton-weed Shinnersoseris rostrata annual sunflower Helianthus couplandii aspen Populus tremuloides Bebb's willow Salix bebbiana bee plant Cleome serrulata blacksamson echinacea Echinacea angustifolia blue grama Bouteloua gracilis blunt sedge Carex obtusata buckbrush Symphoricarpos occidentalis bur ragweed Ambrosia acanthicarpa bur ragweed Franseria acanthicarpa Canada goldenrod Solidago canadensis Canada thistle Cirsium arvense Canada wild rye Elymus canadensis Canada wild rye Leymus canadensis cheatgrass Bromus tectorum chokecherry Prunus virginiana common annual sunflower Helianthus annuus common blue lettuce Lactuca pulchella common blue lettuce Lactuca tartarica var. pulchella common dandelion Taraxacum officinale common horsetail Equisetum arvense common peppergrass Lepidium densiflorum common wild rose Rosa woodsii common yarrow Achillea millefolium creeping bentgrass Agrostis stolonifera curlycup gumweed Grindelia squarrosa cushion cactus Coryphantha vivipara cushion cactus Escobaria vivipara desert goosefoot Chenopodium pratericola dotted blazingstar Liatris punctata dryspike sedge Carex foenea Emory's sedge Carex emoryi Fendler threeawn Aristida purpurea var. longiseta Fendler's cryptanth Cryptantha fendleri field chickweed Cerastium arvense field sagewort Artemisia campestris flixweed Descurainia sophia fowl bluegrass Poa palustris Fremont cottonwood Populus fremontii Fremont's goosefoot Chenopodium fremontii goat's beard Tragopogon dubius golden aster Heterotheca villosa golden bean Thermopsis rhombifolia green ash Fraxinus pennsylvanica Indian rice grass Achnatherum hymenoides Indian rice grass Oryzopsis hymenoides June grass Koeleria macrantha Kentucky bluegrass Poa pratensis lanceleaf fogfruit Phyla lanceolata

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Appendix 1. Glossary of Scientific and Common Plant Species Names

Common Name Scientific Name leafy spurge Euphorbia esula lemon scurfpea Psoralea lanceolata lemon scurfpea Psoralidium lanceolatum little bluestem Schizachyrium scoparium little-leaf pussytoes Antennaria microphylla Manitoba maple Acer negundo mat sandbur Cenchrus longispinus Mexican-fireweed Kochia scoparia Missouri goldenrod Solidago missouriensis narrow-leaf cottonwood Populus angustifolia needle-and thread grass Stipa comata needle-and-thread grass Hesperostipa comata northern wheat grass Agropyron dasystachyum northern wheat grass Elymus lanceolatus ssp. lanceolatus pasture sagewort Artemisia frigida peachleaf willow Salix amygdaloides Pennsylvania cinquefoil Potentilla pensylvanica perennial ragweed Ambrosia psilostachya prairie cord grass Spartina pectinata prairie sagewort Artemisia ludoviciana prairie sunflower Helianthus petiolaris prickly pear Opuntia polyacantha prickly rose Rosa acicularis redosier dogwood Cornus sericea reed canarygrass Phalaris arundinacaea rhombic-leaved sunflower Helianthus pauciflorus ssp. subrhomboideus rhombic-leaved sunflower Helianthus subrhomboideus Russian olive Elaeagnus angustifolia Russian thistle Salsola kali sage Artemisia spp. sand dropseed Sporobolus cryptandrus sand grass Calamovilfa longifolia sand nut-grass Cyperus schweinitzii sandbar willow Salix exigua sandbar willow Salix interior Sandberg bluegrass Poa secunda scouring rush Equisetum hyemale Siberian wheat grass Agropyron fragile Siberian wheat grass Agropyron sibiricum silver sagebrush Artemisia cana silver-berry Elaeagnus commutata slender wheat grass Agropyron trachycaulum small-leave pussytoes Antennaria parvifolia smooth narrow-leaved goosefoot Chenopodium subglabrum star-flowered Solomon's seal Maianthemum stellata star-flowered Solomon's seal Smilacina stellata sunloving sedge Carex pensylvanica sweet-clover Melilotus spp. thymeleaf sandmat Chamaesyce serpyllifolia tufted fleabane Erigeron caespitosus twistspine pricklypear Opuntia macrorhiza western cottonwood Populus deltoides western wheat grass Agropyron smithii

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Appendix 1. Glossary of Scientific and Common Plant Species Names

Common Name Scientific Name western wheat grass Pascopyrum smithii white evening primrose Oenothera nuttallii wild begonia / veined dock Rumex venosus wild gooseberry Ribes oxyacanthoides wild licorice Glycyrrhiza lepidota wild mint Mentha arvensis willow Salix spp. winter fat Eurotia lanata winter fat Krascheninnikovia lanata wire rush Juncus balticus wooly plantain Plantago patagonica wooly sedge Carex lanuginosa wooly sedge Carex pellita Wyoming big sagebrush Artemisia tridentata ssp. wyomingensis yellow willow Salix lutea

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Appendix 2. PC-ORD Output from Detrended Correspondence Analysis of Plot Data

Appendix 2. PC-ORD Output from Detrended Correspondence Analysis of Plot Data

****************** Detrended Correspondence Analysis (DCA) ****************** PC-ORD, Version 4.20 25 Nov 2002, 13:01 SAND DUNE COMMUNITIES Number of non-zero data items: 497 Downweighting selected. Weights applied to columns, in sequential order: 0.615 0.300 0.300 0.300 0.300 0.565 0.565 0.300 0.300 0.300 1.000 0.916 0.913 0.559 1.000 1.000 0.300 0.392 0.300 0.300 0.300 0.900 0.900 0.600 1.000 0.600 0.300 1.000 1.000 1.000 0.600 1.000 1.000 1.000 1.000 1.000 0.600 1.000 0.540 1.000 1.000 1.000 0.300 0.663 0.700 1.000 1.000 0.300 0.800 1.000 0.600 0.300 0.426 1.000 1.000 1.000 1.000 0.300 0.900 0.833 1.000 1.000 1.000 1.000 1.000 Axes are rescaled Number of segments: 30 Threshold: 0.00 Total variance ("inertia") in the species data: 6.2854 ---------- Axis 1 ---------- 0.2684242427 = residual at iteration 0 0.0854052529 = residual at iteration 1 0.0140371500 = residual at iteration 2 0.0061698658 = residual at iteration 3 0.0013625850 = residual at iteration 4 0.0006173362 = residual at iteration 5 0.0001402497 = residual at iteration 6 0.0000646825 = residual at iteration 7 0.0000148964 = residual at iteration 8 0.0000069913 = residual at iteration 9 0.0000016124 = residual at iteration 10 0.0000008443 = residual at iteration 11 0.1639871597 = residual at iteration 12 0.0244774297 = residual at iteration 13 0.0513806567 = residual at iteration 14 0.0032606893 = residual at iteration 15 0.0015779877 = residual at iteration 16 0.0002858440 = residual at iteration 17 0.0001657879 = residual at iteration 18 0.0000303903 = residual at iteration 19 0.0000178559 = residual at iteration 20 0.0000032664 = residual at iteration 21 0.0000019687 = residual at iteration 22 0.0000005150 = residual at iteration 23 0.1456906796 = residual at iteration 24 0.0234203395 = residual at iteration 25 0.0480892435 = residual at iteration 26 0.0030493103 = residual at iteration 27 0.0017713277 = residual at iteration 28 0.0002687894 = residual at iteration 29 0.0001558407 = residual at iteration 30 0.0000304978 = residual at iteration 31 0.0000175863 = residual at iteration 32 0.0000037236 = residual at iteration 33 0.0000022105 = residual at iteration 34 0.0000005672 = residual at iteration 35 0.0000004183 = residual at iteration 36 0.0000003501 = residual at iteration 37 0.2779901028 = residual at iteration 38 0.0074540768 = residual at iteration 39 0.0021347259 = residual at iteration 40 0.0006754500 = residual at iteration 41 0.0002074938 = residual at iteration 42 0.0000793746 = residual at iteration 43 0.0000260332 = residual at iteration 44 0.0000105902 = residual at iteration 45

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Appendix 2. PC-ORD Output from Detrended Correspondence Analysis of Plot Data

0.0000036683 = residual at iteration 46 0.0000015326 = residual at iteration 47 0.0000005304 = residual at iteration 48 0.0119315125 = residual at iteration 49 0.0029634687 = residual at iteration 50 0.0000002078 = residual at iteration 60 0.0000211076 = residual at iteration 70 0.0018477291 = residual at iteration 80 0.0139812361 = residual at iteration 90 0.0000005091 = residual at iteration 100 0.0000062506 = residual at iteration 110 0.0000461937 = residual at iteration 120 0.0222807173 = residual at iteration 130 0.1710713655 = residual at iteration 140 0.0000009847 = residual at iteration 150 0.0000099311 = residual at iteration 160 0.0002753049 = residual at iteration 170 0.0028829316 = residual at iteration 180 0.0192794092 = residual at iteration 190 0.0000006532 = residual at iteration 200 0.0000043344 = residual at iteration 210 0.0000274861 = residual at iteration 220 0.0097351270 = residual at iteration 230 0.0000010114 = residual at iteration 240 0.0000127912 = residual at iteration 250 0.0001706528 = residual at iteration 260 0.0005976434 = residual at iteration 270 0.0020370230 = residual at iteration 280 0.1597174108 = residual at iteration 290 0.0000015046 = residual at iteration 300 0.0000147340 = residual at iteration 310 0.0000765337 = residual at iteration 320 0.0011597162 = residual at iteration 330 0.0019860768 = residual at iteration 340 0.2260046750 = residual at iteration 350 0.0954641625 = residual at iteration 360 0.0000008501 = residual at iteration 370 0.0003140370 = residual at iteration 380 0.0263471641 = residual at iteration 390 0.1734091938 = residual at iteration 400 0.0000005903 = residual at iteration 410 0.0000467348 = residual at iteration 420 0.0000296704 = residual at iteration 430 0.0007561108 = residual at iteration 440 0.0360311270 = residual at iteration 450 0.0000008192 = residual at iteration 460 0.0002691617 = residual at iteration 470 0.0133251371 = residual at iteration 480 0.0000009775 = residual at iteration 490 0.0000034115 = residual at iteration 500 0.0019896838 = residual at iteration 510 0.0212083757 = residual at iteration 520 0.0000005526 = residual at iteration 530 0.0000056518 = residual at iteration 540 0.0001769213 = residual at iteration 550 0.0478879064 = residual at iteration 560 0.0000007582 = residual at iteration 570 0.0000120228 = residual at iteration 580 0.0004150117 = residual at iteration 590 0.0002466936 = residual at iteration 600 0.0018837127 = residual at iteration 610 0.2045992166 = residual at iteration 620 0.0000096100 = residual at iteration 630 0.0000455938 = residual at iteration 640 0.0055995947 = residual at iteration 650 0.1489204913 = residual at iteration 660 0.1107899100 = residual at iteration 670 0.0000003468 = residual at iteration 680 0.0000078266 = residual at iteration 690 0.0004097962 = residual at iteration 700 0.0000001005 = residual at iteration 710

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Appendix 2. PC-ORD Output from Detrended Correspondence Analysis of Plot Data

0.0000026737 = residual at iteration 720 0.0000636807 = residual at iteration 730 0.0006091066 = residual at iteration 740 0.0165218879 = residual at iteration 750 0.0000096641 = residual at iteration 760 0.0000374746 = residual at iteration 770 0.0000017238 = residual at iteration 780 0.0000040091 = residual at iteration 790 0.0000317458 = residual at iteration 800 0.0000037804 = residual at iteration 810 0.0003344046 = residual at iteration 820 0.0202178955 = residual at iteration 830 0.0000006557 = residual at iteration 840 0.0001674164 = residual at iteration 850 0.0006750197 = residual at iteration 860 0.0000157669 = residual at iteration 870 0.0001539329 = residual at iteration 880 0.0045301383 = residual at iteration 890 0.1807350367 = residual at iteration 900 0.0000009182 = residual at iteration 910 0.0000329651 = residual at iteration 920 0.0000177802 = residual at iteration 930 0.0006978700 = residual at iteration 940 0.0364268906 = residual at iteration 950 0.0009799623 = residual at iteration 960 0.0008513225 = residual at iteration 970 0.1945322305 = residual at iteration 980 0.0000022841 = residual at iteration 990 0.0534050353 = residual at iteration 999 0.7860396504 = eigenvalue *** BEWARE *** RESIDUAL BIGGER THAN TOLERANCE, WHICH IS 0.0000001000 Length of gradient: 2.995 Length of segments: 0.32 0.32 0.31 0.30 0.29 0.29 0.26 0.19 0.13 0.11 Length of segments: 0.10 0.10 0.09 0.09 0.09 Length of gradient: 3.567 Length of gradient: 4.127 Length of segments: 0.24 0.24 0.22 0.20 0.19 0.20 0.21 0.21 0.21 0.19 Length of segments: 0.19 0.19 0.20 0.22 0.22 0.21 0.17 0.15 0.15 0.16 Length of segments: 0.17 Length of gradient: 4.129 ---------- Axis 2 ---------- 0.2091501057 = residual at iteration 0 0.0765530691 = residual at iteration 1 0.0229611807 = residual at iteration 2 0.0032644884 = residual at iteration 3 0.0007385664 = residual at iteration 4 0.0001094733 = residual at iteration 5 0.0000250289 = residual at iteration 6 0.0000037378 = residual at iteration 7 0.0000008669 = residual at iteration 8 0.0000001618 = residual at iteration 9 0.0000001470 = residual at iteration 10 0.0000001581 = residual at iteration 11 0.1715056002 = residual at iteration 12 0.0267237853 = residual at iteration 13 0.0032643846 = residual at iteration 14 0.0005265863 = residual at iteration 15 0.0000775312 = residual at iteration 16 0.0000147603 = residual at iteration 17 0.0000022521 = residual at iteration 18 0.0000004430 = residual at iteration 19 0.0000004798 = residual at iteration 20 0.0000002632 = residual at iteration 21 0.0000001324 = residual at iteration 22 0.2258998752 = residual at iteration 23 0.0052952184 = residual at iteration 24 0.0007295895 = residual at iteration 25 0.0000719962 = residual at iteration 26

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Appendix 2. PC-ORD Output from Detrended Correspondence Analysis of Plot Data

0.0000153151 = residual at iteration 27 0.0000024945 = residual at iteration 28 0.0000005695 = residual at iteration 29 0.0000002555 = residual at iteration 30 0.0000001209 = residual at iteration 31 0.1649405807 = residual at iteration 32 0.0030498444 = residual at iteration 33 0.0001900764 = residual at iteration 34 0.0000162592 = residual at iteration 35 0.0000029595 = residual at iteration 36 0.0000004602 = residual at iteration 37 0.0000002008 = residual at iteration 38 0.1445547491 = residual at iteration 39 0.0134180319 = residual at iteration 40 0.0013512193 = residual at iteration 41 0.0001006165 = residual at iteration 42 0.0000235098 = residual at iteration 43 0.0000029193 = residual at iteration 44 0.0000007032 = residual at iteration 45 0.0000002582 = residual at iteration 46 0.1190573350 = residual at iteration 47 0.0200145710 = residual at iteration 48 0.0045830240 = residual at iteration 49 0.0006001128 = residual at iteration 50 0.0000569950 = residual at iteration 60 0.0000140514 = residual at iteration 70 0.0000016084 = residual at iteration 80 0.0000006614 = residual at iteration 90 0.0000002011 = residual at iteration 100 0.1686325073 = residual at iteration 110 0.0000001987 = residual at iteration 120 0.0245861672 = residual at iteration 130 0.0128338402 = residual at iteration 140 0.0009726097 = residual at iteration 150 0.1492897719 = residual at iteration 160 0.0230942033 = residual at iteration 170 0.0347204730 = residual at iteration 180 0.0006071823 = residual at iteration 190 0.0000031297 = residual at iteration 200 0.0000002212 = residual at iteration 210 0.0000000478 = residual at iteration 220 0.6630458236 = eigenvalue Length of gradient: 2.660 Length of segments: 0.27 0.28 0.29 0.29 0.28 0.27 0.25 0.23 0.17 0.08 Length of segments: 0.06 0.06 0.06 0.06 Length of gradient: 3.499 Length of gradient: 4.663 Length of segments: 0.11 0.11 0.12 0.14 0.19 0.23 0.25 0.25 0.24 0.24 Length of segments: 0.24 0.24 0.25 0.25 0.25 0.24 0.24 0.23 0.22 0.16 Length of segments: 0.12 0.12 0.12 0.12 Length of gradient: 4.639 ---------- Axis 3 ---------- 0.1746972799 = residual at iteration 0 0.0342275575 = residual at iteration 1 0.0056336881 = residual at iteration 2 0.0004523548 = residual at iteration 3 0.0000723316 = residual at iteration 4 0.0000058883 = residual at iteration 5 0.0000009449 = residual at iteration 6 0.0000000834 = residual at iteration 7 0.4721443057 = eigenvalue Length of gradient: 3.666 Length of segments: 0.13 0.14 0.15 0.19 0.23 0.28 0.31 0.32 0.30 0.28 Length of segments: 0.24 0.22 0.20 0.18 0.15 0.11 0.08 0.08 0.08 Length of gradient: 3.973 Length of gradient: 3.773

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Appendix 2. PC-ORD Output from Detrended Correspondence Analysis of Plot Data

Length of segments: 0.17 0.17 0.18 0.19 0.20 0.21 0.21 0.22 0.23 0.24 Length of segments: 0.23 0.22 0.20 0.18 0.18 0.18 0.18 0.18 0.19 Length of gradient: 3.695 SAND DUNE COMMUNITIES SPECIES SCORES N NAME AX1 AX2 AX3 | RANKED 1 | RANKED 2 | EIG=0.786 | EIG=0.663 | 1 POPUDEL1 -37 282 387 | 7 PRUNVIR4 428 | 44 RUMEVEN6 496 | 2 POPUTRE2 -128 282 356 | 11 PRUNVIR5 424 | 45 FRANACA6 490 | 3 POPUDEL2 35 295 443 | 44 RUMEVEN6 405 | 63 ELYMCAN7 412 | 4 SALIAMY3 112 280 387 | 45 FRANACA6 402 | 62 ORYZHYM7 350 | 5 ELEACOM4 -70 149 -9 | 26 SALSKAL6 398 | 30 THERRHO6 347 | 6 SALIAMY4 71 330 103 | 28 EQUIFLU6 380 | 6 SALIAMY4 330 | 7 PRUNVIR4 428 -14 177 | 58 AGROSMI7 370 | 15 ROSAWOO5 308 | 8 SALIAMY5 77 239 101 | 41 LYGOROS6 361 | 27 HELISUB6 295 | 9 ARTECAN5 -67 87 395 | 62 ORYZHYM7 351 | 3 POPUDEL2 295 | 10 RIBEOXY5 14 262 26 | 50 HELIANN6 346 | 60 CARELAN7 292 | 11 PRUNVIR5 424 -15 180 | 63 ELYMCAN7 305 | 64 SPORCRY7 291 | 12 ELAECOM5 -27 91 -43 | 51 CERAARV6 296 | 31 TARAOFF6 289 | 13 SALIEXI5 -24 175 -13 | 33 CRYPFEN6 281 | 1 POPUDEL1 282 | 14 EUROLAN5 206 112 282 | 65 CALALON7 246 | 2 POPUTRE2 282 | 15 ROSAWOO5 116 308 38 | 64 SPORCRY7 236 | 4 SALIAMY3 280 | 16 SOLIMIS6 104 197 201 | 57 AGRODAS7 235 | 52 BOUTGRA7 280 | 17 PLANPAT6 -425 49 370 | 18 ARTECAM 228 | 59 AGROSIB7 278 | 18 ARTECAM 228 94 306 | 40 CHENFRE6 226 | 37 SMILSTE6 265 | 19 ERIGCAE6 -67 87 395 | 49 LATUPUL6 215 | 49 LATUPUL6 265 | 20 POTEPEN6 -67 87 395 | 34 CHENSUB6 211 | 10 RIBEOXY5 262 | 21 ANTEPAR6 -67 87 395 | 14 EUROLAN5 206 | 39 SOLICAN6 249 | 22 LEPIDEN6 -46 70 380 | 46 CHRYVIL6 197 | 54 JUNCBAL7 249 | 23 ACHIMIL6 -99 96 353 | 42 OPUNPOL6 191 | 50 HELIANN6 245 | 24 CLEOSER6 66 184 391 | 53 CYPESCH7 175 | 61 POAPRA7 241 | 25 CORYMIS6 -136 111 338 | 35 CHENPRA6 165 | 8 SALIAMY5 239 | 26 SALSKAL6 398 1 270 | 55 STIPCOM7 135 | 48 ANTIMIC6 239 | 27 HELISUB6 35 295 443 | 30 THERRHO6 134 | 43 OENONUT6 233 | 28 EQUIFLU6 380 33 364 | 38 ARTEFRI6 117 | 32 TRAGDUB6 230 | 29 ARTELUD6 26 137 187 | 15 ROSAWOO5 116 | 47 GLYCLEP6 213 | 30 THERRHO6 134 347 210 | 4 SALIAMY3 112 | 16 SOLIMIS6 197 | 31 TARAOFF6 110 289 406 | 52 BOUTGRA7 112 | 40 CHENFRE6 197 | 32 TRAGDUB6 -54 230 300 | 56 KOELMAC7 112 | 36 DESCSOP6 192 | 33 CRYPFEN6 281 40 261 | 31 TARAOFF6 110 | 24 CLEOSER6 184 | 34 CHENSUB6 211 136 250 | 16 SOLIMIS6 104 | 13 SALIEXI5 175 | 35 CHENPRA6 165 161 329 | 60 CARELAN7 81 | 46 CHRYVIL6 168 | 36 DESCSOP6 -20 192 378 | 8 SALIAMY5 77 | 35 CHENPRA6 161 | 37 SMILSTE6 -69 265 388 | 48 ANTIMIC6 77 | 5 ELEACOM4 149 | 38 ARTEFRI6 117 127 319 | 6 SALIAMY4 71 | 29 ARTELUD6 137 | 39 SOLICAN6 -47 249 251 | 24 CLEOSER6 66 | 34 CHENSUB6 136 | 40 CHENFRE6 226 197 310 | 59 AGROSIB7 60 | 56 KOELMAC7 131 | 41 LYGOROS6 361 37 60 | 3 POPUDEL2 35 | 38 ARTEFRI6 127 | 42 OPUNPOL6 191 78 290 | 27 HELISUB6 35 | 14 EUROLAN5 112 | 43 OENONUT6 -192 233 93 | 47 GLYCLEP6 30 | 25 CORYMIS6 111 | 44 RUMEVEN6 405 496 182 | 29 ARTELUD6 26 | 53 CYPESCH7 110 | 45 FRANACA6 402 490 216 | 54 JUNCBAL7 17 | 23 ACHIMIL6 96 | 46 CHRYVIL6 197 168 254 | 10 RIBEOXY5 14 | 55 STIPCOM7 96 | 47 GLYCLEP6 30 213 189 | 36 DESCSOP6 -20 | 18 ARTECAM 94 | 48 ANTIMIC6 77 239 101 | 13 SALIEXI5 -24 | 12 ELAECOM5 91 | 49 LATUPUL6 215 265 16 | 12 ELAECOM5 -27 | 51 CERAARV6 89 | 50 HELIANN6 346 245 199 | 1 POPUDEL1 -37 | 9 ARTECAN5 87 | 51 CERAARV6 296 89 205 | 22 LEPIDEN6 -46 | 19 ERIGCAE6 87 | 52 BOUTGRA7 112 280 387 | 39 SOLICAN6 -47 | 20 POTEPEN6 87 | 53 CYPESCH7 175 110 290 | 32 TRAGDUB6 -54 | 21 ANTEPAR6 87 | 54 JUNCBAL7 17 249 227 | 61 POAPRA7 -55 | 42 OPUNPOL6 78 | 55 STIPCOM7 135 96 334 | 21 ANTEPAR6 -67 | 65 CALALON7 76 | 56 KOELMAC7 112 131 234 | 19 ERIGCAE6 -67 | 22 LEPIDEN6 70 | 57 AGRODAS7 235 57 76 | 9 ARTECAN5 -67 | 57 AGRODAS7 57 | 58 AGROSMI7 370 37 313 | 20 POTEPEN6 -67 | 17 PLANPAT6 49 | 59 AGROSIB7 60 278 87 | 37 SMILSTE6 -69 | 33 CRYPFEN6 40 | 60 CARELAN7 81 292 31 | 5 ELEACOM4 -70 | 58 AGROSMI7 37 | 61 POAPRA7 -55 241 291 | 23 ACHIMIL6 -99 | 41 LYGOROS6 37 | 62 ORYZHYM7 351 350 196 | 2 POPUTRE2 -128 | 28 EQUIFLU6 33 |

Geowest Environmental Consultants Ltd. 5

Appendix 2. PC-ORD Output from Detrended Correspondence Analysis of Plot Data

63 ELYMCAN7 305 412 128 | 25 CORYMIS6 -136 | 26 SALSKAL6 1 | 64 SPORCRY7 236 291 73 | 43 OENONUT6 -192 | 7 PRUNVIR4 -14 | 65 CALALON7 246 76 93 | 17 PLANPAT6 -425 | 11 PRUNVIR5 -15 | SAND DUNE COMMUNITIES SAMPLE SCORES - WHICH ARE WEIGHTED MEAN SPECIES SCORES N NAME AX1 AX2 AX3 | RANKED 1 | RANKED 2 | EIG=0.786 | EIG=0.663 | 1 1 257 248 141 | 10 10 412 | 30 30 463 | 2 2 19 225 175 | 14 14 412 | 6 6 461 | 3 3 239 252 87 | 6 6 390 | 29 29 314 | 4 4 206 219 104 | 13 13 371 | 31 31 310 | 5 5 140 293 55 | 30 30 367 | 21 21 305 | 6 6 390 461 183 | 34 34 362 | 35 35 303 | 7 7 42 215 195 | 21 21 324 | 28 28 303 | 8 8 235 140 252 | 37 37 307 | 26 26 300 | 9 9 0 254 278 | 35 35 282 | 37 37 297 | 10 10 412 15 178 | 29 29 263 | 5 5 293 | 11 11 33 168 132 | 1 1 257 | 27 27 279 | 12 12 46 257 369 | 25 25 250 | 25 25 265 | 13 13 371 72 170 | 3 3 239 | 12 12 257 | 14 14 412 0 177 | 8 8 235 | 9 9 254 | 15 15 230 196 186 | 15 15 230 | 17 17 253 | 16 16 119 244 101 | 31 31 214 | 3 3 252 | 17 17 13 253 307 | 4 4 206 | 1 1 248 | 18 18 9 119 0 | 23 23 182 | 16 16 244 | 19 19 46 176 218 | 33 33 176 | 2 2 225 | 20 20 92 156 261 | 38 38 169 | 4 4 219 | 21 21 324 305 185 | 40 40 163 | 7 7 215 | 22 22 136 128 291 | 26 26 150 | 15 15 196 | 23 23 182 146 105 | 5 5 140 | 19 19 176 | 24 24 110 116 316 | 39 39 140 | 11 11 168 | 25 25 250 265 197 | 22 22 136 | 36 36 157 | 26 26 150 300 60 | 28 28 130 | 20 20 156 | 27 27 99 279 133 | 16 16 119 | 23 23 146 | 28 28 130 303 119 | 36 36 115 | 8 8 140 | 29 29 263 314 125 | 24 24 110 | 22 22 128 | 30 30 367 463 169 | 32 32 99 | 18 18 119 | 31 31 214 310 135 | 27 27 99 | 24 24 116 | 32 32 99 95 63 | 20 20 92 | 38 38 114 | 33 33 176 102 259 | 19 19 46 | 40 40 107 | 34 34 362 21 181 | 12 12 46 | 33 33 102 | 35 35 282 303 131 | 7 7 42 | 39 39 101 | 36 36 115 157 181 | 11 11 33 | 32 32 95 | 37 37 307 297 156 | 2 2 19 | 13 13 72 | 38 38 169 114 276 | 17 17 13 | 34 34 21 | 39 39 140 101 284 | 18 18 9 | 10 10 15 | 40 40 163 107 273 | 9 9 0 | 14 14 0 | *************************** Calculations finished ***************************

Geowest Environmental Consultants Ltd. 6

Appendix 3. Species Code Descriptions

Appendix 3. Species Code Descriptions

Code Species Stratum POPUDEL1 Populus deltoides Main Canopy Tree (> 5 m) POPUTRE2 Populus tremuloides Understorey Tree (> 5 m but at least 3 m shorter than overstorey trees) POPUDEL2 Populus deltoides Understorey Tree (> 5 m but at least 3 m shorter than overstorey trees) SALIAMY3 Salix amygdaloides Tall Shrub (2.5 m - 5 m) ELEACOM4 Elaeagnus commutata Medium Shrub (1 - 2.5 m) PRUNVIR4 Prunus virginiana Medium Shrub (1 - 2.5 m) SALIAMY4 Salix amygdaloides Medium Shrub (1 - 2.5 m) ARTECAN5 Artemisia cana Low Shrub ( < 1 m) ELAECOM5 Elaeagnus commutata Low Shrub ( < 1 m) EUROLAN5 Eurotia lanata Low Shrub ( < 1 m) PRUNVIR5 Prunus virginiana Low Shrub ( < 1 m) RIBEOXY5 Ribes oxyacanthoides Low Shrub ( < 1 m) ROSAWOO5 Rosa woodsii Low Shrub ( < 1 m) SALIAMY5 Salix amygdaloides Low Shrub ( < 1 m) SALIEXI5 Salix exigua Low Shrub ( < 1 m) ACHIMIL6 Achillea millefolium Forb / Herb ANTIMIC6 Antennaria microphylla Forb / Herb ANTEPAR6 Antennaria parvifolia Forb / Herb ARTECAM6 Artemisia campestris Forb / Herb ARTEFRI6 Artemisia frigida Forb / Herb ARTELUD6 Artemisia ludoviciana Forb / Herb CERAARV6 Cerastium arvense Forb / Herb CHENFRE6 Chenopodium fremontii Forb / Herb CHENPRA6 Chenopodium pratericola Forb / Herb CHENSUB6 Chenopodium subglabrum Forb / Herb CLEOSER6 Cleome serrulata Forb / Herb CORYVIV6 Coryphantha vivipara Forb / Herb CRYPFEN6 Cryptantha fendleri Forb / Herb DESCSOP6 Descurainia sophia Forb / Herb EQUIHYE6 Equisetum hyemale Forb / Herb ERIGCAE6 Erigeron caespitosus Forb / Herb FRANACA6 Franseria acanthicarpa Forb / Herb GLYCLEP6 Glycyrrhiza lepidota Forb / Herb HELIANN6 Helianthus annuus Forb / Herb HELISUB6 Helianthus subrhomboideus Forb / Herb HETEVIL6 Heterotheca villosa Forb / Herb LATUPUL6 Lactuca pulchella Forb / Herb LEPIDEN6 Lepidium densiflorum Forb / Herb LYGOROS6 Lygodesmia rostrata Forb / Herb OENONUT6 Oenothera nuttallii Forb / Herb OPUNPOL6 Opuntia polyacantha Forb / Herb PLANPAT6 Plantago patagonica Forb / Herb POTEPEN6 Potentilla pensylvanica Forb / Herb RUMEVEN6 Rumex venosus Forb / Herb SALSKAL6 Salsola kali Forb / Herb SMILSTE6 Smilacina stellata Forb / Herb SOLICAN6 Solidago canadensis Forb / Herb SOLIMIS6 Solidago missouriensis Forb / Herb TARAOFF6 Taraxacum officinale Forb / Herb THERRHO6 Thermopsis rhombifolia Forb / Herb TRAGDUB6 Tragopogon dubius Forb / Herb AGRODAS7 Agropyron dasystachyum Graminoid AGROSIB7 Agropyron sibiricum Graminoid

Geowest Environmental Consultants Ltd. 1

Appendix 3. Species Code Descriptions

Code Species Stratum AGROSMI7 Agropyron smithii Graminoid BOUTGRA7 Bouteloua gracilis Graminoid CALALON7 Calamovilfa longifolia Graminoid CARELAN7 Carex lanuginosa Graminoid CYPESCH7 Cyperus schweinitzii Graminoid ELYMCAN7 Elymus canadensis Graminoid JUNCBAL7 Juncus balticus Graminoid KOELMAC7 Koeleria macrantha Graminoid ORYZHYM7 Oryzopsis hymenoides Graminoid POAPRA7 Poa pratensis Graminoid SPORCRY7 Sporobolus cryptandrus Graminoid STIPCOM7 Stipa comata Graminoid

Geowest Environmental Consultants Ltd. 2

Appendix 4. Correlation Table with Literature From Within Alberta

Appe

ndix

4. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om w

ithin

Alb

erta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g1 C

omm

ents

Fore

st

Popu

lus d

elto

ides

/ G

lycy

rrhi

za le

pido

ta /

Junc

us b

altic

us

Popu

lus d

elto

ides

moi

st c

oule

e co

mm

unity

(Sm

olia

k 19

85)

3 Fo

und

occa

sion

ally

in m

oist

cou

lees

(Man

yber

ries)

. Sha

re

dom

inan

t ove

rsto

rey

spec

ies,

but d

iffer

ent s

ite c

ondi

tions

(i.e

. co

ulee

vs.

dune

s). D

etai

led

info

rmat

ion

not p

rovi

ded.

Po

pulu

s tre

mul

oide

s / S

tipa

spp.

- Car

ex

ross

ii (J

aque

s 197

7)

3 Fo

und

prim

arily

in d

epre

ssio

nal a

reas

and

cou

lees

(CFB

Su

ffie

ld-M

iddl

e Sa

ndhi

lls) w

here

sand

y so

ils a

llow

dee

p-w

ater

pe

rcol

atio

n. D

iffer

ent o

vers

tore

y bu

t som

ewha

t sim

ilar s

ite

cond

ition

s.

Po

pulu

s del

toid

es a

ssoc

iatio

n (J

aque

s 19

77)

2 Fo

und

on fl

oodp

lain

s and

allu

vial

terr

aces

of S

outh

Sa

skat

chew

an ri

ver (

CFB

-Suf

field

). ).

Shar

e do

min

ant

over

stor

ey sp

ecie

s, bu

t diff

eren

t site

con

ditio

ns (i

.e. f

lood

plai

n an

d te

rrac

es v

s. du

nes)

. Det

aile

d in

form

atio

n no

t pro

vide

d.

Popu

lus X

jack

ii (A

dam

s et a

l. 19

97)

3 N

oted

this

com

mun

ity ty

pe w

as re

late

d to

the

Popu

lus

delto

ides

com

mun

ity re

porte

d by

Jaqu

es (1

977)

Po

pulu

s tre

mul

oide

s (Po

pulu

s de

ltoid

es) (

Kom

ex 1

993)

2

Foun

d on

dun

es/p

lain

s in

1993

in a

noth

er su

rvey

of t

he

Pako

wki

San

dhill

s. N

oted

isol

ated

Pop

ulus

del

toid

es fo

und

in

low

are

as, t

houg

h as

pen

clon

es re

porte

d be

ing

mor

e co

mm

on.

Popu

lus t

rem

uloi

des /

Sym

phor

icar

pos

occi

dent

alis

(Ada

ms e

t al.

1997

) 3

Not

ed th

is c

omm

unity

type

was

rela

ted

to th

e Po

pulu

s tr

emul

oide

s / S

tipa

spp.

- Car

ex ro

ssii

com

mun

ity re

porte

d by

Ja

ques

(197

7), f

ound

in d

epre

ssio

nal a

reas

and

cou

lees

of C

FB

Suff

ield

-Mid

dle

Sand

hills

, in

sand

y so

ils. D

iffer

ent o

vers

tore

y bu

t aga

in si

mila

r site

con

ditio

ns.

Shru

blan

d Ro

sa w

oods

ii /

Spor

obol

us c

rypt

andr

us

Rosa

woo

dsii

(Kom

ex 1

993)

1

Foun

d on

dun

es in

199

3 in

ano

ther

surv

ey o

f the

Pak

owki

Sa

ndhi

lls. R

epor

ted

to o

ccur

in lo

w a

rea

betw

een

dune

s, of

ten

in a

ssoc

iatio

n w

ith w

ild li

coric

e. S

imila

r gen

eral

com

mun

ity

type

des

crib

ed in

pre

viou

s sur

vey

of st

udy

area

. Sh

rubl

and

Salix

am

ygda

loid

es –

Ro

sa w

oods

ii / J

uncu

s ba

lticu

s – S

poro

bolu

s cr

ypta

ndru

s

Salix

spp.

/ St

ipa

com

ata

asso

ciat

ion

(Jaq

ues 1

977)

3

Foun

d on

floo

dpla

ins a

nd a

lluvi

al te

rrac

es o

f Sou

th

Sask

atch

ewan

rive

r (C

FB-S

uffie

ld).

Com

mun

ity fo

und

on

coar

se te

xtur

ed m

ater

ials

, tho

ugh

site

con

ditio

ns v

ary.

D

omin

ant S

alix

spec

ies u

nkno

wn,

thus

som

e im

porta

nt

diffe

renc

es.

1 Sim

ilarit

y R

atin

g: 1

, ide

ntic

al to

or v

ery

sim

ilar;

2, si

mila

r in

mos

t res

pect

s; 3

, sev

eral

sim

ilarit

ies b

ut im

porta

nt d

iffer

ence

s (sc

ale

from

Cor

ns 1

983)

.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

1

Appe

ndix

4. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om w

ithin

Alb

erta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Shru

blan

d Sa

lix a

myg

dalo

ides

Rosa

woo

dsii

/ Jun

cus

balti

cus –

Spo

robo

lus

cryp

tand

rus

Salix

am

ygda

loid

es (K

omex

199

3)

1 Fo

und

on d

unes

in 1

993

in a

noth

er su

rvey

of t

he P

akow

ki

Sand

hills

. Sal

ix a

myg

dalo

ides

foun

d in

low

are

as a

nd a

s bot

h tre

e an

d sh

rub

form

. Sim

ilar g

ener

al c

omm

unity

type

des

crib

ed

in p

revi

ous s

urve

y of

stud

y ar

ea, h

owev

er n

o de

taile

d flo

ristic

or

site

con

ditio

ns p

rovi

ded.

Sh

rubl

and

Elae

agnu

s com

mut

ata

/ G

lycy

rrhi

za le

pido

ta

Elae

agnu

s com

mut

ata

(Whe

atle

y an

d B

entz

200

2)

3 Si

te d

escr

ibed

bas

ed o

n th

ree

repo

rts in

Cen

tral P

arkl

and,

at

Dill

berr

y La

ke P

rovi

ncia

l Par

k, n

ear R

umse

y an

d in

Dry

Isla

nd

Buf

falo

Jum

p. Is

des

crib

ed a

s occ

urrin

g a

low

shru

blan

ds a

nd

shru

bby

mea

dow

s alo

ng p

erim

eter

of s

alin

e la

kes,

adja

cent

to

mar

shes

and

gra

min

oid

mea

dow

s. Sh

ares

dom

inan

t spe

cies

but

si

te c

ondi

tions

var

y co

nsid

erab

ly.

Elae

agnu

s com

mut

ata

/ Sy

mph

oric

arpo

s occ

iden

talis

– R

osa

woo

dsii

/ Poa

pal

ustr

is (W

heat

ley

and

Ben

tz 2

002)

3 D

escr

ibed

from

Cen

tral P

arkl

and

occu

rrin

g ne

ar W

ainw

right

on

subx

eric

to su

bmes

ic si

tes w

ith g

ood

drai

nage

. It h

as a

wel

l-de

velo

ped

low

shru

b la

yer.

Diff

eren

t flo

ristic

com

posi

tion

but

occu

rred

on

site

s with

sim

ilar m

oist

ure

and

soil

drai

nage

co

nditi

ons.

El

aeag

nus c

omm

utat

aSh

rubl

and

(Kom

ex 1

993)

1

Foun

d on

dun

es in

199

3 in

ano

ther

surv

ey o

f the

Pak

owki

Sa

ndhi

lls. R

epor

ted

to o

ccur

as t

hick

ets o

n so

me

north

-fac

ing

slop

es a

nd a

t bas

e of

som

e du

nes.

Sim

ilar g

ener

al c

omm

unity

ty

pe d

escr

ibed

in p

revi

ous s

urve

y of

stud

y ar

ea, h

owev

er n

o de

taile

d flo

ristic

or s

ite c

ondi

tions

pro

vide

d.

Shru

blan

d El

aeag

nus c

omm

utat

a /

Arte

mis

ia lu

dovi

cian

a /

Cal

amov

ilfa

long

ifolia

Elae

agnu

s com

mut

ata

(Whe

atle

y an

d B

entz

200

2)

3 Si

te d

escr

ibed

bas

ed o

n th

ree

repo

rts in

Cen

tral P

arkl

and,

at

Dill

berr

y La

ke P

rovi

ncia

l Par

k, n

ear R

umse

y an

d in

Dry

Isla

nd

Buf

falo

Jum

p. Is

des

crib

ed a

s occ

urrin

g a

low

shru

blan

ds a

nd

shru

bby

mea

dow

s alo

ng p

erim

eter

of s

alin

e la

kes,

adja

cent

to

mar

shes

and

gra

min

oid

mea

dow

s. Sh

ares

dom

inan

t spe

cies

but

si

te c

ondi

tions

var

y co

nsid

erab

ly.

Elae

agnu

s com

mut

ata

/ Sy

mph

oric

arpo

s occ

iden

talis

– R

osa

woo

dsii

/ Poa

pal

ustr

is (W

heat

ley

and

Ben

tz 2

002)

3 D

escr

ibed

from

Cen

tral P

arkl

and

occu

rrin

g ne

ar W

ainw

right

on

subx

eric

to su

bmes

ic si

tes w

ith g

ood

drai

nage

. It h

ad a

wel

l-de

velo

ped

low

shru

b la

yer.

Diff

eren

t flo

ristic

com

posi

tion,

but

oc

curr

ed o

n si

tes w

ith si

mila

r moi

stur

e an

d so

il dr

aina

ge

cond

ition

s.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

2

Appe

ndix

4. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om w

ithin

Alb

erta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Shru

blan

d Pr

unus

vir

gini

ana

/ C

alam

ovilf

a lo

ngifo

lia

Prun

us v

irgi

nian

a sh

rubl

and

(Kom

ex

1993

) 1

Foun

d on

dun

es in

199

3 in

ano

ther

surv

ey o

f the

Pak

owki

Sa

ndhi

lls. R

epor

ted

to o

ccur

alo

ng lo

w d

une

ridge

s and

sl

opes

. Sim

ilar g

ener

al c

omm

unity

type

des

crib

ed in

pre

viou

s su

rvey

of s

tudy

are

a, h

owev

er n

o de

taile

d flo

ristic

or s

ite

cond

ition

s pro

vide

d.

Prun

us v

irgi

nian

a –

Amel

anch

ier a

lnifo

lia

/ Agr

opyr

on tr

achy

caul

um –

Poa

pra

tens

is

(Whe

atle

y an

d B

entz

200

2)

3 W

as d

escr

ibed

for t

he C

entra

l Par

klan

d, d

escr

ibed

from

a si

te

in th

e B

lack

foot

Pro

vinc

ial R

ecre

atio

n A

rea.

Soi

ls w

ere

not

desc

ribed

but

the

site

was

a st

eep,

sout

h-fa

cing

slop

e. S

ome

sim

ilar s

peci

es n

oted

and

loca

ted

on st

rong

slop

e, b

ut li

mite

d de

tails

oth

erw

ise.

D

war

f Sh

rubl

and

Euro

tia la

nata

/ St

ipa

com

ata

– C

alam

ovilf

a lo

ngifo

lia

Stip

a –

Bou

telo

ua –

Agr

opyr

on ty

pe

(Sm

olia

k 19

85)

3 M

entio

ned

that

this

type

is fo

und

on u

plan

d pr

airie

, with

Eu

rotia

lana

ta a

s a c

omm

on sh

rub.

Ver

y lim

ited

floris

tic

com

posi

tion

prov

ided

and

few

site

cha

ract

eris

tics.

No

men

tion

of sa

nd a

s prim

ary

subs

trate

. H

erba

ceou

s V

eget

atio

n Sa

lix e

xigu

a / G

lycy

rrhi

za

lepi

dota

/ Ju

ncus

bal

ticus

N

one

desc

ribed

-

G

lycy

rrhi

za le

pido

ta /

Cal

amov

ilfa

long

ifolia

G

lycy

rrhi

za le

pido

ta (C

alam

ovilf

a lo

ngifo

lia /

Arte

mis

ia lu

dovi

cian

a)

(Kom

ex 1

993)

1 Fo

und

on d

unes

in 1

993

in a

noth

er su

rvey

of t

he P

akow

ki

Sand

hills

. Als

o re

porte

d to

occ

ur w

ith w

ire ru

sh (J

uncu

s ba

lticu

s). S

imila

r gen

eral

com

mun

ity ty

pe d

escr

ibed

in

prev

ious

surv

ey o

f stu

dy a

rea,

how

ever

no

deta

iled

floris

tic o

r si

te c

ondi

tions

pro

vide

d.

Her

bace

ous

Veg

etat

ion

Gly

cyrr

hiza

lepi

dota

Arte

mis

ia sp

p. /

Stip

a co

mat

a

Gly

cyrr

hiza

lepi

dota

(Cal

amov

ilfa

long

ifolia

/ Ar

tem

isia

ludo

vici

ana)

(K

omex

199

3)

2 Fo

und

on d

unes

in 1

993

in a

noth

er su

rvey

of t

he P

akow

ki

Sand

hills

. Als

o re

porte

d to

occ

ur w

ith w

ire ru

sh (J

uncu

s ba

lticu

s). S

imila

r gen

eral

com

mun

ity ty

pe d

escr

ibed

in

prev

ious

surv

ey o

f stu

dy a

rea,

how

ever

no

deta

iled

floris

tic o

r si

te c

ondi

tions

pro

vide

d. D

iffer

ent d

omin

ant g

rass

not

ed.

Ru

mex

ven

osus

N

one

desc

ribed

-

-

Ory

zops

is h

ymen

oide

s –

Spor

obol

us c

rypt

andr

us

Car

ex fo

enea

– C

alam

ovilf

a lo

ngifo

lia –

El

ymus

can

aden

sis –

Ory

zops

is

hym

enoi

des (

Fehr

198

4)

3 R

epor

ted

for t

he W

ainw

right

sand

dun

e ar

ea, o

n ac

tive

blow

outs

. Sim

ilar s

ite c

ondi

tions

and

seve

ral s

imila

r spe

cies

, bu

t com

mun

ity c

ompo

sitio

n qu

ite d

iffer

ent.

St

ipa

com

ata

– O

ryzo

psis

hy

men

oide

s C

arex

foen

ea –

Cal

amov

ilfa

long

ifolia

Elym

us c

anad

ensi

s – O

ryzo

psis

hy

men

oide

s (Fe

hr 1

984)

3 R

epor

ted

for t

he W

ainw

right

sand

dun

e ar

ea, o

n ac

tive

blow

outs

. Sim

ilar s

ite c

ondi

tions

and

seve

ral s

imila

r spe

cies

, bu

t com

mun

ity c

ompo

sitio

n qu

ite d

iffer

ent.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

3

Appe

ndix

4. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om w

ithin

Alb

erta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Her

bace

ous

Veg

etat

ion

Stip

a co

mat

a –

Cyp

erus

sc

hwei

nitz

ii –

Cal

amov

ilfa

long

ifolia

Cal

amov

ilfa

long

ifolia

– H

espe

rost

ipa

com

ata

(Ada

ms e

t al.

1997

) 2

Des

crib

ed fr

om C

FB S

uffie

ld. S

ite c

ondi

tions

diff

ered

be

caus

e th

is si

te o

n flu

vial

slum

p fe

atur

es a

long

the

Sout

h Sa

skat

chew

an R

iver

, whe

re a

sand

ven

eer w

as p

rese

nt.

Text

ure

loam

y sa

nd, w

ith sl

opes

5-1

5 %

. Als

o fo

und

on

glac

ioflu

vial

out

was

h pl

ain,

with

min

imal

eol

ian

actio

n,

whe

re te

xtur

e is

loam

y sa

nd a

nd sl

ope

is 0

-5%

. Som

e si

mila

ritie

s in

site

con

ditio

ns a

nd se

vera

l gra

ss sp

ecie

s. N

o m

entio

n of

Cyp

erus

schw

eini

tzii

occu

rrin

g ho

wev

er.

Cal

amov

ilfa

long

ifolia

– A

rtem

isia

(S

mol

iak

1985

) 2

Foun

d on

upl

and

prai

rie, s

andy

soils

(Man

yber

ries)

. So

mew

hat s

imila

r com

mun

ity n

oted

in g

ener

al re

gion

, on

sand

y so

ils th

ough

onl

y on

e do

min

ant s

imila

r gra

ss sp

ecie

s.

C

alam

ovilf

a lo

ngifo

lia –

Stip

a co

mat

a (S

mol

iak

1985

) 2

Foun

d on

sand

y so

ils, i

n co

ulee

bot

tom

s (M

anyb

errie

s).

Sim

ilar c

omm

unity

not

ed in

gen

eral

regi

on, o

n sa

ndy

soils

th

ough

com

mun

ity in

this

repo

rt lik

ely

has m

ore

moi

stur

e av

aila

ble.

No

men

tion

of C

yper

us sc

hwei

nitz

ii oc

curr

ing.

Spor

obol

us c

rypt

andr

us –

C

alam

ovilf

a lo

ngifo

lia -

Ory

zops

is h

ymen

oide

s

Spor

obol

us c

rypt

andr

us –

Cal

amov

ilfa

long

ifolia

– K

oele

ria

mac

rant

ha –

Car

ex

obtu

sata

(Whe

atle

y an

d B

entz

200

2;

Mei

jer a

nd K

arpu

k 19

99)

2 D

escr

ibed

from

Cen

tral P

arkl

and

on a

ctiv

e du

nes a

nd

blow

outs

at D

illbe

rry

Lake

Pro

vinc

ial P

ark.

Gen

eral

ly lo

cate

d on

sout

h to

wes

t-fac

ing

aspe

cts a

nd sp

arse

veg

etat

ive

cove

r. H

eter

othe

ca v

illos

a m

ay a

lso

be p

rese

nt. T

wo

dom

inan

t sp

ecie

s in

this

repo

rt sa

me

as th

ose

gras

s spe

cies

foun

d in

Pa

kow

ki S

and

Hill

s. Si

mila

r site

con

ditio

ns, b

oth

in re

spec

t to

subs

trate

and

slop

e an

d as

pect

.

C

alam

ovilf

a lo

ngifo

lia –

Spo

robo

lus

cryp

tand

rus s

pars

ely

vege

tate

d ac

tive

dune

s (K

omex

199

3)

1 Fo

und

on a

ctiv

e du

nes i

n 19

93 in

ano

ther

surv

ey o

f the

Pa

kow

ki S

andh

ills.

Oth

er sp

ecie

s inc

lude

Hel

iant

hus

coup

land

ii, g

olde

n as

ter,

and

gold

en b

ean.

Sim

ilar g

ener

al

com

mun

ity ty

pe d

escr

ibed

in p

revi

ous s

urve

y of

stud

y ar

ea,

how

ever

no

deta

iled

floris

tic o

r site

con

ditio

ns p

rovi

ded.

H

erba

ceou

s V

eget

atio

n Ar

tem

isia

can

a / S

tipa

com

ata

Arte

mis

ia c

ana

/ Stip

a co

mat

a (H

olcr

oft

Wee

rstra

200

1)

2 D

escr

ibed

occ

urrin

g al

ong

old

river

terr

aces

, bad

land

s, ra

vine

si

de sl

opes

and

val

ley

wal

ls o

n a

rang

e of

par

ent m

ater

ials

, bu

t occ

urrin

g m

ost o

ften

on sa

ndy

glac

ial d

rift a

nd a

lluvi

um.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

4

Appe

ndix

4. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om w

ithin

Alb

erta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Her

bace

ous

Veg

etat

ion

Arte

mis

ia c

ana

/ Stip

a co

mat

a (c

ont.)

Ar

tem

isia

can

a –

Rosa

woo

dsii

/ C

alam

ovilf

a lo

ngifo

lia –

H

espe

rost

ipa

com

ata

– K

oele

ria

mac

rant

ha (A

dam

s et a

l. 19

97)

2 D

escr

ibed

at C

FB S

uffie

ld, o

n a

mor

aina

l pla

in w

ith e

olia

n ve

neer

and

sand

dun

es. T

extu

re w

as sa

nd, w

ith sl

opes

rang

ing

from

5-1

5 an

d w

ell t

o ra

pid

drai

nage

. Qui

te si

mila

r site

co

nditi

ons,

desp

ite C

FB S

uffie

ld b

eing

an

eolia

n ve

neer

ove

r m

orai

ne. V

eget

atio

n co

mpo

sitio

n al

so q

uite

sim

ilar,

with

a

few

diff

erin

g sp

ecie

s.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

5

Appendix 5. Correlation Table with Literature From Outside Alberta

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g2 C

omm

ents

Fore

st

Popu

lus d

elto

ides

/ G

lycy

rrhi

za le

pido

ta /

Junc

us b

altic

us

Popu

lus d

elto

ides

- (S

alix

am

ygda

loid

es) /

Sal

ix (e

xigu

a,

inte

rior

) Woo

dlan

d (N

atur

eser

ve

2002

)

2 Th

is c

omm

unity

was

foun

d w

idel

y in

the

cent

ral G

reat

Pla

ins

of th

e U

nite

d St

ates

. Sta

nds o

ccur

red

on re

cent

allu

vial

m

ater

ials

, alo

ng ri

vers

and

stre

ams.

The

soils

wer

e de

rived

fr

om fl

uvia

l san

ds, s

ilts a

nd c

lays

and

wer

e po

orly

dev

elop

ed.

The

wat

er ta

ble

fluct

uate

s with

the

leve

l of t

he a

djac

ent r

iver

or

stre

am. P

opul

us d

elto

ides

was

the

dom

inan

t spe

cies

in th

is

com

mun

ity, a

lthou

gh S

alix

exi

gua

and/

or S

alix

inte

rior

wer

e ge

nera

lly m

ore

dom

inan

t in

the

initi

al st

ages

follo

win

g a

maj

or fl

ood

even

t. Sa

lix a

myg

dalo

ides

was

rare

to

codo

min

ant.

Gly

cyrr

hiza

lepi

dota

may

be

a do

min

ant f

orb

whe

re g

razi

ng a

nd o

ther

dis

turb

ance

is m

inim

al. C

omm

unity

qu

ite si

mila

r to

that

foun

d at

Pak

owki

San

dhill

s, al

thou

gh th

is

com

mun

ity g

ener

ally

foun

d al

ong

fluvi

al ro

utes

, not

not

ed to

oc

cur i

n sa

nd d

une

area

s, al

thou

gh re

cent

allu

vial

mat

eria

ls

are

gene

rally

coa

rse

text

ured

. R

elat

ivel

y si

mila

r flo

ristic

co

mpo

sitio

n.

Po

pulu

s tre

mul

oide

ssan

d ty

pe

(Tho

rpe

and

God

win

199

3)

3 Fo

rest

s of a

spen

foun

d on

upl

and,

nor

th-fa

cing

or l

ower

slop

e po

sitio

ns a

nd o

n m

ore

stab

ilize

d la

ndfo

rms.

Was

foun

d to

be

mos

t wid

espr

ead

occu

rrin

g co

mm

unity

type

in M

anito

Sa

ndhi

lls (S

ask.

). H

ad ra

pidl

y to

mod

erat

ely

wel

l dra

ined

so

ils. C

omm

unity

diff

eren

t due

to d

iffer

ent o

vers

tory

spec

ies,

thou

gh si

te c

ondi

tions

are

ver

y si

mila

r.

Popu

lus t

rem

uloi

des (

Popu

lus

delto

ides

) low

are

as in

sand

flat

s (E

pp a

nd T

ownl

ey-S

mith

198

0)

2 Fo

und

on lo

w a

reas

in sa

nd fl

ats o

f Gre

at S

and

Hill

s (Sa

sk.)

whe

re so

il sa

linity

is n

ot h

igh.

Gly

cyrr

hiza

lepi

dota

list

ed a

s un

ders

tore

y fo

rb sp

ecie

s. N

oted

in si

mila

r eol

ian

land

scap

e,

thou

gh w

ith a

spen

as m

ore

com

mon

than

cot

tonw

ood.

Sim

ilar

site

con

ditio

ns.

Popu

lus d

elto

ides

Woo

dlan

d (E

pp

and

Tow

nley

Sm

ith 1

980)

2

Loca

ted

in a

regi

on o

f hig

h du

nes,

scat

tere

d on

inte

rdun

e sa

nd

flats

, with

no

unde

rsto

rey

vege

tatio

n (G

reat

San

d H

ills)

. A

gain

, sim

ilar s

ite c

ondi

tions

with

com

mon

lead

ing

over

stor

y sp

ecie

s. La

ck o

f und

erst

orey

veg

etat

ion

quite

diff

eren

t.

2 Sim

ilarit

y R

atin

g: 1

, ide

ntic

al to

or v

ery

sim

ilar;

2. si

mila

r in

mos

t res

pect

s; 3

, sev

eral

sim

ilarit

ies b

ut im

porta

nt d

iffer

ence

s (sc

ale

from

Cor

ns 1

983)

.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

1

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Fore

st

Popu

lus d

elto

ides

/ G

lycy

rrhi

za le

pido

ta /

Junc

us b

altic

us

Popu

lus d

elto

ides

/ Sy

mph

oric

arpo

s oc

cide

ntal

is W

oodl

and

(MN

HP

2002

)

? Li

sted

as G

2G3/

S2S3

for M

onta

na. N

o in

form

atio

n pr

ovid

ed.

Can

not a

sses

s sim

ilarit

y.

Popu

lus t

rem

uloi

des (

Popu

lus

bals

amife

ra) (

Cou

plan

d 19

50)

3 O

ften

dom

inan

t on

leew

ard

(eas

t sid

e) o

f dun

es, a

s the

y ar

e ad

apte

d to

with

stan

d bu

rial o

f the

trun

k by

sand

(S

aska

tche

wan

). Si

mila

r eol

ian

cond

ition

s, ho

wev

er d

omin

ant

spec

ies d

iffer

ent t

han

thos

e ob

serv

ed a

t Pak

owki

San

dhill

s.

Po

pulu

s tre

mul

oide

s /

Sym

phor

icar

pos a

lba

Fore

st (H

eide

l et

al.

2000

)

3 Sm

all,

youn

g st

ands

foun

d in

Med

icin

e La

ke S

andh

ills

(Mon

tana

) but

did

not

hav

e na

tive

unde

rsto

rey

and

grow

th

and

expa

nsio

n w

as a

ffec

ted

by g

razi

ng. S

imila

r eol

ian

cond

ition

s; h

owev

er, d

omin

ant s

peci

es d

iffer

ent t

han

thos

e ob

serv

ed a

t Pak

owki

San

dhill

s and

tree

s wer

e qu

ite m

atur

e.

Popu

lus d

elto

ides

– (S

alix

am

ygda

loid

es) /

Sal

ix e

xigu

a W

oodl

and

(USG

S 20

02a)

3 A

t Sco

tts B

luff

NM

(Neb

rask

a) c

omm

unity

was

foun

d on

le

vel t

o ge

ntly

slop

ing

loca

tions

, at t

he b

ase

of lo

w, n

orth

-fa

cing

slop

es. S

oil w

as si

lty. C

onta

ined

mor

e ea

ster

n sp

ecie

s su

ch a

s Fra

xinu

s pen

nsyl

vani

ca a

nd A

cer n

egun

do. S

imila

r le

adin

g sp

ecie

s, bu

t diff

eren

t ove

rall

floris

tic c

ompo

sitio

n.

Soil

cond

ition

s als

o qu

ite d

iffer

ent.

Po

pulu

s del

toid

es –

(Sal

ix

amyg

dalo

ides

) / S

alix

exi

gua

Woo

dlan

d (U

SGS

2002

d)

3 A

t Bad

land

s Nat

iona

l Par

k, in

Sou

th D

akot

a. W

as fo

und

alon

g riv

er a

nd c

reek

floo

dpla

ins,

pond

and

rese

rvoi

r mar

gins

, se

eps a

nd sp

rings

in m

esic

dra

ws a

nd se

eps a

nd sp

rings

that

oc

curr

ed a

long

the

edge

of s

andh

ill c

ompl

exes

. Sam

e le

adin

g tre

e sp

ecie

s, bu

t flo

ristic

com

posi

tion

and

site

con

ditio

ns

varie

d fr

om th

ose

obse

rved

at P

akow

ki S

andh

ills.

Popu

lus d

elto

ides

– (S

alix

am

ygda

loid

es) /

Sal

ix e

xigu

a W

oodl

and

(USG

S 20

02b)

3 A

t Dev

il’s T

ower

NM

(Wyo

min

g) c

omm

unity

was

foun

d on

flo

odpl

ain

of ri

ver.

Soil

was

san

dy. A

t thi

s loc

atio

n co

mm

unity

was

ver

y sm

all a

nd h

ad a

hig

h co

ver o

f inv

asiv

e,

exot

ic sp

ecie

s. Sa

me

lead

ing

tree

spec

ies,

but s

omew

hat

diffe

rent

soil

cond

ition

s (i.e

. flu

vial

vs.

eolia

n), a

lthou

gh st

ill

coar

se te

xtur

ed m

ater

ials

.

Po

pulu

s del

toid

es /

Pasc

opyr

um

smith

ii W

oodl

and

(Jon

es 1

998a

) 3

Loca

ted

in T

hund

er B

asin

Nat

iona

l Gra

ssla

nd, W

yom

ing

alon

g C

heye

nne

Riv

er. F

orm

ed li

near

gro

ves o

f tre

es, p

aral

lel

to st

ream

cha

nnel

on

allu

vial

mat

eria

ls. S

ame

lead

ing

tree

spec

ies,

diff

eren

t und

erst

orey

, and

som

ewha

t diff

eren

t soi

l co

nditi

ons (

i.e. f

luvi

al v

s. eo

lian)

.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

2

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Fore

st

Popu

lus d

elto

ides

/ G

lycy

rrhi

za le

pido

ta /

Junc

us b

altic

us

Popu

lus d

elto

ides

/ C

alam

ovilf

a lo

ngifo

lia W

oodl

and

(Jon

es 1

998b

) 3

Loca

ted

in T

hund

er B

asin

Nat

iona

l Gra

ssla

nd, W

yom

ing

alon

g A

ntel

ope

Cre

ek. F

orm

ed li

near

gro

ves o

f tre

es, p

aral

lel

to st

ream

cha

nnel

on

coar

se te

xtur

ed so

ils. S

ame

lead

ing

tree

spec

ies,

diff

eren

t und

erst

orey

, and

som

ewha

t diff

eren

t soi

l co

nditi

ons (

i.e. f

luvi

al v

s. eo

lian)

), a

lthou

gh st

ill c

oars

e te

xtur

ed m

ater

ials

.

Po

pulu

s del

toid

es /

Sym

phor

icar

pos

occi

dent

alis

Woo

dlan

d (C

oope

r et

al. 2

001)

3 Fo

und

alon

g riv

ers o

n un

stab

ilize

d flo

odpl

ains

whe

re

colo

nize

d al

luvi

al d

epos

its o

n m

eand

ers o

f stre

ams a

nd ri

vers

. A

wel

l-dev

elop

ed sh

rub

laye

r was

typi

cally

pre

sent

. Sam

e le

adin

g tre

e sp

ecie

s, bu

t with

diff

eren

t und

erst

orey

, and

so

mew

hat d

iffer

ent s

oil c

ondi

tions

(i.e

. flu

vial

vs.

eolia

n)

alth

ough

still

coa

rse

text

ured

mat

eria

ls.

Popu

lus d

elto

ides

– (S

alix

am

ygda

loid

es) /

Sal

ix e

xigu

a W

oodl

and

(Fab

er-L

ange

ndoe

n , D

. ed

itor 2

001)

2 Ty

pica

lly fo

und

alon

g ba

nks o

f stre

ams a

nd ri

vers

whe

re it

de

velo

ped

on n

ewly

dep

osite

d al

luvi

um. S

oils

wer

e pr

edom

inan

tly sa

nd, t

houg

h so

me

silt,

cla

y or

loam

may

be

pres

ent.

Not

ed th

at G

lycy

rrhi

za le

pido

ta w

as a

com

mon

forb

w

here

dis

turb

ance

was

low

. Als

o no

ted

that

bec

ause

of h

igh

perm

eabi

lity

of sa

ndy

flood

plai

n, sp

ecie

s typ

ical

of u

plan

d pr

airie

may

inva

de, i

nclu

ding

Art

emis

ia sp

p., C

alam

ovilf

a lo

ngifo

lia, H

eter

othe

ca v

illos

a, P

oa p

rate

nsis

and

Spo

robo

lus

cryp

tand

rus.

Com

mun

ity q

uite

sim

ilar t

o th

at fo

und

at

Pako

wki

San

dhill

s, al

thou

gh th

is c

omm

unity

gen

eral

ly fo

und

alon

g flu

vial

rout

es, n

ot n

oted

to o

ccur

in sa

nd d

une

area

s, al

thou

gh re

cent

allu

vial

mat

eria

ls a

re g

ener

ally

coa

rse

text

ured

. Rel

ativ

ely

sim

ilar f

loris

tic c

ompo

sitio

n.

Popu

lus d

elto

ides

– (S

alix

am

ygda

loid

es) /

Sal

ix e

xigu

a W

oodl

and

(USG

S 20

02c)

3 A

t Aga

te F

ossi

l Bed

s NM

(Neb

rask

a) c

omm

unity

was

foun

d on

floo

dpla

in o

f Nio

bara

rive

r. Lo

cate

d on

leve

l or s

lopi

ng

grou

nd o

n ba

nks o

r in

old

chan

nels

in th

e pr

imar

y flo

odpl

ain.

So

ils w

ere

fine

sand

s and

sand

y lo

ams t

hat w

ere

som

ewha

t po

orly

dra

ined

. Sam

e le

adin

g tre

e sp

ecie

s, bu

t with

diff

eren

t un

ders

tore

y, a

nd d

iffer

ent s

oil c

ondi

tions

(i.e

. flu

vial

vs.

eolia

n, p

oor d

rain

age)

alth

ough

still

coa

rse

text

ured

mat

eria

ls.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

3

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Shru

blan

d Ro

sa w

oods

ii / S

poro

bolu

s cr

ypta

ndru

s El

aeag

nus c

omm

utat

a –

Rosa

woo

dsii

– Sy

mph

oric

arpo

s occ

iden

talis

Prun

us v

irgi

nian

a (E

pp a

nd T

ownl

ey-

Smith

198

0)

2 Fo

rm c

lose

d sh

rubl

ands

foun

d on

stab

ilize

d sl

ip fa

ces,

typi

cally

no

rth-fa

cing

. Shr

ub c

ompo

sitio

n va

ried

loca

tion

to lo

catio

n an

d ea

ch sh

rub

spec

ies m

ay b

e do

min

ant a

t spe

cific

site

s, w

here

at

othe

rs m

ay b

e co

-dom

inan

t. V

aria

ble

floris

tic c

ompo

sitio

n th

ough

ver

y si

mila

r eol

ian

land

scap

e an

d si

te/s

oil c

ondi

tions

.

Ro

sa w

oods

ii (E

pp a

nd T

ownl

ey-

Smith

198

0)

1 C

omm

unity

dom

inan

t in

area

s w

here

sand

has

bee

n w

hipp

ed

off d

une

by st

rong

win

ds, c

reat

ing

area

s of s

low

sand

ac

cum

ulat

ion.

Ver

y si

mila

r (ge

nera

l) flo

ristic

com

posi

tion

and

very

sim

ilar s

ite c

ondi

tions

, bei

ng lo

cate

d on

act

ive

sand

du

nes.

Rosa

woo

dsii

(Art

emis

ia c

ana

/ El

aeag

nus c

omm

utat

a) (C

oupl

and

1950

)

2 Fo

und

in u

ndul

atin

g to

gen

tly ro

lling

are

as b

etw

een

stab

ilize

d du

nes.

Wat

er ta

ble

typi

cally

with

in 8

to 1

2 fe

et o

f soi

l sur

face

in

thes

e lo

catio

ns. V

aria

ble

floris

tic c

ompo

sitio

n an

d ge

nera

lly

sim

ilar e

olia

n la

ndsc

ape

and

site

/soi

l con

ditio

ns. C

omm

unity

oc

curr

ed in

Pak

owki

San

dhill

s on

parti

ally

stab

ilize

d to

act

ive

dune

s, on

leew

ard

slop

es.

Ros

a w

oods

ii Te

mpo

raril

y Fl

oode

d Sh

rubl

and

Alli

ance

(N

atur

eser

ve 2

002)

3 Th

ese

shru

blan

ds o

ccur

red

in th

e fo

othi

lls a

nd p

lain

s of

Mon

tana

and

Idah

o. E

leva

tions

rang

ed fr

om 6

50-1

700

m.

Stan

ds o

ccur

red

in fl

oodp

lain

s and

on

allu

vial

terr

aces

alo

ng

river

s and

stre

ams,

on h

illsi

des b

elow

sprin

gs a

nd in

ravi

nes

and

swal

es w

here

ove

rland

flow

from

snow

mel

t and

sum

mer

th

unde

rsto

rms p

rovi

des a

dditi

onal

moi

stur

e. S

ites w

ere

flat t

o m

oder

atel

y st

eep.

Alth

ough

site

s wer

e te

mpo

raril

y flo

oded

, th

ey w

ere

wel

l dra

ined

and

did

not

hav

e a

shal

low

wat

er ta

ble.

So

ils ra

nged

from

sand

y lo

ams t

o si

lt lo

ams.

Sam

e do

min

ant

shru

b sp

ecie

s, bu

t with

diff

eren

t soi

l con

ditio

ns (i

.e. f

luvi

al v

s. eo

lian,

tem

pora

ry fl

oodi

ng) a

lthou

gh st

ill c

oars

e te

xtur

ed

mat

eria

ls.

Rosa

woo

dsii

Shru

blan

d (C

oope

r et a

l. 19

99)

? A

com

mun

ity ty

pe li

sted

in B

eave

rhea

d M

ount

ain

regi

on

(Mon

tana

) tho

ugh

it is

not

des

crib

ed w

ith a

n ab

stra

ct. D

ue to

la

ck o

f inf

orm

atio

n, c

anno

t ass

ess s

imila

rity.

Ro

sa w

oods

ii Sh

rubl

and

(MN

HP

2002

) ?

List

ed a

s G5/

S5 in

Mon

tana

. No

desc

riptio

n of

com

mun

ity

type

giv

en. D

ue to

lack

of i

nfor

mat

ion,

can

not a

sses

s si

mila

rity.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

4

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Shru

blan

d Ro

sa w

oods

ii / S

poro

bolu

s cr

ypta

ndru

s G

rass

and

shru

b / S

and

type

(Tho

rpe

and

God

win

199

3)

3 Sy

mph

oric

arpo

s occ

iden

talis

was

dom

inan

t shr

ub, a

s far

as

perc

ent c

over

goe

s, bu

t Ros

a sp

p. a

nd P

runu

s vir

gini

ana

wer

e pr

esen

t in

50%

of p

lots

in th

is ty

pe. L

ocat

ed o

n st

abili

zed

dune

s, w

ith ra

pidl

y dr

aine

d, sa

ndy

soils

. Spo

robo

lus

cryp

tand

rus n

ot li

sted

as a

pre

vale

nt sp

ecie

s. Si

mila

r site

co

nditi

ons,

and

eolia

n la

ndsc

ape.

Flo

ristic

com

posi

tion

varia

ble

in li

tera

ture

, whi

le P

akow

ki R

osa

woo

dsii

com

mun

ities

qui

te re

petit

ive

patte

rn.

Rosa

woo

dsii

Shru

blan

d (R

ust 1

997)

?

List

ed a

s a n

atur

al p

lant

com

mun

ity in

Idah

o. N

o de

scrip

tion

of

com

mun

ity ty

pe g

iven

, thu

s can

not a

sses

s sim

ilarit

y.

Shru

blan

d Sa

lix a

myg

dalo

ides

– R

osa

woo

dsii

/ Jun

cus b

altic

us –

Sp

orob

olus

cry

ptan

drus

Salix

am

ygda

loid

es W

oodl

and

(MN

HP

2002

) ?

List

ed a

s G3/

S3 fo

r Mon

tana

but

no

desc

riptio

n gi

ven.

No

desc

riptio

n of

com

mun

ity ty

pe g

iven

, thu

s can

not a

sses

s si

mila

rity.

Sa

lix a

myg

dalo

ides

/ Sa

lix e

xigu

a W

oodl

and

(Nat

ures

erve

200

2)

3 Th

is v

eget

atio

n as

soci

atio

n oc

curr

ed in

ripa

rian

habi

tats

on

the

Col

umbi

an P

late

au in

the

inte

rior N

orth

wes

t and

in

north

east

ern

Uta

h. E

leva

tion

rang

es fr

om 1

00-1

600

m. S

tand

s w

ere

loca

ted

in o

verf

low

cha

nnel

s of l

arge

rive

rs, o

n na

rrow

flo

odpl

ains

of s

mal

l cre

eks a

nd so

il te

xtur

es c

over

a w

ide

rang

e, w

ith th

e ex

cept

ion

of c

lay.

Thi

s com

mun

ity h

ad a

m

oder

atel

y op

en o

vers

tore

y ca

nopy

dom

inat

ed b

y th

e sm

all

tree

Salix

am

ygda

loid

es w

ith S

alix

exi

gua

dom

inat

ing

the

tall-

shru

b la

yer n

ear t

he sh

ore.

Oth

er tr

ee sp

ecie

s inc

lude

d sc

atte

red

Popu

lus f

rem

ontii

, Ace

r neg

undo

, Pop

ulus

an

gust

ifolia

, Pop

ulus

del

toid

es a

nd th

e in

trodu

ced

Elae

agnu

s an

gust

ifolia

. Com

mun

ity d

escr

ibed

her

e fo

und

only

in ri

paria

n ha

bita

ts, a

nd n

ot e

olia

n la

ndsc

apes

. Lik

ely

diffe

rent

moi

stur

e re

gim

e ve

rsus

Pak

owki

regi

on.

Sa

lix a

myg

dalo

ides

Woo

dlan

d (N

atur

eser

ve 2

002)

3

The

Salix

am

ygda

loid

es w

oodl

and

type

was

foun

d in

the

Nor

ther

n R

ocky

Mou

ntai

ns a

nd p

oten

tially

into

par

ts o

f the

w

este

rn G

reat

Pla

ins.

Stan

ds o

ccur

red

in ri

paria

n ar

eas.

The

vege

tatio

n w

as d

omin

ated

by

Salix

am

ygda

loid

es. C

omm

unity

de

scrib

ed h

ere

foun

d on

ly in

ripa

rian

habi

tats

, and

not

eol

ian

land

scap

es. L

ikel

y di

ffere

nt m

oist

ure

regi

me

vers

us P

akow

ki

regi

on.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

5

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Shru

blan

d Sa

lix a

myg

dalo

ides

– R

osa

woo

dsii

/ Jun

cus b

altic

us –

Sp

orob

olus

cry

ptan

drus

(c

ont.)

Salix

am

ygda

loid

es W

oodl

and

(Fab

er-

Lang

endo

en ,

D. e

dito

r 200

1; M

arrio

tt an

d Fa

ber-

Lang

endo

en 2

000)

3 Fo

und

in th

e N

orth

ern

Roc

ky M

ount

ains

and

pos

sibl

y in

to

parts

of t

he w

este

rn G

reat

Pla

ins.

Stan

ds o

ccur

red

in ri

paria

n ar

eas.

Was

doc

umen

ted

in B

lack

Hill

s at c

onflu

ence

of t

wo

cree

ks. I

t for

med

a ta

ll-sh

rub

stra

tum

with

Sal

ix b

ebbi

ana

and

Cor

nus s

eric

ea a

nd w

as m

ore

shru

blan

d th

an w

oodl

and.

C

omm

unity

des

crib

ed h

ere

foun

d on

ly in

ripa

rian

habi

tats

, and

no

t eol

ian

land

scap

es. L

ikel

y di

ffere

nt m

oist

ure

regi

me

vers

us

Pako

wki

regi

on. S

peci

es c

ompo

sitio

n al

so q

uite

diff

eren

t.

Shru

blan

d El

aeag

nus c

omm

utat

a /

Gly

cyrr

hiza

lepi

dota

El

aeag

nus c

omm

utat

a –

Rosa

woo

dsii

– Sy

mph

oric

arpo

s occ

iden

talis

Prun

us v

irgi

nian

a (E

pp a

nd T

ownl

ey-

Smith

198

0)

2 Fo

rmed

clo

sed

shru

blan

ds fo

und

on st

abili

zed

slip

face

s, ty

pica

lly n

orth

-fac

ing.

Shr

ub c

ompo

sitio

n va

ried

loca

tion

to

loca

tion

and

each

shru

b sp

ecie

s may

be

dom

inan

t at s

peci

fic

site

s, w

here

at o

ther

s may

be

co-d

omin

ant.

Spec

ies

com

posi

tion

mor

e va

riabl

e th

an th

at fo

und

at P

akow

ki

Sand

hills

regi

on, b

ut si

te c

ondi

tions

qui

te si

mila

r, be

ing

stab

ilize

d eo

lian

feat

ures

.

El

aeag

nus c

omm

utat

a Sh

rubl

and

(MN

HP

2002

) ?

List

ed a

s G2Q

/S2?

For

Mon

tana

. No

desc

riptio

n gi

ven

thus

no

asse

ssm

ent o

f sim

ilarit

y co

uld

be m

ade.

Ro

sa w

oods

ii (A

rtem

isia

can

a /

Elae

agnu

s com

mut

ata)

(Cou

plan

d 19

50)

2 Fo

und

in u

ndul

atin

g to

gen

tly ro

lling

are

as b

etw

een

stab

ilize

d du

nes.

Wat

er ta

ble

typi

cally

with

in 8

to 1

2 fe

et o

f soi

l sur

face

in

thes

e lo

catio

ns. S

peci

es c

ompo

sitio

n di

ffer

ent,

thou

gh q

uite

ge

nera

l, th

an th

at fo

und

at P

akow

ki S

andh

ills r

egio

n, b

ut si

te

cond

ition

s qui

te si

mila

r. D

epth

to w

ater

tabl

e at

stud

y ar

ea w

as

not k

now

n.

Elae

agnu

s com

mut

ata

shru

blan

d (E

pp

and

Tow

nley

Sm

ith 1

980)

2

Ofte

n fo

und

inha

bitin

g bl

owou

ts a

way

from

bar

e sa

nd.

Pako

wki

San

dhill

s com

mun

ity n

ot fo

und

in b

low

outs

, but

was

fo

und

on p

artia

lly st

abili

zed

sand

dun

es, a

way

from

act

ive

sand

. Det

aile

d de

scrip

tion

of fl

oris

tic c

ompo

sitio

n un

fortu

nate

ly n

ot p

rovi

ded.

Elae

agnu

s com

mut

ata

Shru

blan

d (H

eide

l et a

l. 20

00)

2 R

epor

ted

in n

orth

ern

Mon

tana

, eas

t of C

ontin

enta

l div

ide.

G

ener

ally

cla

ssifi

ed a

s tem

pora

rily

flood

ed. I

n M

edic

ine

Lake

sa

ndhi

lls, s

ites h

ad sh

rub

cove

r of 1

0% a

nd g

rass

cov

er o

f 70

%. S

ites w

ere

not f

lood

ed b

ut th

e w

ater

tabl

e w

as w

ithin

the

root

ing

zone

. Com

mun

ity d

escr

ibed

her

e as

tem

pora

rily

flood

ed, w

here

as P

akow

ki n

ot li

kely

exp

erie

ncin

g flo

odin

g..

Like

ly d

iffer

ent m

oist

ure

regi

me

vers

us P

akow

ki re

gion

.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

6

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Shru

blan

d El

aeag

nus c

omm

utat

a /

Gly

cyrr

hiza

lepi

dota

(con

t.)

Elae

agnu

s com

mut

ata

Shru

blan

d A

llian

ce (N

atur

eser

ve 2

002)

2

This

shru

b al

lianc

e w

as fo

und

in th

e no

rther

n G

reat

Pla

ins i

n a

mix

edgr

ass p

rairi

e m

atrix

. It w

as d

omin

ated

by

mid

to ta

ll sh

rubs

, esp

ecia

lly E

laea

gnus

com

mut

ata.

Pas

copy

rum

smith

ii w

as d

omin

ant i

n th

e he

rbac

eous

laye

r, ty

pica

lly a

ccom

pani

ed

by K

oele

ria

mac

rant

ha, S

chiza

chyr

ium

scop

ariu

m a

nd

Hes

pero

stip

a co

mat

a (=

Stip

a co

mat

a). E

laea

gnus

com

mut

ata

was

mos

t abu

ndan

t on

flat s

andy

site

s in

sout

hern

Sa

skat

chew

an. S

peci

es c

ompo

sitio

n m

ore

varia

ble

than

that

ob

serv

ed a

t Pak

owki

, tho

ugh

dom

inan

t spe

cies

is th

e sa

me.

Si

te c

ondi

tions

, bei

ng so

mew

hat m

ore

leve

l, sa

ndy

subs

trate

s, ar

e si

mila

r.

El

aeag

nus c

omm

utat

a / P

asco

pyru

m

smith

ii Sh

rubl

and

(Nat

ures

erve

200

2)

3 Th

is a

ssoc

iatio

n oc

curr

ed in

the

north

wes

tern

por

tion

of th

e G

reat

Pla

ins o

f the

Uni

ted

Stat

es a

nd C

anad

a. S

tand

s occ

urre

d on

a v

arie

ty o

f gla

cial

land

form

s inc

ludi

ng k

ames

, esk

ers a

nd

area

s of t

ill a

nd o

utw

ash.

Com

mon

on

north

faci

ng sl

opes

and

si

tes w

here

moi

stur

e w

as m

ore

abun

dant

, inc

ludi

ng a

long

rive

r va

lley

slop

es. T

he v

eget

atio

n fo

rmed

ope

n th

icke

ts w

ithin

the

mix

ed-g

rass

pra

irie

land

scap

e. E

laea

gnus

com

mut

ata

was

ge

nera

lly a

shor

t to

med

ium

hei

ght s

hrub

, alth

ough

it c

an g

row

up

to 5

m. P

asco

pyru

m sm

ithii

not a

dom

inan

t spe

cies

at

Pako

wki

San

dhill

s. A

lthou

gh su

bstra

tes d

escr

ibed

in th

is re

port

are

coar

se, t

hey

are

diffe

rent

than

eol

ian

land

form

s.

Shru

blan

d El

aeag

nus c

omm

utat

a /

Arte

mis

ia lu

dovi

cian

a /

Cal

amov

ilfa

long

ifolia

Elae

agnu

s com

mut

ata

– Ro

sa w

oods

ii –

Sym

phor

icar

pos o

ccid

enta

lis –

Pr

unus

vir

gini

ana

(Epp

and

Tow

nley

-Sm

ith 1

980)

2 Fo

rmed

clo

sed

shru

blan

ds fo

und

on st

abili

zed

slip

face

s, ty

pica

lly n

orth

-fac

ing.

Shr

ub c

ompo

sitio

n va

ried

loca

tion

to

loca

tion

and

each

shru

b sp

ecie

s may

be

dom

inan

t at s

peci

fic

site

s, w

here

at o

ther

s may

be

co-d

omin

ant.

Spec

ies

com

posi

tion

mor

e va

riabl

e th

an a

t Pak

owki

San

dhill

s, al

thou

gh

no m

entio

n of

Art

emis

ia sp

p. o

r san

d gr

ass.

Site

con

ditio

ns

quite

sim

ilar h

owev

er.

Elae

agnu

s com

mut

ata

Shru

blan

d (M

NH

P 20

02)

? Li

sted

as G

2Q/S

2? fo

r Mon

tana

. No

desc

riptio

n gi

ven

thus

no

sim

ilarit

y as

sess

men

t cou

ld b

e m

ade.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

7

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Shru

blan

d El

aeag

nus c

omm

utat

a /

Arte

mis

ia lu

dovi

cian

a /

Cal

amov

ilfa

long

ifolia

(c

ont.)

Rosa

woo

dsii

(Art

emis

ia c

ana

/ El

aeag

nus c

omm

utat

a) (C

oupl

and

1950

)

2 Fo

und

in u

ndul

atin

g to

gen

tly ro

lling

are

as b

etw

een

stab

ilize

d du

nes.

Wat

er ta

ble

typi

cally

with

in 8

to 1

2 fe

et o

f soi

l sur

face

in

thes

e lo

catio

ns. S

peci

es c

ompo

sitio

n di

ffer

ent,

thou

gh q

uite

ge

nera

l, th

an th

at fo

und

at P

akow

ki S

andh

ills r

egio

n, b

ut si

te

cond

ition

s qui

te si

mila

r. D

epth

to w

ater

tabl

e at

Pak

owki

stud

y ar

ea w

as n

ot k

now

n.

Elae

agnu

s com

mut

ata

shru

blan

d (E

pp

and

Tow

nley

Sm

ith 1

980)

2

Ofte

n fo

und

inha

bitin

g bl

owou

ts a

way

from

bar

e sa

nd.

Pako

wki

San

dhill

s com

mun

ity n

ot fo

und

in b

low

outs

, but

was

fo

und

on p

artia

lly st

abili

zed

sand

dun

es, a

way

from

act

ive

sand

. Det

aile

d de

scrip

tion

of fl

oris

tic c

ompo

sitio

n un

fortu

nate

ly n

ot p

rovi

ded.

Elae

agnu

s com

mut

ata

Shru

blan

d (H

eide

l et a

l. 20

00)

2 R

epor

ted

in n

orth

ern

Mon

tana

, eas

t of C

ontin

enta

l div

ide.

G

ener

ally

cla

ssifi

ed a

s tem

pora

rily

flood

ed. I

n M

edic

ine

Lake

Sa

ndhi

lls, s

ites h

ad sh

rub

cove

r of 1

0% a

nd g

rass

cov

er o

f 70

%. S

ites a

re n

ot fl

oode

d bu

t the

wat

er ta

ble

was

with

in th

e ro

otin

g zo

ne. C

omm

unity

des

crib

ed h

ere

as te

mpo

raril

y flo

oded

, whe

reas

Pak

owki

not

like

ly e

xper

ienc

ing

flood

ing.

Li

kely

diff

eren

t moi

stur

e re

gim

e ve

rsus

Pak

owki

regi

on.

Elae

agnu

s com

mut

ata

Shru

blan

d A

llian

ce (N

atur

eser

ve 2

002)

2

This

shru

b al

lianc

e w

as fo

und

in th

e no

rther

n G

reat

Pla

ins i

n a

mix

edgr

ass p

rairi

e m

atrix

. It w

as d

omin

ated

by

mid

to ta

ll sh

rubs

, esp

ecia

lly E

laea

gnus

com

mut

ata.

Pas

copy

rum

smith

ii w

as d

omin

ant i

n th

e he

rbac

eous

laye

r, ty

pica

lly a

ccom

pani

ed

by K

oele

ria

mac

rant

ha, S

chiza

chyr

ium

scop

ariu

m a

nd

Hes

pero

stip

a co

mat

a (=

Stip

a co

mat

a). E

laea

gnus

com

mut

ata

was

mos

t abu

ndan

t on

flat s

andy

site

s in

sout

hern

Sa

skat

chew

an. S

peci

es c

ompo

sitio

n m

ore

varia

ble

than

that

ob

serv

ed a

t Pak

owki

, tho

ugh

dom

inan

t spe

cies

is th

e sa

me.

Si

te c

ondi

tions

, bei

ng so

mew

hat m

ore

leve

l, sa

ndy

subs

trate

s, ar

e si

mila

r.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

8

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Shru

blan

d El

aeag

nus c

omm

utat

a /

Arte

mis

ia lu

dovi

cian

a /

Cal

amov

ilfa

long

ifolia

(c

ont.)

Elae

agnu

s com

mut

ata

/ Pas

copy

rum

sm

ithii

Shru

blan

d (N

atur

eser

ve 2

002)

3

This

ass

ocia

tion

occu

rred

in th

e no

rthw

este

rn p

ortio

n of

the

Gre

at P

lain

s of t

he U

nite

d St

ates

and

Can

ada.

Sta

nds o

ccur

red

on a

var

iety

of g

laci

al la

ndfo

rms i

nclu

ding

kam

es, e

sker

s and

ar

eas o

f till

and

out

was

h. C

omm

on o

n no

rth-f

acin

g sl

opes

and

si

tes w

here

moi

stur

e w

as m

ore

abun

dant

, inc

ludi

ng a

long

rive

r va

lley

slop

es. T

he v

eget

atio

n fo

rmed

ope

n th

icke

ts w

ithin

the

mix

ed-g

rass

pra

irie

land

scap

e. E

laea

gnus

com

mut

ata

was

ge

nera

lly a

shor

t to

med

ium

hei

ght s

hrub

, alth

ough

it c

an g

row

up

to 5

m. P

asco

pyru

m sm

ithii

not a

dom

inan

t spe

cies

at

Pako

wki

San

dhill

s. A

lthou

gh su

bstra

tes d

escr

ibed

in th

is re

port

are

coar

se, t

hey

are

diffe

rent

than

eol

ian

land

form

s. Sh

rubl

and

Prun

us v

irgi

nian

a /

Cal

amov

ilfa

long

ifolia

El

aeag

nus c

omm

utat

a –

Rosa

woo

dsii

– Sy

mph

oric

arpo

s occ

iden

talis

Prun

us v

irgi

nian

a (E

pp a

nd T

ownl

ey-

Smith

198

0)

2 Fo

rmed

clo

sed

shru

blan

ds fo

und

on st

abili

zed

slip

face

s, ty

pica

lly n

orth

-fac

ing.

Shr

ub c

ompo

sitio

n va

ried

loca

tion

to

loca

tion

and

each

shru

b sp

ecie

s may

be

dom

inan

t at s

peci

fic

site

s, w

here

at o

ther

s may

be

co-d

omin

ant.

Spec

ies

com

posi

tion

mor

e va

riabl

e th

an th

at o

bser

ved

at P

akow

ki

Sand

hills

, how

ever

site

con

ditio

ns a

re v

ery

sim

ilar.

Prun

us v

irgi

nian

a Sh

rubl

and

(MN

HP

2002

) ?

List

ed a

s G4Q

/S4

in M

onta

na. N

o de

scrip

tion

give

n th

us n

o si

mila

rity

asse

ssm

ent c

ould

be

mad

e.

Prun

us v

irgi

nian

a Sh

rubl

and

(Hei

del

et a

l. 20

00)

2 N

oted

to o

ccur

in sm

all p

atch

es in

Med

icin

e La

ke S

andh

ills,

Mon

tana

. Had

hig

h sh

rub

cove

r and

low

und

erst

orey

cov

er,

thou

gh S

tipa

com

ata

was

com

mon

und

erst

orey

spec

ies.

Prun

us

virg

inia

na h

as a

dee

p ro

ot sy

stem

that

can

reac

h th

e w

ater

tabl

e in

the

Med

icin

e La

ke S

andh

ills.

Else

whe

re in

Mon

tana

was

co

nsid

ered

a ri

paria

n co

mm

unity

. Dom

inan

t gra

ss d

iffer

ent,

but

dens

ity o

f shr

ubs c

ompa

rabl

e to

that

foun

d in

Pak

owki

Sa

ndhi

lls. S

ite c

ondi

tions

ver

y si

mila

r

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

9

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Shru

blan

d Pr

unus

vir

gini

ana

/ C

alam

ovilf

a lo

ngifo

lia

(con

t.)

Prun

us v

irgi

nian

a Sh

rubl

and

Alli

ance

(N

atur

eser

ve 2

002)

3

This

com

mun

ity w

as ty

pica

lly fo

und

alon

g st

ream

s, riv

ers,

lake

s and

pon

ds a

nd o

n te

rrac

es, o

r in

cany

ons o

r ste

ep g

ullie

s. El

evat

ions

rang

ed fr

om 7

16 m

to a

bout

160

0 m

in M

onta

na,

Wyo

min

g an

d C

olor

ado

and

up to

244

0 m

in N

evad

a. In

som

e pl

aces

, the

alli

ance

occ

urre

d on

side

slop

es o

f hill

side

s, im

med

iate

ly b

elow

a se

ep o

r spr

ing.

Som

e ex

ampl

es o

f thi

s al

lianc

e ha

ve b

een

plac

ed in

to a

n in

term

itten

tly o

r tem

pora

rily

flood

ed h

ydro

logi

c re

gim

e. S

oils

wer

e us

ually

wel

l-dev

elop

ed,

olde

r and

wel

l-dra

ined

, for

med

in sh

allo

w to

dee

p al

luvi

al

depo

sits

. Com

mun

ity d

escr

ibed

her

e fo

und

only

in ri

paria

n ha

bita

ts, a

nd n

ot e

olia

n la

ndsc

apes

. Ver

y di

ffer

ent s

oil

cond

ition

s and

diff

eren

t moi

stur

e re

gim

e ve

rsus

Pak

owki

re

gion

.

Pr

unus

vir

gini

ana

– (P

runu

s am

eric

ana)

Shr

ubla

nd (C

oope

r et a

l. 19

99)

3 C

omm

unity

repo

rted

in M

onta

na a

t Bitt

er C

reek

Bad

land

s, at

he

ads o

f cou

lees

feed

ing

into

bad

land

s. C

omm

unity

occ

urre

d as

ver

y sm

all,

dens

e, li

near

pat

ches

. Few

oth

er sp

ecie

s fou

nd,

due

to d

ensi

ty o

f Pru

nus.

Diff

eren

t spe

cies

com

posi

tion,

as

only

one

Pru

nus s

peci

es fo

und

at P

akow

ki S

andh

ills.

Site

co

nditi

ons a

lso

som

ewha

t diff

eren

t, th

ough

like

ly d

rier t

han

aver

age.

Den

sity

and

shap

e of

com

mun

ity si

mila

r.

Pr

unus

vir

gini

ana

– (P

runu

s am

eric

ana)

Shr

ubla

nd (U

SGS

2002

d)

3 D

omin

antly

Pru

nus a

mer

ican

a, w

ith so

me

P. v

irgi

nian

a.

Gen

eral

ly fo

und

in sl

opin

g to

nea

rly le

vel m

esic

dra

ws a

nd

near

ly le

vel o

xbow

s. A

few

stan

ds a

lso

foun

d at

seep

zon

e on

ed

ge o

f san

dhill

s. D

iffer

ent s

peci

es c

ompo

sitio

n, a

s onl

y on

e Pr

unus

spec

ies f

ound

at P

akow

ki S

andh

ills.

Site

con

ditio

ns

also

som

ewha

t diff

eren

t, as

dom

inan

tly a

ripa

rian

com

mun

ity.

Gra

ss a

nd sh

rub

/ San

d ty

pe (T

horp

e an

d G

odw

in 1

993)

3

Sym

phor

icar

pos o

ccid

enta

lis w

as d

omin

ant s

hrub

, as f

ar a

s pe

rcen

t cov

er g

oes,

but R

osa

spp.

and

Pru

nus v

irgi

nian

a w

ere

pres

ent i

n 50

% o

f plo

ts in

this

type

. Loc

ated

on

stab

ilize

d du

nes,

with

rapi

dly

drai

ned,

sand

y so

ils. C

alam

ovilf

a lo

ngifo

lia

also

list

ed a

s occ

urrin

g. S

peci

es c

ompo

sitio

n m

ore

varia

ble

than

that

obs

erve

d at

Pak

owki

San

dhill

s, th

ough

site

con

ditio

ns

are

quite

sim

ilar.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

1

0

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Dw

arf

Shru

blan

d Eu

rotia

lana

ta /

Stip

a co

mat

a –

Cal

amov

ilfa

long

ifolia

Stip

a co

mat

a A

SSO

CIA

TIO

N

(Loo

man

198

0)

3 Fo

und

to b

e co

mm

on (w

ith B

oute

loua

gra

cilis

) on

dry

prai

rie.

Cov

er o

f Bou

telo

ua g

raci

lis in

crea

ses,

grad

ually

repl

acin

g St

ipa

com

ata

as g

razi

ng in

crea

ses.

A v

aria

tion

of th

e co

mm

unity

incl

udes

Cal

amov

ilfa

long

ifolia

and

occ

urre

d on

sa

ndy

loam

or l

oam

y sa

nd so

ils. S

peci

es c

ompo

sitio

n qu

ite

diffe

rent

, and

no

men

tion

of w

inte

rfat

as a

shru

b. C

oars

er

text

ured

soils

, whi

ch a

re si

mila

r to

Pako

wki

San

dhill

s.

K

rasc

heni

nnik

ovia

lana

ta /

Stip

a co

mat

a D

war

f-Sh

rubl

and

(MN

HP

2002

)

? Li

sted

as G

3/S3

for M

onta

na. N

o de

scrip

tion

give

n th

us n

o as

sess

men

t of s

imila

rity

coul

d be

mad

e.

Kra

sche

ninn

ikov

ia la

nata

/ H

espe

rost

ipa

com

ata

Dw

arf-

Shru

blan

d (N

atur

eser

ve 2

002)

2 R

epor

ted

in D

eVel

ice,

R. L

., J.

Lich

thar

dt a

nd P

. S. B

ourg

eron

. 19

91. A

pre

limin

ary

clas

sific

atio

n of

the

plan

t com

mun

ities

of

north

east

ern

Mon

tana

. Pre

pare

d fo

r the

Mon

tana

Nat

ural

H

erita

ge P

rogr

am. H

elen

a, M

T. 1

44 p

p. N

o de

scrip

tion

give

n th

us d

iffic

ult t

o as

sess

, but

bas

ed o

n co

mm

unity

nam

e do

min

ant s

peci

es a

re th

e sa

me

as th

ose

foun

d in

Pak

owki

.

K

rasc

heni

nnik

ovia

lana

ta /

Bout

elou

a gr

acili

s Dw

arf S

hrub

Her

bace

ous

Veg

etat

ion

(Fab

er-L

ange

ndoe

n , D

. ed

itor 2

001)

3 V

eget

atio

n co

ntai

ned

open

shru

b an

d gr

amin

oid

laye

r. Sh

ort

herb

aceo

us la

yer i

s dom

inat

ed b

y Bo

utel

oua

grac

ilis,

Echi

nace

a an

gust

ifolia

and

Lia

tris

pun

ctat

a. F

ound

in

sout

hwes

tern

Gre

at P

lain

s and

Sem

i-des

ert m

ount

ains

, fro

m

Col

orad

o so

uth

to N

ew M

exic

o an

d A

rizon

a. A

lso

foun

d in

K

ansa

s. Sp

ecie

s com

posi

tion

quite

diff

eren

t, an

d no

men

tion

of

need

le-a

nd-th

read

or s

and

gras

s. Lo

cate

d in

a m

uch

mor

e so

uthe

rly re

gion

, with

des

ert c

ondi

tions

.

Eu

rotia

lana

ta /

Poa

secu

nda

Extre

mel

y xe

rom

orph

ic d

war

f-sh

rubl

and

(Rus

t 199

7)

? Li

sted

as n

atur

al p

lant

com

mun

ity ty

pe fo

r Ida

ho. N

o de

scrip

tion

give

n th

us n

o si

mila

rity

asse

ssm

ent c

ould

be

mad

e.

Her

bace

ous

Veg

etat

ion

Salix

exi

gua

/ Gly

cyrr

hiza

le

pido

ta /

Junc

us b

altic

us

Salix

exi

gua

Shru

blan

d (U

SGS

2002

a)

3 C

omm

unity

foun

d al

ong

mar

gins

of N

orth

Pla

tte R

iver

(Sco

tts

Blu

ff N

M) a

nd lo

catio

ns o

n lo

wer

floo

dpla

in te

rrac

e. O

ccur

red

on re

cent

allu

vial

sand

s with

littl

e so

il de

velo

pmen

t. U

nder

stor

ey sp

ecie

s com

posi

tion

quite

diff

eren

t, al

so n

ote

occa

sion

al P

opul

us d

elto

ides

, thu

s qui

te d

iffer

ent t

han

com

mun

ity ty

pe fo

und

in P

akow

ki S

andh

ills.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

1

1

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Her

bace

ous

Veg

etat

ion

Salix

exi

gua

/ Gly

cyrr

hiza

le

pido

ta /

Junc

us b

altic

us

(con

t.)

Salix

exi

gua

/ Mes

ic G

ram

inoi

ds

Shru

blan

d (F

aber

-Lan

gend

oen

, D.

edito

r 200

1)

3 V

eget

atio

n do

min

ated

by

shru

bs w

ith a

fairl

y de

nse

grou

nd

cove

r (at

leas

t 30%

) of m

esic

gra

min

oids

and

forb

s. Ju

ncus

sp

p. n

oted

as a

com

mon

her

bace

ous s

peci

es. C

omm

unity

foun

d on

sand

bars

, isl

ands

and

shor

elin

es o

f stre

am c

hann

els a

nd

brai

ded

river

s. So

ils a

re p

oorly

dev

elop

ed. P

rimar

ily fo

und

in

Gre

at P

lain

s but

als

o pa

rts o

f Roc

ky M

ount

ains

and

In

term

ount

ain

Sem

i-des

ert r

egio

ns. W

yom

ing

wes

t to

poss

ibly

Id

aho,

sout

h to

Uta

h an

d ea

st to

Okl

ahom

a. S

peci

es

com

posi

tion

com

para

ble,

but

site

con

ditio

ns q

uite

diff

eren

t. Th

is c

omm

unity

des

crib

ed m

ainl

y fr

om ri

paria

n ar

eas,

and

alth

ough

they

hav

e po

orly

dev

elop

ed, c

oars

e te

xtur

ed so

ils,

they

wou

ld h

ave

a gr

eate

r moi

stur

e av

aila

bilit

y th

an sa

nd d

une

regi

on.

Salix

exi

gua

Tem

pora

rily

Floo

ded

Shru

blan

d (F

aber

-Lan

gend

oen

, D.

edito

r 200

1)

3 D

omin

ated

by

2-4m

Sal

ix e

xigu

a w

ith a

mod

erat

e to

hig

h st

em

dens

ity. F

ound

on

rece

ntly

dep

osite

d or

dis

turb

ed a

lluvi

al

mat

eria

ls, d

omin

antly

sand

s. Fo

und

at lo

wer

ele

vatio

ns

thro

ugho

ut n

orth

wes

tern

US

and

Gre

at P

lain

s and

into

M

anito

ba. S

peci

es c

ompo

sitio

n co

mpa

rabl

e, b

ut si

te c

ondi

tions

qu

ite d

iffer

ent.

This

com

mun

ity d

escr

ibed

mai

nly

from

ripa

rian

area

s, an

d al

thou

gh th

ey h

ave

coar

se te

xtur

ed so

ils, t

hey

wou

ld

have

a g

reat

er m

oist

ure

avai

labi

lity

than

sand

dun

e re

gion

.

Sa

lix e

xigu

a Te

mpo

raril

y Fl

oode

d Sh

rubl

and

(USG

S 20

02d)

3

Foun

d al

ong

bank

s of s

ever

al c

reek

s. O

ccur

red

adja

cent

to

cree

ks a

nd ri

vers

whe

re m

oist

sedi

men

ts a

ccum

ulat

e an

d ad

jace

nt to

som

e w

etla

nd c

omm

uniti

es. S

ites w

ere

near

ly a

ll le

vel w

ith p

rese

nce

of g

roun

d-w

ater

. Thi

s com

mun

ity

desc

ribed

mai

nly

from

ripa

rian

area

s, an

d w

as n

oted

to h

ave

grou

nd w

ater

pre

sent

.

Sa

lix e

xigu

a Sh

rubl

and

[Pro

visi

onal

] (U

SGS

2002

c)

2 Fo

und

alon

g N

ioba

ra R

iver

, Aga

te F

ossi

l Bed

s NM

in

Neb

rask

a. F

ound

alo

ng lo

wer

floo

dpla

in te

rrac

es, w

ith sa

ndy

loam

soils

that

are

poo

rly to

som

ewha

t poo

rly d

rain

ed. J

uncu

s ba

lticu

s lis

ted

as a

n ab

unda

nt sp

ecie

s. N

oted

spec

ies d

iver

sity

qu

ite h

igh.

Spe

cies

com

posi

tion

com

para

ble,

but

site

co

nditi

ons q

uite

diff

eren

t. Th

is c

omm

unity

des

crib

ed m

ainl

y fr

om ri

paria

n ar

eas,

with

som

ewha

t poo

rly d

rain

ed so

ils.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

1

2

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Her

bace

ous

Veg

etat

ion

Salix

exi

gua

/ Gly

cyrr

hiza

le

pido

ta /

Junc

us b

altic

us

(con

t.)

Salix

exi

gua

Tem

pora

rily

Floo

ded

Shru

blan

d (C

oope

r et a

l. 19

99)

3 Fo

und

in B

eave

rhea

d M

ount

ains

, Mon

tana

, whe

re it

occ

urre

d on

gra

velly

allu

vial

mat

eria

ls o

n flo

odpl

ains

and

rive

r ter

race

s in

rive

r bot

tom

s. U

nder

stor

ey sp

ecie

s min

imal

due

to h

igh

dist

urba

nce

rate

, but

mos

t com

mon

are

Cir

sium

arv

ense

, M

enth

a ar

vens

is a

nd P

hala

ris a

rund

inac

aea.

Spe

cies

co

mpo

sitio

n so

mew

hat s

imila

r, bu

t site

con

ditio

ns q

uite

di

ffere

nt. T

his c

omm

unity

des

crib

ed m

ainl

y fr

om ri

paria

n ar

eas,

with

tem

pora

rily

flood

ed so

ils.

Salix

exi

gua

/ Bar

ren

Seas

onal

ly

flood

ed c

old-

deci

duou

s Shr

ubla

nd

(Rus

t 199

7)

? Li

sted

as a

nat

ural

pla

nt c

omm

unity

for I

daho

, but

no

desc

riptio

n gi

ven

thus

no

asse

ssm

ent o

f sim

ilarit

y co

uld

be

done

.

Sa

lix e

xigu

a / E

quis

etum

arv

ense

Se

ason

ally

floo

ded

cold

-dec

iduo

us

Shru

blan

d (R

ust 1

997)

? Li

sted

as a

nat

ural

pla

nt c

omm

unity

for I

daho

, but

no

desc

riptio

n gi

ven

thus

no

asse

ssm

ent o

f sim

ilarit

y co

uld

be

done

.

Sa

lix e

xigu

a / M

esic

For

b Se

ason

ally

flo

oded

col

d-de

cidu

ous S

hrub

land

(R

ust 1

997)

? Li

sted

as a

nat

ural

pla

nt c

omm

unity

for I

daho

, but

no

desc

riptio

n gi

ven

thus

no

asse

ssm

ent o

f sim

ilarit

y co

uld

be

done

.

Sa

lix e

xigu

a / M

esic

Gra

min

oid

Seas

onal

ly fl

oode

d co

ld-d

ecid

uous

Sh

rubl

and

(Rus

t 199

7)

? Li

sted

as a

nat

ural

pla

nt c

omm

unity

for I

daho

, but

no

desc

riptio

n gi

ven

thus

no

asse

ssm

ent o

f sim

ilarit

y co

uld

be

done

.

Sa

lix e

xigu

a / R

osa

woo

dsii

Seas

onal

ly fl

oode

d co

ld-d

ecid

uous

Sh

rubl

and

(Rus

t 199

7)

? Li

sted

as a

nat

ural

pla

nt c

omm

unity

for I

daho

, but

no

desc

riptio

n gi

ven

thus

no

asse

ssm

ent o

f sim

ilarit

y co

uld

be

done

.

Sa

lix e

xigu

a / B

arre

n Sh

rubl

and

(MN

HP

2002

) ?

List

ed a

s a n

atur

al p

lant

com

mun

ity fo

r Mon

tana

, but

no

desc

riptio

n gi

ven

thus

no

asse

ssm

ent o

f sim

ilarit

y co

uld

be

done

.

Sa

lix e

xigu

a / M

esic

Gra

min

oid

Shru

blan

d (M

NH

P 20

02)

? Li

sted

as a

nat

ural

pla

nt c

omm

unity

for M

onta

na, b

ut n

o de

scrip

tion

give

n th

us n

o as

sess

men

t of s

imila

rity

coul

d be

do

ne.

Salix

exi

gua

Tem

pora

rily

Floo

ded

Shru

blan

d (M

NH

P 20

02)

? Li

sted

as a

nat

ural

pla

nt c

omm

unity

for M

onta

na, b

ut n

o de

scrip

tion

give

n th

us n

o as

sess

men

t of s

imila

rity

coul

d be

do

ne.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

1

3

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Her

bace

ous

Veg

etat

ion

Gly

cyrr

hiza

lepi

dota

/ C

alam

ovilf

a lo

ngifo

lia

Gly

cyrr

hiza

lepi

dota

Her

bace

ous

Veg

etat

ion

(MN

HP

2002

) ?

List

ed a

s S?

for M

onta

na. N

o de

scrip

tion

prov

ided

thus

no

asse

ssm

ent o

f sim

ilarit

y co

uld

be d

one.

H

erba

ceou

s V

eget

atio

n G

lycy

rrhi

za le

pido

ta –

Ar

tem

isia

spp.

/ St

ipa

com

ata

Stip

a co

mat

a A

ssoc

iatio

n (L

oom

an

1980

) 3

Foun

d to

be

com

mon

(with

Bou

telo

ua g

raci

lis) o

n dr

y pr

airie

. C

over

of B

oute

loua

gra

cilis

incr

ease

s, gr

adua

lly re

plac

ing

Stip

a co

mat

a as

gra

zing

incr

ease

s. A

var

iatio

n of

the

com

mun

ity in

clud

es C

alam

ovilf

a lo

ngifo

lia a

nd o

ccur

red

on

sand

y lo

am o

r loa

my

sand

soils

. Ver

y di

ffer

ent s

peci

es

com

posi

tion

thou

gh o

ccur

s on

coar

se te

xtur

ed so

ils.

Stip

a co

mat

a –

Arte

mis

ia fr

igid

a (H

ulet

t et a

l. 19

66)

2 D

omin

ant c

omm

unity

in G

reat

San

d H

ills (

Sask

.) on

stab

ilize

d du

nes.

Cal

amov

ilfa

long

ifolia

is p

rese

nt in

repo

rted

com

mun

ity. S

peci

es c

ompo

sitio

n va

ries s

omew

hat,

thou

gh s

ite

cond

ition

s are

qui

te si

mila

r. N

o m

entio

n of

wild

lico

rice.

G

lycy

rrhi

za le

pido

ta H

erba

ceou

s V

eget

atio

n (M

NH

P 20

02)

? Li

sted

as S

? fo

r Mon

tana

. No

desc

riptio

n pr

ovid

ed th

us n

o as

sess

men

t of s

imila

rity

coul

d be

don

e.

Her

bace

ous

Veg

etat

ion

Rum

ex v

enos

us

Rum

ex v

enos

us A

llian

ce (L

oom

an

1980

) 1

May

be

dom

inan

t on

high

ly m

obile

dun

es/ d

urin

g ea

rly st

ages

of

dev

elop

men

t. V

ery

limite

d de

scrip

tion,

alth

ough

dom

inan

t sp

ecie

s coi

ncid

es, a

nd c

omm

unity

foun

d in

Pak

owki

was

on

activ

e sa

nd d

une

area

s.

A

ctiv

e Sa

nd D

une

Com

plex

(Epp

and

To

wnl

ey-S

mith

198

0)

3 Ru

mex

ven

osus

not

ed a

s occ

urrin

g on

act

ive

sand

dun

e co

mpl

exes

, typ

ical

ly to

war

ds th

e ed

ge o

f the

def

latio

n zo

ne

and

on si

des o

f dun

es. N

o Ru

mex

ven

osus

com

mun

ity ty

pe

note

d ho

wev

er. O

ccur

s und

er si

mila

r con

ditio

ns, b

ut a

utho

rs

did

not d

escr

ibe

this

par

ticul

ar c

omm

unity

. H

erba

ceou

s V

eget

atio

n O

ryzo

psis

hym

enoi

des –

Sp

orob

olus

cry

ptan

drus

O

ryzo

psis

hym

enoi

des O

rder

(Loo

man

19

80)

3 R

epor

ted

as a

n or

der w

ithin

the

Cal

amov

ilfet

ea c

lass

. Ver

y lim

ited

desc

riptio

n, th

ough

not

ed to

occ

ur o

n co

arse

text

ured

so

ils.

Psor

alea

lanc

eola

ta –

Ory

zops

is

hym

enoi

des (

Hul

ett e

t al.

1966

) 2

Dom

inan

t com

mun

ity in

Gre

at S

and

Hill

s (Sa

sk.)

on a

ctiv

e sa

nd d

une

com

plex

es. D

omin

ant g

rass

sim

ilar t

o th

at fo

und

at

Pako

wki

San

dhill

s, al

thou

gh P

sora

lea

lanc

eola

ta w

as n

ot

foun

d in

ass

ocia

tion.

Site

con

ditio

ns v

ery

sim

ilar.

Psor

alea

lanc

eola

ta –

Ory

zops

is

hym

enoi

des (

Epp

and

Tow

nley

-Sm

ith

1980

)

2 Fo

rmed

a sp

arse

cov

er lo

cate

d on

edg

e of

def

latio

n zo

ne a

way

fr

om d

une.

Veg

etat

ive

cove

r fou

nd to

incr

ease

as d

ista

nce

from

de

flatio

n zo

ne in

crea

ses.

Dom

inan

t gra

ss si

mila

r to

that

foun

d at

Pak

owki

San

dhill

s, al

thou

gh P

sora

lea

lanc

eola

ta w

as n

ot

foun

d in

ass

ocia

tion.

Site

con

ditio

ns v

ery

sim

ilar.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

1

4

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Her

bace

ous

Veg

etat

ion

Ory

zops

is h

ymen

oide

s –

Spor

obol

us c

rypt

andr

us

(con

t.)

Ory

zops

is h

ymen

oide

s – P

sora

lidiu

m

lanc

eola

tum

(Hei

del e

t al.

2000

) 2

In M

onta

na, f

ound

to b

e re

stric

ted

to sl

opes

and

cre

sts o

f san

d du

nes r

ecen

tly d

istu

rbed

by

soil

eros

ion.

San

d dr

opse

ed w

as

also

pre

sent

, ofte

n fo

rmin

g up

to 1

0% c

over

. Fou

nd in

blo

w-

outs

and

is d

riest

and

ear

liest

stag

e of

succ

essi

on (M

edic

ine

Lake

San

dhill

s, M

onta

na).

Dom

inan

t gra

ss si

mila

r to

that

fo

und

at P

akow

ki S

andh

ills,

alth

ough

Pso

rale

a la

nceo

lata

was

no

t fou

nd in

ass

ocia

tion.

Site

con

ditio

ns v

ery

sim

ilar.

Ac

hnat

heru

m h

ymen

oide

sHer

bace

ous

Alli

ance

(Nat

ures

erve

200

2)

2 St

ands

of t

his a

llian

ce o

ccur

red

in tw

o di

stin

ctiv

ely

diff

eren

t ha

bita

ts (s

andy

are

as a

nd sh

ale

barr

ens)

in d

iffer

ent g

eogr

aphi

c ar

eas.

Sand

y ar

eas i

nclu

ded

'blo

wou

ts' i

n th

e G

reat

Pla

ins a

nd

in a

rid a

nd se

mi-a

rid d

une

syst

ems i

n th

e C

hihu

ahua

n D

eser

t, Sa

n Lu

is V

alle

y, C

olor

ado

Plat

eau

and

Gre

at B

asin

. Sub

stra

tes

are

sand

or s

hale

. Thi

s alli

ance

was

cha

ract

eriz

ed b

y a

spar

se to

m

oder

atel

y de

nse

herb

aceo

us la

yer t

hat i

s dom

inat

ed b

y Ac

hnat

heru

m h

ymen

oide

s (=

Ory

zops

is h

ymen

oide

s).

Dom

inan

t gra

ss th

e sa

me,

thou

gh n

o m

entio

n of

sand

dro

psee

d.

Sim

ilar s

ite c

ondi

tions

, exc

ludi

ng sh

ale

barr

ens.

Achn

athe

rum

hym

enoi

des -

Ps

oral

idiu

m la

nceo

latu

m H

erba

ceou

s V

eget

atio

n (N

atur

eser

ve 2

002)

? N

o de

scrip

tion

give

n th

us n

o as

sess

men

t of s

imila

rity

coul

d be

m

ade.

Ory

zops

is h

ymen

oide

s – P

sora

lidiu

m

lanc

eola

tum

Her

bace

ous v

eget

atio

n (M

NH

P 20

02)

? N

o de

scrip

tion

give

n th

us n

o as

sess

men

t of s

imila

rity

coul

d be

m

ade.

Cal

amov

ilfa

long

ifolia

- Ac

hnat

heru

m

hym

enoi

des H

erba

ceou

s Veg

etat

ion

(Nat

ures

erve

200

2)

? N

o de

scrip

tion

give

n th

us n

o as

sess

men

t of s

imila

rity

coul

d be

m

ade.

Her

bace

ous

Veg

etat

ion

Stip

a co

mat

a –

Ory

zops

is

hym

enoi

des

Stip

a co

mat

a A

ssoc

iatio

n (L

oom

an

1980

) 3

Foun

d to

be

com

mon

(with

Bou

telo

ua g

raci

lis) o

n dr

y pr

airie

. C

over

of B

oute

loua

gra

cilis

incr

ease

s, gr

adua

lly re

plac

ing

Stip

a co

mat

a as

gra

zing

incr

ease

s. O

ccur

red

on sa

ndy

loam

or

loam

y sa

nd so

ils. S

ite c

ondi

tions

sim

ilar i

n th

at it

occ

urre

d on

co

arse

r tex

ture

d sa

ndy

soils

, alth

ough

not

eol

ian

parti

cula

rily.

Fl

oris

tic c

ompo

sitio

n qu

ite d

iffer

ent.

Psor

alea

lanc

eola

ta -

Stip

a co

mat

a (H

ulet

t et a

l. 19

66)

3 D

omin

ant c

omm

unity

in D

undu

rn S

and

Hill

s (Sa

sk.)

on

stab

ilize

d du

nes.

Site

con

ditio

ns w

ould

be

quite

sim

ilar,

but n

o Ps

oral

ea la

nceo

lata

foun

d in

Pak

owki

com

mun

ities

.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

1

5

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Her

bace

ous

Veg

etat

ion

Stip

a co

mat

a –

Ory

zops

is

hym

enoi

des (

cont

.) Ps

oral

ea la

nceo

lata

– O

ryzo

psis

hy

men

oide

s (Ep

p an

d To

wnl

ey-S

mith

19

80)

3 Fo

rms a

spar

se c

over

loca

ted

on e

dge

of d

efla

tion

zone

aw

ay

from

dun

e. V

eget

ativ

e co

ver f

ound

to in

crea

se a

s dis

tanc

e fr

om

defla

tion

zone

incr

ease

s. Si

te c

ondi

tions

wou

ld b

e qu

ite

sim

ilar,

but n

o Ps

oral

ea la

nceo

lata

foun

d in

Pak

owki

co

mm

uniti

es.

Hes

pero

stip

a co

mat

a - A

chna

ther

um

hym

enoi

des H

erba

ceou

s Veg

etat

ion

(Nat

ures

erve

200

2)

2 Th

is g

rass

type

has

bee

n de

scrib

ed fr

om th

e G

reat

Div

ide

Bas

in in

sout

h-ce

ntra

l Wyo

min

g. H

espe

rost

ipa

com

ata

and

Achn

athe

rum

hym

enoi

des c

odom

inat

edth

e ve

geta

tion

and

Pasc

opyr

um sm

ithii

was

secc

ndar

y sp

ecie

s. Sc

atte

red

shru

bs

pres

ent,

prim

arily

Art

emis

ia tr

iden

tata

ssp.

wyo

min

gens

is. T

his

type

app

aren

tly h

as n

ot b

een

desc

ribed

out

side

the

Gre

at

Div

ide

Bas

in o

f sou

th-c

entra

l Wyo

min

g. O

ther

bas

ins i

n so

uth-

cent

ral a

nd so

uthw

este

rn W

yom

ing

and

the

north

wes

tern

qu

arte

r of C

olor

ado

are

sim

ilar i

n cl

imat

e an

d ge

olog

y an

d th

is

asso

ciat

ion

may

wel

l ext

end

over

a w

ide

area

of t

he tw

o st

ates

. Sp

ecie

s com

posi

tion

quite

sim

ilar,

thou

gh w

ith so

me

varia

tion.

N

o de

scrip

tion

of si

te c

ondi

tions

how

ever

.

Hes

pero

stip

a co

mat

aB

unch

H

erba

ceou

s Alli

ance

(Nat

ures

erve

20

02)

3 Th

is g

rass

land

alli

ance

was

foun

d on

sand

y so

ils in

the

inte

rmou

ntai

n st

eppe

, Wyo

min

g B

asin

, Col

orad

o Pl

atea

u,

Gre

at B

asin

and

Col

umbi

a Pl

atea

u. S

tand

s typ

ical

ly o

ccur

red

on u

plan

d si

tes w

ith c

oars

e-te

xtur

ed so

ils su

ch a

s san

dsto

ne

outc

rop

ridge

s in

the

plai

ns, d

ry-s

andy

site

s in

the

Col

umbi

a B

asin

and

on

diss

ecte

d al

luvi

al fa

ns b

elow

sand

ston

e pl

atea

us,

but n

ot d

unes

. Not

ed to

occ

ur o

n co

arse

text

ured

soils

. H

owev

er a

utho

rs st

ate

that

com

mun

ity d

oes n

ot o

ccur

on

sand

du

nes,

thus

qui

te d

iffer

ent f

rom

type

foun

d at

Pak

owki

.

St

ipa

com

ata

/ Pso

ralid

ium

la

nceo

latu

m H

erba

ceou

s Veg

etat

ion

(Hei

del e

t al.

2000

)

2 Fo

und

in M

edic

ine

Lake

sand

hills

. Res

trict

ed to

win

d-bl

own

sand

dep

osits

with

und

evel

oped

soils

and

is fo

und

on c

hopp

y du

nes t

o ro

lling

pla

ins.

Was

thou

ght t

o be

a se

ral s

tage

bet

wee

n O

ryzo

psis

hym

enoi

des /

Pso

ralid

ium

lanc

eola

tum

and

Pa

scop

yrum

smith

ii - S

tipa

com

ata

asso

ciat

ion.

Gra

ss c

over

w

as 2

0-40

% a

nd m

ost w

as S

tipa

com

ata.

Occ

urre

d on

st

abili

zed

to p

artia

lly st

abili

zed

sand

dun

es. S

ite c

ondi

tions

qu

ite si

mila

r, bu

t no

Psor

alea

lanc

eola

ta fo

und

in P

akow

ki

com

mun

ities

.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

1

6

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Her

bace

ous

Veg

etat

ion

Stip

a co

mat

a –

Ory

zops

is

hym

enoi

des (

cont

.) O

ryzo

psis

hym

enoi

des –

Pso

ralid

ium

la

nceo

latu

m H

erba

ceou

s veg

etat

ion

(MN

HP

2002

)

? N

o de

scrip

tion

give

n th

us n

o si

mila

rity

asse

ssm

ent c

ould

be

mad

e.

Her

bace

ous

Veg

etat

ion

Arte

mis

ia sp

p. /

Stip

a co

mat

a –

Cal

amov

ilfa

long

ifolia

Stip

a co

mat

a A

ssoc

iatio

n (L

oom

an

1980

) 3

Foun

d to

be

com

mon

on

dry

prai

rie. C

over

of B

oute

loua

gr

acili

s inc

reas

ed, g

radu

ally

repl

acin

g St

ipa

com

ata

as g

razi

ng

incr

ease

d. A

var

iatio

n of

the

com

mun

ity in

clud

es C

alam

ovilf

a lo

ngifo

lia a

nd o

ccur

red

on sa

ndy

loam

or l

oam

y sa

nd so

ils.

Som

ewha

t sim

ilar s

peci

es c

ompo

sitio

n, a

nd a

lso

occu

rrin

g on

m

ore

coar

se te

xtur

ed so

ils. S

peci

es c

ompo

sitio

n co

uld

be q

uite

va

riabl

e ho

wev

er.

Her

bace

ous

Veg

etat

ion

St

ipa

com

ata

– Ar

tem

isia

frig

ida

(Hul

ett e

t al.

1966

) 1

Dom

inan

t com

mun

ity in

Gre

at S

and

Hill

s (Sa

sk.)

on st

abili

zed

dune

s. C

alam

ovilf

a lo

ngifo

lia is

pre

sent

in re

porte

d co

mm

unity

. Virt

ually

iden

tical

site

con

ditio

ns, a

nd fl

oris

tic

com

posi

tion.

H

erba

ceou

s V

eget

atio

n St

ipa

com

ata

– C

yper

us

schw

eini

tzii

– C

alam

ovilf

a lo

ngifo

lia

Stip

a co

mat

a A

ssoc

iatio

n (L

oom

an

1980

) 2

Foun

d to

be

com

mon

(with

Bou

telo

ua g

raci

lis) o

n dr

y pr

airie

. C

over

of B

oute

loua

gra

cilis

incr

ease

d, g

radu

ally

repl

acin

g St

ipa

com

ata

as g

razi

ng in

crea

sed.

A v

aria

tion

of th

e co

mm

unity

incl

udes

Cal

amov

ilfa

long

ifolia

and

occ

urre

d on

sa

ndy

loam

or l

oam

y sa

nd so

ils. S

omew

hat s

imila

r spe

cies

co

mpo

sitio

n, a

nd a

lso

occu

rrin

g on

mor

e co

arse

text

ured

soils

. Sp

ecie

s com

posi

tion

mor

e va

riabl

e ho

wev

er a

t Pak

owki

Sa

ndhi

lls.

Stip

a co

mat

a –

Arte

mis

ia fr

igid

a (H

ulet

t et a

l. 19

66)

2 D

omin

ant c

omm

unity

in G

reat

San

d H

ills (

Sask

.) on

stab

ilize

d du

nes.

Cal

amov

ilfa

long

ifolia

is p

rese

nt in

repo

rted

com

mun

ity. V

irtua

lly id

entic

al si

te c

ondi

tions

, and

sim

ilar

floris

tic c

ompo

sitio

n.

Psor

alea

lanc

eola

ta -

Stip

a co

mat

a (H

ulet

t et a

l. 19

66)

3 D

omin

ant c

omm

unity

in D

undu

rn S

and

Hill

s (Sa

sk.)

on

stab

ilize

d du

nes.

Cal

amov

ilfa

long

ifolia

is p

rese

nt in

repo

rted

com

mun

ity. S

ite c

ondi

tions

qui

te si

mila

r, bu

t no

Psor

alea

la

nceo

lata

foun

d in

Pak

owki

com

mun

ities

.

St

ipa

com

ata

– C

alam

ovilf

a lo

ngifo

lia

– Ag

ropy

ron

spp.

(Hul

ett e

t al.

1966

) 1

Dom

inan

t com

mun

ity in

Dun

durn

San

d H

ills (

Sask

) in

dune

de

pres

sion

s and

app

ears

to b

e in

term

edia

te b

etw

een

stab

ilize

d bl

owou

ts a

nd st

abili

zed

dune

s. V

irtua

lly id

entic

al si

te

cond

ition

s, an

d si

mila

r flo

ristic

com

posi

tion.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

1

7

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Her

bace

ous

Veg

etat

ion

Stip

a co

mat

a –

Cyp

erus

sc

hwei

nitz

ii –

Cal

amov

ilfa

long

ifolia

(con

t.)

Cal

amov

ilfa

long

ifolia

- H

espe

rost

ipa

com

ata

Her

bace

ous V

eget

atio

n (N

atur

eser

ve 2

002)

2 Th

is p

rairi

e sa

ndre

ed g

rass

land

com

mun

ity ty

pe o

ccur

red

in

the

cent

ral a

nd n

orth

ern

Gre

at P

lain

s reg

ion

of th

e U

nite

d St

ates

. Sta

nds o

ccur

on

stab

ilize

d sa

nd d

unes

, as w

ell a

s in

inte

rdun

al v

alle

ys, c

ollu

vial

sand

s and

, les

s com

mon

ly, s

ilty

terr

aces

of i

nter

mitt

ent s

tream

s. So

ils w

ere

med

ium

to fi

ne

sand

s for

med

eith

er fr

om e

olia

n or

col

luvi

al p

roce

sses

. The

ve

geta

tion

had

an o

pen

cano

py, d

omin

ated

by

mid

to ta

ll gr

asse

s. C

alam

ovilf

a lo

ngifo

lia a

nd H

espe

rost

ipa

com

ata

(=

Stip

a co

mat

a) w

ere

the

mos

t con

spic

uous

and

dom

inan

t gr

asse

s. V

irtua

lly id

entic

al si

te c

ondi

tions

, and

sim

ilar f

loris

tic

com

posi

tion

alth

ough

no

men

tion

of C

yper

us sc

hwei

nitz

ii.

Cal

amov

ilfa

long

ifolia

- H

espe

rost

ipa

com

ata

Gra

ssla

nd (J

ones

199

8a)

3 Fo

und

on sa

ndy

soils

at a

n in

term

edia

te h

eigh

t abo

ve th

e riv

er

chan

nel (

Wyo

min

g). M

ajor

spec

ies a

re C

alam

ovilf

a lo

ngifo

lia,

Stip

a co

mat

a an

d Ps

oral

ea la

nceo

lata

. Site

con

ditio

ns

som

ewha

t sim

ilar,

but f

ound

dom

inan

tly a

long

fluv

ial

chan

nels

. No

Psor

alea

lanc

eola

ta fo

und

in P

akow

ki

com

mun

ities

.

C

alam

ovilf

a lo

ngifo

lia –

Hes

pero

stip

a co

mat

a G

rass

land

(Jon

es 1

998b

) 3

Foun

d on

sand

y so

ils a

t an

inte

rmed

iate

hei

ght a

bove

the

river

ch

anne

l (W

yom

ing)

. Maj

or sp

ecie

s wer

e C

alam

ovilf

a lo

ngifo

lia, S

tipa

com

ata

and

Psor

alea

lanc

eola

ta. A

lso

foun

d on

sand

dun

es a

nd h

ighe

r flu

vial

surf

aces

with

sand

y so

ils.

Was

a m

ajor

com

mun

ity ty

pe in

the

area

. Site

con

ditio

ns

som

ewha

t sim

ilar,

but f

ound

dom

inan

tly a

long

fluv

ial

chan

nels

. No

Psor

alea

lanc

eola

ta fo

und

in P

akow

ki

com

mun

ities

.

C

alam

ovilf

a lo

ngifo

lia –

Hes

pero

stip

a co

mat

a H

erba

ceou

s Veg

etat

ion

(Fab

er-L

ange

ndoe

n , D

. edi

tor 2

001)

2 V

eget

atio

n ha

d op

en c

anop

y do

min

ated

by

Cal

amov

ilfa

long

ifolia

. Sta

nds o

ccur

red

on st

abili

zed

sand

dun

es a

s wel

l as

in in

terd

unal

val

leys

or d

raw

s, co

lluvi

al sa

nds a

nd le

ss

com

mon

ly o

n si

lty te

rrac

es o

f int

erm

itten

t stre

ams.

Soils

wer

e m

ediu

m to

fine

sand

s for

med

from

eith

er e

olia

n or

col

luvi

al

proc

esse

s. N

oted

occ

urrin

g in

cen

tral a

nd n

orth

ern

Gre

at

Plai

ns, r

angi

ng fr

om C

olor

ado

to N

ebra

ska

and

north

to

Wyo

min

g an

d So

uth

Dak

ota.

Site

con

ditio

ns v

ery

sim

ilar a

nd

floris

tic c

ompo

sitio

n al

so q

uite

sim

ilar.

No

men

tion

of C

yper

us

sche

wei

nitz

ii ho

wev

er.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

1

8

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Her

bace

ous

Veg

etat

ion

Stip

a co

mat

a –

Cyp

erus

sc

hwei

nitz

ii –

Cal

amov

ilfa

long

ifolia

(con

t.)

Cal

amov

ilfa

long

ifolia

– H

espe

rost

ipa

com

ata

Her

bace

ous V

eget

atio

n (C

oope

r et a

l. 20

01)

2 O

ccur

red

mos

t abu

ndan

tly w

here

sand

y su

bstra

tes d

omin

ant,

on st

abili

zed

dune

s, in

terd

unal

swal

es a

nd c

ollu

vial

sand

s. W

as

foun

d in

Roc

k C

reek

Can

yon

and

a fe

w sa

ndy

outc

rops

in

Bitt

er C

reek

Bad

land

s are

a, M

onta

na. W

as h

ighl

y re

stric

ted

in

area

, occ

urrin

g on

mai

nly

collu

vial

sand

s. Si

te c

ondi

tions

ver

y si

mila

r and

flor

istic

com

posi

tion

also

qui

te si

mila

r. N

o m

entio

n of

Cyp

erus

sche

wei

nitz

ii ho

wev

er.

Cal

amov

ilfa

long

ifolia

– S

tipa

com

ata

Her

bace

ous V

eget

atio

n (H

eide

l et a

l. 20

00)

2 Fo

und

at M

edic

ine

Lake

San

dhill

s, M

onta

na, a

s a m

inor

type

. D

id n

ot a

ppea

r to

be a

wid

e-sp

read

com

mun

ity, o

ccur

ring

in

smal

l pat

ches

on

low

ridg

es a

nd in

mos

aic

patte

rns o

n ge

ntle

pl

ains

of M

edic

ine

Lake

. Site

con

ditio

ns v

ery

sim

ilar a

nd

floris

tic c

ompo

sitio

n al

so q

uite

sim

ilar.

No

men

tion

of C

yper

us

sche

wei

nitz

ii ho

wev

er.

Her

bace

ous

Veg

etat

ion

Spor

obol

us c

rypt

andr

us –

C

alam

ovilf

a lo

ngifo

lia –

O

ryzo

psis

hym

enoi

des

Cal

amov

ilfa

long

ifolia

CLA

SS

(Loo

man

198

0)

2 Sa

nd g

rass

repo

rted

to b

e do

min

ant i

n w

ell d

evel

oped

sand

hill

prai

rie. O

ther

cha

ract

eris

tic sp

ecie

s inc

lude

d El

ymus

ca

nade

nsis

, Hel

iant

hus c

oupl

andi

i and

Spo

robo

lus

cryp

tand

rus.

Flor

istic

com

posi

tion

som

ewha

t sim

ilar,

thou

gh

with

som

e va

riatio

n. S

ite c

ondi

tions

not

des

crib

ed in

det

ail,

thou

gh a

re e

xpec

ted

to b

e qu

ite si

mila

r.

C

arex

pen

nsyl

vani

ca –

Spo

robo

lus

cryp

tand

rus –

Cyp

erus

schw

entz

eii –

C

alam

ovilf

a lo

ngifo

lia o

n ac

tive

sand

(T

horp

e an

d G

odw

in 1

993)

3 Fo

und

on sp

arse

ly v

eget

ated

, act

ive

east

/wes

t orie

nted

sand

du

nes t

hat w

ere

rapi

dly

drai

ned.

Soi

ls w

ere

coar

se-te

xtur

ed a

nd

had

little

to n

o or

gani

c m

atte

r to

reta

in m

oist

ure.

Site

co

nditi

ons v

ery

sim

ilar,

alm

ost i

dent

ical

. How

ever

flor

istic

co

mpo

sitio

n m

uch

mor

e va

riabl

e th

an th

at fo

und

at P

akow

ki

Sand

hills

.

Sp

orob

olus

cry

ptan

drus

– P

oa

secu

nda

Med

ium

-tall

bunc

h te

mpe

rate

or

sub-

pola

r gra

ssla

nd (R

ust 1

997)

? Li

sted

as c

omm

unity

type

for I

daho

but

no

desc

riptio

n gi

ven.

N

o si

mila

rity

asse

ssm

ent c

ould

be

mad

e.

Spor

obol

us c

rypt

andr

us m

ediu

m-ta

ll te

mpe

rate

or s

ubpo

lar g

rass

land

with

a

need

le-le

aved

or m

icro

phyl

lous

ev

ergr

een

shru

b la

yer (

Rus

t 199

7)

? Li

sted

as c

omm

unity

type

for I

daho

but

no

desc

riptio

n gi

ven.

N

o si

mila

rity

asse

ssm

ent c

ould

be

mad

e.

Het

erot

heca

vill

osa

/ Spo

robo

lus

cryp

tand

rus L

ow te

mpe

rate

or

subp

olar

forb

veg

etat

ion

(Rus

t 199

7)

? Li

sted

as c

omm

unity

type

for I

daho

but

no

desc

riptio

n gi

ven.

N

o si

mila

rity

asse

ssm

ent c

ould

be

mad

e.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

1

9

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Her

bace

ous

Veg

etat

ion

Spor

obol

us c

rypt

andr

us –

C

alam

ovilf

a lo

ngifo

lia –

O

ryzo

psis

hym

enoi

des

Spor

obol

us c

rypt

andr

us S

hrub

H

erba

ceou

s Veg

etat

ion

(MN

HP

2002

) ?

List

ed a

s G2/

S2 fo

r Mon

tana

but

no

desc

riptio

n gi

ven.

No

sim

ilarit

y as

sess

men

t cou

ld b

e m

ade

Spor

obol

us c

rypt

andr

usH

erba

ceou

s A

llian

ce (N

atur

eser

ve 2

002)

3 Th

is g

rass

land

alli

ance

was

foun

d in

the

low

er S

alm

on a

nd

Snak

e riv

er c

anyo

ns o

f Ida

ho, O

rego

n an

d W

ashi

ngto

n, th

e C

olum

bia

Riv

er in

cen

tral W

ashi

ngto

n an

d th

e G

reen

and

V

irgin

rive

rs in

Uta

h. S

tand

s occ

urre

d on

rive

r ter

race

s, fo

otsl

opes

of b

ench

es a

nd a

lluvi

al fa

ns. T

he e

leva

tion

rang

ed

from

240

-146

0 m

. Site

s are

flat

to g

ently

slop

ing

(to 3

0%) a

nd

occu

rred

on

all a

spec

ts. S

oils

wer

e m

oder

atel

y de

ep a

nd

deriv

ed fr

om lo

ess a

nd a

lluvi

um-c

ollu

vium

. Sur

face

soil

text

ure

varie

d fr

om sa

ndy

loam

to si

lt lo

am. L

imite

d flo

ristic

de

scrip

tion

prov

ided

, alth

ough

site

con

ditio

ns q

uite

sim

ilar

exce

pt fo

r met

hod

of d

epos

ition

.

Spor

obol

us c

rypt

andr

usSh

rub

Her

bace

ous A

llian

ce (N

atur

eser

ve

2002

)

3 G

rass

land

s in

this

alli

ance

wer

e de

scrib

ed fr

om M

onta

na,

Idah

o an

d N

ew M

exic

o. In

New

Mex

ico,

the

allia

nce

occu

rred

in

the

north

wes

tern

par

t of t

he st

ate

on a

lluvi

al fl

ats a

t an

elev

atio

n of

app

roxi

mat

ely

2140

m. C

limat

e w

as se

mi-a

rid

with

mos

t of t

he h

ighl

y va

riabl

e an

nual

pre

cipi

tatio

n fa

lling

du

ring

the

sum

mer

as h

igh-

inte

nsity

con

vect

iona

l sto

rms.

Site

s w

ere

near

ly le

vel.

Soils

are

cal

care

ous,

loam

y an

d sh

allo

w (l

ess

than

25

cm d

eep)

. Lim

ited

floris

tic d

escr

iptio

n pr

ovid

ed a

nd

site

and

clim

atic

con

ditio

ns q

uite

diff

eren

t. H

erba

ceou

s V

eget

atio

n Sp

orob

olus

cry

ptan

drus

Cal

amov

ilfa

long

ifolia

Ory

zops

is h

ymen

oide

s

Spor

obol

us c

rypt

andr

us -

Poa

secu

nda

Her

bace

ous V

eget

atio

n (N

atur

eser

ve 2

002)

3 Th

is p

lant

ass

ocia

tion

was

des

crib

ed fo

r the

Col

umbi

a B

asin

an

d lo

wer

Sna

ke R

iver

, whe

re it

occ

urre

d on

gen

tle, l

ower

sl

ope

and

river

terr

ace

posi

tions

in th

e va

lleys

of t

he S

nake

and

C

lear

wat

er ri

vers

. Sta

nds w

ere

dom

inat

ed b

y Sp

orob

olus

cr

ypta

ndru

s. Po

a se

cund

a w

as c

omm

on b

ut v

arie

d in

ab

unda

nce.

Ari

stid

a pu

rpur

ea v

ar. l

ongi

seta

(= A

rist

ida

long

iset

a) a

nd H

espe

rost

ipa

com

ata

(= S

tipa

com

ata)

wer

e fr

eque

ntly

pre

sent

in lo

w a

bund

ance

. Diff

eren

ces i

n si

te a

nd

floris

tic c

ompo

sitio

n th

an w

hat i

s fou

nd a

t Pak

owki

San

dhill

s.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

2

0

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Her

bace

ous

Veg

etat

ion

Arte

mis

ia c

ana

/ Stip

a co

mat

a Ro

sa w

oods

ii (A

rtem

isia

can

a /

Elae

agnu

s com

mut

ata)

(Cou

plan

d 19

50)

2 Fo

und

in u

ndul

atin

g to

gen

tly ro

lling

are

as b

etw

een

stab

ilize

d du

nes.

Wat

er ta

ble

typi

cally

with

in 8

to 1

2 fe

et o

f soi

l sur

face

in

thes

e lo

catio

ns. S

peci

es c

ompo

sitio

n m

ore

varia

ble

than

that

fo

und

at P

akow

ki S

andh

ills,

but s

ite c

ondi

tions

qui

te si

mila

r. D

epth

to w

ater

tabl

e no

t kno

wn

at P

akow

ki S

andh

ills.

Arte

mis

ia c

ana

/ Hes

pero

stip

a co

mat

a Sh

rub

Her

bace

ous V

eget

atio

n (N

atur

eser

ve 2

002)

1 Th

is sh

rub

prai

rie a

ssoc

iatio

n, w

hich

gen

eral

ly o

ccur

red

in

smal

l pat

ches

(les

s tha

n 1

hect

are)

, occ

urre

d in

the

north

wes

tern

Gre

at P

lain

s. In

Mon

tana

, it w

as fo

und

on

benc

hes t

o ge

ntly

incl

ined

slop

es (3

0% m

axim

um re

cord

ed) i

n th

e vi

cini

ty o

f bre

akla

nds.

Site

s occ

urre

d on

var

ious

par

ent

mat

eria

ls, b

ut m

ostly

wel

l-dra

ined

, ofte

n sa

ndy,

gla

cial

drif

t an

d sa

ndy

allu

vium

. Art

emis

ia c

ana

was

dom

inan

t shr

ub w

ith

cano

py c

over

ages

to 5

0%, b

ut a

vera

ging

aro

und

25%

, whi

ch

plac

ed it

on

the

cusp

of b

eing

a tr

ue sh

rub

type

. Virt

ually

id

entic

al si

te a

nd fl

oris

tic c

ompo

sitio

n.

Arte

mis

ia c

ana

/ Hes

pero

stip

a co

mat

a Sh

rub

Her

bace

ous V

eget

atio

n (F

aber

-La

ngen

doen

, D. e

dito

r 200

1)

1 Th

is sm

all p

atch

type

cur

rent

ly h

ad a

nar

row

geo

grap

hic

dist

ribut

ion,

thou

gh it

may

be

expe

cted

to o

ccur

in

Sask

atch

ewan

and

Nor

th D

akot

a. T

his t

ype's

aff

inity

for w

ell

drai

ned

benc

hes a

nd g

ently

incl

ined

land

form

s in

a pr

imar

ily

agric

ultu

ral l

ands

cape

put

s it a

t a m

oder

ate

risk

for a

gric

ultu

re

conv

ersi

on. F

ortu

nate

ly th

is la

ndfo

rm a

lso

occu

rred

in

brea

klan

d an

d ba

dlan

d en

viro

nmen

ts le

ss d

esira

ble

for

agric

ultu

re, t

hus l

esse

ning

the

chan

ces o

f thi

s unc

omm

on ty

pe

bein

g co

nver

ted

to a

gric

ultu

re. V

irtua

lly id

entic

al fl

oris

tic

com

posi

tion,

thou

gh so

mew

hat d

iffer

ent s

ite c

ondi

tions

.

Ar

tem

isia

can

a / H

espe

rost

ipa

com

ata

Shru

b H

erba

ceou

s Veg

etat

ion

(Coo

per

et a

l. 20

01)

1 In

Mon

tana

, was

foun

d on

ben

ches

to g

ently

incl

ined

slop

es

(30%

max

imum

reco

rded

) in

the

vici

nity

of b

reak

land

s. Si

tes

occu

rred

on

vario

us p

aren

t mat

eria

ls b

ut m

ostly

wel

l-dra

ined

, of

ten

sand

y gl

acia

l drif

t and

sand

y al

luvi

um. C

onsi

dere

d to

be

a m

inor

type

in th

e B

itter

Cre

ek /

Fren

chm

an C

reek

are

a in

M

onta

na, d

ue to

lim

ited

dist

ribut

ion

of c

oars

e te

xtur

ed

mat

eria

ls. V

irtua

lly id

entic

al fl

oris

tic c

ompo

sitio

n, th

ough

so

mew

hat d

iffer

ent s

ite c

ondi

tions

.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

2

1

Appe

ndix

5. C

orre

latio

n ta

ble

with

lite

ratu

re fr

om o

utsi

de A

lber

ta

Cla

ss

Com

mun

ity T

ype

Sim

ilar C

omm

uniti

es a

nd C

itatio

ns

Sim

ilarit

y R

atin

g C

omm

ents

Her

bace

ous

Veg

etat

ion

Arte

mis

ia c

ana

/ Stip

a co

mat

a (c

ont.)

Ar

tem

isia

can

a / S

tipa

com

ata

Shru

b H

erba

ceou

s Veg

etat

ion

(MN

HP

2002

) ?

List

ed a

s nat

ural

pla

nt c

omm

unity

for M

onta

na, b

ut n

o de

scrip

tion

give

n. R

ated

S3

for M

onta

na. N

o si

mila

rity

asse

ssm

ent c

ould

be

mad

e.

Geo

wes

t Env

ironm

enta

l Con

sulta

nts L

td.

2

2