Zooplankton community changes on the Canadian northwest ...

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Zooplankton community changes on the Canadian northwest Atlantic continental shelves during recent warm years Catherine L. Johnson 1 , Stéphane Plourde 2 , Pierre Pepin 3 , Emmanuel Devred 1 , David Brickman 1 , David Hebert 1 , Peter S. Galbraith 2 , Eugene Colbourne 3 PICES ECCWO18, 4 June 2018 Acknowledgements Benoit Casault, K. Alexandra Curtis, Atlantic Zone Monitoring Program teams and data management groups in the DFO Maritimes, Quebec, and Newfoundland regions, and captains and crew of survey vessels 1 Fisheries and Oceans Canada, Bedford Institute of Oceanography 2 Fisheries and Oceans Canada, Institut Maurice-Lamontagne 3 Fisheries and Oceans Canada, Northwest Atlantic Fisheries Centre

Transcript of Zooplankton community changes on the Canadian northwest ...

Page 1: Zooplankton community changes on the Canadian northwest ...

Zooplankton community changes on the Canadian northwest Atlantic continental shelves during recent warm years

Catherine L. Johnson1, Stéphane Plourde2, Pierre Pepin3, Emmanuel Devred1, David Brickman1, David Hebert1, Peter S. Galbraith2, Eugene Colbourne3

PICES ECCWO18, 4 June 2018

Acknowledgements Benoit Casault, K. Alexandra Curtis, Atlantic Zone Monitoring Program teams and data management groups in the DFO Maritimes, Quebec, and Newfoundland regions, and

captains and crew of survey vessels

1 Fisheries and Oceans Canada, Bedford Institute of Oceanography 2 Fisheries and Oceans Canada, Institut Maurice-Lamontagne

3 Fisheries and Oceans Canada, Northwest Atlantic Fisheries Centre

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Zooplankton community structure and change

Marine zooplankton community structure is an emergent property of interactions among • Upstream supply: circulation and species composition and abundance • Transport pathways • Vertical migration behavior • Time and space varying production, growth, and development • Time and space varying mortality

HL-7 Autumn 2017 BBL-7 Autumn 2015 LL-2 Spring 2017

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Presentation Objectives

Characterize dominant patterns in the Canadian NW Atlantic shelf zooplankton community and response to recent environmental changes

Canadian NW Atlantic shelf zooplankton community

▪ 1999-2011 copepod community composition ▪ 1999-2011 zooplankton community spatial pattern ▪ Temperature trends ▪ Changes in dominant taxa and groups in the 2010s

Scotian Shelf region copepod community

▪ Changes in diversity ▪ Changes in rank abundance and biomass

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Atlantic Zone Monitoring Program Domain

BBL

TESL

LL HL SEGB

SI

FC

BB

TIDM

TSI TBB TASO

Sections sampled 2X / year since 1999 High frequency stations sampled 1-2X / month

HL-2

Vertical ring net • ¾ m diameter • 200 μm mesh • Towed from near-

bottom or 1000 m to surface

CTD and rosette • Temperature,

salinity, oxygen, nutrients, chlorophyll…

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Northwest Atlantic shelf system Annual range of surface temperature NW Atlantic circulation

Schematic circulation based on Fratantoni & MacCartney (2010) Deep-Sea Res. 57: 258-283; Hannah et al. (2001) J. Phys. Oceangr. 31: 591-615; Drinkwater & Gilbert (2004) J. NW Atl. Fish. Org. 34: 85-101.

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Rank abundance of NW Atlantic shelf copepods, 1999-2011

Copepods were divided into dominant, subdominant, uncommon, and rare taxa based on occurrence and relative abundance thresholds

Johnson, Pepin, Casault, Harvey (in prep.) NW Atlantic zooplankton atlas

• Dominants (3) are ubiquitous • Distributions of 12 subdominants

show habitat associations, e.g., -shallow banks -deep shelf water and latitudinal gradients

• Many of the 20 uncommon taxa are associated with marginal habitats: -slope water -nearshore -deep water

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Rank biomass of dominant and subdominant copepods plus large, uncommon species Paraeuchaeta norvegica,1999-2011

Copepod biomass estimated from published length and length-dry weight relationships

• Calanus species were biomass dominants

• P. norvegica was also in the top four copepods ranked by biomass

• Small-sized dominant copepods make up a small fraction of community biomass despite their high abundance

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Spatial zooplankton community pattern, 1999-2011

•The dominant mode of community spatial variation in both spring and fall is associated with depth – shallow and shelf community vs. deep-water and offshore species

• Influence of fall slope water intrusion is evident on the western Scotian Shelf

•The second mode of community spatial variation reflects latitudinal (fall) or along-shelf (spring) environmental gradients

Pepin, Johnson, Harvey, et al. (2015) A multivariate evaluation of environmental effects on zooplankton community structure in the western North Atlantic Progr. Oceanogr. 134:197-220 70 40 55 70 40 55

21.4%

15.3% 14.9%

23.1%

Principal component analysis of zooplankton community composition

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Standard anomalies (1981 - 2010 reference period) DFO (2017) Ocean conditions in the Atlantic Zone in 2016. CSAS Sci. Advis. Rep. 2017/031

1980 2016

Sea

Surf

ace

Tem

p.

N

S

Bott

om Te

mp.

N

S

Canadian northwest Atlantic temperature anomaly trends

Labrador Newfoundland

Shelves

Gulf of St. Lawrence

Scotian Shelf E. Gulf of Maine

Labrador Newfoundland

Shelves

Gulf of St. Lawrence

Scotian Shelf E. Gulf of Maine

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Abundance anomalies in dominant NW Atlantic taxa and groups

Pseudocalanus spp.

Copepods Calanus finmarchicus

Non-copepods

N

S

N

S

DFO (2017) Ocean conditions in the Atlantic Zone in 2016. CSAS Sci. Advis. Rep. 2017/031.

Labrador Newfoundland

Shelves

Gulf of St. Lawrence

Scotian Shelf Eastern Gulf of Maine

Year Year

Labrador Newfoundland

Shelves

Gulf of St. Lawrence

Scotian Shelf Eastern Gulf of Maine

1999-2010 reference period

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Central Scotian Shelf (Halifax-2) copepod richness and evenness

Richness and evenness metrics based on adult copepods

Metric p r2 Temperature (0-50 m) 0.0014 0.457 Bottom temperature <0.001 0.515 Stratification 0.012 0.319

Metric p r2 Temperature (0-50 m) <0.001 0.647 Bottom temperature <0.001 0.541 Stratification 0.057 0.196

Species Richness Evenness

Mean: 7.27

Mean: 0.652

Correlation with environmental metrics Correlation with environmental metrics

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Changes in Scotian Shelf copepod rank abundance (top 95%) between 1999-2010 and 2011-2017

• Abundance of dominant species has declined • Moderate changes in rank order in both seasons

1

2 3

4 5 6 9 8 7 10 13 14

New to top 95% 11 Clausocalanus 12 Metridia

1

2

3 4 5 6 7 8 11 9 10 15 12 14 13

Spring Fall

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1

2

3 4 5 6 9 8 7 12 14 11

Changes in Scotian Shelf copepod rank biomass (top 99%) between 1999-2010 and 2011-2017

New to top 99% 10 O. atlantica 13 Oithona

• Biomass of dominant species has declined • Calanus species retain top two ranks in both seasons

3 4 5 17 9 8 7 12 14 11

1

2 13 10

New to top 99% 6 Centropages 15 Oithona 16 Mecynocera clausi

Spring Fall

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Conclusions

• The Canadian NW Atlantic shelf copepod community exhibits relatively strong, recurring annual and spatial variability patterns

• Abundances of dominant species and groups have shown persistent, large scale changes on the NW Atlantic shelves since about 2010-2012

• On the Scotian Shelf in the 2010s, the copepod community shifted toward: - Lower abundance and biomass of dominant species, especially Calanus - Higher species richness and evenness - Moderate changes in rank abundance - Moderate changes in rank biomass

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Implications of recent warm conditions • Abundances of regional “immigrant” species are strongly related to shifts in

water mass contributions. -e.g. Arctic Calanus vs. warm-water offshore copepods on Scotian Shelf

• Calanus species responses are more complex – although a decline was observed, interactions of diapause timing and vertical migration with shelf circulation and spring bloom timing may mitigate impact of warming in some areas.

• Shifts in the developmental stage ratios of some small copepod species suggest changes in timing of seasonal production cycle.

• Community changes suggest a potential shift in energy pathways for primary production in recent warm years, with production possibly consumed by smaller copepods and greater transport to deep water.

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Thank you for your attention