12 ecosystems

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Announcements March 7, 2011 Exam 1 results are in! Please see your TA if you want to go over your exam In discussion this week: Global Climate Change Water Use vs. Distribution

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Transcript of 12 ecosystems

Page 1: 12 ecosystems

AnnouncementsMarch 7, 2011

Exam 1 results are in! Please see your TA if you

want to go over your exam

In discussion this week: Global Climate Change Water Use vs. Distribution

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Exam 1 distribution

Mean = 87

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Lecture Objectives:

1. Understand Succession2. Learn the characteristics of the

major ecosystems

Types of Ecosystems I & II

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Recurring Themes…Terrestrial vs. Aquatic

Type of ecosystem influenced by: rock/soil type temperature precipitation producers/consumers surrounding ecosystems time

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Community Properties Abundance -Total number of organisms in

a community.

Diversity - Number of different species, ecological niches, or genetic variation.As a general rule, diversity decreases when

moving from the equator to the poles

Don’t forget, its not only about the number of species but also the number of interactions…

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Succession - communities proceeding through predictable changes through time

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Succession

Outcome is a climax community- stable, long-lasting community

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Two types of succession

Primary - begins with total lack of organisms, bare mineral surface

bssv01.lancs.ac.uk/bs/research/ soilecol/linkgrd.htm

Succession following melting of the Muir Glacier

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Primary successionStarts with bare rock, sand, clay, etc.Colonized by pioneer community

First to colonize bare rock Mainly lichens = mutualistic

association of algae or bacteria and fungi

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Primary successionAcids produced by lichens, physical, chemical weathering break down rock

Dead organic matter and weathered rock create soil

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Primary succession Lichens eventually replaced by small, annual

plants Replaced by smaller perennial plants: herbs and

grasses Replaced by grasses, shrubs, shade intolerant

trees Climax forest composed of shade tolerant trees

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“Climax” community is not a preordained set of species

Rate of succession and kind of climax community determined by:

Type of initial substrate Climate

Rate of soil accumulationWater availabilityTemperature

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Secondary - begins with destruction or disturbance of existing ecosystem

Primary takes longer than secondary

http://content.lib.washington.edu/mtsthelens/

© Roger del Moral

Mount St. Helens1980 1996

Two types of succession

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Secondary successionMain difference from primary succession:

Results from disturbance to “climax” community

- Soil already formed

- Pool of species in soil or nearby that can quickly colonize

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Biomes - climax communities with wide geographical distributions

Terrestrial biomes primarily influenced by: Precipitation:

total amount per year seasonal distribution form (rain, snow)

Temperature: range of temperatures seasonal patterns

Other factors: soil type, wind, fire, etc.

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Precipitation and temperature influenced by latitude, longitude, and altitude

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% IB 105 students who have visited:

Tropical Forest: 26%Prairie or other grassland: 69%Desert: 39%

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Major Terrestrial Biomes

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Tundra Occurs at extreme northern latitudes, or high elevations (mountain tundra)

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Tundra Key characteristics

low precipitation (<35cm)

Permanently frozen soil layer = permafrost

Waterlogged soils common in summer

Low evaporation, permafrost

Short plants dominate Grasses, dwarf birch,

dwarf willow, lichens

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Desert Key characteristics

Very little water (<25 cm/year)High evaporationLarge daily temperature fluctuationsSpecies not very denseSpecies have adaptations to hot, dry

environment Plants – small leaves, store water, dormancy Animals – Night activity, conserve water

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Common myths about deserts:

•They are nothing but sand

Joshua Tree National Park, CA

Gobi Desert, Asia

Mohawk Dunes, AZ

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Common myths about deserts:

•Not much lives there

Burrowing animals, rodents, lizards, snakes

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Common misperceptions about deserts:

•They are always unbearably hot

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results from over grazing, intense agricultural use, erosion, water runoff, and over heating of soil.

Desertification: change from fertile land to desert.

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Boreal Forest Also called taiga,

northern coniferous forest

Occurs in southern Canada, northern Europe, much of Russia

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Boreal Forest Key characteristics

Moderate to low precipitation (25-100 cm)

Short, cool summer; Long harsh winters

Spruce and fir, dominant vegetation

Humid due to precipitation and low evaporation, but winter dry because precipitation is snow

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Temperate Deciduous Forest Occur in eastern half of U.S., south central

and eastern Canada, southern Africa, Europe, Asia

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Temperate Deciduous Forest Key characteristics

Moderate rainfall (75-100 cm), relatively evenly distributed

Warm summers and relatively mild winters

Trees dominant vegetation, type of tree varies geographically

In North America, dominant trees are maples, aspen, oaks, hickories, etc.

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Grasslands Occur in temperate

areas Also called prairies

or steppes

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Grasslands Key characteristics

Medium precipitation (25-75 cm)

Hot summers, cold to mild winters

Grasses dominant vegetation

Need fire to prevent invasion of trees, release nutrients

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Grasslands Key characteristics

Lots of grazing animals Wastes fertilize prairies,

grazing helps keep out trees

Most grassland has been converted to agriculture

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Savanna Occurs in Africa,

South America, Australia

Key characteristicsHigh rainfall (50-

150 cm), but unevenly distributed

Periods of high rainfall, followed by droughts

Temperature warm, relatively constant

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SavannaKey characteristics

Plants dominated by grasses and drought resistant trees

Dominant animals are grazers

Plant and animal reproduction timed around rainy season, when resources least limiting

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Mediterranean Shrublands Also known as

Chaparral. Receives 40-100 cm

annual precipitation.Wet, cool winters and hot,

dry summers. Typical of Mediterranean

coast and coastal southern California.

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Mediterranean Shrublands Vegetation dominated by woody shrubs

adapted to hot, dry summers. Fire is a common feature.

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Tropical Dry Forest

Annual precipitation ranges 50-200 cm.

Many exhibit monsoon climate. Rainfall highly

seasonal. Drought resistant

plants.

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Tropical Rainforest Occur along equator in Central and South

America, Africa, Southeast Asia, Caribbean and Pacific Islands

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Tropical Rainforest Key characteristics

Temperature warm and relatively constant

Very high rainfall (>200 cm/year)

Rapid growth, but nutrient poor soils

Multi-layered forests of emergent trees, canopy trees, understory trees, shade-tolerant plants, and epiphytes

Most diverse biome on earth

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