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Ecology

Chapter 50

AP Biology

What is ecology?

Ecology

Is the scientific study of the interactions between organisms and the environment

These interactions

Determine both the distribution of organisms and their abundance

 Where organisms are found and how many of them there are

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What is ecology?

Ecology

Both observational/descriptive and experimental

 Observing what’s there and seeing how it changes

 Rigorous - mathematical modeling of populations and ecosystems

Ecological time

Minute-to-minute interactions

Compare to evolutionary time

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Environmental factors

Abiotic factors

 non-living chemical & physical factors

 Temperature

 Light

 Water, including salinity

 Nutrients, including soil and rocks

 Dissolved oxygen!

Biotic factors

 living components

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Environmental Factors

Affect the distribution and abundance of organisms

Kangaroos/km 2

> 20

10 –20

5 –10

1 –5

0.1

–1

< 0.1

Limits of distribution

Climate in northern Australia is hot and wet, with seasonal drought.

Red kangaroos occur in most semiarid and arid regions of the interior, where precipitation is relatively low and variable from year to year.

Southeastern Australia has a wet, cool climate.

Southern Australia has cool, moist winters and warm, dry summers.

Tasmania

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The figure below (Figure 52.5 in the textbook) shows the distribution of red kangaroos in Australia. From this figure, you can predict that kangaroos: a.

b.

c.

d.

e.

eat plants prefer a hot dry climate don’t like saltwater prefer to live in areas where people don’t live are more abundant in some years than in other years

Kangaroos/km 2

> 20

10 –20

5 –10

1 –5

0.1

–1

< 0.1

Limits of distribution

Climate in northern Australia is hot and wet, with seasonal drought.

Southern Australia has cool, moist winters and warm, dry summers.

Tasmania

Red kangaroos occur in most semiarid and arid regions of the interior, where precipitation is relatively low and variable from year to year.

Southeastern Australia has a wet, cool climate.

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Dispersal

Dispersal - the movement of individuals away from their area of origin or from centers of high population density

Natural range expansion

 Early humans “out of Africa”

 Different from migration

Species transplants

 Potential vs. actual ranges

Where organisms could be versus where they are

Invasive/introduced species

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Earth’s biomes

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Environmental factors

Climate - Long-term prevailing weather in a particular area

Macroclimate - Patterns on a global, regional and local level

Microclimate - Patterns on a smaller scale

 Ex. A community living under a log

Lichen Rotting Logs Tide Pools

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Why do we have weather?

Latitudinal variation in sunlight intensity

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Why do we have weather?

Seasonal variation in sunlight intensity

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Why do we have weather?

Global air circulation and precipitation patterns.

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Why do we have weather?

Global wind patterns

Currents and other bodies of water

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Why do we have weather?

Mountains and elevation

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Marine/Aquatic Biomes

benthos coral reef intertidal

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Marine/Aquatic Biomes

30

N

Tropic of

Cancer

Equator

Tropic of

Capricorn

30

S

Continental shelf benthos

Key

Lakes

Coral reefs

Rivers

Oceanic pelagic zone intertidal

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Estuaries

Intertidal zone

Abyssal zone

(below oceanic pelagic zone) coral reef

Aquatic/Marine Biomes

Account for the largest part of the biosphere in terms of area

Can contain fresh (aquatic), brackish, or salt (marine) water

Oceans

Cover about 75% of Earth’s surface

Have an enormous impact on the biosphere

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Zonation

Are stratified into zones or layers defined by light penetration, temperature, and depth

Thermoclines Intertidal zone - Narrow vertical zone of

Neritic zone Oceanic zone abrupt temperature change. zone

Limnetic zone

0

200 m

Continental shelf

Photic zone

Pelagic zone

Benthic zone

Photic zone

Aphotic zone

Benthic zone

Pelagic zone

Aphotic zone

2,500

–6,000 m

Abyssal zone

(deepest regions of ocean floor)

(a)

Zonation in a lake. Based on light penetration, distance from short and water depth, and open water or bottom.

(b) Marine zonation.

Like lakes, the marine environment is generally classified on the basis of light penetration (photic and aphotic zones), distance from shore and water depth (intertidal, neritic, and oceanic zones), and whether it is open water (pelagic zone) or bottom (benthic and abyssal zones).

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Nutrient turnover

1

Lakes and other marine/aquatic biomes experience turnover

2

In spring, as the sun melts the ice, the surface water warms to 4 °C

In winter, the coldest water in the lake (0 °C) lies just below the surface ice; water is progressively warmer at deeper levels of the lake, typically 4 –5°C at the bottom.

and sinks below the cooler layers immediately below, eliminating the thermal stratification. Spring winds mix the water to great depth, bringing oxygen (O

2

) to the bottom waters (see graphs) and nutrients to the surface.

Spring O

2

(mg/L)

0 4 8

Winter

0

O

2

(mg/L)

4 8 12 12

8

16

24

4

C

4

4

4

2

0

4

C

4

4

4

4

4

O

2 concentration

High

Medium

Low

8

16

24

8

16

24

O

2

(mg/L)

0 4 8 12

Autumn

AP Biology underlying layers, remixing the water until the surface begins to freeze and the winter temperature profile is reestablished.

4

4

C

4

4

4

4

O

2

(mg/L)

0 4 8 12

Thermocline

4

C

5

6

8

20

18

22

Summer

8

16

24

3

In summer, the lake regains a distinctive thermal profile, with warm surface water separated from cold bottom water by a narrow vertical zone of rapid temperature change, called a thermocline.

Lakes

Oligotrophic nutrient poor, oxygen rich

Eutrophic - nutrient rich, oxygen poor

Periodic oxygen depletion; large amount of decomposition

Biota - fish, invertebrates depending on O

2 levels, phyto- and zooplankton

An oligotrophic lake in

Grand Teton, Wyoming

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LAKES

A eutrophic lake in Okavango delta, Botswana

Wetlands

Inundated with water at least periodically

Plants adapted to water-saturated soil

Highly productive

Important filters and breeding grounds

Birds, carnivores, crustaceans, plants, reptiles

WETLANDS

Okefenokee National Wetland Reserve in Georgia

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Streams and Rivers

Current with lots of aeration

Aquatic plants and phytoplankton, fish, invertebrates, etc.

Ex. Potomac and

Anacostia rivers,

Rock and Sligo creeks, Chesapeake

Bay watershed

STREAMS AND RIVERS

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Figure 50.17

A headwater stream in the

Great Smoky Mountains

The Mississippi River far form its headwaters

Estuaries

Transition between rivers and sea - brackish water with flow between the two

Variable salinity depending on temperature, depth, and tides

Worms, oysters, crabs, fish, etc.

Highly productive and important in filtering water

ESTUARIES

Figure 50.17

An estuary in a low coastal plain of Georgia

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Intertidal Zones

Periodically submerged and exposed

Physical environment varies vertically, so species range varies vertically

Oxygen and nutrients renewed tidally

Sea grass, algae, worms, crustaceans, crabs, etc.

INTERTIDAL ZONES

Figure 50.17

Rocky intertidal zone on the Oregon coast

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Oceanic Pelagic Biome

OCEANIC PELAGIC BIOME

Figure 50.17

Open ocean off the island of Hawaii

Open ocean, particularly deep water

Driven by currents - lots of light and oxygen; large photic zone

Experience nutrient turn over - depends on temperature

 70 percent of world’s surface

Phytoplankton and photosynthetic bacteria - makes our oxygen!

Zooplankton, fish, cephalopods, marine mammals, etc.

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Coral Reefs

Formed from coral

“skeletons”

Photic zone - zooxanthellae need light for

CORAL REEFS photosynthesis; sensitive to change in temperature

Fringing reef --> barrier reef

--> atoll island

Unicellular algae, coral animals, fish and invertebrate diversity

Figure 50.17

A coral reef in the Red Sea

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Marine Benthic Zone

Below neritic (near,

MARINE BENTHIC ZONE coastal) and pelagic

(noncoastal, open water) zones

Deep benthic = abyssal zone; deep sea vents with chemoautotrophs

Shallow benthic - oxygen from algae and seaweed

Chemo- or photoautotrophs; worms, arthopods, echinoderms, etc.

A deep-sea hydrothermal vent community

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Tropical rainforest

distribution: equatorial precipitation: very wet temperature: always warm characteristics: many plants & animals, thin soil

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Savanna

distribution: equatorial precipitation: seasonal, dry season/wet season temperature: always warm characteristics: fire-adapted, drought tolerant plants; herbivores; fertile soil

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Desert

distribution: 30 °N & S latitude band precipitation: almost temperature: variable daily & seasonally, hot & cold characteristics: sparse vegetation & animals, cacti, succulents, drought tolerant, reptiles, insects, rodents, birds

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Temperate Grassland

distribution: mid-latitudes, mid-continents precipitation: seasonal, dry season/wet season temperature: cold winters/hot summers characteristics: prairie grasses, fire-adapted, drought tolerant plants; many herbivores; deep, fertile soil

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Temperate Deciduous Forest

distribution: mid-latitude, northern hemisphere precipitation: adequate, summer rains, winter snow temperature: moderate warm summer/cool winter characteristics: many mammals, insects, birds, etc.; deciduous trees; fertile soils

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Coniferous Forest (Taiga)

distribution: high-latitude, northern hemisphere precipitation: adequate to dry (temperate rain forest on coast) temperature: cool year round

2005-2006

Arctic Tundra

distribution: arctic, high-latitude, northern hemisphere precipitation: dry temperature: cold year round characteristics: permafrost, lichens & mosses, migrating animals

2005-2006

Alpine Tundra

distribution: high elevation at all latitudes precipitation: dry temperature: cold year round characteristics: permafrost, lichens, mosses, grasses; migrating

2005-2006

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