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Unit 4 - Chapter 6, Part 1 Unit 4 - Chapter 6, Part 1

Unit 4 - Chapter 6, Part 1 - PowerPoint Presentation

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Unit 4 - Chapter 6, Part 1 - PPT Presentation

Kinds of Ecosystems and Communities David Rude Kinds of Ecosystems and Communities Outline 61 Succession 62 Biomes Are Determined by Climate 63 Major Biomes of the World Succession Communities ID: 802674

climax succession communities primary succession climax primary communities biomes community major terrestrial water types organisms soil plants climate secondary

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Slide1

Unit 4 - Chapter 6, Part 1

Kinds of Ecosystems and Communities

David Rude

Slide2

Kinds of Ecosystems and Communities

Slide3

Outline

6.1 Succession

6.2 Biomes Are Determined by Climate

6.3 Major Biomes of the World

Slide4

Succession

Communities

proceed through is a series of regular, predictable changes in community structure over time

.

Activities of organisms change their surroundings

& make

the environment suitable for other kinds of

organisms.

Slide5

Succession

Climax community

A relatively stable, long-lasting community that is the result of succession.

Not always

predictable

Ecological Succession of the Climax

Forest - video

Slide6

Succession

Types of factors that determine the kind of climax community

Climate

Water

Substrate/soil

Colonizing organisms

Slide7

Slide8

Succession

Primary succession

Begins with

Total lack of organisms

Bare mineral surfaces or water

Slide9

Succession

Primary succession

(continued)

Examples

Volcanic lava flow

Glaciers retreating

Lower of sea level

Takes a long timeFew available nutrients for plants

Slide10

Succession

Secondary succession

Begins with

Disturbance of an existing ecosystem.

Much more commonly observed

Proceeds more rapidly than primary succession.

Slide11

Primary Succession

Terrestrial primary succession

Pioneer community

A collection of organisms able to colonize bare rock

Lichens

Break down rock and accumulate debris

Helps to form a thin soil layer

Soil begins to support small forms of lifeMay take 100 years to grow as large as dinner plate

Slide12

Primary Succession

Pioneer organisms

Slide13

Primary Succession

Later Stages

Lichen community replaced by annual plants.

Annuals replaced by perennial community.

Perennial community replaced by shrubs.

Shrubs replaced by shade-intolerant trees.

Shade-intolerant trees replaced by shade-tolerant trees.

Stable, complex, climax community eventually reached.

Slide14

Primary Succession

Primary succession on land

Page 111

Slide15

Primary Succession

Successional (seral) stage

Each step in the process of succession

Sere

The entire sequence of stages

Slide16

Primary Succession

Characteristics of climax communities

Maintain species diversity for an extended period.

Contain multiple specialized ecological niches.

Maintain high levels of organism interactions.

Recycle nutrients

Maintain a relatively constant biomass.

Slide17

Primary Succession

The general trend in succession

Increasing complexity

More efficient use of matter and energy

Slide18

Primary Succession

Aquatic primary succession

Except for oceans, most are considered temporary

All receive inputs of

Soil particles

Organic matter from surrounding land

Results in gradual filling of shallow bodies of water

Slide19

Primary Succession

Early stages

In deeper parts only floating plants and algae

As water depth becomes less

Submerged plants establish roots in sediment

Roots and stems below water accumulate more material

Help to trap sediments

Slide20

Primary Succession

As water depth becomes less

Submerged plants establish roots in the sediments

Elodea and algal mats

Emergent plants become established

Have leaves that float on the surface of the water or project into the air.

Water lilies and cattails

Slide21

Primary Succession

Later Stages – Transition to Terrestrial Community

Wet meadow forms

Grasses & sedges that can tolerate wet roots

Sometimes sphagnum moss forms a thick floating mat

Bog

Eventually becomes dryer

Transitions to climax community typical of the area

Slide22

Primary Succession

Primary

succession

from a pond to a wet meadow.

Page 112

Slide23

Floating Bog

Slide24

Bog

Slide25

Rainforest Bog

Slide26

Secondary Succession

Secondary succession

Occurs when an existing community is disturbed or destroyed

Much of the soil and some organisms remain

Soil and nutrients allow process to advance more rapidly than primary succession

Plants and organisms that survive disturbance can grow quickly and reestablish themselves

Slide27

Secondary Succession

Nearby undamaged communities serve as sources of seeds and animals.

New climax community likely resembles the destroyed community.

Slide28

Secondary Succession

Example of seral stages

Annual plants

Grasses and biennial herbs

Perennial herbs & shrubs

Pines

Oak & Hickory trees

Slide29

Secondary Succession

Secondary succession on land

Page 113

Slide30

Historical Perspective on

Succession and Climax

Original communities that European explorers found:

East – hardwood forests

North – evergreen forests

Central – grasslands

South - desert

Early ecologists saw these as the endpoint

Slide31

Historical Perspective on

Succession and Climax

Settlers changed “original” ecosystems to agriculture

Poor farming practices destroyed soil

When farms were abandoned, began returning to its “original” condition.

New climax forest resembled original

Fewer species

Sometimes entirely different kinds of communities

Slide32

Historical Perspective on

Succession and Climax

New species from other parts of the world changed the mix of organisms

Diseases removed species that were formerly dominant

Chestnut blight

Dutch Elm disease

Slide33

Modern Concepts of

Succession and Climax

Not a fixed, pre-determined community for each part of the world.

Main difference

between climax community and successional community is its time scale.

Climate is only one of many factors that determine climax community

Slide34

Modern Concepts of

Succession and Climax

Human activities that alter climax communities

Agricultural practices

Logging

Suppression of fire

Changing the amount of water present

Draining an areaIrrigation and flooding

Slide35

Biomes Are Determined By Climate

Biomes

Terrestrial climax communities with wide geographic distributions.

Different communities within a biome will show differences in exact species present

General structure and the kinds of niches and habitats present are similar

Slide36

Biomes: Major Types of

Terrestrial Climax Communities

Two primary non-biological factors that determine climax communities

Temperature

Patterns of precipitation

Total amount

Form – rain, snow, sleet

Distribution

Slide37

Biomes: Major Types of

Terrestrial Climax Communities

Major Biomes

Rainforest

Tropical

Temperate

Slide38

Biomes: Major Types of

Terrestrial Climax Communities

Major Biomes

Forest

Deciduous

Northern Coniferous

Dry

Slide39

Biomes: Major Types of

Terrestrial Climax Communities

Slide40

Biomes: Major Types of

Terrestrial Climax Communities

Major Biomes

Grassland

Savanna

American Prairie

Slide41

Pampas – South America

Slide42

Savanna - Tanzania

Slide43

Biomes: Major Types of

Terrestrial Climax Communities

Major Biomes

Tundra

Caribou Crossing the Tundra

Slide44

Tundra

Slide45

Biomes: Major Types of

Terrestrial Climax Communities

Major Biomes

Desert

Hot

Cold

Slide46

Northern India

Slide47

Gobi Desert - Mongolia

Slide48

Slide49

Biomes: Major Types of

Terrestrial Climax Communities

Biomes of the world

Slide50

The Effect of Elevation

on Climate and Vegetation

Temperature

Warmest near equator, cooler toward the poles

Temperature decreases as altitude increases

Moving from sea level to mountain tops

Possible to pass through a series of biomes

Similar moving from the equator to the North Pole

Slide51

The Effect of Elevation

on Climate and Vegetation

Relationship between height above sea level, latitude, and vegetation.

Slide52

The Effect of Elevation

on Climate and Vegetation

Other non-biological factors

Periodic fires help maintain some grasslands

Frequent strong winds prevent establishment of trees

Type of soil

Sandy soil dry out quickly

Hinders water demanding species such as treesWet soils only allow certain types of trees