Chapter 20 - Succession Stability

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Last updated 11:04 PM on 3/29/26
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26 Terms

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Succession and Pioneer Community

Succession - Gradual change in plant/animal communities post-disturbance

-Primary Succession - Newly exposed geological substrates (not very common)

-Secondary Succession - Following disturbance that doesn’t destroy soil (ex; wildfires)

Pioneer Community - Plants/lichen colonize in the first few years after disturbance

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Climax and Disclimax Community

Climax Community - late successional community that remains stable until disrupted by disturbance

Disclimax Community - maintained only under continual disturbance

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Community Changes by Succession

Succession changes all aspects of community structure;

  1. Richness

  2. Dominance/evenness

  3. Composition of species

  4. Species diversity

-Changes are both predictable/unpredictable

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Primary Succession at Glacier Bay

As glaciers receded, number of plant species in the bay increased

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Secondary Succession at Boreal Forest

Frequently disturbed (by humans and fires)

Killed plants → Increase in light penetration → woody recruitment/early colonizers → increase in nutrient availability → stimulate microbial activity

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Recently Burned Differences

Pre-Fire - Variation in forest species composition

Post-Fire - regular pattern changes over time

-Moderate fire, no primary succession just hardwood regeneration

  • Replacement by confiers/spruce budworm

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Succession in Rocky Intertidal Communities

Boulders cleaned bare of organisms

-Wanted to examine what occurs with successions

Results: Number of species increased until 1-1.5 years after disturbance; begins to level off at 5 species

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Succession in Stream Communities

98% of algal and invertebrates biomass lost, ecological succession occurred in < 2 months

-Flash floods remove the diversity, but diversity returned in 20 days

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Shallow Lake Succession

Experience succession on 2 time scales;

  1. Seasons or years; Disturbance

  2. Geological time scales; Sedimentation

-Most lake eventually disappear

-Sedimentation - Drives successions

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Paludification

Most common way of peatland formation

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Ecosystem Changes During Succession

Succession Increases;

  1. Biomass

  2. Primary production

  3. Respiration

  4. Nutrient retention

-Time is also important: weathering of bedrock releases lots of nutrients (like phosphorus)

-Physical and biological systems therefore inseperable

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Succession and Soil Change in Glacier Bay

Succession change the soil’s

  1. Organics

  2. Water

  3. Phosphorus

  4. Bulk Density

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Hubbard Experimental Forest and Nutrient Retention

Clear logged forest

-Then used herbicides to slow down succession

Result: Significant lowering of nutrient retention in the forest

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Nutrient Loss on Logged Peatlands

After logging, exposed peat does not recover over time, peat depth continued to be reduced

-Only a temporary spike in nutrients, then they returned back to normal

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Successional Change Models

  1. Clements

-Serial replacement of species that facilitate each other

-Climax community seen as a “super-organism”

  1. Gleason

-Species distributed independently of each other

-Individualistic approach — outcome can be altered

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Why Gleason More Accepted

  1. Not always the climax community

  2. Climax concept = general concept of succession

Communities are groups of individuals, not a “super-organism”

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Egler

Clarified distinction between Clement and Gleason, provided validity to both

Two alternative ways of succession:

  1. Relay Floristics - one wave of species replaced by the next until climax — little overlap

  2. Initial Floristics - different species dominate at different time periods — great deal of overlap

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Western Boreal Forest and Succession

Follows the initial floristics

-Explains the high amount of productivity (which attracts lots of bird species) —> Greater diversity

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Connell and Slayter Mechanism of Succession

  1. Facilitation

  2. Tolerance

  3. Inhibition

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Facilitation

Many species attempt colonization, those with particular characteristics can do it

-Colonization of new sites done by Pioneer Species

  1. Species modifies environment to be less suitable for them, but more suitable for later species

Climax Community = Replacement of early stages until no longer facilitate colonization

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Tolerance

Initial Stage - not limited to a few pioneer species

-Juvenile of species dominant at climax can establish in earliest successional stages

-Early colonizers do not facilitate colonization

Climax Community = When list of tolerance species is exhausted

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Inhibition

Any species can colonize area during early stages of succession

-Early occupants modify environment to make area less suitable for any other species

Climax Community - long lived species resistant to damage (physical or biological)

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Successional Mechanism in Rocky Intertidal Zone

Evidence for inhibition of later successional species

-Ulva algae species inhibits the colonization by red algae

-Evidence for facilitation; colonization by intertidal plants allow for other species to grow

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Primary Succession Following Deglaciation

In Glacier Bay Alaska, no single mechanism determines the pattern of succession

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Community and Ecosystem Stability

Stability results from:

  1. Resistance - ability to maintain structure/function

  2. Resilience - ability to recover from disturbance

Time - long time required to understand the stability of an ecosystem

Scale - depends on how we view stability

a) Community life form - little change, very stable

b) Species level - lots of change/differences, unstable

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Other Factors in Community Stability

Stable spatial structure in landscape;

E.g., Desert (bedrock) and streams (hydrology)

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