Lecture 15 Flashcards

1
Q

Mount St Helens Eruption

A
  • 1980
  • Largest avalanche in recorded history
  • New habitats devoid of living organisms
  • Effects of the eruption: varied depending on the distance from the volcano and habitat type
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2
Q

Many Animals Survived the Eruption Because

A
  • Some were still dormant (animals hiding from the cold underground)
  • Animals that live in burrows (under ice-covered lakes)
  • Or plants with underground parts
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3
Q

Mechanisms Responsible for Primary Succession

A
  1. facilitation
  2. lupines
  3. tolerance
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4
Q

Facilitation

A
  • By dwarf lupines on the Pumice Plain
  • They trap seeds and detritus
  • Have nitrogen-fixing bacteria
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5
Q

Lupines

A
  • Inhibited by insect herbivores
  • Which controlled the pace of succession
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6
Q

Tolerance

A
  • Douglas fir and herbaceous species lived together in some habitats
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7
Q

Agents of Change

A
  • Act on communities across all temporal and spatial scales
  • Vary in frequency and intensity
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8
Q

Agents of Change Example

A
  • Coral reef community
  • Abiotic features interact, such as predation, competition, and other interactions between organisms
  • Slow, subtle changes, as well as catastrophic ones have occurred over the last few decades
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9
Q

Sucession

A
  • The directional change in species composition over time as a result of abiotic and biotic agents of change
  • Studies of succession often focus on vegetative change
  • The roles of animals, fungi, bacteria, and other microbes are equally important
  • Agents of change vary in frequency and intensity
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10
Q

Two Types of Succession

A
  1. Primary Succession
  2. Secondary Succession
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11
Q

Primary Succession

A
  • Ex. Volcanic Rock
  • involves the colonization of habitats devoid of life
  • Very slow due to inhospitable conditions
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12
Q

Secondary Succession

A
  • involves the reestablishment of a community in which some, but not all, organisms have been destroyed
  • Occurs after fires, storms, logging, etc
  • Legacy of the preexisting species and their interactions with colonizing species play larger roles than in primary succession
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13
Q

The First Colonizers

A
  • Tend to be stress-tolerant
  • Transform habitat in ways that benefit their growth
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14
Q

Henry Cowels

A
  • 1899
  • Studied succession on sand dunes along Lake Michigan
  • Assumed plant assemblages farthest from the lake’s edge were the oldest
  • Ones nearest to the lake were the youngest
  • Representing a time series of successional stages
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15
Q

Frederick Clements

A
  • 1916
  • Believed plant communities are like “superorganisms”
  • Groups of species working together toward some deterministic end
  • succession is similar to the development of an organism
  • Each community reaches a stable endpoint called the “climax community”
  • composed of dominant species that persist over many years and provide stability that can be maintained indefinitely
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16
Q

Henry Gleason

A
  • 1917
  • thought communities are the random product of fluctuating environmental conditions acting on individual species
  • Communities are not predictable and repeatable
  • result of coordinated interactions among species; each community is unique
17
Q

Charles Elton

A
  • 1927
  • Organisms and the environment interact to shape the direction succession will take
  • Animals can affect the timing and sequence of succession
18
Q

Connell and Slayter

A
  • 1977
  • Reviewed the literature on succession and proposed three models:
    1. Facilitation Model
    2. Tolerance Model
    3. Inhibition Model
19
Q

Facilitation Model

A
  • inspired by Clements
  • Early species modify the environment in ways that benefit later species
  • The sequence of species facilitations leads to a climax community
20
Q

Tolerance Model

A
  • assumes the earliest species modify the environment, but in neutral ways that neither benefit nor inhibit later species
21
Q

Inhibition Model

A
  • assumes early species modify conditions in negative ways that hinder later successional species
22
Q

Mechanisms of Succession

A
  • Glacier Bay, Alaska one of the best-studied examples of primary successions
  • Glaciers scrap everything clear
  • Melting glaciers have led to a sequence of communities that reflect succession for centuries
  • Organic material provides substrates that hold water and nutrients (bacteria)
  • Pioneer stage doesn’t have much bacteria seen compared to spruce stage
23
Q

Nitrogen

A
  • an important limiting factor
24
Q

Glacier Bay illustrated all Three Mechanisms in Connell and Slyater’s Models:

A
  • early stages showed facilitation
    - changes in habitat
  • inhibition seen through species such as alders having a negative effect on later successional species
  • succession was driven by life history characteristics, a signiture of the tolerance model
25
Q

Rocky Intertidal Zone

A
  • Disturbance is created mostly by storms— waves and debris rip out the organisms
  • Low tides: expose organisms to high or low temperatures
  • which can kill them or cause them to detach
26
Q

Sousa

A
  • 1979
  • Studied algal succession on the boulders
27
Q

Alternate Stable States

A
  • The theory of alternative stable states can be depicted as a topographic surface
  • Different communities follow different successional paths
  • Develop in the same area under similar environmental conditions
  • A community is thought to be stable when it returns to its original state after some perturbation
28
Q

2 Different Stable Communities Seemed to Result

A
  • One dominated by Styela, a solitary tunicate
  • One dominated by Schizoporella, a bryozoan, on tiles placed out in late summer
  • Both were impervious to colonization by other species
  • Styela can escape predation once it reaches a certain size
  • The system might show hysteresis given that it does not shift back to the original community type once the original conditions are restored
29
Q

Regime Shifts

A
  • caused by the removal or addition of strong interactors that maintain a community-type
  • It is unclear whether the results can be reversed