Lecture 3: Geographies of biodiversity 4 Flashcards

1
Q

Complexity in Succession

A

Now accepted that succession is very complex and contains many elements of randomness or stochasticity (e.g. propagule availability, interspecific and intraspecific competition, site characteristics, disturbance)

• Allogenic succession = externally induced
• Autogenic succession = internally induced

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2
Q

Ecosystem changes

A

There are several important changes in plant communities and their ecosystem during the seral process

  1. In plant morphology and organisation:
    • Increasing height of dominant vegetation • Increasing variation in growth form
    • Stratification of communities
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3
Q

Ecosystem changes- abiotic environment

A

soil characteristics (breakdown of parent material , soil formation, increasing organic matter, pH, texture, structure and horizon development)

  • light intensity (increased shade)
  • relative humidity/hydrological cycle • temperature
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4
Q

Climax concepts

A

‘Climax community’ represents the endpoint of the successional process, after which further changes in community do not take place

  • There were (historically) two main arguments regarding climax stages – Clements maintained that all successions within a climatic region would approach the same climax stage (mono climax)
  • Other views are variations of Tansley’s theme that other abiotic factors (e.g. soil, topography, moisture) would also influence the climax stage (polyclimax model and its variations)
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5
Q

Mono climax succession

A

‘Vegetation in stable equilibrium with climate and soil, given undisturbed conditions and free drainage’

  • Concept of the plant community as an organism developing into a mature state, which would be in equilibrium provided the environment was stable
  • The same climax would be achieved for a given climatic region no matter what the starting point (e.g. oak woodland in Southern Britain)
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6
Q

Poly climax succession

A

Refuted the concept that communities behaved as organisms, and that there would be one climatic climax in a given location

  • Other environmental factors would be strong enough to hold a community stable for long periods of time so that a climax was not reached (e.g. soil drainage/chemistry, topography, or the influence of humans and other animals)
  • In a given climatic region these factors would mean that different plant communities would be in a stable equilibrium for long periods of time
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7
Q

Mosaic Succession

A

Similar to the polyclimax theory, except that patterns in environmental and biotic pressures are observed which relate to climax pattern, and so a mosaic of ‘climax’ vegetation types is formed

• Noted that 40% of plant communities could not be placed in climax communities and that a gradient existed between community boundaries – these are ecotones, and are a very important concept in ecology

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8
Q

Cyclical Climax succession

A

Explains the mosaics observed in climax vegetation as being due to cyclical patterns of growth and decay (based on observations of tropical rainforests)

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