Lecture 3: Geographies of biodiversity 4 Flashcards
Complexity in Succession
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
Ecosystem changes
There are several important changes in plant communities and their ecosystem during the seral process
- In plant morphology and organisation:
• Increasing height of dominant vegetation • Increasing variation in growth form
• Stratification of communities
Ecosystem changes- abiotic environment
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
Climax concepts
‘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)
Mono climax succession
‘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)
Poly climax succession
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
Mosaic Succession
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
Cyclical Climax succession
Explains the mosaics observed in climax vegetation as being due to cyclical patterns of growth and decay (based on observations of tropical rainforests)