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Section 2: Plant Succession
Plant communities develop through a succession of changes.
Key Ideas: - Seral Stages- Climatic Climax Vegetation- Plagioclimax Vegetation
Case study : Psammoseres (sand dunes) e.g. Murlough Nature Reserve outside Newcastle
Biogeography: The study of the distribution of plants and animals over
the earth’s surface.• ‘Nature abhors a vacuum’• i.e. if plants die something will always replace
them. When new land is created, e.g. a lava flow, new species will move into that area and take over.
• Algae & lichen will colonize rock and break it down (weather it) to form soil.
• The formation of soil then allows other plants to take over.
What is vegetation succession?
• PRISERE is the term for vegetation succession. It is the complete chain of successive seres beginning with a pioneer community and ending with a climax vegetation.
• Vegetation succession occurs because the environmental conditions change. This happens gradually for lots of plants to develop.
• Each stage is called a SERAL STAGE.• Each stage sees the development of species
which cause the micro environment to change which in turn lets new species move in and become dominant.
The MONOCLIMAX CONCEPT• F.E. Clements (1916) said that
for each climatic zone only one type of climax vegetation could evolve.
• He called this the climatic climax vegetation. It is now more commonly known as the monoclimax concept.
• This occurs when the vegetation is in harmony with the local environment.
• As seral stages develop the number of species and height of the plants increase.
• Each sere tends to be named after the dominant species ( the largest or most numerous species).
• The Monoclimax Concept
Pioneer Community
Climatic climax(natural vegetation)
pris
ere Seral stages:
temporary conditions which develop over time(plant succession)
Britain’s Climate
• Cool temperate due to our island position• Cool summers (winds off Atlantic cooling
influence– water slower to heat up than land)• Mild winters (winds off Atlantic warming
influence – water holds its heat for longer & warm ocean current North Atlantic Drift)
• Rain in all seasons
• HOW DOES THIS INFLUENCE VEGETATION?
Britain’s Vegetation
• Our natural Climatic Climax Vegetation is broad leaved deciduous forest.
• The dominant vegetation is influenced by soil type, rock type and climate if people do not interfere.
• So why is Britain not covered in woodland?• Human activities have cut down many trees (farming &
urban growth).• Trees do not exist on mountains – relief, soils & climatic
factors.• Coniferous trees (fast growing) are planted which are not
native.
Britain’s Vegetation:
• The vegetation cover in much of Britain is a PLAGIOCLIMAX VEGETATION.
• This is a deflected climax vegetation that occurs when people have damaged the natural climatic climax so much that regeneration is not possible.
• In the UK you now have grassland instead of woodland.
Possible interruptions:Natural interruptions Human interruptions
Tectonic activity e.g. volcanic eruptions
Temporary climatic changes e.g. drought,
colder conditions
e.g. deforestation
Plagioclimax Vegetation(if permanent)
The Polyclimax Theory• The monoclimax concept has been
replaced by the polyclimax theory.• This theory acknowledges the importance
not only of climate, but of several (poly) local factors including :- drainage- parent rock- relief- microclimate- human activity
New or previously sterile land surface,
or in water
Land on which previousmanagement has been
discontinued e.g. abandoned farmland dueto shifting cultivation inthe tropical rainforest
Primary Succession
Secondary Succession
Ecosystem EvolutionBare surface
SubclimaxEcosystem
RelicEcosystemX
Climatic ClimaxEcosystem
Plagio ClimaxEcosystem
DeflectedSuccession e.g.
relief restrictsdevelopment
DeflectedSuccession e.g.
severe disturbance fire, hurricane
Prim
ary
succ
ess
ion
Sudden displacement e.g.logging
Secondary succession e.g.natural regrowth
Secondary succession e.g.development of a farmed ecosystem
Partial displacement e.g.grazing
Transect showing a primary succession in a HALOSERE(river estuaries where silt deposited by the
ebbing tides and inflowing rivers)
Primary succession in a HYDROSERE(lakes and ponds – sediment carried into the lake
will enrich the water and begin to infill it)