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Priseres K.I 4
Xerosere (Dry)
Lithosereswhere the plants
colonise bare rock
e.g. after glacial retreat, Snowdonia or a rocky shore, Oxwich Point, Gower or a newly created volcanic island (e.g. Surtsey, Iceland)
Psammoserewhere plants colonise coastal sand dunes
e.g. The south Gower - Oxwich Bay.
Hydrosere (Wet)
Hydrosereswhere the plants
colonise fresh water, as at a pond margin
e.g. Llanfihangel Gobion, Monmouthshire - ox-bow lakes
Halosereswhere plants colonise salt marshes and sea
estuaries
e.g. The North shore of the Gower, Lanrhidian salt marsh
Prisere : complete succession from initial inorganic (1) too wet/dry conditions to climatic climax vegetation (5?).
e.g. Psammosere
1 5?
Initial conditions either
too wet
Or too dry
Or too alternating wet / dry
Possibly with salt
Therefore only a few plants can tolerate these harsh conditions
No soil
BARE INORGANIC SURFACE Mosses and lichens
COLONISERSPIONEER COMMUNITY
Climax vegetation is the vegetation which establishes itself on a given site for given climatic conditions (in the absence of human action) after a long time
Climatic climax vegetation
Witham Woods Oxfordshire
Climax Vegetation
Plagioclimax subclimax (after deforestation, ploughing, burning
Secondary succession
Primary succession
New inorganic (non-vegetated surface)
Biotic subclimax
Edaphic (soil) subclimax
THE POLYCLIMAX THEORY
1
2
2
34
1
2
3
4
Primary succession
natural interruptions in primary succession
Retrogressive succession due to disturbance (natural or human)
Secondary succession
Seral Stages – temporary stages which develop over time leading to plant succession
1 2 3 4 5
Time goes by (100s of years)
or different spatial positions at one time
Subclimax
An arresting factor halts development
e.g. biotic (rabbits, goats, sheep: graze the land and prevent tree growth)
e.g. edaphic (salty soil – hinders tree growth)
Birch tree subclimax
Plagioclimax
Primary Succcession on heather moorlands (U.K.)
Mosses, lichens,
hardy grasses
Grasses, herbs, some heather
Tall shrubs e.g birch
Pine, hazel
Oak forest
Post glacial recolonisation in the lower hills
From Oak Trees to Heather Moorland
1. After the Ice Age the primary succession to heather moorland occurred.
2. Humans cleared the trees for farming. The soils lost became leached and lost their fertility. The acid soils did suit heather.
3. Young shoots of heather are ideal for sheep grazing and the moorlands are used for hill farming. The grazing prevented the regrowth of shrubs and trees.
4. Periodic burning (muirburn) removes old wood, releases nutrients and encourages new shoots. The heather is maintained as a plagioclimax.
Oak forestPLAGIOCLIMAX
Deflection by humans : cutting, burning, grazing
Blanket bog
Poor drainage
Grassy heaths
overgrazing
burning
Heather moorland
Liming, fertiliser
Improved pasture or arable farmland
SHRUBBY HEATH