Primary succession involves the changes from pioneer species which colonise an environment
Changes in abiotic factors lead to more favourable conditions and increasing species diversity
primary succession Begins in a place without any soil
Sides of volcanoes
Landslides
Flooding
Starts with the arrival of living things such as lichens that do not need soil to survive
Called pioneer species
Features of pioneer species -
Can tolerate extreme conditions e.g. low nutrient levels
Have very good means of dispersal, usually by wind
Are not able to compete for resources e.g. light
Are not influenced by or dependent on animal species
May be able to fix nitrogen (e.g. legumes) and build up soil nutrients
primary succesion -
Soil starts to form as lichens and the forces of weather and erosion help break down rocks into smaller pieces
When lichens die, they decompose, adding small amounts of organic matter (humus – not the chickpea dip ) to the rock to make soil
climax community -
A stable group of plants and animals that is the end result of the succession process
The climax community produced is controlled by the climate.
Eg. water present all year – generally woodland
distinct wet and dry seasons – grassland
wet and acidic – blanket bog
Does not always mean big trees
secondary succession -
Begins in a place that already has soil and was once the home of living organisms
Occurs faster and has different pioneer species than primary succession
Example: After forest fires, human activity
The succession process is altered, this is called deflected succession
Types of activity that can interrupt succession include: deforestation; ploughing; grazing; water drainage; weeding/coppicing; introducing new species.
Plagioclimaxes are what is produced at the end of a deflected succession.
Most habitats in the UK are plagioclimaxes produced by grazing, burning, mowing or cutting.
Examples include grassland and heathlands which are used of agriculture