Succession occurs as a
result of changes to the environment (the abiotic factors), causing the plant and animal species present to change.
There are two types of succession:
There are two types of succession:
1 Primary succession - this occurs on an area of land that has been newly formed or exposed such as bare rock. There is no soil or organic material present to begin with.
2 Secondary succession - this occurs on areas of land where soil is present, but it contains no plant or animal species. An example would be the bare earth that remains after a forest fire.
Although much of the natural landscape has taken hundreds of years to reach its existing form, primary succession is still taking place.
Primary succession occurs when:
• volcanoes erupt, depositing lava - when lava cools and solidifies
Igneous rock is createdi
• sand is blown by the wind or deposited by the sea to create new sand dunes
• silt and mud are deposited at river estuaries
• glaciers retreat depositing rubble and exposing rock.
Stages of succession
Succession takes place in a number of steps, each one known as a seral stage (or sere). At each seral stage key species can be identified that change the abiotic factors, especially the soil, to make it more suitable for the subsequent existence of other species.
The main seral stages are pioneer community, intermediate community, and climax community, these are summarised in Figure 1.
Summary of the main stages in succession
Pioneer community
Primary succession begins by the colonisation of an inhospitable environment, by organisms known as pioneer species (or pioneer colonisers). This represents the first seral stage. These species arrive as spores or seeds carried by the wind from nearby land masses or sometimes by the droppings of birds or animals passing through.
Examples of pioneer species
algae and lichen.
Pioneer species have a number of adaptations that enable them to colonise this bare environment, including:
• the ability to produce large quantities of seeds or spores, which are blown by the wind and deposited on the ‘new land’
• seeds that germinate rapidly
• the ability to photosynthesise to produce their own energy - light, rainfall, and air (and so carbon dioxide) are often the only abiotic factors present
• tolerance to extreme environments
• the ability to fix nitrogen from the atmosphere, so adding to the mineral content of the soil.
Intermediate community p1
Intermediate community p2
Climax community
Animal succession
Deflected succession
Human activities can halt the natural flow of succession and prevent the ecosystem from reaching a climax community. When succession is stopped artificially, the final stage that is formed is known as a plagioclimax. Agriculture is one of the main reasons deflected succession occurs. For example:
Agriculture is one of the main reasons deflected succession occurs. For example:
• grazing and trampling of vegetation by domesticated animals - this results in large areas remaining as grassland
• removing existing vegetation (such as shrub land) to plant crops - the crop becomes the final community
• burning as a means of forest clearance - this often leads to an increase in biodiversity as it provides space and nutrient-rich ash for other species to grow, such as shrubs.
Conservation
A range of conservation techniques are being used:
• Physical removal of established bracken, and saplings such as birch and pine.
Gorse, which is a legume, adds to the nutrient value of the soil. Heathlands are traditionally nutrient-poor areas of land, and so areas of gorse are also removed through physical means (cutting, crushing, and controlled burning).
These techniques are used to restore the heathland to its former state.
• Mimicking the controlled grazing to limit the spread of bracken, gorse, and tree saplings. Livestock crush and nibble new growth, therefore limiting the spread of these species. This technique is used to maintain the heathland in its current state.
Through using a combination of these techniques, low nutrient levels are maintained in the soil. This produces a varied vegetation structure, thus supporting a biodiverse heathland community.
Succession on a sand dune p1
One of the few examples where all the stages of succession can often be seen clearly in one place is when a series of sand dunes form on a beach. The youngest dunes will be found closest to the shore and the oldest furthest away.
Succession on a sand dune p2