Vegetation Change Over Time Essay, Research Paper
Vegetation develops in many different and varied
environments with each environment having different effects on the vegetation
change over time. This essay will examine these different factors, in different
environments. It will examine different sereal stages in different environment,
the lithosere or rock environment, the psammosere or sand environment, the
halosere or saltwater environment and hydrosere or fresh water environment. A sere is a stage of events by which the vegetation of an
area develops over time. This begins with the pioneer community and end with
the climatic climax vegetation. The first plants to colonise an area are called
the pioneer community. The climatic climax vegetation is when the ultimate
vegetation development has taken place and the environment has reached
equilibrium e.g. when the natural vegetation has reached a stable balance with
the climate and soil of an area. As an environment goes through more sereal
stages the number of species of plants will increase as will their height. The
island of Krakatoa in the Sundra strait between Java and Sumatra is a volcanic
island, which erupted in 1883. Its development was rapid only taking
twenty-five years to develop from the pioneer community to climatic climax
vegetation because of the high humidity and temperatures and the rapid
weathering of the volcanic rock. The diagram below shows the way an environment
such as Krakatoa develops.There are two types of sereal succession primary and
secondary. Primary sereal succession occurs on a new or previously sterile
land. It occurs in four different types of environment lithosere, psammosere,
halosere and hydrosere. A lithosere is a rock environment. These are initially
colonised by blue-green bacteria, which are completely self-sufficient.
Therefore the pioneer community is the mosses and lichens which are capable of
living in areas which lack soil. The lichens and mosses help to weather the
rock along with other types of weathering. This along with the decayed matter
of mosses and lichens helps to form a veneer of soil, which can support more
advanced plant life. Seeds usually of grass then colonise this soil as time
passes the grasses will give way to fast growing shrubs which in turn will be
replaced by fast growing trees. Finally these will face competition from slow
growing trees such as ash and oak. Although each stage of the succession has
been superseded the vegetation from each previous sereal stage still remains
but in smaller amounts. Two examples of areas where the lithosereal development
has taken place are Krakatoa and Sutsey. Sutsey is like Krakatoa in the fact
that it is a newly formed island. The island was created after a volcanic
eruption on 14th November 1963. The island is located off the
south-western coast of Iceland. Unlike Krakatoa it has not developed quickly
because of the local climate which is extremely cold and very windy. These
conditions don?t lead to the quick establishment of life. The diagram below
shows a typical progression for a lithosere ecosystem. Another type of succession is one, which occurs on sand this
is known as a psammosere. The first coloniser of the sand are usually lyme
grass, sea twitch and maram grass these start dune formation known as embryo
dunes. The grasses slowly move back from the high tide mark on to different
dunes. These dunes are very arid and therefore are usually only populated by
maram grass which has adapted to the harsh conditions. Further back from the
main ridge are the older grey dunes, which are shelter from the wind and have
more humus in their soil due to the increased decomposition of the maram grass.
This humus in the soil supports different species and these start to break the
maram grasses dominance on the dunes. Finally around 400m away from the sea the
climatic climax is reached as oak and ash trees develop. One example of a
psammosere is Camber Sands, which has developed over time to have a full
diversity of plants on the different dunes. The diagram below shows the
development of the environment in a psammosere.Freshwater lakes and ponds are known as hydrosere
environments. These also develop through sereal stages. The pioneer coloniser
is usually algae and mosses whose spores have been blown on to the water
surface. These grow to form vegetation rafts, which then support other life
such as bacteria and insects. The next colonisers are the water loving plants,
which may grow on the water surface like lilies or may grow completely
submerged. Bacteria recycle nutrients from these plants encouraging the
encroachment of plants such as bulrushes. The increased sediment created by the
decomposition of these plant leads to increased sediment, which continues to in
fill the lake. Over time the marsh areas at the edge of the lake will be
colonised by small trees and shrubs. And finally the lake is completely in
filled as a result of the sediment build up. When this occurs the oak and ash
trees will be able to take root and the climatic climax vegetation will be
reached. An example of an area where this is occurring is the Norfolk Broads
where some of the broads are nearly completely in filled whereas others are
still at the first stage of development. The diagram below shows the different
stages in the development of a hydrosere.Haloseres are environment based in a salt-water environment
usually at the mouth of a river where there is a large amount of silt and mud
deposition. The pioneer colonisers are algae, which can stand being submerged
in wa
accumulate. Spartina townsendii is
the next coloniser. It can tolerate saline conditions and grows on the slob
zone with only four hours of oxygen in every twelve-hour period. In contrast
the sward zone is inhabited by plants, which can only be submerged for four
hours in every twelve hours. The dominant species here are sea lavender and
grasses. The upper sward zone is only covered by the high spring tides allowing
different types of plants to establish. Further inland from here different
types of plants grow including grasses and shrubs followed by small trees and
ultimately ash and oak trees. The Medway estuary is one example of an area
where this type of progression is taking place. The diagram below shows the
primary succession of a typical halosere.When a climatic climax occurs this means that the ecosystem
or biome is in a state of equilibrium with a stability of transfers material
and energy. However the are a number of factors which can arrest the
development of the ecosystem before it has reached it dynamic equilibrium.
These include mudflow, landslide, disease or changing climate. One example is a
fire, which is likely to destroy the whole ecosystem. But it does allow for new
development as the ash created increase the nutrient quality of the soil
dramatically. But it does leave the soil more vulnerable to erosion. Some
ecosystems depend on a fire to clear the area and to allow the growth of new
seedlings, which will thrive in the good quality soil with little or no
competition for light. Some examples of ecosystems, which depend on a fire to
allow growth, are the forest of the Australian bush. There are three factors, which will dramatically effect the
vegetation change over time in an ecosystem. These are climate, soil quality
and water availability. If the climate that an ecosystem is developing in is
harsh such as that on Sutsey then vegetation change will be slow and very
difficult whereas if the climate is ideal then the ecosystem will develop
quickly such as that on Krakatoa. The soil quality is important because the
number of nutrients in a soil will affect the type of plants able to grow
there. A poor quality soil will only be able to support a small amount of small
plants whereas a good quality soil will support larger plants. Water
availability is key because it affects the number of plants which can grow in a
certain area. If there is little water available then only a few plants can
survive. In contrast if there is an abundance of water then the number of
plants able to be supported will be large. This can also be taken to another
extreme where there is too much water and the plants drown. Human factors are major arresting factors, which usually
lead to secondary. These can include deforestation, which leads to the removal
of many of the nutrients from the ecosystem and can lead to erosion. This has
occurred in the Gola forest in Sierra Leone. Sierra Leone has a climate, which
would allow a high proportion of it s landmass to be covered with rainforest.
But due to constant deforestation the rainforest has been dramatically reduced
in size and now only covers a small amount of the land. Pollution caused by humans can affect vegetation on three different
scales globally, nationally and locally. An example of a global pollution,
which affects vegetation change, is acid rain, which via air currents can
travel globally precipitating at any point of the world. Acid rain kills plants
and can change the balance of nutrients in the soil favouring certain types of
plants. An example of pollution on a national scale is global warming which can
affect whole countries and leads to the deaths of many plants and the increase
water levels around the world. Trampling is an example of pollution on a local
scale. Trampling kill plants and leads to the compacting of soils making water
absorption difficult and plant growth therefore difficult. Other examples of Human arresting factors, which affect
vegetation change over time, include desertification the progressive
downgrading of land usually caused by human mismanagement through things like
over grazing or via drought. Urbanisation and the gradual expansion of towns
into the countryside in Great Britain and other countries has led to the
destruction of ecosystems to allow space for expansion. This is particularly
true in less economically developed countries, which are in a stage of hyper
urbanisation and create space for this by destroying ecosystems. One example of
this is Mexico City, which has experienced massive expansion in recent years. Conservation is another way in which humans can affect the
natural vegetation change. The Norfolk Broads is a good example of this. The
Norfolk Broads area has been an area of conservation for a number of years the
area houses a number of rare species of plant and animal which conservationists
are trying to save. One thing they are trying to prevent is the gradual in
filling of the broads. This therefore disrupts the natural vegetation change. A
policy of aforestation has been applied in a number of areas to try and
repopulate certain areas with trees that were once there. This therefore has a
large effect on the vegetation change over time. In conclusion we can see that there are many different
things, which affect vegetation change over time. These are both physical
factors and human factors and both types have the power to completely change an
ecosystem affect its progression towards its climatic climax vegetation and its
establishment as a biome.