ECOLOGICAL SUCCESSION & EQUILIBRIUM
Ecological succession
is the term that expresses how a community changes over time in regards to the
composition and dominant species found in that community. Equilibrium in
ecology refers to a state that occurs such that a small disturbance or change
is counter balanced by another change so that the community is restored to its
original state. Thus, as a community goes through multiple changes through each
stage of succession, it is not in equilibrium. New species enter the community
and take the place of others and the community does not return to the way it
was formerly.
When a community
eventually reaches the last stage of succession, what is typically referred to
as a climax community, the composition of the community is stable. Thus, any
small disturbances will be counterbalanced. The system is at a relative
equilibrium.
Meaning of Climax
Community: Climax community is
the stable end product of successional sequence or sere. It is a community that
has reached a steady state of species composition, structure and energy flow,
under a particular set of environmental conditions. Steady state indicates the
dynamic nature of the climax.
Also the end of successional change does not mean that community
development has come to an end. As has been stated above, climax community is
always in a state of flux and its structure undergoes changes due to birth,
death and growth processes. However, these changes are less dramatic than the
community transformations observed during succession.
The characteristics of a climax community are:
1. The climax community is able to tolerate its
own reaction.
2. It tends to be mesic (medium moisture content)
rather than xeric (dry) or hydric (wet).
3. The climax community is more highly organised.
4. The climax community with its more complex
organisation has large number of species and more niches.
5. The organisms of earlier successional stages
tend to be smaller, shorter lived with a higher biotic potential (r-selected).
In contrast, the species of climax community tend to be relatively large, long
lived and with a low biotic potential (K-selected).
6. In climax community, energy is at a steady
state (net primary production is zero), whereas, in immature stage of
succession, gross primary production tends to be greater than community
respiration, signifying accumulation of energy.
7. Immature ecosystems are temporary while in
climax community the stability is high.
8. Climax communities show less broader changes
and are more resistant to invasions than immature ecosystems.
Nature of Climax
Community:
A. Mono-climax and
poly-climax:
According to Clements (1916) succession resulted in a single
true climax community, determined primarily by the climate of the region. This
view of his is called the mono-climax theory of succession, which elaborates
that the many different vegetation communities found in a region are
successional stages of the true climax community.
These different vegetation communities were
often called subclimax, preclimax or post-climax communities. This theory
further stresses that, given sufficient time, the difference in local
conditions of soil moisture, temperature, nutrient availability, hydrology and
so on (that give rise to different vegetation types) would be over comed and a
homogeneous true climax would develop.
Many observations seem to conflict this
hypothesis as it is evident that even under primeval conditions it was
difficult to find large areas of uniform vegetation. Rather, it is appropriate
to recognise several different communities as climax.
Poly-climax theory of
succession; stresses that many
different types of vegetation form the climax community, depending on local
conditions. The climax community should be in harmony with the whole
environment and not just climate. However, the hypothesis of poly-climax is
also basically terminological.
B. Climax pattern
theory:
More recently a third hypothesis was proposed
by Robert H. Whittaker (1953) known as climax pattern theory, which rejects the
classification approach. It recognises a regional pattern of open climax
communities whose composition at any particular locality depends on the
specific environmental conditions present at that time. The climax pattern concept, in a sense, views
only one big community that changes according to soil, slope and other habitat
factors. This approach is considered to be more useful and closer to reality to
describe such pattern of variation.
Factors Determining
the Nature of Climax Community:
Many factors such as soil nutrients, moisture,
slope, exposure etc. determine the nature of the climax community. Fire is
another important feature of many climax communities. Fire-resisting species
are favoured while other species that would have dominated are excluded. Fire
triggers the release of seeds in some pine species. After the fire has receded
the pine seedlings grow rapidly in the absence of competitors. Grazing pressure
is another factor that determines the nature of climax community. Intense
grazing may turn grassland into shrub-land. Shrubs and cacti may establish
themselves as they are unsuitable for forage. The grazing of many herbivores
may suppress many species of plants and favouring competitors that are less
desirable as food.

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