Arthur Tansley, a
British ecologist, was the first person to use the term 'ecosystem' in a
published work. He regarded ecosystems not simply as natural units, but as
mental isolates.
Okay,so there is
such a thing we call “Ecosystem Processes”, in which the energy and carbon
enter ecosystems through photosynthesis, and are incorporated into living
tissue, transferred to other organisms that feed on the living and dead plant
matter, and eventually released through respiration. Most mineral nutrients, on
the other hand, are recycled within ecosystems.
Primary production
Primary production is the production of organic
matter from inorganic carbon sources. Overwhelmingly, this occurs through
photosynthesis. The energy incorporated through this process supports life on
earth, while the carbon makes up much of the organic matter in living and dead
biomass, soil carbon and fossil fuels. It also drives the carbon
cycle, which influences global climate via the greenhouse effect.
Through the process of photosynthesis, plants
capture energy from light and use it to combine carbon dioxide and
water to produce carbohydrates and oxygen. The photosynthesis
carried out by all the plants in an ecosystem is called the gross primary
production (GPP). About 48–60% of the GPP is consumed in plant respiration. The
remainder, that portion of GPP that is not used up by respiration, is known as
the net primary production (NPP). Total photosynthesis is limited by a
range of environmental factors. These include the amount of light available,
the amount of leaf area a plant has to capture light (shading by
other plants is a major limitation of photosynthesis), rate at which carbon
dioxide can be supplied to the chloroplasts to support photosynthesis, the
availability of water, and the availability of suitable temperatures for
carrying out photosynthesis.
Energy flow
The carbon and energy incorporated into plant tissues (net
primary production) is either consumed by animals while the plant is alive, or
it remains uneaten when the plant tissue dies
and becomes detritus. In terrestrial ecosystems, roughly 90% of the
NPP ends up being broken down by decomposers. The remainder is either
consumed by animals while still alive and enters the plant-based trophic
system, or it is consumed after it has died, and enters the detritus-based
trophic system. In aquatic systems, the proportion of plant biomass that
gets consumed by herbivores is much higher. In trophic systems
photosynthetic organisms are the primary producers. The organisms The carbon
and energy incorporated into plant tissues is either consumed by animals while
the plant is alive, or it that consume their tissues are called primary
consumers or secondary producers—herbivores. Organisms which feed on microbes (bacteria andfungi)
are termed microbivores.
Animals that feed on primary consumers—carnivores—are secondary consumers. Each
of these constitutes atrophic level. The sequence of consumption—from
plant to herbivore, to carnivore—forms a food chain. Real systems are much
more complex than this—organisms will generally feed on more than one form of
food, and may feed at more than one trophic level. Carnivores may capture some
prey which are part of a plant-based trophic system and others that are part of
a detritus-based trophic system (a bird that feeds both on herbivorous
grasshoppers and earthworms, which consume detritus). Real systems, with all
these complexities, form food webs rather than food chains.
Decomposition
The carbon and nutrients in dead organic
matter are broken down by a group of processes known as decomposition.
This releases nutrients that can then be re-used for plant and microbial
production, and returns carbon dioxide to the atmosphere (or water) where it
can be used for photosynthesis. In the absence of decomposition, dead organic
matter would accumulate in an ecosystem and nutrients and atmospheric carbon
dioxide would be depleted. Approximately 90% of terrestrial NPP goes
directly from plant to decomposer.
Ecosystem
dynamics
Ecosystem management
When natural resource
management is applied to whole ecosystems, rather than single species, it
is termed ecosystem management. A variety of definitions exist: F.
Stuart Chapin and coauthors define it as "the application of
ecological science to resource management to promote long-term sustainability
of ecosystems and the delivery of essential ecosystem goods and services", while
Norman Christensen and coauthors defined it as "management driven by
explicit goals, executed by policies, protocols, and practices, and made
adaptable by monitoring and research based on our best understanding of the
ecological interactions and processes necessary to sustain ecosystem structure
and function" and Peter Brussard and colleagues defined it as
"managing areas at various scales in such a way that ecosystem services
and biological resources are preserved while appropriate human use and options
for livelihood are sustained".
Although definitions of ecosystem
management abound, there is a common set of principles which underlie these
definitions. A fundamental
principle is the long-term sustainability of the production of goods and
services by the ecosystem; "intergenerational sustainability [is] a
precondition for management, not an afterthought". It also requires clear goals with
respect to future trajectories and behaviors of the system being managed. Other
important requirements include a sound ecological understanding of the system,
including connectedness, ecological dynamics and the context in which the
system is embedded. Other important principles include an understanding of the
role of humans as components of the ecosystems and the use of adaptive management. While ecosystem management can be used
as part of a plan forwilderness conservation,
it can also be used in intensively managed ecosystems (see, for example, agroecosystems and close to nature forestry).
Ecosystem
dynamics
Ecosystems are dynamic
entities—invariably, they are subject to periodic disturbances and are in the
process of recovering from some past disturbance. When an ecosystem is subject to some
sort of perturbation, it responds
by moving away from its initial state. The tendency of a system to remain close
to its equilibrium state, despite that disturbance, is termed its resistance. On the other hand, the
speed with which it returns to its initial state after disturbance is called
its resilience.
The theoretical
ecologist Robert
Ulanowicz has used information
theory tools to describe the structure of ecosystems, emphasizing
mutual information (correlations) in studied systems. Drawing on this
methodology and prior observations of complex ecosystems, Ulanowicz depicts
approaches to determining the stress levels on ecosystems and predicting system
reactions to defined types of alteration in their settings (such as increased
or reduced energy flow, and eutrophication.
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