The ecosystem concept
Almost all ecosystems run on energy captured from the sun by primary producers via photosynthesis. This energy then flows through
the food chains to primary consumers
(herbivores who eat and digest the plants),
and on to secondary
and tertiary consumers
(either carnivores or omnivores). Energy is lost to living
organisms when it is used by the organisms to do work, or is lost as waste heat.
An ecosystem is a natural unit consisting of all
plants, animals and micro-organisms(biotic factors) in an area functioning together with all of
the non-living physical (abiotic) factors of the
environment
The term ecosystem was coined in 1930 by Roy Clapham to denote the combined physical and
biological components of an environment. British ecologist Arthur Tansley later refined the term,
describing it as "The whole system,… including not only the
organism-complex, but also the whole complex of physical factors forming what
we call the environment". Tansley regarded ecosystems not simply as
natural units, but as "mental isolates". Tansley later defined the
spatial extent of ecosystems using the term "ecotope".
Central to the ecosystem concept is the idea that living organisms interact with every other
element in their local environment.
Eugene Odum, a founder of ecology, stated: "Any unit that includes all of
the organisms (ie: the "community") in a given area interacting with
the physical environment so that a flow of energy leads to clearly defined
trophic structure, biotic diversity, and material cycles (ie: exchange of
materials between living and nonliving parts) within the system is an
ecosystem." The human ecosystem concept is then grounded in the deconstruction
of the human/nature dichotomy and the premise
that all species are ecologically integrated with each other, as well as with
the abiotic constituents of their biotope.
A central principle of ecology is that each living
organism has an ongoing and continual relationship with every other element
that makes up its environment. The sum total of interacting living organisms
(the biocoenosis) and their non-living environment
(the biotope) in an area is termed an ecosystem.
Studies of ecosystems usually focus on the movement of energy and matter
through the system.
STRUCTURE AND
FUNCTION
Photosynthetic plants fix carbon from carbon dioxide and nitrogen
from atmospheric nitrogen or nitrates present in the soil to produce amino
acids. Much of the carbon and nitrogen contained in ecosystems is created by
such plants, and is then consumed by secondary and tertiary consumers and
incorporated into themselves. Nutrients are usually returned to the ecosystem
via decomposition. The
entire movement of chemicals in an ecosystem is termed a biogeochemical
cycle, and includes the carbon and nitrogen cycle.
Ecosystems of any size can be studied; for example, a
rock and the plant life growing on it might be considered an ecosystem. This
rock might be within a plain, with many such rocks, small grass, and grazing
animals -- also an ecosystem. This plain might be in the tundra, which is also an ecosystem
(although once they are of this size, they are generally termed ecozones or biomes). In fact, the entire terrestrial
surface of the earth, all the matter which composes it, the air that is
directly above it, and all the living organisms living within it can be
considered as one, large ecosystem.
Ecosystems can be roughly divided into terrestrial ecosystems (including forest ecosystems, steppes, savannas, and so on), freshwater
ecosystems (lakes, ponds and rivers), and marine ecosystems,
depending on the dominant biotope.
Examples of ecosystems
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