Definition of Ecosystem
An ecosystem consists of the biological community that
occurs in some locale, and the physical and chemical factors that make up its
non-living or abiotic environment. There are many examples of ecosystems -- a
pond, a forest, an estuary, a grassland. The boundaries are not fixed in any
objective way, although sometimes they seem obvious, as with the shoreline of a
small pond. Usually the boundaries of an ecosystem are chosen for practical
reasons having to do with the goals of the particular study.
The study of ecosystems mainly consists of the study
of certain processes that link the living, or biotic, components to the
non-living, or abiotic, components. Energy transformations and biogeochemical
cycling are the main processes that comprise the field of ecosystem
ecology. As we learned earlier, ecology generally is defined as the
interactions of organisms with one another and with the environment in which
they occur. We can study ecology at the level of the individual, the
population, the community, and the ecosystem.
Studies of individuals are concerned
mostly about physiology, reproduction, development or behavior, and studies of populations
usually focus on the habitat and resource needs of individual species, their
group behaviors, population growth, and what limits their abundance or causes
extinction. Studies of communities examine how populations of
many species interact with one another, such as predators and their prey, or
competitors that share common needs or resources.
Component of Ecosystem
You are already familiar with the parts of an
ecosystem. You have learned about climate and soils from past lectures. From
this course and from general knowledge, you have a basic understanding of the
diversity of plants and animals, and how plants and animals and microbes obtain
water, nutrients, and food. We can clarify the parts of an ecosystem by listing
them under the headings "abiotic" and "biotic".
ABIOTIC COMPONENTS
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BIOTIC COMPONENTS
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Sunlight
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Primary producers
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Temperature
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Herbivores
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Precipitation
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Carnivores
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Water or moisture
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Omnivores
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Soil or water chemistry (e.g., P, NH4+)
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Detritivores
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etc.
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etc.
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All of these vary over space/time
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By and large, this set of environmental factors is
important almost everywhere, in all ecosystems.
Usually, biological communities include the
"functional groupings" shown above. A functional group
is a biological category composed of organisms that perform mostly the same
kind of function in the system; for example, all the photosynthetic plants or
primary producers form a functional group. Membership in the functional group
does not depend very much on who the actual players (species) happen to be,
only on what function they perform in the ecosystem.
Process of Ecosystem
This figure with the plants, zebra, lion, and so forth
illustrates the two main ideas about how ecosystems function: ecosystems
have energy flows and ecosystems cycle materials. These
two processes are linked, but they are not quite the same (see Figure 1).
Figure 1.
Energy flows and material cycles.
Energy enters the biological system as light energy,
or photons, is transformed into chemical energy in organic molecules by
cellular processes including photosynthesis and respiration, and ultimately is
converted to heat energy. This energy is dissipated, meaning it is lost to the
system as heat; once it is lost it cannot be recycled. Without the
continued input of solar energy, biological systems would quickly shut down.
Thus the earth is an open system with respect to energy.
Elements such as carbon, nitrogen, or phosphorus enter
living organisms in a variety of ways. Plants obtain elements from the
surrounding atmosphere, water, or soils. Animals may also obtain elements
directly from the physical environment, but usually they obtain these mainly as
a consequence of consuming other organisms. These materials are transformed
biochemically within the bodies of organisms, but sooner or later, due to
excretion or decomposition, they are returned to an inorganic state. Often
bacteria complete this process, through the process called decomposition or
mineralization.
During decomposition these materials are not destroyed
or lost, so the earth is a closed system with respect to elements
(with the exception of a meteorite entering the system now and then). The
elements are cycled endlessly between their biotic and abiotic states within
ecosystems. Those elements whose supply tends to limit biological activity are
called nutrients.
The Transformation of Energy
The transformations of energy in an ecosystem begin
first with the input of energy from the sun. Energy from the sun is captured by
the process of photosynthesis. Carbon dioxide is combined with hydrogen
(derived from the splitting of water molecules) to produce carbohydrates (CHO).
Energy is stored in the high energy bonds of adenosine triphosphate, or ATP
(see lecture on photosynthesis).
The prophet Isaah said "all flesh is grass",
earning him the title of first ecologist, because virtually all energy
available to organisms originates in plants. Because it is the first step in
the production of energy for living things, it is called primary
production. Herbivores
obtain their energy by consuming plants or plant products, carnivores
eat herbivores, and detritivores consume the droppings and
carcasses of us all.
Figure 2 portrays a simple food chain, in which energy from the sun, captured by plant photosynthesis, flows from trophic level to trophic level via the food chain. A trophic level is composed of organisms that make a living in the same way, that is they are all primary producers (plants), primary consumers (herbivores) or secondary consumers (carnivores). Dead tissue and waste products are produced at all levels. Scavengers, detritivores, and decomposers collectively account for the use of all such "waste" -- consumers of carcasses and fallen leaves may be other animals, such as crows and beetles, but ultimately it is the microbes that finish the job of decomposition. Not surprisingly, the amount of primary production varies a great deal from place to place, due to differences in the amount of solar radiation and the availability of nutrients and water.
For reasons that we will explore more fully in
subsequent lectures, energy transfer through the food chain is
inefficient. This means that less energy is available at the herbivore
level than at the primary producer level, less yet at the carnivore level, and
so on. The result is a pyramid of energy, with important implications for
understanding the quantity of life that can be supported.
Usually when we think of food chains we visualize
green plants, herbivores, and so on. These are referred to as grazer food
chains, because living plants are directly consumed. In many
circumstances the principal energy input is not green plants but dead organic
matter. These are called detritus food chains. Examples include
the forest floor or a woodland stream in a forested area, a salt marsh, and
most obviously, the ocean floor in very deep areas where all sunlight is extinguished
1000's of meters above. In subsequent lectures we shall return to these
important issues concerning energy flow.
Finally, although we have been talking about
food chains, in reality the organization of biological systems is much more
complicated than can be represented by a simple "chain". There are
many food links and chains in an ecosystem, and we refer to all of these
linkages as a food web. Food webs can be very complicated, where
it appears that "everything is connected to everything else",
and it is important to understand what are the most important linkages in any
particular food web.
In this article, I will share some of the paludarium construction tips that I have used to successfully construct my own paludarium. Paludarium aquarium is an ancient form of water garden.
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