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THE FLOW OF ENERGY THROUGH ECOSYSTEMS
THE FLOW OF ENERGY
THROUGH ECOSYSTEMS
The passage of
energy in one direction through an ecosystem is known as energy flow.
Energy enters an ecosystem in the form of the radiant energy of
sunlight. Some of it is trapped by plants during the process of
photosynthesis. Now in chemical form, it is stored in the bonds of
organic (carbon-containing) molecules such as glucose. When these
molecules are broken apart by cell respiration, the energy becomes
available to do work such as repairing tissues, producing body heat, or
reproducing. As the work is accomplished, the energy escapes the living
organism and dissipates into the environment as low-quality heat.
Ultimately, this heat energy radiates into space. Thus, once energy has
been used by living things, it becomes unavailable for reuse.
Producers,
Consumers, and Decomposers
Three categories
based on how they get nourishment: producers, consumers, and
decomposers. Most communities contain representatives of all three
groups, which interact extensively with one another.
Sunlight is the
source of energy that powers almost all life processes on the face of
the Earth-Producers, also called autotrophs (Greek auto, "self," and
tropho, "nourishment"), manufacture complex organic molecules from
simple inorganic substances (carbon dioxide and water), usually using
the energy of sunlight to do so. In other words, producers perform the
process of photosynthesis. By incorporating the chemicals that they
manufacture into their own bodies, producers make their bodies or body
parts a potential food resource for other organisms. Whereas plants are
the most significant producers on land, algae and certain types of
bacteria are important producers in aquatic
Grass, algae,
and photosynthetic bacteria are all important producers. In abyssal hot
spring communities deep in the ocean, non photosynthetic bacteria are
the producers (see Focus On: Life without the Sun).
Animals are
consumers; that is, they use the bodies of other plant and animal
organisms as sources of food energy and body-building materials.
Consumers are also called heterotrophs (Greek heter, "different,"
and tropho, "nourishment"). Consumers that eat producers are
called primary
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consumers,
which usually means that they are exclusively herbivores (plant
eaters). Cattle and deer are examples of primary consumers, as is
the marsh periwinkle in the salt marsh community. Secondary,
consumers which consume primary consumers, include carnivores,
animals that consume other animals exclusively. Lions and tigers are
examples of carnivores, as are the northern diamond-hack terrapin
and the northern water snake in the salt marsh community. Other
consumers, called omnivores, eat a variety of plant and animal
organisms. Bears, pigs, and humans are examples of omnivores; the
meadow vole, which eats both insects and cordgrass in the salt marsh
community, is also an omnivore. Many animals do not fit readily into
one of these three categories because they modify their food
preferences to some degree when the need arises. |
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Some consumers,
called detritus feeders or detritovores, consume the organic matter
originating in plant and animal remains. Detririvores are especially
abundant in aquatic habitats, where they
burrow in the bottom muck and consume the
organic matter that collects there. For example, marsh crabs are
detritus feeders in the salt marsh community. Earthworms are terrestrial
(land-dwelling) detritus feeders, as are termites and maggots (the
larvae of flies). Detritus feeders work together with decomposers to
destroy dead organisms and waste products. An earthworm, for example,
actually eats its way through the soil, digesting much of the organic
matter contained there. Earthworms also aerate the soil and redistribute
its minerals and organic matter with their extensive tunneling.
Decomposers
(also called saprophytes) are heterotrophs chat break down organic
material and use the decomposition products to supply themselves with
energy. They typically release simple inorganic molecules, such as
carbon dioxide and mineral salts that can then be reused by producers.
Bacteria and fungi are important examples of decomposers. Dead wood,
for example, is invaded first by sugar-metabolizing fungi that consume
the wood's simple carbohydrates, such as glucose.
When these
carbohydrates are exhausted, fungi, often aided by termites and
bacteria, complete the digestion of the wood by breaking down cellulose,
a complex carbohydrate that is the main constituent of wood.
Communities such
as the Chesapeake Bay salt marsh contain balanced representations of all
three ecological categories of organisms—producers, consumers, and
decomposers. Producers and decomposers have indispensable roles in
ecosystems. Producers provide both food and oxygen for all life.
Decomposers are also necessary for the long-term survival of any
community because without them, dead organisms and waste products would
accumulate indefinitely. Without decomposers, important
elements such as potassium, nitrogen, and
phosphorus would permanently remain in dead organisms and therefore be
unavailable for use by new generations of living things. Although
consumers are an important part of most ecosystems, they are not
essential to the long-term survival of producers or decomposers.
The Path of
Energy Flow: Who Eats Whom in Ecosystems
Energy flow in
an ecosystem occurs in food chains, in which energy from food passes
from one organism to the next in a sequence. Producers start the food
chain by capturing the respire organic molecules in the remains (the
carcasses and body wastes} of all other members of the food chain.
Each level in a
food chain is called a trophic level. The first trophic level is formed
by producers (photosynthesizes), the second trophic level by primary
consumers (herbivores), the third trophic level by secondary consumers
(carnivores), and so on.
Simple food
chains such as the one just described rarely occur in nature, because
few organisms eat just one other kind of organism. More typically, the
flow of energy and materials through an ecosystem takes place in
accordance with a range of choices of food on the part of each organism
involved. In an ecosystem of average complexity numerous alternative
pathways are possible. Thu1-a food web, a complex of
interconnected food chains in an ecosystem, is a more realistic model of
the flow of energy and materials through ecosystems. (See Focus On:
Changes in Antarctic Food Webs, page 50, for an examination of how
human:-have affected the complex food web in Antarctic.
The most
important thing to remember about energy flow in ecosystems is that it
is linear, or one way. That is, energy can move along a food
chain or food web from one organism to the next as long as it is not
used. When energy is used, it becomes unavailable for use by any other
organism in the ecosystem.
Ecological
Pyramids
An important
feature of energy flow is that most of the energy going from one trophic
level to another in a food chain or food web dissipates into the
environment. The relative energy values of trophic levels are often
graphically represented by ecological pyramids. There are three main
types of pyramids—pyramid of energy.
A pyramid of
numbers shows the number of organisms at each trophic level in a given
ecosystem, with greater numbers illustrated by wider sections of the
pyramid (Figure 3-11). In most pyramids of numbers, each successive
trophic level is occupied by fewer organisms. Thus, in typical grassland
the number of zebras and wildebeests (herbivores) is greater than the
number of lions (carnivores). Reverse pyramids of numbers, in which
higher trophic levels have more organisms than lower trophic levels, are
often observed among decomposers, parasites, tree-dwelling herbivorous
insects, and similar organisms. One tree can provide food fur hundreds
of leaf-eating insects, for example.
A pyramid of
biomass illustrates the total bio-mass at each successive trophic level.
Biomass is a quantitative estimate of the total mass, or amount, of
living material. Their units of measure vary: biomass may be represented
as total volume, as dry weight, or as live weight. Typically, pyramids
of biomass illustrate a progressive reduction of biomass in successive
trophic levels. On the assumption that there is, on the average, about
a 90 percent reduction of biomass for each trophic level,4
10,000 kg of grass should be able to support 1,000 kg of crickets, which
in turn support 100 kg of frogs. By this logic, the biomass of frog
eaters (such as herons) could be, at the most, only about 10 kg. From
this brief exercise you can see that, although carnivores may eat no
vegetation, a great deal of vegetation is still required to support
them.
A pyramid of
energy illustrates the energy relationships of an ecosystem by
indicating the energy content (usually expressed in caloric) of the
biomass of each trophic level. On the whole, energy pyramids resemble
biomass pyramids in shape, but they help to make another consequence of
the nature of trophic levels clearer: most food chains are short
because of the dramatic reduction in energy content that occurs at each
trophic
A secondary
consumer requires an enormous. Home range—the area needed Co obtain
enough food—to encompass all the necessary producers, especially if it
is a large animal. Thus, a large solitary predator such as a tiger may
have a home range exceeding 250 square kilometers (96.5 square miles),
whereas a cottontail rabbit, which occupies a lower trophic level, can
live confortably on 6 hectares (14.8 acres). These area estimates
reflect not only diet, but also other factors such as size of the
organism, so the best comparison of the home ranges of primary consumers
and secondary consumers is between animals similar in every way except
eating habits. Such a comparison is possible, for example, between the
home ranges of two species of mice. Living in the same community, the
seed-eating white-footed mouse requires about 1.5 hectares {3.7 acres),
but the carnivorous grasshopper mouse requires 5 hectares (12.4 acres).
Variation in
Productivity of Ecosystems
The gross
primary productivity of an ecosystem is the rate at which
energy accumulates (as biomass) during photosynthesis—that is, the total
amount of photosynthesis in a given period of time. Of course, plants
must respire to provide energy for their life processes, and cell
respiration acts as a drain on photosynthesis. Energy that remains (as
biomass) after cell respiration have occurred is called net
primary productivity. In other words, net primary productivity
is the amount of biomass found in excess of that broken down by a
plant's cell respiration. Net primary productivity represents the
rate at which organic matter is
actually incorporated into plant bodies so as to produce growth net
primary productivity = plant growth
gross primary productivity — plant respiration
total photosynthesis
Only the energy
represented by net primary productivity is available for the nutrition
of consumers, and of this energy only a portion is actually
utilized by them. Both gross primary productivity and net primary
productivity can be expressed in terms of kilocalories (of energy fixed
by photosynthesis) per square meter per year, or in terms of dry weight
(grams of carbon incorporated into tissue) per square meter per year.
What determines
productivity? A number of factors may interact. Some plants are more
efficient photosynthesizers than others. Environmental factors are also
important. The influx of solar energy,availability of mineral nutrients,
availability of water, and other climatic factors are important, as are
the degree of maturity of the community, the severity of human
modification, and other factors that are difficult to assess. For
example, the high productivity of intertidal communities along an ocean
shoreline is largely due to wave action. Many intertidal organisms are
sedentary detritus filter feeders (such as mussels) that have their food
carried to them by wave action and so need to expend less of their own
energy to obtain food.
Ecosystems
differ strikingly in their productivity. Terrestrial communities are
generally more productive than aquatic ones, partly because of the
greater availability of light for photosynthesis5 and partly
because of higher concentrations of available mineral nutrients.
However, adverse temperatures and lack of water limit the productivity
of certain terrestrial ecosystems. Aquatic ecosystems have an abundance
of water, which moderates temperatures, but are usually limited by the
scarcity of mineral nutrients (especially in the open sea) and the low
light intensity.
The net primary
productivity of an ecosystem tells us little about how much biomass is
present at any given time. Despite plant growth, under natural
conditions there is about as much grass in a section of prairie this
year as there was last year. The reason is that the turnover of plant
biomass from its consumption by animals and decomposers is usually about
the same as the net primary productivity of the ecosystem. It is this
balance that determines the current plant biomass, or standing crop.
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