As community ecology and ecosystem ecology matured, and as popular concern for the loss of species arose in the 1960’s, natural resource management agen-cies began to look at the effects
Trang 1evolutionary history, developmental processes, and
behavioral adaptations and interactions of organisms
from all over the world for the purpose of studying
biodiversity This type of study operates mainly at the
levels of population, species, and communities and
utilizes many subsets of ecology Scientists employ
pa-leoecology to establish historic patterns of
biodiver-sity; genetic ecology, especially DNA techniques, to
study variation and to make genealogical connections
among organisms; telemetry and satellites to study
patterns in distribution of various species; and
com-puter simulations and field experimentation to test
out hypotheses Both genetic and evolutionary
ecol-ogy are important for the conservation of biodiversity
and for developing applications to solve biological
problems
Applied Ecology
Ecology also involves many aspects of applied science
in which the results of scientific study are applied to
real-life situations, from natural resource
manage-ment to urban planning Biotic natural resources
have been managed at the individual and population
levels since the agricultural revolution occurred eight
thousand to ten thousand years ago Until the 1960’s,
forestry, fish, and wildlife management techniques
were aimed at increasing the productivity of single
species—usually game species, such as quail and trout,
or commercial tree species, such as loblolly pine As
community ecology and ecosystem ecology matured,
and as popular concern for the loss of species arose
in the 1960’s, natural resource management
agen-cies began to look at the effects of single-speagen-cies
man-agement techniques on the entire community Range
management has always taken the community ecology
perspective in managing native grass and shrub
com-munities for livestock forage production However,
range conservationists also manage forage
produc-tion for wildlife as well as for livestock Conservaproduc-tion
biology applies the understanding of all ecological
levels in the attempt to prevent species extinction, to
maintain species genetic diversity, and to restore
self-sustaining populations of rare species or entire
com-munities
Population ecology remains the core of these
ap-plied ecological disciplines Population ecology mainly
deals with mortality rates, birthrates, and migration
into and out of local populations These are the biotic
factors that influence population size and
productiv-ity The goal of consumptive natural resource
man-agement is the harvesting of population or community productivity The goal of nonconsumptive natural resource management is to manage for natural aes-thetic beauty, for the maintenance of diverse commu-nities, for the stability of communities and ecosystems, and for a global environment that retains regional bi-otic processes
Issues in Ecology Among the applications of ecological studies are some
of the following:
• climate change; and global warming;
• loss of species populations and concomitant loss
of biodiversity, including threatened species and endangered species (such as the collapse of bee colonies important for pollination) and the intro-duction of exotic invasive species into unnatural habitats;
• changes in global ocean currents and their effect
on terrestrial biomes such as forests and deserts;
• human activities, including the release of pollut-ants and their impact on the food chain and animal species, and global resource consumption levels and their impact on ecosystems, land conversion and habitat loss, infrastructure development, and overexploitation;
• blockage of solar energy and holes in the ozone layer; and
• the potential impact of space debris on the global environment
Internationally, environmental scientists and oth-ers are entering into treaties, conducting serious dis-cussions at global conferences, and collaborating on solutions to resolve these and many other issues— including the availability of food and other re-sources—that may affect future survival Making hu-mans aware of the many ecological concerns and gaining their support in protecting, conserving, and preserving the environment and global resources for future generations, thus enhancing the health of the Earth, may be the most important goal of the study of ecology
James F Fowler, updated by Carol A Rolf
Further Reading
Bertorelle, Giorgio, et al Population Genetics for Animal Conservation New York: Cambridge University
Press, 2009
Trang 2Cain, Michael L., William D Bowman, and Sally D.
Hacker Ecology Sunderland, Mass.: Sinauer
Associ-ates, 2008
Morin, Peter Jay Community Ecology 2d ed Oxford,
Oxfordshire, England: Blackwell, 2008
Sherratt, Thomas N., and David M Wilkinson Big
Questions in Ecology and Evolution New York: Oxford
University Press, 2009
Weisman, Alan The World Without Us New York:
Pica-dor, 2008
Web Sites
Cell Press
Trends in Ecology and Evolution
http://www.trends.com/tree/default.htm
Ecology Global Network
http://ecology.com/index.php
The Global Education Project
http://www.theglobaleducationproject.org/earth/
global-ecology.php
See also: Aggregates; Conservation biology; Deep
ecology; Ecosystems; Ecozones and biogeographic
realms; Fisheries; Food chain; Forest management;
Overgrazing; Species loss; Wildlife; Wildlife biology
Ecosystem services
Category: Ecological resources
Ecosystem services are the means by which societal
efits and support are provided by ecosystems Such
ben-efits and support are also known as natural capital.
They include climate regulation, water availability,
the maintenance of wildlife and their habitats, fodder,
and the production of raw materials such as wood,
fi-ber, medicines, and a range of foods All are
funda-mental components in people-environment
relation-ships, given their necessity for human well-being, and
all contribute to the provision and/or maintenance of
global resources.
Background
Ecosystem services are closely linked with
biogeochem-ical cycles and energy transfer In biogeochembiogeochem-ical
cy-cles nutrients are continuously transferred between
the constituent parts of the Earth’s surface: rocks,
soils, water (freshwater and marine), plants, animals, and the atmosphere These processes are vital in en-ergy transfers within food chains and webs The spa-tial and temporal distribution of these processes is de-termined to a large extent by climatic characteristics but also influences global climate via the carbon cycle Such processes affect the quality of the “commons” (air, water, oceans), the maintenance of which is es-sential to human well-being These processes also control the natural capital that accrues within all eco-systems and that is used for society’s needs Ecosystem services underpin all human activity through the con-tinuous generation of resources and the environmen-tal processes that are essential to that generation In-evitably, ecosystem services are complex, are under pressure from a growing global population, and
re-quire careful management The Millennium Ecosystem Assessment (MEA), compiled as a collaborative effort
by 1,360 scientists worldwide between 2001 and 2005, summarizes the state of and major trends in global ecosystems and their services under the four headings used below
Supporting Services The primary supporting services are nutrient cycling, soil formation, and primary production Nutrient, or biogeochemical, cycling involves the transfer of ele-ments and compounds within and between the bio-sphere (organisms and their environment), atmo-sphere, and pedosphere (soils) They consist of pools
or stores between which fluxes occur For example, in the carbon cycle the major pools are living organisms, dead organic matter, the oceans, and the atmosphere Fluxes occur between these pools at rates that vary ac-cording to factors such as climate Nutrient cycles also link the inorganic and organic components of the en-vironment and operate at various spatial and tempo-ral scales For example, photosynthesis, respiration, and decomposition link microbes, plants, and ani-mals with water, soils, and the atmosphere through carbon, hydrogen, nitrogen, phosphorus, and many other elemental cycles Most major nutrients—carbon
is the most obvious example—have a pool in the at-mosphere and are thus an influence on climate These are gaseous biogeochemical cycles Those nutrients without an atmospheric pool—for example, phos-phorus, iron, and calcium—are sedimentary biogeo-chemical cycles
Soil formation involves the breakdown of solid bedrock into small particles by biological, chemical,
Trang 3and physical processes known collectively as
weather-ing Dead organic matter from microbes, insects, and
pioneer plants is mixed with the particles to create
new habitats for organisms; this aids water retention,
which continues the weathering process and
con-tributes to the release of nutrients for use by plants
Many factors—the most important being climate—
influence the processes and rates of soil formation,
water availability, and degree of acidity or alkalinity
Primary production is the amount of organic
mat-ter produced per unit area per unit time by organisms
that can photosynthesize (green plants on land and
algae in the oceans) These organisms have the ability
to absorb solar energy and convert it to chemical
en-ergy through the generation of complex organic
com-pounds such as sugars and carbohydrates Although
less than 1 percent of the solar energy that reaches
Earth is used in photosynthesis, this small amount
fu-els the biosphere Primary production is the first stage
in energy transfer through ecosystems and is thus the
basis of all food chains and webs All animals,
includ-ing humans, depend on primary production for
sur-vival—not only for food and shelter but also for a wide
range of goods, including fiber, wood, and medicine
Rates of primary production (primary productivity)
are influenced by environmental factors such as water
availability, annual temperature regimes, soil types,
and nutrient availability Nutrient cycling, soil
forma-tion, and primary production are vital for the
ecosys-tem services described below
Provisioning Services
Provisioning services encompass food, wood, fiber,
genetic resources, fuel, and fresh water Primary
pro-duction on land and in the oceans underpins the
gen-eration and replenishment of many resources on
which humanity depends Apart from fossil fuels,
these are all renewable resources and are all organic
or biological in origin The provision of fresh water is
renewable but is inorganic in essence, though
influ-enced by ecosystem (biological) characteristics
Global food production is a vast enterprise that
es-sentially processes carbon and is a major generator of
wealth It involves crop and animal agriculture at
vari-ous scales (subsistent or commercial); may have a
fos-sil-fuel subsidy, as in the case of “industrialized”
agri-culture; and requires a reliable supply of fresh water
An indication of the magnitude of this production is
reflected in the Food and Agriculture Organization’s
(FAO’s) 2006 data for the major staple crops: 695
mil-lion metric tons of maize, 634 milmil-lion metric tons of rice, and 605 million metric tons of wheat A propor-tion of this is used as animal feed to create secondary productivity such as meat and milk products These and other crops, including cotton fiber, are produced
on about 15 million square kilometers of cropland
An increasing proportion of crop production— notably that of corn, soybean, and canola—is used to generate biofuels, while several crops are grown spe-cifically as biofuels However, the value of growing ma-terials to use as biofuels is controversial because the crops take up land that could be used for food produc-tion An additional roughly 28 million square kilome-ters of pasture support a large proportion of the world’s cattle and sheep Cotton is the world’s major fiber; about 25 million metric tons were produced in 2005
Fish derived from inland and marine waters form
an important component of human diets According
to FAO statistics, some 141.4 million metric tons of fish were produced in 2005, about 35 percent of which was from inland waters, where aquaculture pre-dominates, and about 65 percent of which was from marine waters, where the harvesting of wild popula-tions is predominant Some 97 percent of this is con-sumed directly by humans; the remainder is pro-cessed for animal feed However, the global fishing industry is facing problems because fish stocks have been seriously depleted The reduction or loss of this service illustrates the difficulties that arise when con-servation and management are inadequate: Marine ecosystems are altered and social consequences arise The world’s natural forests and plantations are an-other major resource with a host of uses, the most im-portant of which are as materials for construction, furniture, fencing, pulp and paper, garden products, and fuel Forests are also a source of nonwood re-sources, including nuts, berries, fodder, and game In
2007, about 3.6 billion cubic meters of roundwood was produced globally The chief producers were India, China, the United States, Brazil, and Canada The proportion removed for wood fuel is unknown However, the loss of forest cover because of agricul-ture, logging, and poor management reduces the capacity of the terrestrial biosphere to store carbon FAO indicates that between 1990 and 2005 carbon stocks in forest biomass decreased by 1.1 billion met-ric tons of carbon annually; this reflects impairment
of an ecosystem service
The organisms in the world’s ecosystems contain a
Trang 4wealth of genetic resources with vast potential
Biodi-versity prospecting is the term given to programs
de-signed to tap this resource by identifying species and
screening them for useful properties such as crop
pro-tection chemicals and pharmaceuticals About 25
per-cent of prescription medicines are plant based,
in-cluding the widely used aspirin, while the bacterium
Bacillus thuringiensis is the basis of insect pest control
in a range of crops The bacterium itself is produced
as a commercial spray, but the gene component
re-sponsible for insect mortality has been identified and
inserted into a number of crops, notably cotton and
maize, so that these genetically modified varieties
pro-duce their own insecticide As further advances in
bio-technology and genetic modification ensue, further
opportunities to harness genetic resources will arise
Fossil fuels are also generated through primary
productivity but relate to geological eras many
mil-lions of years in the past, when the carbon cycle
in-volved the storage or sequestration of huge volumes
of plant-based carbon in reservoirs that eventually
be-came rocks For example, coal formed in wetlands,
and limestone formed in the oceans These processes
continue to operate but at such slow rates that fossil
fuels cannot be considered renewable
Fresh water, a vital resource for human well-being,
is renewable It is a component of the hydrological
cycle, a fundamental facilitating factor in ecosystem
and society functioning Water from precipitation
reaches the Earth’s surface and its subsequent
pas-sage depends largely on how evaporation, recharge of
groundwater reservoirs, and runoff are affected by
the ecosystems through which it passes Forest and
mountain ecosystems are especially important in this
context, accounting for about 85 percent of total
run-off, which supports approximately 4 billion of the
world’s estimated 6.7 billion people Cultivated land
accounts for most of the remainder Wetlands are also
important as water stores and hydrological regulators
Regulating Services
Climate, flood, and disease regulation, water
purifica-tion, and pollination are major regulating services
Climate and the Earth’s ecosystems have been
inter-dependent throughout geologic time; the major link
between the two is the global carbon cycle, though
other biogeochemical cycles are also involved This
mutual development has manifested in various ways
but is especially significant in terms of global
tempera-ture regimes and atmospheric composition
The Earth and its atmosphere form a closed sys-tem, or nearly so, in terms of chemical constitution The redistribution of atoms and molecules between the Earth’s core, lithosphere, biosphere, and atmo-sphere has been, and continues to be, mediated by life-forms on land and in the oceans Overall, this rela-tionship has maintained life in the biosphere and helped to spur evolution It also has caused major shifts in the carbon cycle as carbon is removed from the atmosphere into the biosphere and, eventually, the lithosphere The evolution of photosynthesis, for example, was particularly important because it not only fixed carbon from the atmosphere but also re-leased oxygen, paving the way for the evolution of mammals, including humans
Beginning with the Industrial Revolution, humans began to alter the carbon cycle profoundly through fossil-fuel consumption and deforestation Evidence indicates that these may contribute to global warm-ing The speed of the alteration in the carbon cycle
is more rapid than the gradual processes that charac-terize the geological past; thus, concerns about seri-ous consequences for human well-being seem to be justified
Flood regulation is a function of all ecosystems but
is most important in forests, grasslands, and wetlands Following receipt of high rainfall or snowfall such eco-systems store water in the vegetation and soils and temper its release to groundwater, streams, and rivers This reduces the impact of floodwaters on ecosystems and society in built-up areas like river valleys, estuar-ies, and deltas Degradation of upstream ecosystems can impair this capacity and imperils millions of peo-ple Erosion control is also linked with the preserva-tion of an adequate vegetapreserva-tion cover in river catch-ments and safeguards downstream land use and settlements The passage of water through ecosys-tems—in which vegetation, microorganisms, and soils act as filters—contributes to water purification Pol-lutants such as metals, excess nutrients such as nitro-gen, and sediments are removed, which improves conditions for downstream ecosystems and land use Many diseases experienced by crops and animals (including humans) are influenced by ecosystem di-versity; pest and disease outbreaks are not likely in biodiverse regions because the passage of viruses is made difficult by the buffering capacity of non-host species The natural control of vectors is also en-hanced with high biodiversity
Pollination is another vital ecosystem service It
Trang 5cilitates the sexual reproduction of many plants,
in-cluding crops, with genetically diverse offspring as a
result Without such fertilization, fruiting would not
occur Many animal species—bats, birds, and insects
such as bees, butterflies, flies, moths, and beetles—
are involved in pollination About 33 percent of
hu-man food production depends on these wild
pollina-tors; thus, the service is of economic importance
Cultural Services
Cultural services—aesthetic, spiritual, educational,
and recreational—do not provide immediately
tangi-ble resources akin to food, for example, but they
con-tribute to human well-being in many ways
Further-more, in the context of education, they may improve
understanding of ecosystem form and function and
contribute to sustainable management strategies
Dis-tinct types of ecosystem provide a sense of place,
influ-ence culture, inspire art forms, and are important
in many religions Wealth generation—through the
value of landscape, wildlife, and recreation—is
an-other cultural ecosystem service Other forms of
em-ployment, such as forestry, conservation, and
man-agement, also contribute to wealth generation
Future Context
Global population is estimated to increase to 8 billion
by 2030 This will compound pressure on already
stretched ecosystem services and require an increase
in food production by at least 25 percent According
to the MEA, humans have altered global ecosystems
more substantially since the mid-twentieth century
than at any other time in history This happened
be-cause of a threefold growth in population, rapid
con-version of forests and grasslands to agricultural land,
technologies such as automobiles requiring fossil
fu-els, and rising standards of living that encompass
in-creased resource use More than half of the services
provided are being degraded mostly at the expense of
the poorest people One aspect of this degradation is
the high rate of plant and animal extinction such as
the loss of genetic resources, a process that, unlike
many other environmental problems, is irreversible
Unsustainable practices and resulting inequity require
immediate attention from local, national, and
inter-national political and environmental institutions Each
requires the inventory and valuation of ecosystem
ser-vices, monitoring, investment in management,
educa-tion programs, and cooperaeduca-tion at all scales
A M Mannion
Further Reading
Botkin, Daniel B., and Edward A Keller Environmen-tal Science: Earth as a Living Planet 7th ed New York:
John Wiley & Sons, 2009
Mannion, Antoinette M Carbon and Its Domestication.
Dordrecht, Netherlands: Springer, 2006
Melillo, Jerry, and Osvaldo Sala “Ecosystem
Ser-vices.” In Sustaining Life: How Human Health De-pends on Biodiversity, edited by Eric Chivian and
Aaron Bernstein New York: Oxford University Press, 2008
Ninan, K N., ed Conserving and Valuing Ecosystem Ser-vices and Biodiversity: Economic, Institutional and So-cial Challenges Sterling, Va.: Earthscan, 2008.
Web Sites Food and Agriculture Organization of the United Nations
FAOSTAT http://faostat.fao.org/default.aspx Millennium Ecosystem Assessment Millennium Assessment 2009
http://www.millenniumassessment.org/en/
index.aspx See also: Agriculture industry; Biosphere; Carbon cy-cle; Ecology; Ecosystems; Ecozones and biogeo-graphic realms; Fisheries; Geochemical cycles; Green-house gases and global climate change; Hydrology and the hydrologic cycle; Natural capital; Nitrogen cycle; Phosphorus cycle
Ecosystems
Category: Ecological resources
An ecosystem is formed by the complex interactions of a community of individual organisms of different spe-cies with one another and with their abiotic (nonliv-ing) environment.
Background
A biological community consists of a mixture of popu-lations of individual species; a population consists of potentially interbreeding members of a species Indi-vidual organisms interact with members of their own species as well as with other species An ecosystem is
Trang 6formed by this web of interactions among species
along with the physical, chemical, and climatic
condi-tions of the area
Abiotic environmental conditions include
temper-ature, water availability, soil nutrient content, and
many other factors that depend on the climate, soil,
and geology of an area Living organisms can alter
their environment to some degree A canopy formed
by large forest trees, for example, will change the
light, temperature, and moisture available to
herba-ceous plants growing near the forest floor The
envi-ronmental conditions in a particular area can also be
affected by the conditions of neighboring areas; the
disturbance of a stream bank can lead to erosion,
which will affect aquatic habitat for a considerable
dis-tance downstream It can be difficult to anticipate the
wide-ranging affects of ecosystem disturbance
Species and individuals within an ecosystem may
interact directly with one another through the
ex-change of energy and material Predators, for
exam-ple, obtain their energy and nutritional needs through consumption of prey species Organisms also interact indirectly through modification of their surrounding environment Earthworms modify soil structure phys-ically, affecting aeration and the transport of water through the soil In turn, these alterations of the phys-ical environment affect root growth and development
as well as the ability of plants to secure nutrients Ecosystems are not closed systems: Energy and ma-terial are transferred to and from neighboring sys-tems The flow of energy or material between the components of an ecosystem, and exchanges with neighboring ecosystems, are governed by functions of the abiotic and biotic ecosystem components These ecological processes operate simultaneously at many different temporal and spatial scales At the same time that a microorganism is consuming a fallen leaf, the process of soil formation is occurring through chemi-cal and physichemi-cal weathering of parent material; plants are competing with one another for light, water, and
Taiga, featuring coniferous forests and located in the northern portion of the Northern Hemisphere, is one type of ecosystem (©Irina
Bekulova/Dreamstime.com)
Trang 7nutrients; and weather may be changing—a storm
front, for example, may be approaching
Ecosystem Boundaries and Temporal Scales
Because of the exchange of energy and material, it is
not possible to draw clear boundaries around an
eco-system A watershed is formed by topographic
condi-tions forming physical barriers guiding the
gravita-tional flow of water, yet wind carries seeds and pollen
over these barriers, and animals can still move from
watershed to watershed The strength of the
interac-tions among neighboring systems is the basis on which
humans delineate ecosystem boundaries In truth, all
ecosystems around the world interact with one
an-other to some degree or anan-other
Ecological processes operate at many different
timescales Some operate over such long timescales
that they are almost imperceptible to human
observa-tion The process of soil formation occurs over many human life spans Other processes operate over ex-tremely short time intervals The reproduction of soil bacteria, the response of leaves to changing tempera-ture over the length of a day, and the time required for chemical reactions in the soil are all very short when compared to a human life span Usually the timescale
of a process is related to its spatial scale; processes that operate at short timescales also tend to operate over short distances
Ecosystem Disturbance Ecosystems are subject to disturbance, or perturba-tion, when one or more ecosystem processes are inter-rupted Disturbance is a natural ecological process, and the character of many ecosystems is shaped by natural disturbance patterns The successful repro-duction of many prairie species may be dependent on
Gazelles graze on an African savanna, one type of ecosystem (©Birute Vijeikiene/Dreamstime.com)
Trang 8periodic fire Suppression of fire as a means of
pro-tecting an ecosystem may lead to the local extinction
of small plants, which depend on periodic fires to
in-crease light availability by removing larger grasses and
providing nutrients to the soil The formation of
sand-bars in streams may be controlled by periodic flood
events that remove great amounts of sediment from
stream banks Protection of existing ecosystems can
depend on the protection or simulation of natural
dis-turbances This is even true of old-growth forests; the
natural disturbance interval due to fire or windstorm
may be centuries, and yet interruption of the natural
disturbance pattern may lead to shifts in species
com-position or productivity
Increasing the frequency of disturbance can also
affect ecosystem structure and function Repeated
vegetation removal will favor species that take
advan-tage of early-successional conditions at the expense of
species that are more adapted to late-successional
conditions In order to ensure continued functioning
of ecosystem processes and the survival of all species,
it is necessary to have a mix of systems in
early-successional and late-early-successional stages in a
land-scape Human resource utilization must be managed
within this context in order to ensure the long-term
sustainability of all ecosystem components and to
re-duce the chances of extinction of some species
be-cause of human alteration of natural disturbance
in-tervals
Ecosystem Stability
A system is stable if it can return to its previous
condi-tion at some time after disturbance The length of
time required to return to the original condition is
the recovery time Stability is an important property
of ecosystems that are utilized by humans The
recov-ery of fish populations, the reestablishment of a forest
following harvesting, and the renewed production of
forage following grazing all depend on the inherent
stability of the affected ecosystem The stability of an
ecosystem is dependent on its components and their
interrelationships Disturbance may primarily affect
one component of an ecosystem, as with salmon
fish-ing in the Pacific Ocean The ability of the entire
eco-system to adjust to this disturbance depends on the
complexities of the interrelationships between the
sal-mon, their predators and prey, and their competitors
The length of the recovery time varies with the type
of system, the natural disturbance interval, and the
se-verity of the disturbance The population of algae
along the bottom of a streambed may be severely dis-turbed by spring flooding, yet may be resilient and re-turn to its pre-disturbance condition in a short time A forest containing one-thousand-year-old mature trees may be extremely resilient and able eventually to rees-tablish itself following a windstorm or harvesting, but the recovery time extends over many human life-times
There are species that require disturbance in order
to regenerate themselves These species may be pres-ent in great abundance following a disturbance Their abundance then decreases over time, and if there is
no disturbance to renew the population, they will eventually die out and no longer be present in the ecosystem
A system is usually stable only within some bounds
If disturbed beyond these recovery limits the system may not return to its previous state but may settle into
a new equilibrium There are examples in the Medi-terranean region of systems that were overgrazed in ancient times and that have never returned to their previous species composition and productivity Forest managers, farmers, fishermen, and others must un-derstand the natural resiliency of the systems within which they work and stay within the bounds of stability
in order to ensure sustainable resource utilization into the future
Matter and Energy Cycles Ecological processes work through the cycling of mat-ter and energy within the system Nutrient cycling consists of the uptake of nutrients from the soil and the transfer of these nutrients through plants, herbi-vores, and predators until their eventual return to the soil to begin the cycle anew Interruption of these cy-cles can have far-reaching consequences in the sur-vival of different ecosystem components These cycles also govern the transport and fate of toxic substances within a system It took many years before it was real-ized that persistent pesticides such as dichloro-diphenyl-trichloroethane (DDT) would eventually be concentrated in top predators, such as raptors The decline in populations of birds of prey because of reproductive failure caused by DDT was a conse-quence of the transport of the chemical through eco-system food webs Likewise, radionucleides from the disaster at the Chernobyl nuclear reactor have be-come concentrated in certain components of the eco-systems where they were deposited This is particu-larly true of fungi, which take radionucleides and
Trang 9heavy metals from their food sources but do not shed
the substances Humans eating mushrooms from these
forests can receive larger than expected doses of
radi-ation, since the concentration in the fungi is much
greater than in the surrounding system
A basic understanding of ecosystem properties and
processes is critical in designing management
meth-ods to allow continued human utilization of systems
while sustaining ecosystem structure and function
With increasing human population and advancing
liv-ing standards, more and more natural ecosystems
have been pushed to near their limits of stability It is
therefore critical for humans to understand how
eco-systems are structured and function in order to
en-sure their sustainability in the face of continued, and
often increasing, utilization
David D Reed
Further Reading
Aber, John D., and Jerry M Melillo Terrestrial
Ecosys-tems 2d ed San Diego, Calif.: Harcourt Academic
Press, 2001
Allen, T F H., and Thomas W Hoekstra Toward a
Unified Ecology New York: Columbia University
Press, 1992
Bormann, F Herbert, and Gene E Likens Pattern and
Process in a Forested Ecosystem: Disturbance,
Develop-ment, and the Steady State Based on the Hubbard Brook
Ecosystem Study New York: Springer, 1979.
Dickinson, Gordon, and Kevin Murphy Ecosystems 2d
ed New York: Routledge, 2007
Golley, Frank Benjamin A History of the Ecosystem
Con-cept in Ecology: More than the Sum of the Parts New
Ha-ven, Conn.: Yale University Press, 1993
H John Heinz III Center for Science, Economics, and
the Environment The State of the Nation’s Ecosystems
2008: Measuring the Lands, Waters, and Living
Re-sources of the United States Washington, D.C.: Island
Press, 2008
Hobbs, Richard J., and Katharine N Suding, eds New
Models for Ecosystem Dynamics and Restoration
Wash-ington, D.C.: Island Press, 2009
Schilthuizen, Menno The Loom of Life: Unravelling
Eco-systems Berlin: Springer, 2008.
Trudgill, Stephen The Terrestrial Biosphere:
Environ-mental Change, Ecosystem Science, Attitudes, and Values.
New York: Prentice Hall, 2001
Williams, R J P., and J J R Fraústo da Silva The
Chem-istry of Evolution: The Development of Our Ecosystem.
Boston: Elsevier, 2006
See also: Biodiversity; Biosphere; Carbon cycle; Con-servation; Ecology; Ecosystem services; Ecozones and biogeographic realms; Endangered Species Act; Ni-trogen cycle; Species loss; Sustainable development
Ecozones and biogeographic realms
Categories: Ecological resources; environment, conservation, and resource management; plant and animal resources
Ecozones and biogeographic realms are large-scale classifications that help scientists assess population sizes, histories, and locations of plant and animal spe-cies worldwide The information aids the manage-ment and conservation of biological resources and is used to guide the choices of natural United Nations Educational, Scientific and Cultural Organization (UNESCO) World Heritage sites It also provides clues
to how species evolved.
Background Biogeography is the study of the distribution of living organisms in the world, past and present “Ecozone” (short for “ecological zone”), “biogeographic realm,”
“life zone,” and “biogeographic zone” are broadly syn-onymous terms for the major physical demarcations
in this distribution These terms are similar to the concept of the biome However, whereas a biome is generally held to be a major community defined by principal vegetation and animal groups adapted to a particular environment, the ecozone takes into ac-count the geological and evolutionary history of a region
The idea for dividing the biosphere into distinct re-gions based on biological criteria dates to scientist-explorers of the eighteenth and early nineteenth cen-turies In 1778, after sailing around the world with Captain James Cook, the English scientist J R Forster claimed that the world was composed of belts of simi-lar vegetation, each fostered by a distinct climate In
1804, German scientist Alexander von Humboldt, considered by many to be the father of biogeography, built upon Forster’s conclusions to demonstrate that vegetation varied regularly in accordance with alti-tude just as it did with distance from the equator
Trang 10Biogeographic Realms
Miklos D F Udvardy proposed the modern
biogeo-graphic realm schema in a 1975 paper, “A
Classifica-tion of the Biogeographic Provinces of the World.” He
defined a biogeographic realm as a continental or
subcontinent region with unifying features of
geogra-phy and plant and animal life Each realm could
be further divided into subrealms, or biogeographic
provinces, and these into subprovinces, districts, and
subdistricts, in order to define more precisely local
variations in species types and distribution
Udvardy recognized eight major biogeographic
realms Each represents a region in which life-forms
have adapted as a community to climatic conditions
The realms draw upon the established five classes of
biomes to identify vegetation-climate interrelations:
tropical humid rain forests, subtropical and
temper-ate rain forests, tempertemper-ate needle-leaf forests, tropical
dry or deciduous forests, and temperate broad-leaf
forests and subpolar deciduous thickets The Nearctic
Realm, comprising 22.9 million square kilometers of
the Earth’s surface, includes most of North America
The Palearctic Realm, comprising 54.1 million square
kilometers, covers most of Eurasia and North Africa
The Afrotropical Realm, comprising 22.1 million
square kilometers, contains sub-Saharan Africa The
Indomalayan Realm, comprising 7.5 million square
kilometers, includes Afghanistan-Pakistan, South Asia,
and Southeast Asia The Oceanic Realm, comprising
1 million square kilometers, groups together
Polyne-sia, Fiji, and Micronesia The Australian Realm, which
is 7.7 million square kilometers, similarly groups
to-gether Australia, New Guinea, and associated islands
The Antarctic Realm, 0.3 million square kilometers,
comprises the continent Antarctica Finally, the
Neo-tropical Realm, 19 million square kilometers, includes
South America and the Caribbean
Ecozones
Although the terms “ecozone” and “ecological zone”
are used with varying meanings by others, Jürgen
Schultz supplied the definitive treatment of the
con-cept In The Ecozones of the World (2005), he defines an
ecozone as a large region of land where physical
char-acteristics, such as climate, soil type, landscape, and
geology, create a distinctive environment that
sup-ports a mixture of plant life that in turn supsup-ports a
mixture of animal species As do other classification
schemes, Schultz’s recognizes that vegetation is the
salient feature of a region, and he organizes the
eco-zones spatially by relating vegetation to climate and (as some classification schemes do not) seasonal varia-tions in climate Schultz emphasizes that no strict bor-ders separate the ecozones; rather, they are concen-trations of highly uniform life and landscape Shultz recognizes nine ecozones The polar subpo-lar zone includes the areas between the North and South Poles and their respective polar tree lines, 22 million square kilometers All of it lies within the area
of permafrost; some parts are ice-covered (polar deserts), and some are tundra or bare rock It is quite barren, characterized by very low average tempera-ture, precipitation, and biological production; a short growing season; and low total biomass
The boreal zone, found only in the Northern Hemi-sphere, covers 20 million square kilometers and gen-erally extends from the polar tree line to the central steppes (grassy plains) It is best known as a region of coniferous forests
Most of the temperate midlatitudes zone also is lo-cated in the Northern Hemisphere—in eastern and western Eurasia and North America—although there are small areas of it in South America, Australia, and New Zealand It includes 14.5 million square kilome-ters in narrow corridors between boreal evergreen forests and steppes It is moderate in most of its char-acteristics, such as average temperature, precipita-tion, growing season, and total biomass
The dry midlatitudes zone occupies small areas of North America, large swaths of east-central Eurasia, the eastern part of Patagonia in South America, and part of New Zealand, for a total area of 16.5 million square kilometers Although this zone has various subdivisions, it is arid, with at most five months of plant growth and widely dispersed plants, such as cac-tus, adapted to dry, salty soils
The subtropics with winter rain zone includes 2.5 million square kilometers, most of it along the Medi-terranean coasts of Europe and western North Africa, but it also includes areas in southern Australia Be-cause the Euro-African and the Australia areas are so far apart, their plant and animal life vary considerably The subtropics with year-round rain zone includes
6 million square kilometers total; parts of it occur in the south of the United States, southern China, south-eastern South America, south-eastern South Africa, and eastern Australia The zone sees high average temper-ature and precipitation, a long growing season, and very large biomass
The dry tropics and subtropics zone is the largest: