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Portal:Ecology

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Ecology

Ecology (from Ancient Greek οἶκος (oîkos) 'house' and -λογία (-logía) 'study of') is thenatural science of the relationships among livingorganisms and theirenvironment. Ecology considers organisms at the individual,population,community,ecosystem, andbiosphere levels. Ecology overlaps with the closely related sciences ofbiogeography,evolutionary biology,genetics,ethology, andnatural history.

Ecology is a branch ofbiology, and is the study ofabundance,biomass, and distribution of organisms in the context of the environment. It encompasses life processes, interactions, andadaptations; movement of materials andenergy through living communities;successional development of ecosystems; cooperation, competition, and predation within and betweenspecies; and patterns ofbiodiversity and its effect on ecosystem processes.

Ecology has practical applications in fields such asconservation biology,wetland management,natural resource management, andhuman ecology.

The termecology (German:Ökologie) was coined in 1866 by the German scientistErnst Haeckel. The science of ecology as we know it today began with a group of American botanists in the 1890s.Evolutionary concepts relating to adaptation andnatural selection are cornerstones of modernecological theory.

Ecosystems are dynamically interacting systems of organisms, the communities they make up, and the non-living (abiotic) components of their environment. Ecosystem processes, such asprimary production,nutrient cycling, andniche construction, regulate the flux of energy and matter through an environment. Ecosystems havebiophysical feedback mechanisms that moderate processes acting on living (biotic) and abiotic components of the planet. Ecosystems sustain life-supporting functions and provideecosystem services likebiomass production (food, fuel, fiber, and medicine), the regulation ofclimate, globalbiogeochemical cycles,water filtration,soil formation,erosion control, flood protection, and many other natural features of scientific, historical, economic, or intrinsic value. (Full article...)

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This stream operating together with its environment can be thought of as forming a river ecosystem.

River ecosystems are flowing waters that drain the landscape, and include thebiotic (living) interactions amongst plants, animals and micro-organisms, as well asabiotic (nonliving) physical and chemical interactions of its many parts. Riverecosystems are part of largerwatershed networks or catchments, where smallerheadwater streams drain into mid-size streams, which progressively drain into larger river networks. The major zones in river ecosystems are determined by the river bed's gradient or by the velocity of the current. Faster moving turbulent water typically contains greater concentrations ofdissolved oxygen, which supports greater biodiversity than the slow-moving water of pools. These distinctions form the basis for the division of rivers intoupland and lowland rivers.

The food base of streams within riparian forests is mostly derived from the trees, but wider streams and those that lack acanopy derive the majority of their food base fromalgae.Anadromous fish are also an important source ofnutrients. Environmental threats to rivers include loss of water, dams, chemical pollution andintroduced species. Adam produces negative effects that continue down the watershed. The most important negative effects are the reduction ofspring flooding, which damageswetlands, and the retention ofsediment, which leads to the loss of deltaic wetlands. (Full article...)

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Schoolingbigeye trevally. Inbiology, any group offish that stay together for social reasons are said to be shoaling and if the group is swimming in the same direction in a coordinated manner, they are said to be schooling.

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Entries here consist ofGood andFeatured articles, which meet a core set of high editorial standards.

Climate is the long-termweather pattern in a region, typically averaged over 30 years. More rigorously, it is the mean andvariability ofmeteorological variables over a time spanning from months to millions of years. Some of themeteorological variables that are commonly measured aretemperature,humidity,atmospheric pressure,wind, andprecipitation. In a broader sense, climate is the state of the components of theclimate system, including theatmosphere,hydrosphere,cryosphere,lithosphere andbiosphere and the interactions between them. The climate of a location is affected by itslatitude,longitude,terrain,altitude,land use and nearbywater bodies and their currents.

Climates can beclassified according to the average and typical variables, most commonlytemperature andprecipitation. The most widely used classification scheme is theKöppen climate classification. TheThornthwaite system, in use since 1948, incorporatesevapotranspiration along with temperature andprecipitation information and is used in studyingbiological diversity and howclimate change affects it. The major classifications in Thornthwaite's climate classification are microthermal, mesothermal, and megathermal. Finally, the Bergeron andSpatial Synoptic Classification systems focus on the origin of air masses that define the climate of a region. (Full article...)

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Charles Robert Darwin (/ˈdɑːrwɪn/DAR-win; 12 February 1809 – 19 April 1882) was an Englishnaturalist,geologist, andbiologist, widely known for his contributions toevolutionary biology. His proposition that allspecies of life have descended from acommon ancestor is now generally accepted and considered a fundamental scientific concept. In a joint presentation withAlfred Russel Wallace, he introduced his scientific theory that thisbranching pattern ofevolution resulted from a process he callednatural selection, in which thestruggle for existence has a similar effect to the artificial selection involved inselective breeding. Darwin has been described as one of the most influential figures inhuman history and was honoured byburial in Westminster Abbey.

Darwin's early interest in nature led him to neglect his medical education at theUniversity of Edinburgh; instead, he helpedGrant to investigatemarine invertebrates. His studies at theUniversity of Cambridge'sChrist's College from 1828 to 1831 encouraged his passion fornatural science. However, it was hisfive-year voyage onHMS Beagle from 1831 to 1836 that truly established Darwin as an eminent geologist. The observations and theories he developed during his voyage supportedCharles Lyell'sconcept of gradual geological change. Publication of hisjournal of the voyage made Darwin famous as a popular author. His first scientific work wasThe Structure and Distribution of Coral Reefs (1842). Along with his work onbarnacles, it won him theRoyal Medal in 1853. (Full article...)

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Ethics that focus on human interactions, morals that focus on humanity's relationship to a Creator, fall short of these things we've learned. They fail to encompass the big take-home message, so far, of a century and a half ofbiology andecology:life is—more than anything else—a process; it creates, and depends on, relationships among energy, land, water, air, time and various living things. It's not just about human-to-human interaction; it's not just about spiritual interaction. It's about all interaction. We're bound with the rest of life in a network, a network including not just all living things but the energy and nonliving matter that flows through the living, making and keeping all of us alive as we make it alive. We can keep debating ideologies and sending entreaties toward heaven. But unless we embrace the fuller reality we're in—and reality's implications—we'll face big problems."
— Carl Safina
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Polar Research is a journal of the Norwegian Polar Institute,Norway's central institution for research, on thepolar regions. The journal's articles are interdisciplinary and encompass a wide range of fields frombiology tooceanography. The journal also welcomes socio-economic papers and articles on management. (Full article...)

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... thatants exhibiteusociality, a social organization in ahierarchy?

(Pictured left: Ameat ant.)

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