The écozone is defined as being the part of the terrestrial Surface representative of a ecological Unité with large scales, characterized by abiotic factors (not
alive) and biotic (alive) particuliers.
The system of the écozones was proposed by Miklos Udvardy in an objective of Conservation in 1975. It is now used internationally as system unified at ends of biogeographic identification and conservation.
Another name for écozone is biogeographic area .
They are usually used in Zoogéographie because adapted enough to include/understand the distribution of current fauna (and especially of the Mammifère S), but are less relevant in other biogeographic disciplines.
Analyzes of regional Biodiversité were carried out by the World Wildlife Fund, and led to the definition of the borders of the terrestrial écorégions and to the list of the Global 200.
Classification in écozone is also used within the framework of the World Heritage site S.
The maximum regrouping of the écozones in faunal empires allows the distinction of large biogeographic surfaces corresponding to various glaciations and continental separations, there remains then 3 large faunal surfaces :
The classification of Alfred Russel Wallace allowed the distinction of large écorégions separated by natural constraints more constraining than that from the faunal empires, consequently one distinguished 5 great complexes of écozones, divided they even into areas, plus the écozone the Antarctic, always subjected to controversies.
the écozone Afrotropical E, also called Ethiopian , where one can observe two great under-areas: sub-Saharan Africa and Madagascar which experienced an independent development
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