Biogeographic realm

6 of the 8 biogeographic realms according to the WWF
  Oceania and Antarctic ecozones not shown.

A biogeographic realm or ecozone is the broadest biogeographic division of the Earth's land surface, based on distributional patterns of terrestrial organisms. They are subdivided in ecoregions, which are classified in biomes or habitat types.

The realms delineate large areas of the Earth's surface within which organisms have been evolving in relative isolation over long periods of time, separated from one another by geographic features, such as oceans, broad deserts, or high mountain ranges, that constitute barriers to migration. As such, biogeographic realms designations are used to indicate general groupings of organisms based on their shared biogeography. Biogeographic realms correspond to the floristic kingdoms of botany or zoogeographic regions of zoology.

Biogeographic realms are characterized by the evolutionary history of the organisms they contain. They are distinct from biomes, also known as major habitat types, which are divisions of the Earth's surface based on life form, or the adaptation of animals, fungi, micro-organisms and plants to climatic, soil, and other conditions. Biomes are characterized by similar climax vegetation. Each realm may include a number of different biomes. A tropical moist broadleaf forest in Central America, for example, may be similar to one in New Guinea in its vegetation type and structure, climate, soils, etc., but these forests are inhabited by animals, fungi, micro-organisms and plants with very different evolutionary histories.

The patterns of distribution of living organisms in the world's biogeographic realms were shaped by the process of plate tectonics, which has redistributed the world's land masses over geological history.

Concept history

The "biogeographic realms" of Udvardy (1975) were defined based on taxonomic composition. The rank corresponds more or less to the floristic kingdoms and zoogeographic regions.[1]

The usage of the term "ecozone" is more variable. It was used originally in stratigraphy (Vella, 1962, Hedberg, 1971). In Canadian literature, the term was used by Wiken (1986) in macro level land classification, with geographic criteria (see Ecozones of Canada).[2][3] Later, Schültz (1988) would use it with ecological and physiognomical criteria, in a way similar to the concept of biome.[4]

In the Global 200/WWF scheme (Olson & Dinerstein, 1998), originally the term "biogeographic realm" in Udvardy sense was used.[5] However, in a scheme of BBC, it was replaced by the term "ecozone".[6]

Terrestrial biogeographic realms

Udvardy (1975) biogeographic realms

The hierarchy of the scheme is (with early replaced terms in parenthesis):[1]

The realms and provinces of the scheme are:

WWF / Global 200 biogeographic realms (BBC "ecozones")

Main article: Global 200

The World Wildlife Fund scheme (Olson & Dinerstein, 1998, Olson et al., 2001)[7][8] is broadly similar to Miklos Udvardy's system,[1] the chief difference being the delineation of the Australasian realm relative to the Antarctic, Oceanic, and Indomalayan realms. In the WWF system, The Australasia realm includes Australia, Tasmania, the islands of Wallacea, New Guinea, the East Melanesian islands, New Caledonia, and New Zealand. Udvardy's Australian realm includes only Australia and Tasmania; he places Wallacea in the Indomalayan Realm, New Guinea, New Caledonia, and East Melanesia in the Oceanian Realm, and New Zealand in the Antarctic Realm.

Biogeographic
realm		 Area Notes
million square kilometres million square miles
Palearctic 54.1 20.9 including the bulk of Eurasia and North Africa
Nearctic 22.9 8.8 including most of North America
Afrotropic 22.1 8.5 including Trans-Saharan Africa and Arabia
Neotropic 19.0 7.3 including South America, Central America, and the Caribbean
Australasia 7.6 2.9 including Australia, New Guinea, New Zealand, and neighbouring islands. The northern boundary of this zone is known as the Wallace line.
Indo-Malaya 7.5 2.9 including the Indian subcontinent, Southeast Asia, and southern China
Oceania 1.0 0.39 including Polynesia (except New Zealand), Micronesia, and the Fijian Islands
Antarctic 0.3 0.12 including Antarctica.

The Palearctic and Nearctic are sometimes grouped into the Holarctic realm.

Morrone (2015) biogeographic kingdoms

Following the nomenclatural conventions set out in the International Code of Area Nomenclature, Morrone (2015) defined the next biogeographic kingdoms (or realms) and regions:[9]

Freshwater biogeographic realms

The applicability of Udvardy (1975) scheme to most freshwater taxa is unresolved.[10]

The drainage basins of the principal oceans and seas of the world are marked by continental divides. The grey areas are endorheic basins that do not drain to the ocean.

Marine biogeographic realms

According to Briggs (1995):[11][12]

According to the WWF scheme (Spalding, 2007):[13]

See also: Longhurst provinces

See also

References

  1. 1 2 3 Udvardy, M. D. F. (1975). A classification of the biogeographical provinces of the world. IUCN Occasional Paper no. 18. Morges, Switzerland: IUCN, .
  2. ↑ Wicken, E. B. 1986. Terrestrial ecozones of Canada / Écozones terrestres du Canada. Environment Canada. Ecological Land Classification Series No. 19. Lands Directorate, Ottawa. 26 pp., .
  3. ↑ Scott, G. 1995. Canada's vegetation: a world perspective, p., .
  4. ↑ Schültz, J. Die Ökozonen der Erde, 1st ed., Ulmer, Stuttgart, Germany, 1988, 488 pp.; 2nd ed., 1995, 535 pp.; 3rd ed., 2002. Transl.: The Ecozones of the World: The Ecological Divisions of the Geosphere. Berlin: Springer-Verlag, 1995; 2nd ed., 2005, .
  5. ↑ Olson, D. M. & E. Dinerstein (1998). The Global 200: A representation approach to conserving the Earth’s most biologically valuable ecoregions. Conservation Biol. 12:502–515, .
  6. ↑ BBC Nature - Ecozones.
  7. ↑ Olson, D. M. & E. Dinerstein (1998). The Global 200: A representation approach to conserving the Earth’s most biologically valuable ecoregions. Conservation Biol. 12:502–515, .
  8. ↑ Olson, D. M., Dinerstein, E., Wikramanayake, E. D., Burgess, N. D., Powell, G. V. N., Underwood, E. C., D'Amico, J. A., Itoua, I., Strand, H. E., Morrison, J. C., Loucks, C. J., Allnutt, T. F., Ricketts, T. H., Kura, Y., Lamoreux, J. F., Wettengel, W. W., Hedao, P., Kassem, K. R. (2001). Terrestrial ecoregions of the world: a new map of life on Earth. Bioscience 51(11):933-938, .
  9. ↑ Morrone, J. J. (2015). Biogeographical regionalisation of the world: a reappraisal. Australian Systematic Botany 28: 81-90, .
  10. ↑ Abell, R., M. Thieme, C. Revenga, M. Bryer, M. Kottelat, N. Bogutskaya, B. Coad, N. Mandrak, S. Contreras-Balderas, W. Bussing, M. L. J. Stiassny, P. Skelton, G. R. Allen, P. Unmack, A. Naseka, R. Ng, N. Sindorf, J. Robertson, E. Armijo, J. Higgins, T. J. Heibel, E. Wikramanayake, D. Olson, H. L. Lopez, R. E. d. Reis, J. G. Lundberg, M. H. Sabaj Perez, and P. Petry. (2008). Freshwater ecoregions of the world: A new map of biogeographic units for freshwater biodiversity conservation. BioScience 58:403-414, .
  11. ↑ Briggs, J.C. (1995). Global Biogeography. Amsterdam: Elsevier.
  12. ↑ Morrone, J. J. (2009). Evolutionary biogeography, an integrative approach with case studies. Columbia University Press, New York, .
  13. ↑ Spalding, M. D. et al. (2007). Marine ecoregions of the world: a bioregionalization of coastal and shelf areas. BioScience 57: 573-583, .

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