Maylandia benetos
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| Maylandia benetos Status i världen: Sårbar[1] | |
| Systematik | |
|---|---|
| Domän | Eukaryoter Eukaryota |
| Rike | Djur Animalia |
| Stam | Ryggsträngsdjur Chordata |
| Understam | Ryggradsdjur Vertebrata |
| Överklass | Benfiskar Osteichthyes |
| Klass | Strålfeniga fiskar Actinopterygii |
| Ordning | Abborrartade fiskar Perciformes |
| Familj | Cichlidae |
| Släkte | Maylandia |
| Art | Maylandia benetos |
| Vetenskapligt namn | |
| § Maylandia benetos | |
| Auktor | (Stauffer, Bowers, Kellogg & McKaye, 1997) |
| Utbredning | |
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| Synonymer | |
| Metriaclima benetos Stauffer, Bowers, Kellogg & McKaye, 1997[2] | |
| Hitta fler artiklar om djur med | |
Maylandia benetos[3] är en fiskart som först beskrevs av Stauffer, Bowers, Kellogg och Mckaye, 1997. Maylandia benetos ingår i släktet Maylandia och familjen Cichlidae.[4][5] IUCN kategoriserar arten globalt som sårbar.[1] Inga underarter finns listade i Catalogue of Life.[4]
Källor
- ^ [a b] 2006 Maylandia benetos Från: IUCN 2012. IUCN Red List of Threatened Species. Version 2012.2 <www.iucnredlist.org>. Läst 24 oktober 2012.
- ^ Stauffer, J.R. Jr., N.J. Bowers, K.A. Kellogg and K.R. McKaye (1997) A revision of the blue-black Pseudotropheus zebra (Teleostei: Cichlidae) complex from Lake Malawi, Africa, with a description of a new genus and ten new species., Proc. Acad. Nat. Sci. Philad. 148:189-230.
- ^ Condé, B. and J. Géry (1999) Maylandia Meyer et Foerster, 1984, un nom générique disponible (Teleostei, Perciformes, Cichlidae)., Rev. fr. Aquariol 26(1-2):21-22.
- ^ [a b] Bisby F.A., Roskov Y.R., Orrell T.M., Nicolson D., Paglinawan L.E., Bailly N., Kirk P.M., Bourgoin T., Baillargeon G., Ouvrard D. (red.) (7 februari 2011). ”Species 2000 & ITIS Catalogue of Life: 2011 Annual Checklist.”. Species 2000: Reading, UK. http://www.catalogueoflife.org/annual-checklist/2011/search/all/key/maylandia+benetos/match/1. Läst 24 september 2012.
- ^ FishBase. Froese R. & Pauly D. (eds), 2011-06-14
Externa länkar
Wikispecies har information om Maylandia benetos.
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Lake Malawi seen from orbit.jpg
Leverkusen in Germany, photographed by astronauts aboard the Space Shuttle.
Leverkusen in Germany, photographed by astronauts aboard the Space Shuttle.
Original image courtesy of the Image Analysis Laboratory, NASA Johnson Space Center (eol.jsc.nasa.gov). Image ID: STS061-75-48. Image cropped, sharpened and gamma-corrected.
- This low-oblique, southeast-looking photograph shows Lake Malawi, one of many elongated lakes that form part of the Great Rift Valley of east Africa. The lake, bounded by steep mountains on all sides except the southern end, is approximately 360 miles (580 kilometers) long, averages 25 miles (40 kilometers) in width, and has a maximum depth of 2316 feet (706 meters). Lake Malawi is drained at the south end by the Shire River, which eventually empties into the Zambezi River. The lake and its steep-sloped shoreline were created by faulting that caused a thrust upward as the valley floor subsided between the slopes. The darker area along the northwest coast of the lake is the Nyika Plateau, which has several elevations more than 8000 feet (2440 meters) above sea level. Landlocked Malawi extends along the entire west coast of the lake. The large Luangwa River basin is visible as it drains to the southwest. Immediately west of the Luangwa River Valley stand the northeast-southwest-trending Muchinga Mountains with their dark ridgeline and maximum elevations reaching 6000 feet (1830 meters) above sea level. Northwest of this mountain range, drainage is to the north and west into the much larger Zaire (Congo) River watershed.