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MarBEF Data System |
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Amphipoda taxon details
original description
(of Katius obesus Chevreux, 1905) Chevreux, E. (1905). Description d' un amphipode (Katius obesus, nov. gen. et sp.), suivie d'une liste des amphipodes de la tribu des Gammarina ramenes par le filet a grande. ouverture pendant la derniere campagne de la "Princesse Alice" en 1904. <em>Bulletin du Musée Océanographique de Monaco.</em> 35: 1-5. [details]
original description
(of Alicella scotiae Chilton, 1912) Chilton, C. (1912). The Amphipoda of the Scottish National Antarctic Expedition (reprinted from The Transactions of the Royal Society of Edinburgh. <em>Report on the Scientific Results of the Voyage of S.Y.</em> 48: 455-520. [details]
context source (Deepsea)
Intergovernmental Oceanographic Commission (IOC) of UNESCO. The Ocean Biogeographic Information System (OBIS), available online at http://www.iobis.org/ [details]
additional source
Stoddart H.E. & Lowry J.K. (2004). The deep-sea lysianassoid genus Eurythenes (Crustacea, Amphipoda, Eurytheneidae n. fam.). Zoosystema, 26, 3, 425-468 pp. [details] Available for editors [request]
additional source
LeCroy, S. E.; Gasca, R.; Winfield, I.; Ortiz, M.; Escobar-Briones, E. (2009). Amphipoda (Crustacea) of the Gulf of Mexico. <em>In: Felder, D.L. and D.K. Camp (eds.), Gulf of Mexico–Origins, Waters, and Biota. Biodiversity. Texas A&M Press, College.</em> Pp. 941–972. [details] Available for editors [request]
additional source
D'Udekem d'Acoz, C.; Havermans, C. (2015). Contribution to the systematics of the genus <em>Eurythenes </em>S.I. Smith in Scudder, 1882 (Crustacea: Amphipoda: Lysianassoidea: Eurytheneidae). <em>Zootaxa.</em> 3971(1): 1-80., available online at https://doi.org/10.11646/zootaxa.3971.1.1 [details] Available for editors [request]
From editor or global species database
Association Burrowing into a salp [details]
Depth range Continental slope to lower abyssal (200 m to 7000 m). [details]
Distribution Cosmopolitan, exceptionally near the surface (present material), normally between 128 m and 1600 m, most commonly below 1000 m (Stoddart & Lowry 2004; Senna & Serejo 2008). [details]
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