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东斯科舍洋脊

维基百科,自由的百科全书

东斯科舍洋脊East Scotia Ridge)是南极南大西洋斯科舍板块上极东端的海底火山洋脊[1]。2009年,一种属于基瓦属未命名物种(Kiwa n. sp.)、暂时被称为“霍夫蟹”的生物在这里被发现[2][3]

参考资料

[编辑]
  1. ^ Additional Report for East Scotia Ridge. [2013-07-30]. (原始内容存档于2020-10-22) (英语). 
  2. ^ Andrew R. Thurber, William J. Jones & Kareen Schnabel. Dancing for food in the deep sea: bacterial farming by a new species of yeti crab. PLoS ONE. 2011, 6 (11): e26243 [2013-07-30]. doi:10.1371/journal.pone.0026243. (原始内容存档于2013-11-04). 
  3. ^ Alex D. Rogers, Paul A. Tyler, Douglas P. Connelly, Jon T. Copley, Rachael James; et al. The discovery of new deep-sea hydrothermal vent communities in the Southern Ocean and implications for biogeography. PLoS Biology. 2012, 10 (1): e1001234. PMID 22235194. doi:10.1371/journal.pbio.1001234.