Quaternary deep-sea ostracods from the north-western Pacific Ocean: global biogeography and Drake-Passage, Tethyan, Central American and Arctic pathways

• Main Authors: Moriaki Yasuhara, Hunt, Gene, Okahashi, Hisayo
• Format: Text
• Language: unknown
• Published: Taylor & Francis 2017
• Subjects: Microbiology; FOS Biological sciences; Genetics; Molecular Biology; Evolutionary Biology; 59999 Environmental Sciences not elsewhere classified; FOS Earth and related environmental sciences; 39999 Chemical Sciences not elsewhere classified; FOS Chemical sciences; Ecology; 20199 Astronomical and Space Sciences not elsewhere classified; FOS Physical sciences; 69999 Biological Sciences not elsewhere classified; Marine Biology; Inorganic Chemistry; Arctic; Southern Ocean; Arctic Ocean; Drake Passage; Bering Strait; Pacific; Fram Strait
• Online Access: https://dx.doi.org/10.6084/m9.figshare.5643184.v1; https://tandf.figshare.com/articles/Quaternary_deep-sea_ostracods_from_the_north-western_Pacific_Ocean_global_biogeography_and_Drake-Passage_Tethyan_Central_American_and_Arctic_pathways/5643184/1

Twelve genera and 19 species of deep-sea ostracods from the Shatsky Rise, north-western Pacific, were examined and illustrated for taxonomy. Three new species, Cytheropteron nasutum sp. nov., Poseidonamicus shatskyensis sp. nov. and Legitimocythere stellae sp. nov., are described. Based on these Shatsky Rise ostracods and a comprehensive literature survey of synonyms, we discuss global biogeography and possible migration pathways of deep-sea species. The four possible deep-water pathways connecting the Atlantic and Pacific Oceans are: the Drake Passage (Southern Ocean), established by 30 Ma; the Tethys Seaway, which had closed by 19–14 Ma; the Central American Seaway, which had closed by 3 Ma; and the Arctic Ocean Seaway via the Bering Strait, which opened about 4.8–7.4 Ma, and via the Fram Strait, which opened between 10 and 20 Ma. The Drake Passage is likely the major pathway. We argue that the Arctic was an important pathway for some deep-sea species before the mid-Pleistocene. Most deep-sea organisms have poor fossil records, and thus the rich fossil record of deep-sea ostracods is an ideal model system for the study of deep-time biogeography of deep-sea organisms. It may well be that other deep-sea organisms had similar palaeobiogeographical histories and patterns. http://zoobank.org/urn:lsid:zoobank.org:pub:3B70B7E5-04E0-4FF7-91EF-88CE1B199C8D