Glyphidocythere, a new deep marine, paradoxostomatid (Ostracoda) from the Quaternary and Recent of the Indo-Pacific

Chapman’s (1910) Pseudocythere funafutiensis from 1924m off Funafuti, western Pacific is redescribed and illustrated together with additional Pleistocene and Recent material from the Coral and Tasman seas. A new paradoxostomatid genus, Glyphidocythere, is described to accommodate it and two other sp...

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Bibliographic Details
Published in:Journal of Micropalaeontology
Main Authors: Ayress, M. A., Corrége, T., Whatley, R. C.
Format: Article in Journal/Newspaper
Language:English
Published: GSL Publishing 1993
Subjects:
Online Access:https://doi.org/10.1144/jm.12.1.77
https://noa.gwlb.de/receive/cop_mods_00038206
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00037884/jm-12-77-1993.pdf
https://jm.copernicus.org/articles/12/77/1993/jm-12-77-1993.pdf
Description
Summary:Chapman’s (1910) Pseudocythere funafutiensis from 1924m off Funafuti, western Pacific is redescribed and illustrated together with additional Pleistocene and Recent material from the Coral and Tasman seas. A new paradoxostomatid genus, Glyphidocythere, is described to accommodate it and two other species yet to be formally described from the Banda Sea, eastern Indonesia. The genus is apparently restricted to the marine slope environment of low (less than 20°) southern latitudes. In the Coral and Tasman seas G. funafutiensis occurs within a narrow bathyal depth range (955m to 1754m) coincident with the Antarctic Intermediate Water.