Abstract

Research Article| October 01, 2005 REVISED PALEOGENE PLANKTONIC FORAMINIFERAL BIOZONATION FOR THE AUSTRAL REALM Brian T. Huber; Brian T. Huber 1Department of Paleobiology, MRC 121, Smithsonian Museum of Natural History, Washington, D.C. 20013-7012, USA. E-mail: huberb@si.edu Search for other works by this author on: GSW Google Scholar Frédéric Quillévéré Frédéric Quillévéré 2Laboratoire “PaléoEnvironnements & PaléobioSphère”, UMR CNRS 5125, Université Claude Bernard-Lyon 1, 27-43 Boulevard de 11 Novembre 1918, 69622 Villeurbanne cedex, France. E-mail: frederic.quillevere@univ-lyon1.fr Search for other works by this author on: GSW Google Scholar Journal of Foraminiferal Research (2005) 35 (4): 299–314. https://doi.org/10.2113/35.4.299 Article history received: 06 Dec 2004 accepted: 23 Aug 2005 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Brian T. Huber, Frédéric Quillévéré; REVISED PALEOGENE PLANKTONIC FORAMINIFERAL BIOZONATION FOR THE AUSTRAL REALM. Journal of Foraminiferal Research 2005;; 35 (4): 299–314. doi: https://doi.org/10.2113/35.4.299 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyJournal of Foraminiferal Research Search Advanced Search Abstract A major revision to the Antarctic Paleogene planktonic foraminifer biozonation is presented using the latest species concepts and biostratigraphic studies of Ocean Drilling Program (ODP) sites located between 52°S and 65°S paleolatitude in the southern South Atlantic and southern Indian Oceans. Shorthand prefixes for the Antarctic Paleogene zones are designated as “AP” zones for the “Antarctic Paleocene”, “AE” zones for the “Antarctic Eocene”, and “AO” zones for the “Antarctic Oligocene”. New numerical ages for Paleogene planktonic foraminiferal and calcareous nannofossil first- and last-occurrence events are estimated using new age-depth curves constructed for ODP Sites 738 and 744 in the southern Indian Ocean. The order and timing of these events are compared with bio-, magneto- and chemostratigraphic datums that have been recently published, reinterpreted, or observed in the present study. The revised zonal framework and age models will improve correlation of Paleogene planktonic foraminifer pelagic and hemipelagic carbonate sequences within and outside the Austral Realm. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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