Late Eocene–Oligocene magnetostratigraphy and biostratigraphy at South Atlantic DSDP Site 522

Research Article| October 01, 1982 Late Eocene–Oligocene magnetostratigraphy and biostratigraphy at South Atlantic DSDP Site 522 Richard Z. Poore; Richard Z. Poore 1U.S. Geologica Survey, MS 970, 12201 Sunrise Valley Drive. Reston, Virginia 22092 Search for other works by this author on: GSW Google Scholar Lisa Tauxe; Lisa Tauxe 2Lamont-Doherty Geological Observatory of Columbia University, Palisades, New York 10964 Search for other works by this author on: GSW Google Scholar Stephen F. Percival, Jr.; Stephen F. Percival, Jr. 3Mobil Exploration and Producing Services, Inc., P.O. Box 900, Dallas, Texas 75221 Search for other works by this author on: GSW Google Scholar John L. LaBrecque John L. LaBrecque 4Lamont-Doherty Geological Observatory of Columbia University, Palisades, New York 10964 Search for other works by this author on: GSW Google Scholar Geology (1982) 10 (10): 508–511. https://doi.org/10.1130/0091-7613(1982)10<508:LEMABA>2.0.CO;2 Article history first online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Richard Z. Poore, Lisa Tauxe, Stephen F. Percival, John L. LaBrecque; Late Eocene–Oligocene magnetostratigraphy and biostratigraphy at South Atlantic DSDP Site 522. Geology 1982;; 10 (10): 508–511. doi: https://doi.org/10.1130/0091-7613(1982)10<508:LEMABA>2.0.CO;2 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 SocietyGeology Search Advanced Search Abstract Upper Eocene to lowest Miocene sediments recovered at Deep Sea Drilling Project (DSDP) Site 522 in the South Atlantic Ocean allow direct calibration of magnetostratigraphy and calcareous plankton biostratigraphy. The results from Site 522 show that the Eocene/Oligocene boundary occurs in the reversed interval of magnetic Chron C13 (= C13R) and that the Oligocene/IMiocene boundary probably occurs in the upper part of Chron C6C. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.