Abstract

Research Article| November 01, 1991 Magnetic polarity stratigraphy of Pliocene and Pleistocene fossil vertebrate localities in southeastern Australia MICHAEL J. WHITELAW MICHAEL J. WHITELAW 1Department of Geological Sciences, University of Texas at El Paso, El Paso, Texas 79968-0555 Search for other works by this author on: GSW Google Scholar Author and Article Information MICHAEL J. WHITELAW 1Department of Geological Sciences, University of Texas at El Paso, El Paso, Texas 79968-0555 Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (1991) 103 (11): 1493–1503. https://doi.org/10.1130/0016-7606(1991)103<1493:MPSOPA>2.3.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 MICHAEL J. WHITELAW; Magnetic polarity stratigraphy of Pliocene and Pleistocene fossil vertebrate localities in southeastern Australia. GSA Bulletin 1991;; 103 (11): 1493–1503. doi: https://doi.org/10.1130/0016-7606(1991)103<1493:MPSOPA>2.3.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 SocietyGSA Bulletin Search Advanced Search Abstract A series of magnetic polarity stratigraphy studies are presented from localities in Victoria and southwest New South Wales, Australia. These localities were examined in order to improve the age resolution of Pliocene and Pleistocene fossil vertebrate sites in south-eastern Australia. The following age constraints should now be used for these southeastern Australian local faunas: For-syth's Bank, Kalimnan Stage and >4.42 Ma; Hamilton, Gilbert Chron (4.35-4.42 Ma); Boxlea, Gilbert Chron? (>4.06 Ma); Parwan, Gilbert Chron (4.06-4.20 Ma); Coimadai, Late Gilbert Chron (3.35-3.82 Ma); Fisher-man's Cliff, Gauss Chron (2.42-2.87 Ma); Bone Gulch, Early Matuyama Chron (1.82-2.42 Ma); Dog Rocks, Early Matuyama Chron (1.82-2.42 Ma); Duck Ponds, Late Matuyama Chron (>0.71 Ma and probably <1.63 Ma); Limeburner's Point, Late Matuyama or Brunhes Chron (<0.96 Ma); Hines Quarry, Late Matuyama or Brunhes Chron (<0.96 Ma); and Nelson Bay, Late Matuyama Chron (0.71-1.63 Ma). 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.

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.