Research Article| July 01, 1987 Mid-Cenozoic record of glaciation and sea-level change on the margin of the Victoria Land basin, Antarctica P. J. Barrett; P. J. Barrett 1Antarctic Research Centre, Research School of Earth Sciences, Victoria University of Wellington, Private Bag, Wellington, New Zealand Search for other works by this author on: GSW Google Scholar D. P. Elston; D. P. Elston 2U.S. Geological Survey, Flagstaff, Arizona 86001 Search for other works by this author on: GSW Google Scholar D. M. Harwood; D. M. Harwood 3Institute of Polar Studies and Department of Geology and Mineralogy, Ohio State University, Columbus, Ohio 43210 Search for other works by this author on: GSW Google Scholar B. C. McKelvey; B. C. McKelvey 4Department of Geology, University of New England, Armidale, New South Wales 2601, Australia Search for other works by this author on: GSW Google Scholar P.-N. Webb P.-N. Webb 5Institute of Polar Studies and Department of Geology and Mineralogy, Ohio State University, Columbus, Ohio 43210 Search for other works by this author on: GSW Google Scholar Author and Article Information P. J. Barrett 1Antarctic Research Centre, Research School of Earth Sciences, Victoria University of Wellington, Private Bag, Wellington, New Zealand D. P. Elston 2U.S. Geological Survey, Flagstaff, Arizona 86001 D. M. Harwood 3Institute of Polar Studies and Department of Geology and Mineralogy, Ohio State University, Columbus, Ohio 43210 B. C. McKelvey 4Department of Geology, University of New England, Armidale, New South Wales 2601, Australia P.-N. Webb 5Institute of Polar Studies and Department of Geology and Mineralogy, Ohio State University, Columbus, Ohio 43210 Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1987) 15 (7): 634–637. https://doi.org/10.1130/0091-7613(1987)15<634:MROGAS>2.0.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation P. J. Barrett, D. P. Elston, D. M. Harwood, B. C. McKelvey, P.-N. Webb; Mid-Cenozoic record of glaciation and sea-level change on the margin of the Victoria Land basin, Antarctica. Geology 1987;; 15 (7): 634–637. doi: https://doi.org/10.1130/0091-7613(1987)15<634:MROGAS>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 The MSSTS-1 drill hole in western McMurdo Sound provides the earliest physical record thus far for Antarctic Cenozoic glaciation. The hole penetrated 227 m of muddy marine glacial sediment containing scattered pebble- and cobble-size clasts, including seven diamictite beds deposited from grounded ice during glacial advances. A diatom-based chronology, refined by paleomagnetic stratigraphy, for the interval below 116-m subbottom indicates sediment accumulation from 29 Ma to about 24 Ma. Sediment texture and paleoecology of diatoms and foraminifers indicate nearshore sedimentation on a wave-dominated shelf. The oldest strata record a significant shallowing of water depth, culminating in ice grounding at around 28 Ma and a deepening at 25 Ma that may be glacioeustatic. 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.
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