John B Anderson

Biographic Data

ID4930988
NAMEJohn B Anderson
GIVEN NAMESJohn B
FAMILY NAMEAnderson
SIGNATUREANDERSON J B
AFFILIATIONSRice University
ORCID0000-0002-3104-5557
VERIFIEDYes
TOTAL WORKS10
TOTAL CITATIONS5
WORKS AS AUTHOR10
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1970
LATEST PUBLICATION YEAR2017
H-INDEX1

  • Oceanographic influences on the stability of the Cosgrove Ice Shelf, Antarctica

    Open AccessRebecca L Totten, Wojciech Majewski et al.ARTICLEThe Holocene2017References: 11

    Ferrero Bay, located in eastern Pine Island Bay (PIB) of the Amundsen Sea Embayment, is one of the largest and southernmost fjords yet studied in Antarctica. High-resolution multibeam swath bathymetric data, chirp sonar sub-bottom profiles, and three Kasten cores were collected in Ferrero Bay during the IB Oden Southern Ocean 2009–2010 cruise (OSO0910). Core KC-15 from the inner bay yielded two carbonate ages providing a minimum age for ice sheet…

  • Breaching of Mustang Island in response to the 8.2 ka sea-level event and impact on Corpus Christi Bay, Gulf of Mexico

    Open AccessShannon Ferguson, Sophie Warny et al.ARTICLEThe Holocene2017References: 4

    The results from an investigation of the coupled Mustang Island–Corpus Christi Bay complex, Gulf of Mexico, shows that the island was eliminated as an effective salinity barrier between 8.86 and 8.17 ka. This event is recorded by a 5-fold increase in dinoflagellate cysts within Corpus Christi Bay. During this time, the bay-head delta shifted 15 km landward and oyster reefs within the bay died off. Our age model indicates that this event most like…

  • Gualas Glacier sedimentary record of climate and environmental change, Golfo Elefantes, Western Patagonia (46.5°S)

    Open AccessRodrigo Fernandez, J Anderson et al.ARTICLEThe Holocene2011References: 3

    Gualas Glacier is an outlet glacier of the Northern Patagonian Icefield, one of the largest temperate ice bodies on Earth. Golfo Elefantes, the depositional basin of Gualas Glacier, has a sedimentary record that spans, with some hiatuses, at least the last ~11.3±3.0 ka. During this period the gulf remained free of ice, as suggested by the absence of proximal glacimarine sediment and till in the sedimentary section. This implies that the arcuate t…

  • A record of Holocene glacial and oceanographic variability in Neny Fjord, Antarctic Peninsula

    Open AccessClaire S Allen, Lisa Oakes-Fretwell et al.ARTICLEThe Holocene2010Cited by: 1References: 8

    Analyses of a 12 m marine sediment core from Neny Fjord, Marguerite Bay, Antarctic Peninsula (68.2571°S, 66.9617°W), yield a high-resolution record of Holocene climate variability. The sediments preserve signals of past glacial and marine environments and offer a unique insight into atmospheric and oceanic forcings on the western Antarctic Peninsula climate. Dating of basal material reveals that deglaciation of the fjord occurred prior to 9040 ca…

  • Late Quaternary Glacial History of the South Orkney Plateau, Antarctica

    Open AccessMargaret Jane Herron, John B AndersonARTICLEQuaternary Research1990

    Piston cores from the South Orkney Plateau penetrated overcompacted diamictons in water depths of up to 250 m. Detailed textural and petrological analyses of these diamictons indicate that they are basal tills. Seismic records from the plateau show a widespread surface of glacial erosion and provide additional evidence of an ice cap grounded to a depth of 250 m. Piston cores from the slope of the plateau penetrated diatomaceous muds resting direc…

  • Application of Tandem Accelerator Mass-Spectrometer Dating to Late Pleistocene-Holocene Sediments of the East Antarctic Continental Shelf

    Open AccessEugene W Domack, A J T Jull et al.ARTICLEQuaternary Research1989

    Glacial recession from the Antarctic continental shelf is recorded by glacial-marine diamictons, sands, and overlying siliceous oozes. In order to clarify the chronology for this sequence, use was made of the University of Arizona tandem accelerator mass-spectrometer (TAMS) for 14 C dating. Small samples of benthic and planktonic foraminifera were selectively removed from diamictons, graded sands, and surface sediments which were recovered from t…

  • Glacial-Marine Sedimentation and Quaternary Glacial History of Marguerite Bay, Antarctic Peninsula

    Open AccessDouglas S Kennedy, John B AndersonARTICLEQuaternary Research1989

    Marguerite Bay, situated between the subpolar glacial regime of the northern Antarctic Peninsula and the polar glacial regime of West Antarctica, is ideally located to test various models of glacial and glacial-marine sedimentation and specific scenarios of late Wisconsin ice sheet expansion. Piston cores and single-channel seismic reflection data were collected during the Deep Freeze 85 and 86 expeditions to determine the late Quaternary history…

  • Political Communication

    John B Anderson, Kathleen Hall Jamieson et al.ARTICLECommunication Booknotes1989Cited by: 4

    A PROPER INSTITUTION: GUARANTEEING TELEVISED PRESIDENTIAL DEBATES by John B. Anderson (New York: Twentieth Century Fund, 1988—$18.95, with a paperback also available, ISBN 0-87078-253-3) OF CREATING AN INFORMED ELECTORATE by Kathleen Hall Jamieson and David S. Birdsell (New York: Oxford University Press, 1988—$19.95, ISBN 0-19-505539-X) THE PRIMETIME PRESIDENCY OF RONALD REAGAN: THE ERA OF THE TELEVISION PRESIDENCY by Robert E. Denton, Jr. (New Y…

  • Defense Dialogue

    John B AndersonARTICLEThe US Army War College Quarterly…1980

  • Principles for Participation in Politics

    Open AccessJohn B AndersonARTICLETheology Today1970