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Timing of the Northern Prince Gustav Ice Stream retreat and the deglaciation of northern James Ross Island, Antarctic Peninsula during the last glacial-interglacial transition

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F14%3A10281946" target="_blank" >RIV/00216208:11310/14:10281946 - isvavai.cz</a>

  • Alternative codes found

    RIV/00216224:14310/14:00074231 RIV/00025798:_____/14:00000377

  • Result on the web

    <a href="http://dx.doi.org/10.1016/j.yqres.2014.05.003" target="_blank" >http://dx.doi.org/10.1016/j.yqres.2014.05.003</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.yqres.2014.05.003" target="_blank" >10.1016/j.yqres.2014.05.003</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Timing of the Northern Prince Gustav Ice Stream retreat and the deglaciation of northern James Ross Island, Antarctic Peninsula during the last glacial-interglacial transition

  • Original language description

    The Northern Prince Gustav Ice Stream located in Prince Gustav Channel, drained the northeastern portion of the Antarctic Peninsula Ice Sheet during the last glacial maximum. Here we present a chronology of its retreat based on in situ produced cosmogenic Be-10 from erratic boulders at Cape Lachman, northern James Ross Island. Schmidt hammer testing was adopted to assess the weathering state of erratic boulders in order to better interpret excess cosmogenic Be-10 from cumulative periods of pre-exposureor earlier release from the glacier. The weighted mean exposure age of five boulders based on Schmidt hammer data is 12.9 +/- 1.2 ka representing the beginning of the deglaciation of lower-lying areas (<60 m a.s.l.) of the northern James Ross Island, when Northern Prince Gustav Ice Stream split from the remaining James Ross Island ice cover. This age represents the minimum age of the transition from grounded ice stream to floating ice shelf in the middle continental shelf areas of the no

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DE - Earth magnetism, geodesy, geography

  • OECD FORD branch

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2014

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Quaternary Research

  • ISSN

    0033-5894

  • e-ISSN

  • Volume of the periodical

    82

  • Issue of the periodical within the volume

    2

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    9

  • Pages from-to

    441-449

  • UT code for WoS article

    000343076700014

  • EID of the result in the Scopus database