This core appears in the following publications: | ||
Larter, Robert D and Anderson, John B and Graham, Alastair GC and Gohl, Karsten and Hillenbrand, Claus-Dieter and Jakobsson, Martin and Johnson, Joanne S and Kuhn, Gerhard and Nitsche, Frank O and Smith, James A and others Reconstruction of changes in the Amundsen Sea and Bellingshausen sea sector of the West Antarctic ice sheet since the last glacial maximum Quaternary Science Reviews, 2014 DOI: 10.1016/j.quascirev.2013.10.016 |
Cores in this publication |
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Hillenbrand, C-D and Larter, Robert D and Dowdeswell, JA and Ehrmann, W and Cofaigh, C {\'O} and Benetti, S and Graham, Alastair GC and Grobe, Hannes The sedimentary legacy of a palaeo-ice stream on the shelf of the southern Bellingshausen Sea: Clues to West Antarctic glacial history during the Late Quaternary Quaternary Science Reviews, 2010 DOI: 10.1016/j.quascirev.2010.06.028 |
Cores in this publication |
Core-related info: | ||
Core name | GC371 | |
Setting | marine | |
Region | Belgica Trough, Bellingshausen Sea | |
Collection date | None | |
IGSN ID | ||
Core type | Gravity | |
Latitude | -70.6533 | |
Longitude | -84.54 | |
Water depth (m) | 595.0 | |
Core length (cm) | None | |
Comments | None |
Cruise-related info: | ||
Cruise | JR104 | |
Ship | James Clark Ross | |
Cruise start date | 2004-01-23 | |
Cruise end date | 2004-02-13 |
Samples in this core: | |||||
Sample link | Core depth (cm) | Lithology | Facies interpretation | Carbon type | 14C age |
3223 | 10.0 - 12.0 | foraminifera-bearing mud | seasonal open-marine | planktonic foraminifera | 3721.0 ± 70.0 |
3224 | 20.0 - 20.0 | gravelly sandy mud | iceberg turbation in glacimarine setting | acid insoluble organic matter | 32527.0 ± 1521.0 |
3225 | 29.0 - 29.0 | gravelly sandy mud | iceberg turbation in glacimarine setting | acid insoluble organic matter | 28472.0 ± 689.0 |
3226 | 89.0 - 89.0 | muddy diamicton | iceberg turbation in glacimarine setting | acid insoluble organic matter | 22507.0 ± 436.0 |
Depth-age relationship: | ||
Plot key: black and gray bars represent 68.2% and 95.45% HPD interval(s), respectively. |
Questions about this page: Ryan Venturelli | ||