| 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 |
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| Core-related info: | ||
| Core name | GC359 | |
| Setting | marine | |
| Region | Ronne Entrance, Bellingshausen Sea | |
| Collection date | None | |
| IGSN ID | ||
| Core type | Gravity | |
| Latitude | -71.7183 | |
| Longitude | -76.0383 | |
| Water depth (m) | 685.0 | |
| 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 |
| 3058 | 0.0 - 1.0 | diatomaceous mud | seasonal open-marine | acid insoluble organic matter | 5131.0 ± 50.0 |
| 3205 | 25.0 - 25.0 | diatom-bearing mud | seasonal open-marine | acid insoluble organic matter | 11736.0 ± 120.0 |
| 3206 | 40.0 - 40.0 | gravelly sandy mud | glacimarine under sea ice or thin ice-shelf distal from grounding line | acid insoluble organic matter | 34345.0 ± 1604.0 |
| 3207 | 65.0 - 65.0 | gravelly sandy mud | glacimarine under ice shelf proximal to grounding line | acid insoluble organic matter | 34920.0 ± 1700.0 |
| 3208 | 107.0 - 107.0 | muddy diamicton | subglacial | acid insoluble organic matter | 41792.0 ± 3286.0 |
| Depth-age relationship: | ||
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| Plot key: black and gray bars represent 68.2% and 95.45% HPD interval(s), respectively. | ||
| Questions about this page: Ryan Venturelli |
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