| This core appears in the following publications: | ||
| Cofaigh, Colm {\'O} and Davies, Bethan J and Livingstone, Stephen J and Smith, James A and Johnson, Joanne S and Hocking, Emma P and Hodgson, Dominic A and Anderson, John B and Bentley, Michael J and Canals, Miquel and others Reconstruction of ice-sheet changes in the Antarctic Peninsula since the Last Glacial Maximum Quaternary Science Reviews, 2014 DOI: 10.1016/j.quascirev.2014.06.023 |
Cores in this publication |
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| Pudsey, Carol J and Murray, John W and Appleby, Peter and Evans, Jeffrey Ice shelf history from petrographic and foraminiferal evidence, Northeast Antarctic Peninsula Quaternary Science Reviews, 2006 DOI: 10.1016/j.quascirev.2006.01.029 |
Cores in this publication |
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| Core-related info: | ||
| Core name | VC237 | |
| Setting | marine | |
| Region | Prince Gustav Channel, Eastern Antarctic Peninsula | |
| Collection date | 2000-03-04 | |
| IGSN ID | ||
| Core type | vibrocore | |
| Latitude | -64.22317 | |
| Longitude | -58.47783 | |
| Water depth (m) | 816.0 | |
| Core length (cm) | 600.0 | |
| Comments | ||
| Cruise-related info: | ||
| Cruise | JR48 | |
| Ship | James Clark Ross | |
| Cruise start date | 2000-03-27 | |
| Cruise end date | 2000-04-01 | |
| Samples in this core: | |||||
| Sample link | Core depth (cm) | Lithology | Facies interpretation | Carbon type | 14C age |
| 735 | 10.0 - 10.0 | Diatom-bearing clayey silt | seasonal open-marine | acid insoluble organic matter | 9302.0 ± 40.0 |
| 736 | 120.0 - 120.0 | Diatom-bearing clayey silt | seasonal open-marine | acid insoluble organic matter | 9768.0 ± 43.0 |
| 737 | 290.0 - 290.0 | Diatom-bearing clayey silt | sub-ice shelf? | acid insoluble organic matter | 12080.0 ± 120.0 |
| 738 | 470.0 - 470.0 | Diatom-bearing clayey silt | sub-ice shelf? | acid insoluble organic matter | 15271.0 ± 75.0 |
| 687 | 490.0 - 490.0 | dbGM | acid insoluble organic matter | 15330.0 ± 80.0 | |
| 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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