| 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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| Kirshner, Alexandra E and Anderson, John B and Jakobsson, Martin and O’Regan, Matthew and Majewski, Wojciech and Nitsche, Frank O Post-LGM deglaciation in Pine island Bay, west Antarctica Quaternary Science Reviews, 2012 DOI: 10.1016/j.quascirev.2012.01.017 |
Cores in this publication |
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| Core-related info: | ||
| Core name | KC06 | |
| Setting | marine | |
| Region | Pine Island Trough, Amundsen Sea | |
| Collection date | None | |
| IGSN ID | ||
| Core type | Kasten | |
| Latitude | -72.1325 | |
| Longitude | -106.91 | |
| Water depth (m) | 612.0 | |
| Core length (cm) | None | |
| Comments | None | |
| Cruise-related info: | ||
| Cruise | OSO0910 | |
| Ship | Oden | |
| Cruise start date | 2010-02-08 | |
| Cruise end date | None | |
| Samples in this core: | |||||
| Sample link | Core depth (cm) | Lithology | Facies interpretation | Carbon type | 14C age |
| 3099 | 70.0 - 80.0 | sandy mud with IRD | proximal glacial marine and ice shelf break up | unspecified calcareous shell or shell fragments | 10840.0 ± 65.0 |
| 3100 | 74.0 - 76.0 | sandy mud with IRD | proximal glacial marine and ice shelf break up | planktonic foraminifera | 10560.0 ± 110.0 |
| 3101 | 80.0 - 85.0 | sandy mud with IRD | proximal glacial marine and ice shelf break up | unspecified calcareous shell or shell fragments | 10655.0 ± 75.0 |
| 3102 | 90.0 - 92.0 | sandy mud with IRD | proximal glacial marine and ice shelf break up | planktonic foraminifera | 8645.0 ± 70.0 |
| 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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