| This core appears in the following publications: | ||
| Smith, James A and Hillenbrand, Claus-Dieter and Kuhn, Gerhard and Larter, Robert D and Graham, Alastair GC and Ehrmann, Werner and Moreton, Steven G and Forwick, Matthias Deglacial history of the West Antarctic Ice Sheet in the western Amundsen Sea embayment Quaternary Science Reviews, 2011 DOI: 10.1016/j.quascirev.2010.11.020 |
Cores in this publication |
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| 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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| Core-related info: | ||
| Core name | VC411 | |
| Setting | marine | |
| Region | Dotson-Getz Troughs, Amundsen Sea | |
| Collection date | None | |
| IGSN ID | ||
| Core type | Vibro | |
| Latitude | -73.567 | |
| Longitude | -116.8459 | |
| Water depth (m) | 370.0 | |
| Core length (cm) | None | |
| Comments | None | |
| Cruise-related info: | ||
| Cruise | JR141 | |
| Ship | James Clark Ross | |
| Cruise start date | 2006-01-09 | |
| Cruise end date | 2006-02-15 | |
| Samples in this core: | |||||
| Sample link | Core depth (cm) | Lithology | Facies interpretation | Carbon type | 14C age |
| 3123 | 15.0 - 15.0 | diatom bearing mud | gravity flow or winnowing of glacomarine sediment under sea ice | acid insoluble organic matter | 5945.0 ± 35.0 |
| 3124 | 109.0 - 109.0 | diatom bearing mud | gravity flow or winnowing of glacomarine sediment under sea ice | acid insoluble organic matter | 35373.0 ± 785.0 |
| 3125 | 185.0 - 185.0 | diatom bearing mud | gravity flow or winnowing of glacomarine sediment under sea ice | acid insoluble organic matter | 34715.0 ± 728.0 |
| 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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