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 |
Core-related info: | ||
Core name | KC10 | |
Setting | marine | |
Region | Pine Island Trough, Amundsen Sea | |
Collection date | None | |
IGSN ID | ||
Core type | Kasten | |
Latitude | -72.4923 | |
Longitude | -106.7736 | |
Water depth (m) | 687.0 | |
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 |
3104 | 4.0 - 6.0 | sandy clay with IRD | distal glacimarine | planktonic foraminifera | 5400.0 ± 100.0 |
3105 | 14.0 - 16.0 | sandy clay with IRD | distal glacimarine | planktonic foraminifera | 6590.0 ± 50.0 |
3106 | 30.0 - 32.0 | sandy silt with IRD | distal glacimarine | planktonic foraminifera | 7255.0 ± 35.0 |
3107 | 37.0 - 37.0 | sandy silt with IRD | distal glacimarine | unspecified calcareous shell or shell fragments | 805.0 ± 25.0 |
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 | ||