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 |
|
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 |
Core-related info: | ||
Core name | VC242 | |
Setting | marine | |
Region | Prince Gustav Channel, Eastern Antarctic Peninsula | |
Collection date | 2000-03-04 | |
IGSN ID | ||
Core type | vibrocore | |
Latitude | -64.377 | |
Longitude | -58.519 | |
Water depth (m) | 767.0 | |
Core length (cm) | 580.0 | |
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 |
741 | 10.0 - 10.0 | Diatom-bearing clayey silt | seasonal open-marine | acid insoluble organic matter | 12543.0 ± 90.0 |
746 | 70.0 - 70.0 | Diatom-bearing clayey silt | seasonal open-marine | acid insoluble organic matter | 10605.0 ± 70.0 |
742 | 200.0 - 200.0 | Diatom-bearing clayey silt | sub-ice shelf? | acid insoluble organic matter | 11783.0 ± 80.0 |
743 | 276.0 - 276.0 | Diatom-bearing clayey silt | sub-ice shelf? | acid insoluble organic matter | 12356.0 ± 90.0 |
744 | 290.0 - 290.0 | Diatom-bearing clayey silt | sub-ice shelf? | acid insoluble organic matter | 12811.0 ± 90.0 |
745 | 425.0 - 425.0 | Silty clay | Distal ice shelf | acid insoluble organic matter | 20300.0 ± 160.0 |
689 | 425.0 - 425.0 | transitional glaciomarine | acid insoluble organic matter | 20300.0 ± 160.0 |
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 | ||