This core appears in the following publications: | ||
Stolldorf, Travis and Schenke, Hans-Werner and Anderson, John B LGM ice sheet extent in the Weddell Sea: evidence for diachronous behavior of Antarctic Ice Sheets Quaternary Science Reviews, 2012 DOI: 10.1016/j.quascirev.2012.05.017 |
Cores in this publication |
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Hillenbrand, Claus-Dieter and Bentley, Michael J and Stolldorf, Travis D and Hein, Andrew S and Kuhn, Gerhard and Graham, Alastair GC and Fogwill, Christopher J and Kristoffersen, Yngve and Smith, James A and Anderson, John B and others Reconstruction of changes in the Weddell Sea sector of the Antarctic Ice Sheet since the Last Glacial Maximum Quaternary Science Reviews, 2014 DOI: 10.1016/j.quascirev.2013.07.020 |
Cores in this publication |
Core-related info: | ||
Core name | 002G-PC | |
Setting | marine | |
Region | Helmert Bank, Weddell Sea | |
Collection date | None | |
IGSN ID | ARF000ED9 | |
Core type | piston core | |
Latitude | -75.517 | |
Longitude | -30.117 | |
Water depth (m) | 411.0 | |
Core length (cm) | 525.0 | |
Comments | None |
Cruise-related info: | ||
Cruise | IWSOE69 | |
Ship | Glacier | |
Cruise start date | None | |
Cruise end date | None |
Samples in this core: | |||||
Sample link | Core depth (cm) | Lithology | Facies interpretation | Carbon type | 14C age |
512 | 80.0 - 85.0 | structureless diamicton, with slight variation of sorting and skewness, with few foraminifera (Stolldorf et al. 2012) | proximal glaciomarine (Stolldorf et al. 2012) | undifferentiated or mixed benthic and planktonic foraminifera | 12235.0 ± 30.0 |
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 | ||