This core appears in the following publications: | ||
McKay, RM and Dunbar, GB and Naish, TR and Barrett, PJ and Carter, L and Harper, M Retreat history of the Ross Ice Sheet (Shelf) since the Last Glacial Maximum from deep-basin sediment cores around Ross Island Palaeogeography, Palaeoclimatology, Palaeoecology, 2008 DOI: 10.1016/j.palaeo.2007.08.015 |
Cores in this publication |
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Anderson, John B and Conway, Howard and Bart, Philip J and Witus, Alexandra E and Greenwood, Sarah L and McKay, Robert M and Hall, Brenda L and Ackert, Robert P and Licht, Kathy and Jakobsson, Martin and others Ross Sea paleo-ice sheet drainage and deglacial history during and since the LGM Quaternary Science Reviews, 2014 DOI: 10.1016/j.quascirev.2013.08.020 |
Cores in this publication |
Core-related info: | ||
Core name | HWD03-2 | |
Setting | ice shelf | |
Region | Ross Ice Shelf, Ross Sea | |
Collection date | None | |
IGSN ID | ||
Core type | hot water drill | |
Latitude | -77.83518333 | |
Longitude | 167.336817 | |
Water depth (m) | None | |
Core length (cm) | None | |
Comments | None |
Samples in this core: | |||||
Sample link | Core depth (cm) | Lithology | Facies interpretation | Carbon type | 14C age |
181 | 1.0 - 2.5 | Sandy mud | AIO | 2701.0 ± 50.0 | |
182 | 9.0 - 10.0 | Silty clay | AIO | 4743.0 ± 40.0 | |
183 | 28.0 - 29.0 | Silty clay | AIO | 6562.0 ± 45.0 | |
184 | 58.0 - 59.0 | Silty clay/diamicton boundary | AIO | 12797.0 ± 85.0 |
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 | ||