This core appears in the following publications: | ||
Mackintosh, Andrew N and Verleyen, Elie and O'Brien, Philip E and White, Duanne A and Jones, R Selwyn and McKay, Robert and Dunbar, Robert and Gore, Damian B and Fink, David and Post, Alexandra L and others Retreat history of the East Antarctic Ice Sheet since the last glacial maximum Quaternary Science Reviews, 2014 DOI: 10.1016/j.quascirev.2013.07.024 |
Cores in this publication |
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Harris, Peter T and Brancolini, Giuliano and Armand, Leanne and Busetti, Martina and Beaman, Robin J and Giorgetti, Giovanna and Presti, Massimo and Trincardi, Fabio Continental shelf drift deposit indicates non-steady state Antarctic bottom water production in the Holocene Marine Geology, 2001 DOI: 10.1016/S0025-3227(01)00183-9 |
Cores in this publication |
Core-related info: | ||
Core name | 24PC10 | |
Setting | marine | |
Region | Commonwealth Bay, Wilkes Land Coast | |
Collection date | None | |
IGSN ID | ||
Core type | piston | |
Latitude | -66.4815 | |
Longitude | 143.01 | |
Water depth (m) | 819.0 | |
Core length (cm) | None | |
Comments | None |
Cruise-related info: | ||
Cruise | GA217 | |
Ship | Tangaroa | |
Cruise start date | 2000-02-11 | |
Cruise end date | 2000-03-20 |
Samples in this core: | |||||
Sample link | Core depth (cm) | Lithology | Facies interpretation | Carbon type | 14C age |
1219 | 1.0 - 1.0 | Unit 4, uppermost SMO | Core top age | Acid Insoluble Organic Matter | 2700.0 ± 55.0 |
1220 | 122.0 - 123.0 | Unit 2, IRD rich massive SMO, base | Onset of open marine sedimentation | Acid Insoluble Organic Matter | 16807.0 ± 80.0 |
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 | ||