This core appears in the following publications: | ||
Licht, Kathy J and Andrews, John T The 14C record of Late Pleistocene ice advance and retreat in the central Ross Sea, Antarctica Arctic, Antarctic, and Alpine Research, 2002 DOI: 10.1080/15230430.2002.12003501 |
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 | 011-PC | |
Setting | marine | |
Region | Glomar-Challenger Basin, Ross Sea | |
Collection date | None | |
IGSN ID | ARF000HC0 | |
Core type | piston core | |
Latitude | -76.453 | |
Longitude | -179.087 | |
Water depth (m) | 659.0 | |
Core length (cm) | 165.0 | |
Comments | None |
Cruise-related info: | ||
Cruise | NBP95-01 | |
Ship | Nathaniel B. Palmer | |
Cruise start date | 1995-02-07 | |
Cruise end date | 1995-03-13 |
Samples in this core: | |||||
Sample link | Core depth (cm) | Lithology | Facies interpretation | Carbon type | 14C age |
147 | 3.0 - 5.0 | Stratified diamicton | Open marine | AIO | 6640.0 ± 110.0 |
148 | 61.0 - 63.0 | Massive diamicton | Subglacial, max age of ice advance | AIO | 27120.0 ± 305.0 |
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 | ||