| 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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| Leventer, Amy and Domack, Eugene and Pike, Jennifer and Stickley, Catherine and Maddison, Eleanor and Brachfeld, Stefanie A and Manley, Patricia and McClennen, Charlie Marine sediment record from the East Antarctic margin reveals dynamics of ice sheet recession GSA Today, 2006 DOI: 10.1130/GSAT01612A.1 |
Cores in this publication |
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| Mackintosh, Andrew and Golledge, Nicholas and Domack, Eugene and Dunbar, Robert and Leventer, Amy and White, Duanne and Pollard, David and DeConto, Robert and Fink, David and Zwartz, Dan and others Retreat of the East Antarctic ice sheet during the last glacial termination Nature Geoscience, 2011 DOI: 10.1038/ngeo1061 |
Cores in this publication |
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| Core-related info: | ||
| Core name | 040-JPC | |
| Setting | marine | |
| Region | Mawson Coast Continental Shelf, Mawson Coast Continental Shelf | |
| Collection date | None | |
| IGSN ID | ||
| Core type | piston (giant) | |
| Latitude | -67.17645 | |
| Longitude | 65.73685 | |
| Water depth (m) | 750.0 | |
| Core length (cm) | None | |
| Comments | None | |
| Cruise-related info: | ||
| Cruise | NBP01-01 | |
| Ship | Nathaniel B. Palmer | |
| Cruise start date | 2001-01-30 | |
| Cruise end date | 2001-03-28 | |
| Samples in this core: | |||||
| Sample link | Core depth (cm) | Lithology | Facies interpretation | Carbon type | 14C age |
| 1181 | 101.0 - 101.0 | Core top | Acid Insoluble Organic Matter | 2400.0 ± 35.0 | |
| 1182 | 201.0 - 201.0 | Acid Insoluble Organic Matter | 2690.0 ± 35.0 | ||
| 1183 | 401.0 - 401.0 | Acid Insoluble Organic Matter | 3225.0 ± 40.0 | ||
| 1184 | 601.0 - 601.0 | Acid Insoluble Organic Matter | 4015.0 ± 30.0 | ||
| 1185 | 801.0 - 801.0 | Acid Insoluble Organic Matter | 4480.0 ± 35.0 | ||
| 1186 | 1001.0 - 1001.0 | Acid Insoluble Organic Matter | 5555.0 ± 35.0 | ||
| 1187 | 1401.0 - 1401.0 | Acid Insoluble Organic Matter | 7910.0 ± 35.0 | ||
| 1188 | 1659.0 - 1659.0 | Acid Insoluble Organic Matter | 9825.0 ± 35.0 | ||
| 1189 | 2119.0 - 2119.0 | Rhythmically laminated sediments | Calving bay re-entrant in association with deglaciation | Acid Insoluble Organic Matter | 13895.0 ± 40.0 |
| 1190 | 2141.0 - 2141.0 | Rhythmically laminated sediments | Calving bay re-entrant in association with deglaciation | Acid Insoluble Organic Matter | 13520.0 ± 130.0 |
| 1191 | 2211.0 - 2211.0 | Glacial diamict | Acid Insoluble Organic Matter | 25230.0 ± 110.0 | |
| Depth-age relationship: | ||
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| Plot key: black and gray bars represent 68.2% and 95.45% HPD interval(s), respectively. | ||
| Questions about this page: Ryan Venturelli |
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