| 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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| Core-related info: | ||
| Core name | U1357A-18H | |
| Setting | marine | |
| Region | Ad{\'e}lie Basin, Wilkes Land Coast | |
| Collection date | 2010-02-03 | |
| IGSN ID | ||
| Core type | ||
| Latitude | -66.41331833 | |
| Longitude | 140.42501333 | |
| Water depth (m) | 1017.0 | |
| Core length (cm) | None | |
| Comments | None | |
| Cruise-related info: | ||
| Cruise | IODP Expedition 318 | |
| Ship | JOIDES Resolution | |
| Cruise start date | 2010-01-04 | |
| Cruise end date | 2010-03-08 | |
| Samples in this core: | |||||
| Sample link | Core depth (cm) | Lithology | Facies interpretation | Carbon type | 14C age |
| 1251 | 16217.0 - 16217.0 | Diatom ooze (laminated with >90 percent opal in smear slides) | Onset of open marine sediment with no glacimarine influence | Bulk organic carbon | 10075.0 ± 45.0 |
| 1252 | 16834.0 - 16834.0 | Diatom ooze (laminated with >90 percent opal in smear slides) | Onset of open marine sediment with no glacimarine influence | Bulk organic carbon | 10790.0 ± 40.0 |
| 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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