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 |
Core-related info: | ||
Core name | U1357B-18H | |
Setting | marine | |
Region | Ad{\'e}lie Basin, Wilkes Land Coast | |
Collection date | 2010-02-04 | |
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 |
1253 | 15513.5 - 15513.5 | Diatom ooze (laminated with >90 percent opal in smear slides) | Onset of open marine sediment with no glacimarine influence | Bulk organic carbon | 9605.0 ± 30.0 |
1254 | 15740.5 - 15740.5 | Diatom ooze (laminated with >90 percent opal in smear slides) | Onset of open marine sediment with no glacimarine influence | Bulk organic carbon | 10065.0 ± 35.0 |
1255 | 15956.5 - 15956.5 | Diatom ooze (laminated with >90 percent opal in smear slides) | Onset of open marine sediment with no glacimarine influence | Bulk organic carbon | 10360.0 ± 35.0 |
1256 | 16132.5 - 16132.5 | Diatom ooze (laminated with >90 percent opal in smear slides) | Onset of open marine sediment with no glacimarine influence | Bulk organic carbon | 10565.0 ± 35.0 |
1257 | 16331.5 - 16331.5 | Diatom ooze (laminated with >90 percent opal in smear slides) | Onset of open marine sediment with no glacimarine influence | Bulk organic carbon | 10600.0 ± 35.0 |
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 | ||