This core appears in the following publications:

Larter, Robert D and Anderson, John B and Graham, Alastair GC and Gohl, Karsten and Hillenbrand, Claus-Dieter and Jakobsson, Martin and Johnson, Joanne S and Kuhn, Gerhard and Nitsche, Frank O and Smith, James A and others
Reconstruction of changes in the Amundsen Sea and Bellingshausen sea sector of the West Antarctic ice sheet since the last glacial maximum
Quaternary Science Reviews, 2014
DOI: 10.1016/j.quascirev.2013.10.016
Cores in
this publication

Hillenbrand, C-D and Larter, Robert D and Dowdeswell, JA and Ehrmann, W and Cofaigh, C {\'O} and Benetti, S and Graham, Alastair GC and Grobe, Hannes
The sedimentary legacy of a palaeo-ice stream on the shelf of the southern Bellingshausen Sea: Clues to West Antarctic glacial history during the Late Quaternary
Quaternary Science Reviews, 2010
DOI: 10.1016/j.quascirev.2010.06.028
Cores in
this publication

Core-related info:
Core name GC357
Setting marine
RegionUnknown
Collection date None
IGSN ID
Core type Gravity
Latitude -71.7667
Longitude -80.11
Water depth (m) 565.0
Core length (cm) None
Comments None

Cruise-related info:
CruiseJR104
Ship James Clark Ross
Cruise start date 2004-01-23
Cruise end date 2004-02-13

Samples in this core:
Sample link Core depth (cm) Lithology Facies interpretation Carbon type 14C age
3060 0.0 - 1.0 foraminifera-bearing mud seasonal open-marine acid insoluble organic matter 6429.0 ± 73.0
3212 7.0 - 7.0 foraminifera-bearing mud seasonal open-marine planktonic foraminifera 5817.0 ± 65.0
3213 10.0 - 10.0 gravelly sandy mud glacimarine under sea ice or thin ice-shelf distal from grounding line acid insoluble organic matter 12140.0 ± 191.0
3214 16.0 - 16.0 gravelly sandy mud glacimarine under sea ice or thin ice-shelf distal from grounding line acid insoluble organic matter 23735.0 ± 356.0
3215 55.0 - 55.0 muddy diamicton subglacial acid insoluble organic matter 41814.0 ± 3080.0

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