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 GC374
Setting marine
RegionBelgica Trough, Bellingshausen Sea
Collection date None
IGSN ID
Core type Gravity
Latitude -70.5
Longitude -86.2367
Water depth (m) 650.0
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
3066 0.0 - 1.0 foraminiferal mud seasonal open-marine acid insoluble organic matter 4524.0 ± 62.0
3230 9.5 - 9.5 foraminifera-bearing mud seasonal open-marine planktonic foraminifera 4063.0 ± 64.0
3231 12.0 - 12.0 gravelly sandy mud glacimarine under sea ice or thin ice-shelf distal from grounding line acid insoluble organic matter 27512.0 ± 721.0
3232 28.0 - 28.0 gravelly sandy mud glacimarine under sea ice or thin ice-shelf distal from grounding line acid insoluble organic matter 33916.0 ± 2146.0
3233 93.0 - 93.0 muddy diamicton glacimarine under ice shelf proximal to grounding line acid insoluble organic matter 40138.0 ± 3662.0

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