ANTARCTIC MARINE C-14
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

Kirshner, Alexandra E and Anderson, John B and Jakobsson, Martin and O’Regan, Matthew and Majewski, Wojciech and Nitsche, Frank O
Post-LGM deglaciation in Pine island Bay, west Antarctica
Quaternary Science Reviews, 2012
DOI: 10.1016/j.quascirev.2012.01.017		 Cores in
this publication

Jakobsson, Martin and Anderson, John B and Nitsche, Frank O and Dowdeswell, Julian A and Gyllencreutz, Richard and Kirchner, Nina and Mohammad, Rezwan and O'Regan, Matthew and Alley, Richard B and Anandakrishnan, Sridhar and others
Geological record of ice shelf break-up and grounding line retreat, Pine Island Bay, West Antarctica
Geology, 2011
DOI: 10.1130/G32153.1		 Cores in
this publication
Core-related info:
Core name KC19
Setting marine
RegionPine Island Trough, Amundsen Sea
Collection date None
IGSN ID
Core type Kasten
Latitude -73.1285
Longitude -106.9688
Water depth (m) 782.0
Core length (cm) None
Comments None
Cruise-related info:
CruiseOSO0910
Ship Oden
Cruise start date 2010-02-08
Cruise end date None
Samples in this core:
Sample link Core depth (cm) Lithology Facies interpretation Carbon type 14C age
3113 77.0 - 79.0 sandy mud sub-ice shelf planktonic foraminifera 10600.0 ± 60.0
3114 84.0 - 86.0 sandy mud sub-ice shelf planktonic foraminifera 10960.0 ± 90.0
3115 90.0 - 92.0 sandy mud sub-ice shelf planktonic foraminifera 11775.0 ± 100.0
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