This core appears in the following publications:

Hillenbrand, Claus-Dieter and Kuhn, Gerhard and Smith, James A and Gohl, Karsten and Graham, Alastair GC and Larter, Robert D and Klages, Johann P and Downey, Rachel and Moreton, Steven G and Forwick, Matthias and others
Grounding-line retreat of the west Antarctic ice sheet from inner Pine island Bay
Geology, 2013
DOI: 10.1130/G33469.1
Cores in
this publication

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

Core-related info:
Core name PS75/214-1
Setting marine
RegionAmundsen Sea Embayment, undifferentiated, Amundsen Sea
Collection date None
IGSN ID
Core type Gravity
Latitude -74.532667
Longitude -102.621333
Water depth (m) 641.0
Core length (cm) None
Comments None

Cruise-related info:
CruiseANT-XXVI/3
Ship Polarstern
Cruise start date 2010-01-30
Cruise end date 2010-04-05

Samples in this core:
Sample link Core depth (cm) Lithology Facies interpretation Carbon type 14C age
3072 240.0 - 240.0 mud with silt layers glacimarine under sea ice or thin ice-shelf distal from grounding line undifferentiated or mixed benthic and planktonic foraminifera, ostracods 8830.0 ± 40.0
3073 280.0 - 280.0 mud with silt layers glacimarine under sea ice or thin ice-shelf distal from grounding line undifferentiated or mixed benthic and planktonic foraminifera, ostracods 8540.0 ± 40.0
3074 400.0 - 400.0 mud with silt layers glacimarine under sea ice or thin ice-shelf distal from grounding line undifferentiated or mixed benthic and planktonic foraminifera, ostracods 8580.0 ± 40.0
3075 480.0 - 497.0 mud with sandy and gravelly layers glacimarine under sea ice or thin ice-shelf proximal to grounding line undifferentiated or mixed benthic and planktonic foraminifera 11090.0 ± 50.0
3076 578.0 - 578.0 pebbly gravel glacimarine under sea ice or thin ice-shelf proximal to grounding line bivalves, benthic foraminifera 8280.0 ± 40.0

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