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 PS75/167-1
Setting marine
RegionPine Island Trough, Amundsen Sea
Collection date None
IGSN ID
Core type Gravity
Latitude -74.622833
Longitude -105.801833
Water depth (m) 526.0
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
3085 230.0 - 230.0 mud seasonal open-marine undifferentiated or mixed benthic and planktonic foraminifera 8490.0 ± 40.0
3086 250.0 - 250.0 sandy gravel gravity flow or winnowing of glacomarine sediment under sea ice/ice shelf proximal to grounding line unspecified calcareous shell or shell fragments, undifferentiated or mixed benthic and planktonic foraminifera 8740.0 ± 40.0
3087 280.0 - 280.0 sand gravity flow or winnowing of glacomarine sediment under sea ice/ice shelf proximal to grounding line undifferentiated or mixed benthic and planktonic foraminifera 9080.0 ± 50.0
3088 401.0 - 401.0 sand gravity flow or winnowing of glacomarine sediment under sea ice/ice shelf proximal to grounding line unspecified calcareous shell or shell fragments, undifferentiated or mixed benthic and planktonic foraminifera, ostracods 9210.0 ± 50.0
3089 478.0 - 478.0 sand gravity flow or winnowing of glacomarine sediment under sea ice/ice shelf proximal to grounding line echinoid spines, ostracods, undifferentiated or mixed benthic and planktonic foraminifera 9180.0 ± 40.0
3090 598.0 - 598.0 sand gravity flow or winnowing of glacomarine sediment under sea ice/ice shelf proximal to grounding line undifferentiated or mixed benthic and planktonic foraminifera 9490.0 ± 40.0
3091 625.5 - 625.5 sand gravity flow or winnowing of glacomarine sediment under sea ice/ice shelf proximal to grounding line undifferentiated or mixed benthic and planktonic foraminifera 9660.0 ± 50.0
3092 649.0 - 649.0 sand gravity flow or winnowing of glacomarine sediment under sea ice/ice shelf proximal to grounding line undifferentiated or mixed benthic and planktonic foraminifera 9280.0 ± 40.0
3093 670.0 - 670.0 sand gravity flow or winnowing of glacomarine sediment under sea ice/ice shelf proximal to grounding line undifferentiated or mixed benthic and planktonic foraminifera 9450.0 ± 50.0
3094 746.0 - 746.0 sand gravity flow or winnowing of glacomarine sediment under sea ice/ice shelf proximal to grounding line unspecified calcareous shell or shell fragments, undifferentiated or mixed benthic and planktonic foraminifera 9690.0 ± 50.0
3095 830.0 - 830.0 sand gravity flow or winnowing of glacomarine sediment under sea ice/ice shelf proximal to grounding line undifferentiated or mixed benthic and planktonic foraminifera 9620.0 ± 50.0
3096 900.5 - 900.5 sand gravity flow or winnowing of glacomarine sediment under sea ice/ice shelf proximal to grounding line unspecified calcareous shell or shell fragments, undifferentiated or mixed benthic and planktonic foraminifera 10210.0 ± 60.0

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