This core appears in the following publications:

Cofaigh, Colm {\'O} and Davies, Bethan J and Livingstone, Stephen J and Smith, James A and Johnson, Joanne S and Hocking, Emma P and Hodgson, Dominic A and Anderson, John B and Bentley, Michael J and Canals, Miquel and others
Reconstruction of ice-sheet changes in the Antarctic Peninsula since the Last Glacial Maximum
Quaternary Science Reviews, 2014
DOI: 10.1016/j.quascirev.2014.06.023
Cores in
this publication

Pudsey, Carol J and Murray, John W and Appleby, Peter and Evans, Jeffrey
Ice shelf history from petrographic and foraminiferal evidence, Northeast Antarctic Peninsula
Quaternary Science Reviews, 2006
DOI: 10.1016/j.quascirev.2006.01.029
Cores in
this publication

Pudsey, Carol J and Evans, Jeffrey
First survey of Antarctic sub--ice shelf sediments reveals mid-Holocene ice shelf retreat
Geology, 2001
DOI: 10.1130/0091-7613(2001)029<0787:FSOASI>2.0.CO;2
Cores in
this publication

Core-related info:
Core name VC243
Setting marine
RegionR{\"o}hss Bay, Eastern Antarctic Peninsula
Collection date None
IGSN ID
Core type
Latitude -64.225
Longitude -58.305
Water depth (m) 649.0
Core length (cm) None
Comments

Cruise-related info:
CruiseJR48
Ship James Clark Ross
Cruise start date 2000-03-27
Cruise end date 2000-04-01

Samples in this core:
Sample link Core depth (cm) Lithology Facies interpretation Carbon type 14C age
747 1.0 - 1.0 Diatom-bearing clayey silt seasonal open-marine acid insoluble organic matter 6010.0 ± 50.0
748 155.0 - 155.0 Diatom-bearing clayey silt seasonal open-marine acid insoluble organic matter 7930.0 ± 40.0
749 305.0 - 305.0 Diatom-bearing clayey silt seasonal open-marine acid insoluble organic matter 9030.0 ± 40.0
750 476.0 - 476.0 Diatom-bearing clayey silt sub-ice shelf? acid insoluble organic matter 11350.0 ± 60.0
751 592.0 - 592.0 Diatom-bearing clayey silt sub-ice shelf? acid insoluble organic matter 12450.0 ± 40.0
690 592.0 - 592.0 dbGM acid insoluble organic matter 12450.0 ± 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