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 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 VC244
Setting marine
RegionPrince Gustav Channel, Eastern Antarctic Peninsula
Collection date 2000-03-05
IGSN ID
Core type vibrocore
Latitude -64.2988601306902
Longitude -58.5864566153296
Water depth (m) 757.0
Core length (cm) 486.0
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
752 1.0 - 1.0 Diatom-bearing clayey silt seasonal open-marine acid insoluble organic matter 6550.0 ± 40.0
757 86.0 - 86.0 Diatom-bearing clayey silt seasonal open-marine acid insoluble organic matter 8560.0 ± 40.0
753 166.0 - 166.0 Diatom-bearing clayey silt seasonal open-marine acid insoluble organic matter 10180.0 ± 40.0
754 198.0 - 198.0 Diatom-bearing clayey silt sub-ice shelf? acid insoluble organic matter 11450.0 ± 50.0
755 257.0 - 257.0 Diatom-bearing clayey silt sub-ice shelf? acid insoluble organic matter 14700.0 ± 80.0
682 297.0 - 297.0 transitional glaciomarine acid insoluble organic matter 17450.0 ± 60.0
756 318.0 - 318.0 Silty clay Distal ice shelf acid insoluble organic matter 23950.0 ± 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