ANTARCTIC MARINE C-14
This core appears in the following publications:

Bart, Philip J and Cone, Amy N
Early stall of West Antarctic Ice Sheet advance on the eastern Ross Sea middle shelf followed by retreat at 27,500 14C yr BP
Palaeogeography, Palaeoclimatology, Palaeoecology, 2012
DOI: 10.1016/j.palaeo.2011.08.007		 Cores in
this publication

Anderson, John B and Conway, Howard and Bart, Philip J and Witus, Alexandra E and Greenwood, Sarah L and McKay, Robert M and Hall, Brenda L and Ackert, Robert P and Licht, Kathy and Jakobsson, Martin and others
Ross Sea paleo-ice sheet drainage and deglacial history during and since the LGM
Quaternary Science Reviews, 2014
DOI: 10.1016/j.quascirev.2013.08.020		 Cores in
this publication
Core-related info:
Core name 007-PC
Setting marine
RegionGlomar-Challenger Basin, Ross Sea
Collection date None
IGSN ID
Core type piston core
Latitude -76.40219
Longitude -177.29713
Water depth (m) 621.0
Core length (cm) None
Comments None
Cruise-related info:
CruiseNBP08-02
Ship Nathaniel B. Palmer
Cruise start date 2008-01-30
Cruise end date 2008-02-20
Samples in this core:
Sample link Core depth (cm) Lithology Facies interpretation Carbon type 14C age
9 0.0 - 2.0 Pelagic AIO 5060.0 ± 35.0
10 4.0 - 6.0 Pelagic AIO 6480.0 ± 50.0
11 216.0 - 274.0 Diamict Foraminifera 32400.0 ± 650.0
12 234.0 - 236.0 Diamict AIO 38900.0 ± 880.0
14 248.0 - 250.0 Diamict AIO 42900.0 ± 1400.0
13 346.0 - 376.0 Diamict Foraminifera 31800.0 ± 730.0
15 366.0 - 368.0 Diamict AIO 39700.0 ± 1300.0
16 376.0 - 406.0 Diamict Foraminifera 31500.0 ± 850.0
17 386.0 - 388.0 Diamict AIO 41900.0 ± 1300.0
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