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

Licht, Kathy J and Andrews, John T
The 14C record of Late Pleistocene ice advance and retreat in the central Ross Sea, Antarctica
Arctic, Antarctic, and Alpine Research, 2002
DOI: 10.1080/15230430.2002.12003501		 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
RegionRoss Bank, Ross Sea
Collection date None
IGSN ID ARF000HB2
Core type piston core
Latitude -75.625
Longitude -178.587
Water depth (m) 449.0
Core length (cm) 145.0
Comments None
Cruise-related info:
CruiseNBP95-01
Ship Nathaniel B. Palmer
Cruise start date 1995-02-07
Cruise end date 1995-03-13
Samples in this core:
Sample link Core depth (cm) Lithology Facies interpretation Carbon type 14C age
146 2.0 - 4.0 Stratified diamicton Reworked ice proximal glacial marine Benthic foraminifera 21980.0 ± 290.0
142 2.0 - 4.0 Stratified diamicton Reworked ice proximal glacial marine AIO 22975.0 ± 210.0
145 20.0 - 22.0 Stratified diamicton Reworked ice proximal glacial marine Benthic foraminifera 17790.0 ± 195.0
143 21.0 - 22.0 Stratified diamicton Reworked ice proximal glacial marine AIO 25695.0 ± 300.0
141 63.0 - 66.0 Stratified diamicton Reworked ice proximal glacial marine Benthic foraminifera 14970.0 ± 135.0
144 63.0 - 66.0 Stratified diamicton Reworked ice proximal glacial marine AIO 20780.0 ± 220.0
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