This core appears in the following publications:

Mackintosh, Andrew N and Verleyen, Elie and O'Brien, Philip E and White, Duanne A and Jones, R Selwyn and McKay, Robert and Dunbar, Robert and Gore, Damian B and Fink, David and Post, Alexandra L and others
Retreat history of the East Antarctic Ice Sheet since the last glacial maximum
Quaternary Science Reviews, 2014
DOI: 10.1016/j.quascirev.2013.07.024
Cores in
this publication

Leventer, Amy and Domack, Eugene and Pike, Jennifer and Stickley, Catherine and Maddison, Eleanor and Brachfeld, Stefanie A and Manley, Patricia and McClennen, Charlie
Marine sediment record from the East Antarctic margin reveals dynamics of ice sheet recession
GSA Today, 2006
DOI: 10.1130/GSAT01612A.1
Cores in
this publication

Core-related info:
Core name 024-JPC
Setting marine
RegionSvenner Channel, Prydz Bay
Collection date None
IGSN ID ARF000FW1
Core type piston (giant)
Latitude -68.6943333333333
Longitude 76.7092833333333
Water depth (m) 138.0
Core length (cm) None
Comments None

Cruise-related info:
CruiseNBP01-01
Ship Nathaniel B. Palmer
Cruise start date 2001-01-30
Cruise end date 2001-03-28

Samples in this core:
Sample link Core depth (cm) Lithology Facies interpretation Carbon type 14C age
1200 0.0 - 5.0 Siliceous mud and ooze Core top Acid Insoluble Organic Matter 2020.0 ± 50.0
1201 746.0 - 746.0 Siliceous mud and ooze - laminated Articulated bivalve 8840.0 ± 35.0
1202 891.0 - 891.0 Siliceous mud and ooze - laminated Shell matter 9240.0 ± 40.0
1203 924.0 - 924.0 Siliceous mud and ooze - laminated Shell matter 9395.0 ± 35.0
1204 1312.0 - 1312.0 Siliceous mud and ooze - bioturbated Shell matter 10325.0 ± 35.0
1205 1350.0 - 1350.0 Siliceous mud and ooze - bioturbated Indirectly, the onset of deglaciation Bivalve 10315.0 ± 50.0
1206 1741.0 - 1746.0 Diamicton Acid Insoluble Organic Matter 26960.0 ± 680.0

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