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

Hemer, Mark A and Harris, Peter T
Sediment core from beneath the Amery Ice Shelf, East Antarctica, suggests mid-Holocene ice-shelf retreat
Geology, 2003
DOI: 10.1130/0091-7613(2003)031<0127:SCFBTA>2.0.CO;2
Cores in
this publication

Hemer, MA and Post, AL and O'Brien, Philip Edward and Craven, M and Truswell, EM and Roberts, Donna and Harris, PT
Sedimentological signatures of the sub-Amery Ice Shelf circulation
Antarctic Science, 2007
DOI: 10.1017/S0954102007000697
Cores in
this publication

Core-related info:
Core name AMO2
Setting Ice shelf
RegionAmery Ice Shelf, Prydz Bay
Collection date None
IGSN ID
Core type gravity
Latitude -69.7133
Longitude 72.64
Water depth (m) 840.0
Core length (cm) None
Comments None

Samples in this core:
Sample link Core depth (cm) Lithology Facies interpretation Carbon type 14C age
1210 0.0 - 1.0 Massive siliceous mud and ooze - bioturbated Modern-day sub-ice shelf surface date Acid Insoluble Organic Matter 6548.0 ± 60.0
1211 12.0 - 12.0 Massive siliceous mud and ooze - bioturbated Sub-ice shelf sedimentation +/- reworked carbon? Acid Insoluble Organic Matter 7280.0 ± 60.0
1212 38.0 - 38.0 Massive siliceous mud and ooze - bioturbated Sub-ice shelf sedimentation +/- reworked carbon? Acid Insoluble Organic Matter 16901.0 ± 85.0
1213 51.0 - 52.0 Massive siliceous mud and ooze - bioturbated Sub-ice shelf sedimentation +/- reworked carbon? Acid Insoluble Organic Matter 21680.0 ± 160.0

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