Core

This core appears in the following publications:

	Larter, Robert D and Anderson, John B and Graham, Alastair GC and Gohl, Karsten and Hillenbrand, Claus-Dieter and Jakobsson, Martin and Johnson, Joanne S and Kuhn, Gerhard and Nitsche, Frank O and Smith, James A and others Reconstruction of changes in the Amundsen Sea and Bellingshausen sea sector of the West Antarctic ice sheet since the last glacial maximum Quaternary Science Reviews, 2014 DOI: 10.1016/j.quascirev.2013.10.016	Cores in this publication

	Hillenbrand, C-D and Larter, Robert D and Dowdeswell, JA and Ehrmann, W and Cofaigh, C {\'O} and Benetti, S and Graham, Alastair GC and Grobe, Hannes The sedimentary legacy of a palaeo-ice stream on the shelf of the southern Bellingshausen Sea: Clues to West Antarctic glacial history during the Late Quaternary Quaternary Science Reviews, 2010 DOI: 10.1016/j.quascirev.2010.06.028	Cores in this publication


Samples in this core:
Sample link	Core depth (cm)	Lithology	Facies interpretation	Carbon type	¹⁴C age
3060	0.0 - 1.0	foraminifera-bearing mud	seasonal open-marine	acid insoluble organic matter	6429.0 ± 73.0
3212	7.0 - 7.0	foraminifera-bearing mud	seasonal open-marine	planktonic foraminifera	5817.0 ± 65.0
3213	10.0 - 10.0	gravelly sandy mud	glacimarine under sea ice or thin ice-shelf distal from grounding line	acid insoluble organic matter	12140.0 ± 191.0
3214	16.0 - 16.0	gravelly sandy mud	glacimarine under sea ice or thin ice-shelf distal from grounding line	acid insoluble organic matter	23735.0 ± 356.0
3215	55.0 - 55.0	muddy diamicton	subglacial	acid insoluble organic matter	41814.0 ± 3080.0


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