Associated publications

Title Author(s) Publication DOI View cores
Expansion and rapid retreat of the West Antarctic Ice Sheet in eastern Ross Sea: possible consequence of over-extended ice streams? Mosola, Amanda B and Anderson, John B Quaternary Science Reviews, 2006 https://doi.org/10.1016/j.quascirev.2005.12.013
Ross Sea paleo-ice sheet drainage and deglacial history during and since the LGM 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 Quaternary Science Reviews, 2014 https://doi.org/10.1016/j.quascirev.2013.08.020

Core information

Core name Region Collection date IGSN ID Core type Latitude (DD) Longitude (DD) Water depth
(m)
Core length
(m)
Comments
NBP9902-PC04 Antarctica, Ross Sea None Piston -78.15100 -168.58000 618.0 1.04 The core is slightly disturbed along the core liner from 0-0.15, 0.67-0.9 and 1-1.04 m; The core is slightly disturbed along the core liner from 0-0.15, 0.67-0.9 and 1-1.04 m

Expedition information

Expedition name Ship Start date End date Report DOI
NBP99-02 RV Nathaniel B. Palmer Feb. 12, 1999 March 22, 1999 None

Samples in this core

Sample ID Core depth
(m)
Lithology Facies interpretation Carbon type Sample preparation type Age (14C yr ± 1σ) Calibrated age, median probability (cal. yr BP) Calibrated age, 2σ range (cal. yr BP) Comments
AA49693 0.0 - 0.02 None None AIOM Bulk combustion 21160.0 ± 140.0 Calibrated age for default reservoir correction not available Calibrated age for default reservoir correction not available None
AA49694 0.08 - 0.1 Dark greenish gray (Gley 1, 4/1), stiff, silty mud with an increasing subangular to subrounded sand and abundant (> 50%), subangular to subrounded, very fine to rare very coarse pebble component down core. Several silty mud layers and lenses, with abrupt contacts, occur in the upper part of the core. Subangular to subrounded, very fine to rare very coarse pebbles occur singularly and within a layer in the core. Glacial marine AIOM Bulk combustion 23950.0 ± 230.0 Calibrated age for default reservoir correction not available Calibrated age for default reservoir correction not available None

Associated documents

No associated documents.