| 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 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 name | Ship | Start date | End date | Report DOI |
|---|---|---|---|---|
| NBP99-02 | RV Nathaniel B. Palmer | Feb. 12, 1999 | March 22, 1999 | None |
| 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 |
No associated documents.