| This core appears in the following publications: | ||
| Domack, Eugene W and Jacobson, Erik A and Shipp, Stephanie and Anderson, John B Late Pleistocene--Holocene retreat of the West Antarctic Ice-Sheet system in the Ross Sea: Part 2—sedimentologic and stratigraphic signature Geological Society of America Bulletin, 1999 DOI: 10.1130/0016-7606(1999)111<1517:LPHROT>2.3.CO;2 |
Cores in this publication |
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| 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 Ross Sea paleo-ice sheet drainage and deglacial history during and since the LGM Quaternary Science Reviews, 2014 DOI: 10.1016/j.quascirev.2013.08.020 |
Cores in this publication |
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| Core-related info: | ||
| Core name | 037-KC | |
| Setting | marine | |
| Region | Drygalski Trough, Ross Sea | |
| Collection date | None | |
| IGSN ID | ARF000GA8 | |
| Core type | Kasten core | |
| Latitude | -74.498 | |
| Longitude | 167.743 | |
| Water depth (m) | 924.0 | |
| Core length (cm) | 173.0 | |
| Comments | None | |
| Cruise-related info: | ||
| Cruise | NBP95-01 | |
| Ship | Nathaniel B. Palmer | |
| Cruise start date | 1995-02-07 | |
| Cruise end date | 1995-03-13 | |
| Samples in this core: | |||||
| Sample link | Core depth (cm) | Lithology | Facies interpretation | Carbon type | 14C age |
| 236 | 0.0 - 2.0 | Massive mud | Open water | AIO | 2775.0 ± 50.0 |
| 29 | 0.0 - 2.0 | Diatom mud and ooze | Open marine | AIO | 2780.0 ± 50.0 |
| 242 | 10.0 - 11.0 | Massive mud | Open water | AIO | 3020.0 ± 50.0 |
| 30 | 10.0 - 11.0 | Diatom mud and ooze | Open marine | AIO | 3020.0 ± 50.0 |
| 237 | 20.0 - 21.0 | Massive mud | Open water | AIO | 4715.0 ± 50.0 |
| 31 | 20.0 - 21.0 | Diatom mud and ooze | Open marine | AIO | 4720.0 ± 50.0 |
| 32 | 30.0 - 31.0 | Diatom mud and ooze | Open marine | AIO | 6210.0 ± 55.0 |
| 241 | 30.0 - 31.0 | Massive mud | Open water | AIO | 6205.0 ± 55.0 |
| 238 | 40.0 - 41.0 | Ash-rich sand | Transitional | AIO | 8630.0 ± 85.0 |
| 33 | 40.0 - 41.0 | Diatom mud and ooze | Open marine | AIO | 8630.0 ± 85.0 |
| 34 | 55.0 - 56.0 | Sandy diatom mud | Calving line | AIO | 10500.0 ± 75.0 |
| 240 | 55.0 - 56.0 | Ash-rich sand | Transitional | AIO | 10495.0 ± 75.0 |
| 35 | 67.0 - 68.0 | Silty clay | Distal ice shelf | AIO | 13840.0 ± 95.0 |
| 239 | 67.0 - 68.0 | Massive mud | Transitional | AIO | 13835.0 ± 95.0 |
| 243 | 83.0 - 84.0 | Massive mud | Transitional | AIO | 17800.0 ± 175.0 |
| 246 | 93.0 - 95.0 | Massive mud | Transitional | AIO | 19385.0 ± 135.0 |
| 245 | 125.0 - 127.0 | Sandy mud | Transitional | AIO | 30695.0 ± 460.0 |
| 244 | 146.0 - 148.0 | Pebbly, massive diamicton | Glacial | AIO | 26895.0 ± 375.0 |
| Depth-age relationship: | ||
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| Plot key: black and gray bars represent 68.2% and 95.45% HPD interval(s), respectively. | ||
| Questions about this page: Ryan Venturelli |
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