| This core appears in the following publications: | ||
| Arndt, Jan Erik and Hillenbrand, Claus-Dieter and Grobe, Hannes and Kuhn, Gerhard and Wacker, Lukas Evidence for a dynamic grounding line in outer Filchner Trough, Antarctica, until the early Holocene Geology, 2017 DOI: 10.1130/G39398.1 |
Cores in this publication |
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| Core-related info: | ||
| Core name | PS96/80-1 | |
| Setting | marine | |
| Region | Filchner Trough, Weddell Sea | |
| Collection date | None | |
| IGSN ID | None | |
| Core type | gravity | |
| Latitude | -75.689 | |
| Longitude | -31.7983 | |
| Water depth (m) | 720.0 | |
| Core length (cm) | 223.0 | |
| Comments | None | |
| Cruise-related info: | ||
| Cruise | ANT-XXXI/2 | |
| Ship | Polarstern | |
| Cruise start date | 2015-12-06 | |
| Cruise end date | 2016-02-14 | |
| Samples in this core: | |||||
| Sample link | Core depth (cm) | Lithology | Facies interpretation | Carbon type | 14C age |
| 3448 | 20.0 - 20.0 | Massive, purely terrigenous muddy diamicton. | Subglacial till deposition, IRD rainout proximal to grounding line, glacigenic debris flow. | Benthic foraminifera (Globocassidulina spp.) | 14120.0 ± 90.0 |
| 3449 | 120.0 - 120.0 | Massive, purely terrigenous muddy diamicton. | Subglacial till deposition, IRD rainout proximal to grounding line, glacigenic debris flow. | Benthic foraminifera (Globocassidulina spp.) | 11415.0 ± 85.0 |
| 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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