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 |
Core-related info: | ||
Core name | PS96/79-3 | |
Setting | marine | |
Region | Filchner Trough, Weddell Sea | |
Collection date | None | |
IGSN ID | None | |
Core type | gravity | |
Latitude | -75.625 | |
Longitude | -31.8722 | |
Water depth (m) | 763.0 | |
Core length (cm) | 181.0 | |
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 |
3446 | 17.0 - 17.0 | Laminated and stratified mud alternating with gravelly sandy mud and gravelly muddy sand. | Suspension settline from turbid plumes, current-influenced glacimarine deposition, hemipelagic sedimentation with deposition of ice-rafted debris. | Benthic foraminifera (Globocassidulina spp. and Cibicides spp.) | 9995.0 ± 75.0 |
3447 | 150.0 - 150.0 | Laminated and stratified mud alternating with gravelly sandy mud and gravelly muddy sand. | Suspension settline from turbid plumes, current-influenced glacimarine deposition, hemipelagic sedimentation with deposition of ice-rafted debris. | Benthic and planktonic foraminifera (Globocassidulina spp., Neogloboquadrina pachyderma sinistral, and Cibicides spp.) | 24560.0 ± 250.0 |
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 | ||