Planktic foraminifers, ice-rafted debris and stable isotopes from three sediment cores along the East/South Greenland margin ...
Sediment core GS16-204-22CC-A (58° 02.83 N, 47° 02.36 W, water depth 3160 m) was retrieved at the Eirik drift with R/V G.O. Sars in 2016. The core was sampled every 2 cm between 200 and 530.5 cm with a sample width of 0.5 cm. Bulk sample weights were taken prior to and after freeze-drying. Subsequen...
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ftdatacite:10.1594/pangaea.904065 2024-04-28T08:11:07+00:00 Planktic foraminifers, ice-rafted debris and stable isotopes from three sediment cores along the East/South Greenland margin ... Griem, Lisa Voelker, Antje H L Berben, Sarah M P Dokken, Trond Jansen, Eystein 2019 application/zip https://dx.doi.org/10.1594/pangaea.904065 https://doi.pangaea.de/10.1594/PANGAEA.904065 en eng PANGAEA https://dx.doi.org/10.1029/2019pa003605 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Arctic Sea Ice and Greenland Ice Sheet Sensitivity ice2ice article Supplementary Publication Series of Datasets Collection 2019 ftdatacite https://doi.org/10.1594/pangaea.90406510.1029/2019pa003605 2024-04-02T11:42:33Z Sediment core GS16-204-22CC-A (58° 02.83 N, 47° 02.36 W, water depth 3160 m) was retrieved at the Eirik drift with R/V G.O. Sars in 2016. The core was sampled every 2 cm between 200 and 530.5 cm with a sample width of 0.5 cm. Bulk sample weights were taken prior to and after freeze-drying. Subsequently, the bulk samples were wet sieving (63 µm-sieve) and the coarse fraction was dry sieved into size fractions 63-106 µm, 106-150 µm, 150-500 µm, 500-1000 µm and > 1mm. Size fraction 150-500 µm was split (max. 4x) for foraminifer and IRD counts and the number was added to numbers counted in size fractions 500-1000 µm and > 1mm (results in >150 µm/g dry sediment). In order to calculate the according fluxes we multiplied the respective concentrations with the bulk mass accumulation rate following Peck et al. (2007). Hereby, a sediment particle, carbonate and water density of 2.650, 2.730 and 1.025 g cm-3 were assumed, respectively. Additionally, the ratio between lithic grains and planktic foraminifers was ... : Supplement to: Griem, Lisa; Voelker, Antje H L; Berben, Sarah M P; Dokken, Trond; Jansen, Eystein (2019): Insolation and Glacial Meltwater Influence on Sea‐Ice and Circulation Variability in the Northeastern Labrador Sea During the Last Glacial Period. Paleoceanography and Paleoclimatology, 34(11), 1689-1709 ... Article in Journal/Newspaper Arctic Greenland Ice Sheet Labrador Sea Sea ice DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Arctic Sea Ice and Greenland Ice Sheet Sensitivity ice2ice |
spellingShingle |
Arctic Sea Ice and Greenland Ice Sheet Sensitivity ice2ice Griem, Lisa Voelker, Antje H L Berben, Sarah M P Dokken, Trond Jansen, Eystein Planktic foraminifers, ice-rafted debris and stable isotopes from three sediment cores along the East/South Greenland margin ... |
topic_facet |
Arctic Sea Ice and Greenland Ice Sheet Sensitivity ice2ice |
description |
Sediment core GS16-204-22CC-A (58° 02.83 N, 47° 02.36 W, water depth 3160 m) was retrieved at the Eirik drift with R/V G.O. Sars in 2016. The core was sampled every 2 cm between 200 and 530.5 cm with a sample width of 0.5 cm. Bulk sample weights were taken prior to and after freeze-drying. Subsequently, the bulk samples were wet sieving (63 µm-sieve) and the coarse fraction was dry sieved into size fractions 63-106 µm, 106-150 µm, 150-500 µm, 500-1000 µm and > 1mm. Size fraction 150-500 µm was split (max. 4x) for foraminifer and IRD counts and the number was added to numbers counted in size fractions 500-1000 µm and > 1mm (results in >150 µm/g dry sediment). In order to calculate the according fluxes we multiplied the respective concentrations with the bulk mass accumulation rate following Peck et al. (2007). Hereby, a sediment particle, carbonate and water density of 2.650, 2.730 and 1.025 g cm-3 were assumed, respectively. Additionally, the ratio between lithic grains and planktic foraminifers was ... : Supplement to: Griem, Lisa; Voelker, Antje H L; Berben, Sarah M P; Dokken, Trond; Jansen, Eystein (2019): Insolation and Glacial Meltwater Influence on Sea‐Ice and Circulation Variability in the Northeastern Labrador Sea During the Last Glacial Period. Paleoceanography and Paleoclimatology, 34(11), 1689-1709 ... |
format |
Article in Journal/Newspaper |
author |
Griem, Lisa Voelker, Antje H L Berben, Sarah M P Dokken, Trond Jansen, Eystein |
author_facet |
Griem, Lisa Voelker, Antje H L Berben, Sarah M P Dokken, Trond Jansen, Eystein |
author_sort |
Griem, Lisa |
title |
Planktic foraminifers, ice-rafted debris and stable isotopes from three sediment cores along the East/South Greenland margin ... |
title_short |
Planktic foraminifers, ice-rafted debris and stable isotopes from three sediment cores along the East/South Greenland margin ... |
title_full |
Planktic foraminifers, ice-rafted debris and stable isotopes from three sediment cores along the East/South Greenland margin ... |
title_fullStr |
Planktic foraminifers, ice-rafted debris and stable isotopes from three sediment cores along the East/South Greenland margin ... |
title_full_unstemmed |
Planktic foraminifers, ice-rafted debris and stable isotopes from three sediment cores along the East/South Greenland margin ... |
title_sort |
planktic foraminifers, ice-rafted debris and stable isotopes from three sediment cores along the east/south greenland margin ... |
publisher |
PANGAEA |
publishDate |
2019 |
url |
https://dx.doi.org/10.1594/pangaea.904065 https://doi.pangaea.de/10.1594/PANGAEA.904065 |
genre |
Arctic Greenland Ice Sheet Labrador Sea Sea ice |
genre_facet |
Arctic Greenland Ice Sheet Labrador Sea Sea ice |
op_relation |
https://dx.doi.org/10.1029/2019pa003605 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.90406510.1029/2019pa003605 |
_version_ |
1797578675328122880 |