Age determinations, biomarker analyses, and accumulation rates of three sediment cores from the Fram Strait ...
A reconstruction of Holocene sea ice conditions in the Fram Strait provides insight into the palaeoenvironmental and palaeoceanographic development of this climate sensitive area during the past 8,500 years BP. Organic geochemical analyses of sediment cores from eastern and western Fram Strait enabl...
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ftdatacite:10.1594/pangaea.779628 2024-09-15T18:04:20+00:00 Age determinations, biomarker analyses, and accumulation rates of three sediment cores from the Fram Strait ... Müller, Juliane Werner, Kirstin Stein, Ruediger Fahl, Kirsten Moros, Matthias Jansen, Eystein 2012 application/zip https://dx.doi.org/10.1594/pangaea.779628 https://doi.pangaea.de/10.1594/PANGAEA.779628 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2012.04.024 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Kasten corer Gravity corer Kiel type MSM05/5 ARK-X/2 Maria S. Merian Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 2012 ftdatacite https://doi.org/10.1594/pangaea.77962810.1016/j.quascirev.2012.04.024 2024-07-03T13:10:33Z A reconstruction of Holocene sea ice conditions in the Fram Strait provides insight into the palaeoenvironmental and palaeoceanographic development of this climate sensitive area during the past 8,500 years BP. Organic geochemical analyses of sediment cores from eastern and western Fram Strait enable the identification of variations in the ice coverage that can be linked to changes in the oceanic (and atmospheric) circulation system. By means of the sea ice proxy IP25, phytoplankton derived biomarkers and ice rafted detritus (IRD) increasing sea ice occurrences are traced along the western continental margin of Spitsbergen throughout the Holocene, which supports previous palaeoenvironmental reconstructions that document a general cooling. A further significant ice advance during the Neoglacial is accompanied by distinct sea ice fluctuations, which point to short-term perturbations in either the Atlantic Water advection or Arctic Water outflow at this site. At the continental shelf of East Greenland, the ... : Supplement to: Müller, Juliane; Werner, Kirstin; Stein, Ruediger; Fahl, Kirsten; Moros, Matthias; Jansen, Eystein (2012): Holocene cooling culminates in sea ice oscillations in Fram Strait. Quaternary Science Reviews, 47, 1-14 ... Article in Journal/Newspaper East Greenland Fram Strait Greenland Phytoplankton Sea ice Spitsbergen DataCite |
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language |
English |
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Kasten corer Gravity corer Kiel type MSM05/5 ARK-X/2 Maria S. Merian Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo |
spellingShingle |
Kasten corer Gravity corer Kiel type MSM05/5 ARK-X/2 Maria S. Merian Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Müller, Juliane Werner, Kirstin Stein, Ruediger Fahl, Kirsten Moros, Matthias Jansen, Eystein Age determinations, biomarker analyses, and accumulation rates of three sediment cores from the Fram Strait ... |
topic_facet |
Kasten corer Gravity corer Kiel type MSM05/5 ARK-X/2 Maria S. Merian Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo |
description |
A reconstruction of Holocene sea ice conditions in the Fram Strait provides insight into the palaeoenvironmental and palaeoceanographic development of this climate sensitive area during the past 8,500 years BP. Organic geochemical analyses of sediment cores from eastern and western Fram Strait enable the identification of variations in the ice coverage that can be linked to changes in the oceanic (and atmospheric) circulation system. By means of the sea ice proxy IP25, phytoplankton derived biomarkers and ice rafted detritus (IRD) increasing sea ice occurrences are traced along the western continental margin of Spitsbergen throughout the Holocene, which supports previous palaeoenvironmental reconstructions that document a general cooling. A further significant ice advance during the Neoglacial is accompanied by distinct sea ice fluctuations, which point to short-term perturbations in either the Atlantic Water advection or Arctic Water outflow at this site. At the continental shelf of East Greenland, the ... : Supplement to: Müller, Juliane; Werner, Kirstin; Stein, Ruediger; Fahl, Kirsten; Moros, Matthias; Jansen, Eystein (2012): Holocene cooling culminates in sea ice oscillations in Fram Strait. Quaternary Science Reviews, 47, 1-14 ... |
format |
Article in Journal/Newspaper |
author |
Müller, Juliane Werner, Kirstin Stein, Ruediger Fahl, Kirsten Moros, Matthias Jansen, Eystein |
author_facet |
Müller, Juliane Werner, Kirstin Stein, Ruediger Fahl, Kirsten Moros, Matthias Jansen, Eystein |
author_sort |
Müller, Juliane |
title |
Age determinations, biomarker analyses, and accumulation rates of three sediment cores from the Fram Strait ... |
title_short |
Age determinations, biomarker analyses, and accumulation rates of three sediment cores from the Fram Strait ... |
title_full |
Age determinations, biomarker analyses, and accumulation rates of three sediment cores from the Fram Strait ... |
title_fullStr |
Age determinations, biomarker analyses, and accumulation rates of three sediment cores from the Fram Strait ... |
title_full_unstemmed |
Age determinations, biomarker analyses, and accumulation rates of three sediment cores from the Fram Strait ... |
title_sort |
age determinations, biomarker analyses, and accumulation rates of three sediment cores from the fram strait ... |
publisher |
PANGAEA |
publishDate |
2012 |
url |
https://dx.doi.org/10.1594/pangaea.779628 https://doi.pangaea.de/10.1594/PANGAEA.779628 |
genre |
East Greenland Fram Strait Greenland Phytoplankton Sea ice Spitsbergen |
genre_facet |
East Greenland Fram Strait Greenland Phytoplankton Sea ice Spitsbergen |
op_relation |
https://dx.doi.org/10.1016/j.quascirev.2012.04.024 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.77962810.1016/j.quascirev.2012.04.024 |
_version_ |
1810441823818088448 |