Late Quaternary sea-ice history of northern Fram Strait/Arctic Ocean
One of the main characteristics of the Arctic Ocean is its seasonal to perennial sea-ice cover. Variations of sea-ice conditions affect the Earth’s albedo, primary production, rate of deep-water etc. During the last decades, a drastic decrease in sea ice has been recorded, and the causes of which, i...
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ftawi:oai:epic.awi.de:44280 2024-09-15T17:35:56+00:00 Late Quaternary sea-ice history of northern Fram Strait/Arctic Ocean Kremer, Anne Stein, Rüdiger Fahl, Kirsten Matthiessen, Jens Forwick, Matthias O'Regan, Matt 2016 application/pdf https://epic.awi.de/id/eprint/44280/ https://epic.awi.de/id/eprint/44280/1/EGU2016-6838.pdf https://hdl.handle.net/10013/epic.50616 https://hdl.handle.net/10013/epic.50616.d001 unknown https://epic.awi.de/id/eprint/44280/1/EGU2016-6838.pdf https://hdl.handle.net/10013/epic.50616.d001 Kremer, A. , Stein, R. orcid:0000-0002-4453-9564 , Fahl, K. orcid:0000-0001-9317-4656 , Matthiessen, J. orcid:0000-0002-6952-2494 , Forwick, M. and O'Regan, M. (2016) Late Quaternary sea-ice history of northern Fram Strait/Arctic Ocean , EGU General Assembly, 17 April 2016 - 22 April 2016 . hdl:10013/epic.50616 EPIC3EGU General Assembly, 2016-04-17-2016-04-22 Conference notRev 2016 ftawi 2024-06-24T04:17:43Z One of the main characteristics of the Arctic Ocean is its seasonal to perennial sea-ice cover. Variations of sea-ice conditions affect the Earth’s albedo, primary production, rate of deep-water etc. During the last decades, a drastic decrease in sea ice has been recorded, and the causes of which, i.e. natural vs. anthropogenic forcings, and their relevance within the global climate system, are subject of intense scientific and societal debate. In this context, records of past sea-ice conditions going beyond instrumental records are of major significance. These records may help to better understand the processes controlling natural sea-ice variability and to improve models for forecasts of future climatic conditions. During RV Polarstern Cruise PS92 in summer 2015, a 860 cm long sediment core (PS92/039-2) was re- covered from the eastern flank of Yermak Plateau north of the Svalbard archipelago (Peeken, 2015). Based on a preliminary age model, this sediment core probably represents the time interval from MIS 6 to MIS 1. This core, located close to the modern summer ice edge, has been selected for reconstruction of past Arctic sea-ice variability based on specific biomarkers. In this context, we have determined the ice-algae-derived sea-ice proxy IP25 (Belt et al., 2007), in combination with other biomarkers indicative for open-water conditions (cf., Müller et al., 2009, 2011). Furthermore, organic carbon fluxes were differentiated using specific biomarkers indicative for marine primary production (brassicasterol, dinosterol) and terrigenous input (campesterol, β-sitosterol). In this poster, preliminary results of our organic-geochemical and sedimentological investigations are presented. Distinct fluctuations of these biomarkers indicate several major, partly abrupt changes in sea-ice cover in the Yermak Plateau area during the late Quaternary. These changes are probably linked to changes in the inflow of Atlantic Water along the western coastline of Svalbard into the Arctic Ocean. Furthermore, the repetitive ... Conference Object albedo Arctic Arctic Ocean Fram Strait ice algae Sea ice Svalbard Yermak plateau Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
institution |
Open Polar |
collection |
Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
description |
One of the main characteristics of the Arctic Ocean is its seasonal to perennial sea-ice cover. Variations of sea-ice conditions affect the Earth’s albedo, primary production, rate of deep-water etc. During the last decades, a drastic decrease in sea ice has been recorded, and the causes of which, i.e. natural vs. anthropogenic forcings, and their relevance within the global climate system, are subject of intense scientific and societal debate. In this context, records of past sea-ice conditions going beyond instrumental records are of major significance. These records may help to better understand the processes controlling natural sea-ice variability and to improve models for forecasts of future climatic conditions. During RV Polarstern Cruise PS92 in summer 2015, a 860 cm long sediment core (PS92/039-2) was re- covered from the eastern flank of Yermak Plateau north of the Svalbard archipelago (Peeken, 2015). Based on a preliminary age model, this sediment core probably represents the time interval from MIS 6 to MIS 1. This core, located close to the modern summer ice edge, has been selected for reconstruction of past Arctic sea-ice variability based on specific biomarkers. In this context, we have determined the ice-algae-derived sea-ice proxy IP25 (Belt et al., 2007), in combination with other biomarkers indicative for open-water conditions (cf., Müller et al., 2009, 2011). Furthermore, organic carbon fluxes were differentiated using specific biomarkers indicative for marine primary production (brassicasterol, dinosterol) and terrigenous input (campesterol, β-sitosterol). In this poster, preliminary results of our organic-geochemical and sedimentological investigations are presented. Distinct fluctuations of these biomarkers indicate several major, partly abrupt changes in sea-ice cover in the Yermak Plateau area during the late Quaternary. These changes are probably linked to changes in the inflow of Atlantic Water along the western coastline of Svalbard into the Arctic Ocean. Furthermore, the repetitive ... |
format |
Conference Object |
author |
Kremer, Anne Stein, Rüdiger Fahl, Kirsten Matthiessen, Jens Forwick, Matthias O'Regan, Matt |
spellingShingle |
Kremer, Anne Stein, Rüdiger Fahl, Kirsten Matthiessen, Jens Forwick, Matthias O'Regan, Matt Late Quaternary sea-ice history of northern Fram Strait/Arctic Ocean |
author_facet |
Kremer, Anne Stein, Rüdiger Fahl, Kirsten Matthiessen, Jens Forwick, Matthias O'Regan, Matt |
author_sort |
Kremer, Anne |
title |
Late Quaternary sea-ice history of northern Fram Strait/Arctic Ocean |
title_short |
Late Quaternary sea-ice history of northern Fram Strait/Arctic Ocean |
title_full |
Late Quaternary sea-ice history of northern Fram Strait/Arctic Ocean |
title_fullStr |
Late Quaternary sea-ice history of northern Fram Strait/Arctic Ocean |
title_full_unstemmed |
Late Quaternary sea-ice history of northern Fram Strait/Arctic Ocean |
title_sort |
late quaternary sea-ice history of northern fram strait/arctic ocean |
publishDate |
2016 |
url |
https://epic.awi.de/id/eprint/44280/ https://epic.awi.de/id/eprint/44280/1/EGU2016-6838.pdf https://hdl.handle.net/10013/epic.50616 https://hdl.handle.net/10013/epic.50616.d001 |
genre |
albedo Arctic Arctic Ocean Fram Strait ice algae Sea ice Svalbard Yermak plateau |
genre_facet |
albedo Arctic Arctic Ocean Fram Strait ice algae Sea ice Svalbard Yermak plateau |
op_source |
EPIC3EGU General Assembly, 2016-04-17-2016-04-22 |
op_relation |
https://epic.awi.de/id/eprint/44280/1/EGU2016-6838.pdf https://hdl.handle.net/10013/epic.50616.d001 Kremer, A. , Stein, R. orcid:0000-0002-4453-9564 , Fahl, K. orcid:0000-0001-9317-4656 , Matthiessen, J. orcid:0000-0002-6952-2494 , Forwick, M. and O'Regan, M. (2016) Late Quaternary sea-ice history of northern Fram Strait/Arctic Ocean , EGU General Assembly, 17 April 2016 - 22 April 2016 . hdl:10013/epic.50616 |
_version_ |
1810486035127205888 |