Palaeo Sea Ice and Climate Dynamics: Biomarker-based sea ice reconstructions

Sea ice is a key component of the climate system as it exerts a strong control on the heat and gas exchange between the ocean and the atmosphere and the formation of dense deepwater driving thermohaline circulation processes. Changes in sea ice cover are also considered to affect the calving rate of...

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Main Authors: Müller, Juliane, Vorrath, Maria-Elena, Esper, Oliver, Kuhn, Gerhard
Format: Conference Object
Language:unknown
Published: 2017
Subjects:
Online Access:https://epic.awi.de/id/eprint/45763/
https://hdl.handle.net/10013/epic.51899
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spelling ftawi:oai:epic.awi.de:45763 2024-09-15T17:39:10+00:00 Palaeo Sea Ice and Climate Dynamics: Biomarker-based sea ice reconstructions Müller, Juliane Vorrath, Maria-Elena Esper, Oliver Kuhn, Gerhard 2017-09 https://epic.awi.de/id/eprint/45763/ https://hdl.handle.net/10013/epic.51899 unknown Müller, J. orcid:0000-0003-0724-4131 , Vorrath, M. E. orcid:0000-0001-7208-1186 , Esper, O. orcid:0000-0002-4342-3471 and Kuhn, G. orcid:0000-0001-6069-7485 (2017) Palaeo Sea Ice and Climate Dynamics: Biomarker-based sea ice reconstructions , Past Antarctic Ice Sheet Dynamics (PAIS) Conference, Trieste, 10 September 2017 - 15 September 2017 . hdl:10013/epic.51899 EPIC3Past Antarctic Ice Sheet Dynamics (PAIS) Conference, Trieste, 2017-09-10-2017-09-15 Conference notRev 2017 ftawi 2024-06-24T04:18:50Z Sea ice is a key component of the climate system as it exerts a strong control on the heat and gas exchange between the ocean and the atmosphere and the formation of dense deepwater driving thermohaline circulation processes. Changes in sea ice cover are also considered to affect the calving rate of icebergs at marine-terminating glaciers. So far, sea ice reconstructions in the Southern Ocean are mainly based on diatom assemblage studies and specific transfer functions permitting even quantitative estimates of sea ice concentrations. The sea ice biomarker IPSO25, a highly branched isoprenoid akin to the well-established Arctic sea ice proxy IP25, offers an additional method for the reconstruction of past sea ice conditions in the Southern Ocean. This may be particularly valuable in areas (or time intervals) where the preservation of diatoms is limited due to silica dissolution. Here we present first results of the new Helmholtz Young Investigator Group PALICE, settled at the Alfred Wegener Institute in Bremerhaven and the University of Bremen. Main objectives of the group are the assessment of past sea ice-ocean-atmosphere (and ice-sheet) interactions and the further evaluation and application of highly branched isoprenoids (including IPSO25) for robust sea ice reconstructions across different time scales. Specifically, direct comparisons between biomarker and diatom data may provide for an evaluation of both approaches. Current focus is on recently collected surface sediments and long cores from the Bransfield Strait, the southern Drake Passage (PS97) and the Amundsen Sea (PS104) as well as on upcoming expeditions in the Weddell Sea (PS111) and the Ross Sea (IODP 374). Conference Object Amundsen Sea Bransfield Strait Drake Passage Ice Sheet Iceberg* Ross Sea Sea ice Southern Ocean Weddell Sea 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 Sea ice is a key component of the climate system as it exerts a strong control on the heat and gas exchange between the ocean and the atmosphere and the formation of dense deepwater driving thermohaline circulation processes. Changes in sea ice cover are also considered to affect the calving rate of icebergs at marine-terminating glaciers. So far, sea ice reconstructions in the Southern Ocean are mainly based on diatom assemblage studies and specific transfer functions permitting even quantitative estimates of sea ice concentrations. The sea ice biomarker IPSO25, a highly branched isoprenoid akin to the well-established Arctic sea ice proxy IP25, offers an additional method for the reconstruction of past sea ice conditions in the Southern Ocean. This may be particularly valuable in areas (or time intervals) where the preservation of diatoms is limited due to silica dissolution. Here we present first results of the new Helmholtz Young Investigator Group PALICE, settled at the Alfred Wegener Institute in Bremerhaven and the University of Bremen. Main objectives of the group are the assessment of past sea ice-ocean-atmosphere (and ice-sheet) interactions and the further evaluation and application of highly branched isoprenoids (including IPSO25) for robust sea ice reconstructions across different time scales. Specifically, direct comparisons between biomarker and diatom data may provide for an evaluation of both approaches. Current focus is on recently collected surface sediments and long cores from the Bransfield Strait, the southern Drake Passage (PS97) and the Amundsen Sea (PS104) as well as on upcoming expeditions in the Weddell Sea (PS111) and the Ross Sea (IODP 374).
format Conference Object
author Müller, Juliane
Vorrath, Maria-Elena
Esper, Oliver
Kuhn, Gerhard
spellingShingle Müller, Juliane
Vorrath, Maria-Elena
Esper, Oliver
Kuhn, Gerhard
Palaeo Sea Ice and Climate Dynamics: Biomarker-based sea ice reconstructions
author_facet Müller, Juliane
Vorrath, Maria-Elena
Esper, Oliver
Kuhn, Gerhard
author_sort Müller, Juliane
title Palaeo Sea Ice and Climate Dynamics: Biomarker-based sea ice reconstructions
title_short Palaeo Sea Ice and Climate Dynamics: Biomarker-based sea ice reconstructions
title_full Palaeo Sea Ice and Climate Dynamics: Biomarker-based sea ice reconstructions
title_fullStr Palaeo Sea Ice and Climate Dynamics: Biomarker-based sea ice reconstructions
title_full_unstemmed Palaeo Sea Ice and Climate Dynamics: Biomarker-based sea ice reconstructions
title_sort palaeo sea ice and climate dynamics: biomarker-based sea ice reconstructions
publishDate 2017
url https://epic.awi.de/id/eprint/45763/
https://hdl.handle.net/10013/epic.51899
genre Amundsen Sea
Bransfield Strait
Drake Passage
Ice Sheet
Iceberg*
Ross Sea
Sea ice
Southern Ocean
Weddell Sea
genre_facet Amundsen Sea
Bransfield Strait
Drake Passage
Ice Sheet
Iceberg*
Ross Sea
Sea ice
Southern Ocean
Weddell Sea
op_source EPIC3Past Antarctic Ice Sheet Dynamics (PAIS) Conference, Trieste, 2017-09-10-2017-09-15
op_relation Müller, J. orcid:0000-0003-0724-4131 , Vorrath, M. E. orcid:0000-0001-7208-1186 , Esper, O. orcid:0000-0002-4342-3471 and Kuhn, G. orcid:0000-0001-6069-7485 (2017) Palaeo Sea Ice and Climate Dynamics: Biomarker-based sea ice reconstructions , Past Antarctic Ice Sheet Dynamics (PAIS) Conference, Trieste, 10 September 2017 - 15 September 2017 . hdl:10013/epic.51899
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