Reconstruction of paleo sea ice and climate dynamics based on highly branched isoprenoids at the Western Antartic Peninsula

In context of rapid environmental change, the investigation of vulnerable parts of the global climate system is the focus of recent research. The assessment of global interactions between a changing climate and Antarctic sea ice, especially at the rapidly warming Western Antarctic Peninsula (WAP), a...

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Bibliographic Details
Main Author: Vorrath, Maria-Elena
Format: Thesis
Language:English
Published: Universität Bremen 2020
Subjects:
550
Online Access:https://dx.doi.org/10.26092/elib/197
https://media.suub.uni-bremen.de/handle/elib/4412
id ftdatacite:10.26092/elib/197
record_format openpolar
spelling ftdatacite:10.26092/elib/197 2023-05-15T13:56:27+02:00 Reconstruction of paleo sea ice and climate dynamics based on highly branched isoprenoids at the Western Antartic Peninsula Vorrath, Maria-Elena 2020 https://dx.doi.org/10.26092/elib/197 https://media.suub.uni-bremen.de/handle/elib/4412 en eng Universität Bremen Attribution 3.0 Germany http://creativecommons.org/licenses/by/3.0/de/ CC-BY Biomarker Sea ice Antarctica 550 Thesis Other Dissertation thesis 2020 ftdatacite https://doi.org/10.26092/elib/197 2021-11-05T12:55:41Z In context of rapid environmental change, the investigation of vulnerable parts of the global climate system is the focus of recent research. The assessment of global interactions between a changing climate and Antarctic sea ice, especially at the rapidly warming Western Antarctic Peninsula (WAP), aims to improve climate and ice sheet modelling for future projections. For this, the reconstruction of past sea ice distribution provides crucial information to enhance the capability of climate models. The goal of this thesis is the evaluation of the novel organic sea ice biomarker IPSO25 (ice proxy for the Southern Ocean with 25 carbon atoms) and its application as a new tool for past sea ice reconstructions analogously to its counterpart IP25 in the Arctic Ocean. This organic biomarker is a source specific organic compound from sea ice algae and associated with Antarctic spring sea ice. Information about the significance and limitations of this sea ice biomarker is still sparse and shall be revealed by using surface and downcore marine sediments. Comparisons to independent data such as biomarkers for open marine conditions, diatom assemblages, satellites data, ice core and marine sediment records improve the precise assessment of IPSO25. The distribution and evaluation of IPSO25 with recent sea ice data is the topic of the first study (Part I). The following two investigations (Part II and III) cover the last 200 a and 17 ka BP, respectively, based on three short and one long sediment records, and highlight the regional significance of IPSO25. This thesis provides new reference data for paleo sea ice studies and provides a first research approach in further application of IPSO25, PIPSO25 and paleo sea ice investigations in Antarctica and the Southern Ocean. Thesis Antarc* Antarctic Antarctic Peninsula Antarctica antartic* Arctic Arctic Ocean ice algae ice core Ice Sheet Sea ice Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Antarctic Antarctic Peninsula Arctic Arctic Ocean Southern Ocean
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Biomarker
Sea ice
Antarctica
550
spellingShingle Biomarker
Sea ice
Antarctica
550
Vorrath, Maria-Elena
Reconstruction of paleo sea ice and climate dynamics based on highly branched isoprenoids at the Western Antartic Peninsula
topic_facet Biomarker
Sea ice
Antarctica
550
description In context of rapid environmental change, the investigation of vulnerable parts of the global climate system is the focus of recent research. The assessment of global interactions between a changing climate and Antarctic sea ice, especially at the rapidly warming Western Antarctic Peninsula (WAP), aims to improve climate and ice sheet modelling for future projections. For this, the reconstruction of past sea ice distribution provides crucial information to enhance the capability of climate models. The goal of this thesis is the evaluation of the novel organic sea ice biomarker IPSO25 (ice proxy for the Southern Ocean with 25 carbon atoms) and its application as a new tool for past sea ice reconstructions analogously to its counterpart IP25 in the Arctic Ocean. This organic biomarker is a source specific organic compound from sea ice algae and associated with Antarctic spring sea ice. Information about the significance and limitations of this sea ice biomarker is still sparse and shall be revealed by using surface and downcore marine sediments. Comparisons to independent data such as biomarkers for open marine conditions, diatom assemblages, satellites data, ice core and marine sediment records improve the precise assessment of IPSO25. The distribution and evaluation of IPSO25 with recent sea ice data is the topic of the first study (Part I). The following two investigations (Part II and III) cover the last 200 a and 17 ka BP, respectively, based on three short and one long sediment records, and highlight the regional significance of IPSO25. This thesis provides new reference data for paleo sea ice studies and provides a first research approach in further application of IPSO25, PIPSO25 and paleo sea ice investigations in Antarctica and the Southern Ocean.
format Thesis
author Vorrath, Maria-Elena
author_facet Vorrath, Maria-Elena
author_sort Vorrath, Maria-Elena
title Reconstruction of paleo sea ice and climate dynamics based on highly branched isoprenoids at the Western Antartic Peninsula
title_short Reconstruction of paleo sea ice and climate dynamics based on highly branched isoprenoids at the Western Antartic Peninsula
title_full Reconstruction of paleo sea ice and climate dynamics based on highly branched isoprenoids at the Western Antartic Peninsula
title_fullStr Reconstruction of paleo sea ice and climate dynamics based on highly branched isoprenoids at the Western Antartic Peninsula
title_full_unstemmed Reconstruction of paleo sea ice and climate dynamics based on highly branched isoprenoids at the Western Antartic Peninsula
title_sort reconstruction of paleo sea ice and climate dynamics based on highly branched isoprenoids at the western antartic peninsula
publisher Universität Bremen
publishDate 2020
url https://dx.doi.org/10.26092/elib/197
https://media.suub.uni-bremen.de/handle/elib/4412
geographic Antarctic
Antarctic Peninsula
Arctic
Arctic Ocean
Southern Ocean
geographic_facet Antarctic
Antarctic Peninsula
Arctic
Arctic Ocean
Southern Ocean
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
antartic*
Arctic
Arctic Ocean
ice algae
ice core
Ice Sheet
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
antartic*
Arctic
Arctic Ocean
ice algae
ice core
Ice Sheet
Sea ice
Southern Ocean
op_rights Attribution 3.0 Germany
http://creativecommons.org/licenses/by/3.0/de/
op_rightsnorm CC-BY
op_doi https://doi.org/10.26092/elib/197
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