Geochemical biomarker analyses on sediment cores PS51/154-11 and PS51/159-10 from the western Laptev Sea (Arctic Ocean) ...

Multi-proxy biomarker measurements were applied on two sediment cores (PS51/154, PS51/159) to reconstruct sea ice cover (IP25), biological production (brassicasterol, dinosterol) and river run-off (campesterol, beta-sitosterol) in the western Laptev Sea over the last ~17 ka with unprecedented tempor...

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Main Authors: Hörner, Tanja, Stein, Ruediger, Fahl, Kirsten, Birgel, Daniel
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2016
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.854067
https://doi.pangaea.de/10.1594/PANGAEA.854067
id ftdatacite:10.1594/pangaea.854067
record_format openpolar
spelling ftdatacite:10.1594/pangaea.854067 2024-09-15T17:53:27+00:00 Geochemical biomarker analyses on sediment cores PS51/154-11 and PS51/159-10 from the western Laptev Sea (Arctic Ocean) ... Hörner, Tanja Stein, Ruediger Fahl, Kirsten Birgel, Daniel 2016 application/zip https://dx.doi.org/10.1594/pangaea.854067 https://doi.pangaea.de/10.1594/PANGAEA.854067 en eng PANGAEA https://dx.doi.org/10.1016/j.quascirev.2016.04.011 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 2016 ftdatacite https://doi.org/10.1594/pangaea.85406710.1016/j.quascirev.2016.04.011 2024-08-01T11:01:17Z Multi-proxy biomarker measurements were applied on two sediment cores (PS51/154, PS51/159) to reconstruct sea ice cover (IP25), biological production (brassicasterol, dinosterol) and river run-off (campesterol, beta-sitosterol) in the western Laptev Sea over the last ~17 ka with unprecedented temporal resolution. The absence of IP25 from 17.2 to 15.5 ka, in combination with minimum concentration of phytoplankton biomarkers, suggests that the western Laptev Sea shelf was mostly covered with permanent sea ice. Very minor river run-off and restricted biological production occurred during this cold interval. From ~16 ka until 7.5 ka, a long-term decrease of terrigenous (riverine) organic matter and a coeval increase of marine organic matter reflect the gradual establishment of fully marine conditions in the western Laptev Sea, caused by the onset of the post-glacial transgression. Intensified river run-off and reduced sea ice cover characterized the time interval between 15.2 and 12.9 ka, including the ... : Supplement to: Hörner, Tanja; Stein, Ruediger; Fahl, Kirsten; Birgel, Daniel (2016): Post-glacial variability of sea ice cover, river run-off and biological production in the western Laptev Sea (Arctic Ocean) – A high-resolution biomarker study. Quaternary Science Reviews, 143, 133-149 ... Article in Journal/Newspaper Arctic Ocean laptev Laptev Sea Phytoplankton Sea ice DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Hörner, Tanja
Stein, Ruediger
Fahl, Kirsten
Birgel, Daniel
Geochemical biomarker analyses on sediment cores PS51/154-11 and PS51/159-10 from the western Laptev Sea (Arctic Ocean) ...
topic_facet Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description Multi-proxy biomarker measurements were applied on two sediment cores (PS51/154, PS51/159) to reconstruct sea ice cover (IP25), biological production (brassicasterol, dinosterol) and river run-off (campesterol, beta-sitosterol) in the western Laptev Sea over the last ~17 ka with unprecedented temporal resolution. The absence of IP25 from 17.2 to 15.5 ka, in combination with minimum concentration of phytoplankton biomarkers, suggests that the western Laptev Sea shelf was mostly covered with permanent sea ice. Very minor river run-off and restricted biological production occurred during this cold interval. From ~16 ka until 7.5 ka, a long-term decrease of terrigenous (riverine) organic matter and a coeval increase of marine organic matter reflect the gradual establishment of fully marine conditions in the western Laptev Sea, caused by the onset of the post-glacial transgression. Intensified river run-off and reduced sea ice cover characterized the time interval between 15.2 and 12.9 ka, including the ... : Supplement to: Hörner, Tanja; Stein, Ruediger; Fahl, Kirsten; Birgel, Daniel (2016): Post-glacial variability of sea ice cover, river run-off and biological production in the western Laptev Sea (Arctic Ocean) – A high-resolution biomarker study. Quaternary Science Reviews, 143, 133-149 ...
format Article in Journal/Newspaper
author Hörner, Tanja
Stein, Ruediger
Fahl, Kirsten
Birgel, Daniel
author_facet Hörner, Tanja
Stein, Ruediger
Fahl, Kirsten
Birgel, Daniel
author_sort Hörner, Tanja
title Geochemical biomarker analyses on sediment cores PS51/154-11 and PS51/159-10 from the western Laptev Sea (Arctic Ocean) ...
title_short Geochemical biomarker analyses on sediment cores PS51/154-11 and PS51/159-10 from the western Laptev Sea (Arctic Ocean) ...
title_full Geochemical biomarker analyses on sediment cores PS51/154-11 and PS51/159-10 from the western Laptev Sea (Arctic Ocean) ...
title_fullStr Geochemical biomarker analyses on sediment cores PS51/154-11 and PS51/159-10 from the western Laptev Sea (Arctic Ocean) ...
title_full_unstemmed Geochemical biomarker analyses on sediment cores PS51/154-11 and PS51/159-10 from the western Laptev Sea (Arctic Ocean) ...
title_sort geochemical biomarker analyses on sediment cores ps51/154-11 and ps51/159-10 from the western laptev sea (arctic ocean) ...
publisher PANGAEA
publishDate 2016
url https://dx.doi.org/10.1594/pangaea.854067
https://doi.pangaea.de/10.1594/PANGAEA.854067
genre Arctic Ocean
laptev
Laptev Sea
Phytoplankton
Sea ice
genre_facet Arctic Ocean
laptev
Laptev Sea
Phytoplankton
Sea ice
op_relation https://dx.doi.org/10.1016/j.quascirev.2016.04.011
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.85406710.1016/j.quascirev.2016.04.011
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