Relative abundance and opal input of radiolarians measured on sediment core PS1768-8 and PS2498-1 ...

We present a new proxy, the oxygen isotope measurements (d18O) of radiolarian opal from sediment cores in the Subantarctic Zone (SAZ) and Permanent Open Ocean Zone (POOZ) of the Atlantic Southern Ocean. The SAZ core records of radiolarian and foraminiferal d18O are well correlated. In the POOZ core,...

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Bibliographic Details
Main Author: Abelmann, Andrea
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2009
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.719184
https://doi.pangaea.de/10.1594/PANGAEA.719184
id ftdatacite:10.1594/pangaea.719184
record_format openpolar
spelling ftdatacite:10.1594/pangaea.719184 2024-03-31T07:55:18+00:00 Relative abundance and opal input of radiolarians measured on sediment core PS1768-8 and PS2498-1 ... Abelmann, Andrea 2009 application/zip https://dx.doi.org/10.1594/pangaea.719184 https://doi.pangaea.de/10.1594/PANGAEA.719184 en eng PANGAEA https://dx.doi.org/10.1016/j.dsr.2008.12.019 Data access is restricted (moratorium, sensitive data, license constraints) Licensing unknown: Please contact principal investigator/authors to gain access and request licensing terms unknown Gravity corer Kiel type ANT-VIII/3 ANT-XI/2 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Publication Series of Datasets Collection 2009 ftdatacite https://doi.org/10.1594/pangaea.71918410.1016/j.dsr.2008.12.019 2024-03-04T13:35:39Z We present a new proxy, the oxygen isotope measurements (d18O) of radiolarian opal from sediment cores in the Subantarctic Zone (SAZ) and Permanent Open Ocean Zone (POOZ) of the Atlantic Southern Ocean. The SAZ core records of radiolarian and foraminiferal d18O are well correlated. In the POOZ core, only radiolarian 18O shifts to distinctly lower values during the glacial (when this core was in the Sea Ice Zone (SIZ)), while relevant foraminiferal and diatomaceous d18O records exhibit no such shift. This suggests a seasonal salinity change derived from the melting of snow accumulated on sea ice. We propose that a northward relocation of the Southern Ocean zonal system and enhanced water-vapor transport from lower latitudes forced the development of a stratified sea-surface in the northern SIZ during late glacial spring time. This raises unexpected aspects for numerical modeling of past atmospheric coupling and moisture transport, as well as on glacial Southern Ocean stratification and its implication for ... : Data submitted 2009-06-11; set to protected on request of first author (2014-08-13, PDI-8220). ... Article in Journal/Newspaper Sea ice Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Southern Ocean
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Gravity corer Kiel type
ANT-VIII/3
ANT-XI/2
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
spellingShingle Gravity corer Kiel type
ANT-VIII/3
ANT-XI/2
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Abelmann, Andrea
Relative abundance and opal input of radiolarians measured on sediment core PS1768-8 and PS2498-1 ...
topic_facet Gravity corer Kiel type
ANT-VIII/3
ANT-XI/2
Polarstern
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
description We present a new proxy, the oxygen isotope measurements (d18O) of radiolarian opal from sediment cores in the Subantarctic Zone (SAZ) and Permanent Open Ocean Zone (POOZ) of the Atlantic Southern Ocean. The SAZ core records of radiolarian and foraminiferal d18O are well correlated. In the POOZ core, only radiolarian 18O shifts to distinctly lower values during the glacial (when this core was in the Sea Ice Zone (SIZ)), while relevant foraminiferal and diatomaceous d18O records exhibit no such shift. This suggests a seasonal salinity change derived from the melting of snow accumulated on sea ice. We propose that a northward relocation of the Southern Ocean zonal system and enhanced water-vapor transport from lower latitudes forced the development of a stratified sea-surface in the northern SIZ during late glacial spring time. This raises unexpected aspects for numerical modeling of past atmospheric coupling and moisture transport, as well as on glacial Southern Ocean stratification and its implication for ... : Data submitted 2009-06-11; set to protected on request of first author (2014-08-13, PDI-8220). ...
format Article in Journal/Newspaper
author Abelmann, Andrea
author_facet Abelmann, Andrea
author_sort Abelmann, Andrea
title Relative abundance and opal input of radiolarians measured on sediment core PS1768-8 and PS2498-1 ...
title_short Relative abundance and opal input of radiolarians measured on sediment core PS1768-8 and PS2498-1 ...
title_full Relative abundance and opal input of radiolarians measured on sediment core PS1768-8 and PS2498-1 ...
title_fullStr Relative abundance and opal input of radiolarians measured on sediment core PS1768-8 and PS2498-1 ...
title_full_unstemmed Relative abundance and opal input of radiolarians measured on sediment core PS1768-8 and PS2498-1 ...
title_sort relative abundance and opal input of radiolarians measured on sediment core ps1768-8 and ps2498-1 ...
publisher PANGAEA
publishDate 2009
url https://dx.doi.org/10.1594/pangaea.719184
https://doi.pangaea.de/10.1594/PANGAEA.719184
geographic Southern Ocean
geographic_facet Southern Ocean
genre Sea ice
Southern Ocean
genre_facet Sea ice
Southern Ocean
op_relation https://dx.doi.org/10.1016/j.dsr.2008.12.019
op_rights Data access is restricted (moratorium, sensitive data, license constraints)
Licensing unknown: Please contact principal investigator/authors to gain access and request licensing terms
unknown
op_doi https://doi.org/10.1594/pangaea.71918410.1016/j.dsr.2008.12.019
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