Stable isotope ratios of foraminifera in sediment core PS1458-2 from Maud Rise, Southern Ocean ...

Foraminifera picked, cleaned and isotope measurements carried out on the 315-400µm size fraction (unless otherwise mentioned, *e.g. 2+3 means 2 sinistral and 3 dextral tests) by Kyaw Winn in 1986/87 with the CARBO KIEL.Massenspectrometer Finnigan MAT 251, Christian-Albrechts-University, Kiel.61 sing...

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Bibliographic Details
Main Author: Winn, Kyaw
Format: Dataset
Language:English
Published: PANGAEA 2014
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.834971
https://doi.pangaea.de/10.1594/PANGAEA.834971
id ftdatacite:10.1594/pangaea.834971
record_format openpolar
spelling ftdatacite:10.1594/pangaea.834971 2024-09-15T18:19:24+00:00 Stable isotope ratios of foraminifera in sediment core PS1458-2 from Maud Rise, Southern Ocean ... Winn, Kyaw 2014 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.834971 https://doi.pangaea.de/10.1594/PANGAEA.834971 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Number of tests Neogloboquadrina pachyderma sinistral, δ18O Neogloboquadrina pachyderma sinistral, δ13C Sample comment Cibicidoides wuellerstorfi, δ18O Cibicidoides wuellerstorfi, δ13C Gravity corer Kiel type Isotope ratio mass spectrometry ANT-IV/4 Polarstern Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG Dataset dataset 2014 ftdatacite https://doi.org/10.1594/pangaea.834971 2024-07-03T13:11:36Z Foraminifera picked, cleaned and isotope measurements carried out on the 315-400µm size fraction (unless otherwise mentioned, *e.g. 2+3 means 2 sinistral and 3 dextral tests) by Kyaw Winn in 1986/87 with the CARBO KIEL.Massenspectrometer Finnigan MAT 251, Christian-Albrechts-University, Kiel.61 single specimen measurements not listed because of high (>0.12) sigma values.MIS stratigraphy is not possible, even with detailed sampling, because of the very low sedimentation rate and hiatuses in the sedimentary sequence. The Brunhes-Matuyama is just under 1.6m. Each sample represents a time span of 2-3 ka. Nevertheless, the carbon isotope ratios gave a good record of the nutrient history of the Southern Sea. ... Dataset Neogloboquadrina pachyderma Southern Ocean DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic DEPTH, sediment/rock
Number of tests
Neogloboquadrina pachyderma sinistral, δ18O
Neogloboquadrina pachyderma sinistral, δ13C
Sample comment
Cibicidoides wuellerstorfi, δ18O
Cibicidoides wuellerstorfi, δ13C
Gravity corer Kiel type
Isotope ratio mass spectrometry
ANT-IV/4
Polarstern
Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG
spellingShingle DEPTH, sediment/rock
Number of tests
Neogloboquadrina pachyderma sinistral, δ18O
Neogloboquadrina pachyderma sinistral, δ13C
Sample comment
Cibicidoides wuellerstorfi, δ18O
Cibicidoides wuellerstorfi, δ13C
Gravity corer Kiel type
Isotope ratio mass spectrometry
ANT-IV/4
Polarstern
Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG
Winn, Kyaw
Stable isotope ratios of foraminifera in sediment core PS1458-2 from Maud Rise, Southern Ocean ...
topic_facet DEPTH, sediment/rock
Number of tests
Neogloboquadrina pachyderma sinistral, δ18O
Neogloboquadrina pachyderma sinistral, δ13C
Sample comment
Cibicidoides wuellerstorfi, δ18O
Cibicidoides wuellerstorfi, δ13C
Gravity corer Kiel type
Isotope ratio mass spectrometry
ANT-IV/4
Polarstern
Institute for Geosciences, Christian Albrechts University, Kiel GIK/IfG
description Foraminifera picked, cleaned and isotope measurements carried out on the 315-400µm size fraction (unless otherwise mentioned, *e.g. 2+3 means 2 sinistral and 3 dextral tests) by Kyaw Winn in 1986/87 with the CARBO KIEL.Massenspectrometer Finnigan MAT 251, Christian-Albrechts-University, Kiel.61 single specimen measurements not listed because of high (>0.12) sigma values.MIS stratigraphy is not possible, even with detailed sampling, because of the very low sedimentation rate and hiatuses in the sedimentary sequence. The Brunhes-Matuyama is just under 1.6m. Each sample represents a time span of 2-3 ka. Nevertheless, the carbon isotope ratios gave a good record of the nutrient history of the Southern Sea. ...
format Dataset
author Winn, Kyaw
author_facet Winn, Kyaw
author_sort Winn, Kyaw
title Stable isotope ratios of foraminifera in sediment core PS1458-2 from Maud Rise, Southern Ocean ...
title_short Stable isotope ratios of foraminifera in sediment core PS1458-2 from Maud Rise, Southern Ocean ...
title_full Stable isotope ratios of foraminifera in sediment core PS1458-2 from Maud Rise, Southern Ocean ...
title_fullStr Stable isotope ratios of foraminifera in sediment core PS1458-2 from Maud Rise, Southern Ocean ...
title_full_unstemmed Stable isotope ratios of foraminifera in sediment core PS1458-2 from Maud Rise, Southern Ocean ...
title_sort stable isotope ratios of foraminifera in sediment core ps1458-2 from maud rise, southern ocean ...
publisher PANGAEA
publishDate 2014
url https://dx.doi.org/10.1594/pangaea.834971
https://doi.pangaea.de/10.1594/PANGAEA.834971
genre Neogloboquadrina pachyderma
Southern Ocean
genre_facet Neogloboquadrina pachyderma
Southern Ocean
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.834971
_version_ 1810457645094535168