Deep-water temperatures from the Southern Ocean during HS4 ...

Foraminiferal magnesium to calcium ratios (Mg/Ca) are reported for two benthic species, drawn from down-core marine sediment samples obtained from the deep Southern Ocean. Samples of 4-10 individual benthic foraminifera, of the species Globobulimina affinis and/or Uvigerina sp., were oxidatively cle...

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Bibliographic Details
Main Author: Skinner, Luke C
Format: Dataset
Language:English
Published: PANGAEA 2020
Subjects:
AGE
Online Access:https://dx.doi.org/10.1594/pangaea.922135
https://doi.pangaea.de/10.1594/PANGAEA.922135
id ftdatacite:10.1594/pangaea.922135
record_format openpolar
spelling ftdatacite:10.1594/pangaea.922135 2024-03-31T07:55:25+00:00 Deep-water temperatures from the Southern Ocean during HS4 ... Skinner, Luke C 2020 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.922135 https://doi.pangaea.de/10.1594/PANGAEA.922135 en eng PANGAEA https://dx.doi.org/10.1038/s43247-020-00024-3 https://dx.doi.org/10.1594/pangaea.922136 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 deep convection deep-water temperature Mg/Ca Southern Ocean DEPTH, sediment/rock AGE Melonis affinis, Magnesium/Calcium ratio Uvigerina sp., Magnesium/Calcium ratio Deep water temperature Calypso Square Core System Inductively coupled plasma - mass spectrometry ICP-MS MD159 Marion Dufresne 1995 dataset Dataset 2020 ftdatacite https://doi.org/10.1594/pangaea.92213510.1038/s43247-020-00024-310.1594/pangaea.922136 2024-03-04T14:06:53Z Foraminiferal magnesium to calcium ratios (Mg/Ca) are reported for two benthic species, drawn from down-core marine sediment samples obtained from the deep Southern Ocean. Samples of 4-10 individual benthic foraminifera, of the species Globobulimina affinis and/or Uvigerina sp., were oxidatively cleaned according to a standard protocol, involving clay/detrital material removal, methanol rinses, buffered oxidation of organic matter, weak acid leaching, and deionised water rinses, followed by visual inspection of the remaining calcite fragments. After dissolution, samples were analysed by inductively coupled plasma mass spectrometry (ICP-MS). The analytical internal reproducibility is better than 2%. The efficiency of cleaning to remove external contaminant phases was screened on the basis of Fe/Ca ratios, which here remain below 0.05 mmol/mol. ... Dataset 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 deep convection
deep-water temperature
Mg/Ca
Southern Ocean
DEPTH, sediment/rock
AGE
Melonis affinis, Magnesium/Calcium ratio
Uvigerina sp., Magnesium/Calcium ratio
Deep water temperature
Calypso Square Core System
Inductively coupled plasma - mass spectrometry ICP-MS
MD159
Marion Dufresne 1995
spellingShingle deep convection
deep-water temperature
Mg/Ca
Southern Ocean
DEPTH, sediment/rock
AGE
Melonis affinis, Magnesium/Calcium ratio
Uvigerina sp., Magnesium/Calcium ratio
Deep water temperature
Calypso Square Core System
Inductively coupled plasma - mass spectrometry ICP-MS
MD159
Marion Dufresne 1995
Skinner, Luke C
Deep-water temperatures from the Southern Ocean during HS4 ...
topic_facet deep convection
deep-water temperature
Mg/Ca
Southern Ocean
DEPTH, sediment/rock
AGE
Melonis affinis, Magnesium/Calcium ratio
Uvigerina sp., Magnesium/Calcium ratio
Deep water temperature
Calypso Square Core System
Inductively coupled plasma - mass spectrometry ICP-MS
MD159
Marion Dufresne 1995
description Foraminiferal magnesium to calcium ratios (Mg/Ca) are reported for two benthic species, drawn from down-core marine sediment samples obtained from the deep Southern Ocean. Samples of 4-10 individual benthic foraminifera, of the species Globobulimina affinis and/or Uvigerina sp., were oxidatively cleaned according to a standard protocol, involving clay/detrital material removal, methanol rinses, buffered oxidation of organic matter, weak acid leaching, and deionised water rinses, followed by visual inspection of the remaining calcite fragments. After dissolution, samples were analysed by inductively coupled plasma mass spectrometry (ICP-MS). The analytical internal reproducibility is better than 2%. The efficiency of cleaning to remove external contaminant phases was screened on the basis of Fe/Ca ratios, which here remain below 0.05 mmol/mol. ...
format Dataset
author Skinner, Luke C
author_facet Skinner, Luke C
author_sort Skinner, Luke C
title Deep-water temperatures from the Southern Ocean during HS4 ...
title_short Deep-water temperatures from the Southern Ocean during HS4 ...
title_full Deep-water temperatures from the Southern Ocean during HS4 ...
title_fullStr Deep-water temperatures from the Southern Ocean during HS4 ...
title_full_unstemmed Deep-water temperatures from the Southern Ocean during HS4 ...
title_sort deep-water temperatures from the southern ocean during hs4 ...
publisher PANGAEA
publishDate 2020
url https://dx.doi.org/10.1594/pangaea.922135
https://doi.pangaea.de/10.1594/PANGAEA.922135
geographic Southern Ocean
geographic_facet Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_relation https://dx.doi.org/10.1038/s43247-020-00024-3
https://dx.doi.org/10.1594/pangaea.922136
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.92213510.1038/s43247-020-00024-310.1594/pangaea.922136
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