Development of a deep-water carbonate ion concentration proxy based on preservation of planktonic foraminifera shells quantified by X-ray CT scanning ...

The quantitative and objective characterization of dissolution intensity in fossil planktonic foraminiferal shells could be used to reconstruct past changes in bottom water carbonate ion concentration. Among proxies measuring the degree of dissolution of planktonic foraminiferal shells, X-ray micro-...

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Main Authors: Iwasaki, Shinya, Kimoto, Katsunori, Kucera, Michal
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2023
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.960316
https://doi.pangaea.de/10.1594/PANGAEA.960316
id ftdatacite:10.1594/pangaea.960316
record_format openpolar
spelling ftdatacite:10.1594/pangaea.960316 2023-11-05T03:44:40+01:00 Development of a deep-water carbonate ion concentration proxy based on preservation of planktonic foraminifera shells quantified by X-ray CT scanning ... Iwasaki, Shinya Kimoto, Katsunori Kucera, Michal 2023 application/zip https://dx.doi.org/10.1594/pangaea.960316 https://doi.pangaea.de/10.1594/PANGAEA.960316 en eng PANGAEA https://dx.doi.org/10.1029/2022pa004601 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 carbonate dissolution planktic foraminifera Center for Marine Environmental Sciences MARUM article Collection Bundled Publication of Datasets 2023 ftdatacite https://doi.org/10.1594/pangaea.96031610.1029/2022pa004601 2023-10-09T11:02:44Z The quantitative and objective characterization of dissolution intensity in fossil planktonic foraminiferal shells could be used to reconstruct past changes in bottom water carbonate ion concentration. Among proxies measuring the degree of dissolution of planktonic foraminiferal shells, X-ray micro-Computed Tomography (CT) based characterization of apparent shell density appears to have good potential to facilitate quantitative reconstruction of carbonate chemistry. To assess the accuracy and reliability of the proxy based on X-ray micro-CT scanning, we evaluated the planktonic foraminiferal shell dissolution intensity using seafloor sediment samples obtained at 13 sites in the South Atlantic Ocean. The sea floor sediment samples are located at water depth ranging between 940 and 4401 m. The data of benthic foraminiferal shell B/Ca ratio in these sediment samples have been measured by previous studies. The CT-based Dissolution Index (CTDX) of four species of planktonic foraminifera (G. bulloides, G. inflata, ... Article in Journal/Newspaper Planktonic foraminifera South Atlantic Ocean DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic carbonate dissolution
planktic foraminifera
Center for Marine Environmental Sciences MARUM
spellingShingle carbonate dissolution
planktic foraminifera
Center for Marine Environmental Sciences MARUM
Iwasaki, Shinya
Kimoto, Katsunori
Kucera, Michal
Development of a deep-water carbonate ion concentration proxy based on preservation of planktonic foraminifera shells quantified by X-ray CT scanning ...
topic_facet carbonate dissolution
planktic foraminifera
Center for Marine Environmental Sciences MARUM
description The quantitative and objective characterization of dissolution intensity in fossil planktonic foraminiferal shells could be used to reconstruct past changes in bottom water carbonate ion concentration. Among proxies measuring the degree of dissolution of planktonic foraminiferal shells, X-ray micro-Computed Tomography (CT) based characterization of apparent shell density appears to have good potential to facilitate quantitative reconstruction of carbonate chemistry. To assess the accuracy and reliability of the proxy based on X-ray micro-CT scanning, we evaluated the planktonic foraminiferal shell dissolution intensity using seafloor sediment samples obtained at 13 sites in the South Atlantic Ocean. The sea floor sediment samples are located at water depth ranging between 940 and 4401 m. The data of benthic foraminiferal shell B/Ca ratio in these sediment samples have been measured by previous studies. The CT-based Dissolution Index (CTDX) of four species of planktonic foraminifera (G. bulloides, G. inflata, ...
format Article in Journal/Newspaper
author Iwasaki, Shinya
Kimoto, Katsunori
Kucera, Michal
author_facet Iwasaki, Shinya
Kimoto, Katsunori
Kucera, Michal
author_sort Iwasaki, Shinya
title Development of a deep-water carbonate ion concentration proxy based on preservation of planktonic foraminifera shells quantified by X-ray CT scanning ...
title_short Development of a deep-water carbonate ion concentration proxy based on preservation of planktonic foraminifera shells quantified by X-ray CT scanning ...
title_full Development of a deep-water carbonate ion concentration proxy based on preservation of planktonic foraminifera shells quantified by X-ray CT scanning ...
title_fullStr Development of a deep-water carbonate ion concentration proxy based on preservation of planktonic foraminifera shells quantified by X-ray CT scanning ...
title_full_unstemmed Development of a deep-water carbonate ion concentration proxy based on preservation of planktonic foraminifera shells quantified by X-ray CT scanning ...
title_sort development of a deep-water carbonate ion concentration proxy based on preservation of planktonic foraminifera shells quantified by x-ray ct scanning ...
publisher PANGAEA
publishDate 2023
url https://dx.doi.org/10.1594/pangaea.960316
https://doi.pangaea.de/10.1594/PANGAEA.960316
genre Planktonic foraminifera
South Atlantic Ocean
genre_facet Planktonic foraminifera
South Atlantic Ocean
op_relation https://dx.doi.org/10.1029/2022pa004601
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.96031610.1029/2022pa004601
_version_ 1781705156337860608