Calcium isotopic composition of planktonic foraminifera from ODP Site 154-925 ...

An 18 million year record of the Ca isotopic composition (d44/42Ca) of planktonic foraminiferans from ODP site 925, in the Atlantic, on the Ceara Rise, provides the opportunity for critical analysis of Ca isotope-based reconstructions of the Ca cycle. ?44/42Ca in this record averages +0.37+/-0.05 (1...

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Main Authors: Sime, N G, De La Rocha, Christina L, Tipper, Edward T, Tripati, Aradhna K, Galy, Albert, Bickle, Michael J
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2007
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.711216
https://doi.pangaea.de/10.1594/PANGAEA.711216
id ftdatacite:10.1594/pangaea.711216
record_format openpolar
spelling ftdatacite:10.1594/pangaea.711216 2024-09-15T18:31:03+00:00 Calcium isotopic composition of planktonic foraminifera from ODP Site 154-925 ... Sime, N G De La Rocha, Christina L Tipper, Edward T Tripati, Aradhna K Galy, Albert Bickle, Michael J 2007 application/zip https://dx.doi.org/10.1594/pangaea.711216 https://doi.pangaea.de/10.1594/PANGAEA.711216 en eng PANGAEA https://dx.doi.org/10.1016/j.gca.2007.06.009 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Leg154 Joides Resolution Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 2007 ftdatacite https://doi.org/10.1594/pangaea.71121610.1016/j.gca.2007.06.009 2024-09-02T08:37:33Z An 18 million year record of the Ca isotopic composition (d44/42Ca) of planktonic foraminiferans from ODP site 925, in the Atlantic, on the Ceara Rise, provides the opportunity for critical analysis of Ca isotope-based reconstructions of the Ca cycle. ?44/42Ca in this record averages +0.37+/-0.05 (1 sigma SD) and ranges from +0.21‰ to +0.52‰. The record is a good match to previously published Neogene Ca isotope records based on foraminiferans, but is not similar to the record based on bulk carbonates, which has values that are as much as 0.25‰ lower. Bulk carbonate and planktonic foraminiferans from core tops differ slightly in their d44/42Ca (i.e., by 0.06+/-0.06‰ (n = 5)), while the difference between bulk carbonate and foraminiferan values further back in time is markedly larger, leaving open the question of the cause of the difference. Modeling the global Ca cycle from downcore variations in d44/42Ca by assuming fixed values for the isotopic composition of weathering inputs (d44/42Ca_w) and for isotope ... : Supplement to: Sime, N G; De La Rocha, Christina L; Tipper, Edward T; Tripati, Aradhna K; Galy, Albert; Bickle, Michael J (2007): Interpreting the Ca isotope record of marine biogenic carbonates. Geochimica et Cosmochimica Acta, 71(16), 3979-3989 ... Article in Journal/Newspaper Planktonic foraminifera DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Composite Core
Leg154
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Composite Core
Leg154
Joides Resolution
Ocean Drilling Program ODP
Sime, N G
De La Rocha, Christina L
Tipper, Edward T
Tripati, Aradhna K
Galy, Albert
Bickle, Michael J
Calcium isotopic composition of planktonic foraminifera from ODP Site 154-925 ...
topic_facet Composite Core
Leg154
Joides Resolution
Ocean Drilling Program ODP
description An 18 million year record of the Ca isotopic composition (d44/42Ca) of planktonic foraminiferans from ODP site 925, in the Atlantic, on the Ceara Rise, provides the opportunity for critical analysis of Ca isotope-based reconstructions of the Ca cycle. ?44/42Ca in this record averages +0.37+/-0.05 (1 sigma SD) and ranges from +0.21‰ to +0.52‰. The record is a good match to previously published Neogene Ca isotope records based on foraminiferans, but is not similar to the record based on bulk carbonates, which has values that are as much as 0.25‰ lower. Bulk carbonate and planktonic foraminiferans from core tops differ slightly in their d44/42Ca (i.e., by 0.06+/-0.06‰ (n = 5)), while the difference between bulk carbonate and foraminiferan values further back in time is markedly larger, leaving open the question of the cause of the difference. Modeling the global Ca cycle from downcore variations in d44/42Ca by assuming fixed values for the isotopic composition of weathering inputs (d44/42Ca_w) and for isotope ... : Supplement to: Sime, N G; De La Rocha, Christina L; Tipper, Edward T; Tripati, Aradhna K; Galy, Albert; Bickle, Michael J (2007): Interpreting the Ca isotope record of marine biogenic carbonates. Geochimica et Cosmochimica Acta, 71(16), 3979-3989 ...
format Article in Journal/Newspaper
author Sime, N G
De La Rocha, Christina L
Tipper, Edward T
Tripati, Aradhna K
Galy, Albert
Bickle, Michael J
author_facet Sime, N G
De La Rocha, Christina L
Tipper, Edward T
Tripati, Aradhna K
Galy, Albert
Bickle, Michael J
author_sort Sime, N G
title Calcium isotopic composition of planktonic foraminifera from ODP Site 154-925 ...
title_short Calcium isotopic composition of planktonic foraminifera from ODP Site 154-925 ...
title_full Calcium isotopic composition of planktonic foraminifera from ODP Site 154-925 ...
title_fullStr Calcium isotopic composition of planktonic foraminifera from ODP Site 154-925 ...
title_full_unstemmed Calcium isotopic composition of planktonic foraminifera from ODP Site 154-925 ...
title_sort calcium isotopic composition of planktonic foraminifera from odp site 154-925 ...
publisher PANGAEA
publishDate 2007
url https://dx.doi.org/10.1594/pangaea.711216
https://doi.pangaea.de/10.1594/PANGAEA.711216
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation https://dx.doi.org/10.1016/j.gca.2007.06.009
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.71121610.1016/j.gca.2007.06.009
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