Assessing Sedimentary Boundary Layer Calcium Carbonate Precipitation and Dissolution Using the Calcium Isotopic Composition of Pore Fluids ...
We present pore fluid geochemistry, including major ion and trace metal concentrations and the isotopic composition of pore fluid calcium and sulfate, from the uppermost meter of sediments from the Gulf of Aqaba (Northeast Red Sea) and the Iberian Margin (North Atlantic Ocean). In both the locations...
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2021
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Online Access: | https://dx.doi.org/10.17863/cam.74106 https://www.repository.cam.ac.uk/handle/1810/326657 |
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ftdatacite:10.17863/cam.74106 2024-02-04T10:02:38+01:00 Assessing Sedimentary Boundary Layer Calcium Carbonate Precipitation and Dissolution Using the Calcium Isotopic Composition of Pore Fluids ... James, DH Bradbury, HJ Antler, G Steiner, Z Hutchings, AM Sun, X Saar, R Greaves, M Turchyn, AV 2021 https://dx.doi.org/10.17863/cam.74106 https://www.repository.cam.ac.uk/handle/1810/326657 en eng Frontiers Media SA open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 carbonate precipitation calcium isotopes early diagenesis microbial sulfate reduction microbial iron reduction sedimentary boundary layer carbonate dissolution Article ScholarlyArticle JournalArticle article-journal 2021 ftdatacite https://doi.org/10.17863/cam.74106 2024-01-05T14:24:00Z We present pore fluid geochemistry, including major ion and trace metal concentrations and the isotopic composition of pore fluid calcium and sulfate, from the uppermost meter of sediments from the Gulf of Aqaba (Northeast Red Sea) and the Iberian Margin (North Atlantic Ocean). In both the locations, we observe strong correlations among calcium, magnesium, strontium, and sulfate concentrations as well as the sulfur isotopic composition of sulfate and alkalinity, suggestive of active changes in the redox state and pH that should lead to carbonate mineral precipitation and dissolution. The calcium isotope composition of pore fluid calcium (δ 44 Ca) is, however, relatively invariant in our measured profiles, suggesting that carbonate mineral precipitation is not occurring within the boundary layer at these sites. We explore several reasons why the pore fluid δ 44 Ca might not be changing in the studied profiles, despite changes in other major ions and their isotopic composition, including mixing between the ... Article in Journal/Newspaper North Atlantic 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 precipitation calcium isotopes early diagenesis microbial sulfate reduction microbial iron reduction sedimentary boundary layer carbonate dissolution |
spellingShingle |
carbonate precipitation calcium isotopes early diagenesis microbial sulfate reduction microbial iron reduction sedimentary boundary layer carbonate dissolution James, DH Bradbury, HJ Antler, G Steiner, Z Hutchings, AM Sun, X Saar, R Greaves, M Turchyn, AV Assessing Sedimentary Boundary Layer Calcium Carbonate Precipitation and Dissolution Using the Calcium Isotopic Composition of Pore Fluids ... |
topic_facet |
carbonate precipitation calcium isotopes early diagenesis microbial sulfate reduction microbial iron reduction sedimentary boundary layer carbonate dissolution |
description |
We present pore fluid geochemistry, including major ion and trace metal concentrations and the isotopic composition of pore fluid calcium and sulfate, from the uppermost meter of sediments from the Gulf of Aqaba (Northeast Red Sea) and the Iberian Margin (North Atlantic Ocean). In both the locations, we observe strong correlations among calcium, magnesium, strontium, and sulfate concentrations as well as the sulfur isotopic composition of sulfate and alkalinity, suggestive of active changes in the redox state and pH that should lead to carbonate mineral precipitation and dissolution. The calcium isotope composition of pore fluid calcium (δ 44 Ca) is, however, relatively invariant in our measured profiles, suggesting that carbonate mineral precipitation is not occurring within the boundary layer at these sites. We explore several reasons why the pore fluid δ 44 Ca might not be changing in the studied profiles, despite changes in other major ions and their isotopic composition, including mixing between the ... |
format |
Article in Journal/Newspaper |
author |
James, DH Bradbury, HJ Antler, G Steiner, Z Hutchings, AM Sun, X Saar, R Greaves, M Turchyn, AV |
author_facet |
James, DH Bradbury, HJ Antler, G Steiner, Z Hutchings, AM Sun, X Saar, R Greaves, M Turchyn, AV |
author_sort |
James, DH |
title |
Assessing Sedimentary Boundary Layer Calcium Carbonate Precipitation and Dissolution Using the Calcium Isotopic Composition of Pore Fluids ... |
title_short |
Assessing Sedimentary Boundary Layer Calcium Carbonate Precipitation and Dissolution Using the Calcium Isotopic Composition of Pore Fluids ... |
title_full |
Assessing Sedimentary Boundary Layer Calcium Carbonate Precipitation and Dissolution Using the Calcium Isotopic Composition of Pore Fluids ... |
title_fullStr |
Assessing Sedimentary Boundary Layer Calcium Carbonate Precipitation and Dissolution Using the Calcium Isotopic Composition of Pore Fluids ... |
title_full_unstemmed |
Assessing Sedimentary Boundary Layer Calcium Carbonate Precipitation and Dissolution Using the Calcium Isotopic Composition of Pore Fluids ... |
title_sort |
assessing sedimentary boundary layer calcium carbonate precipitation and dissolution using the calcium isotopic composition of pore fluids ... |
publisher |
Frontiers Media SA |
publishDate |
2021 |
url |
https://dx.doi.org/10.17863/cam.74106 https://www.repository.cam.ac.uk/handle/1810/326657 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_rights |
open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 |
op_doi |
https://doi.org/10.17863/cam.74106 |
_version_ |
1789969456760356864 |