Large calcium isotope fractionations by zeolite minerals from Iceland
Abstract Zeolites are secondary tectosilicates produced during the hydrothermal alteration of basalt. The minerals serve as major sinks of calcium, which readily exchanges with calcium from surrounding groundwater. However, no studies have specifically investigated the calcium isotope geochemistry (...
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2021
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crspringernat:10.1038/s43247-021-00274-9 2023-05-15T16:47:11+02:00 Large calcium isotope fractionations by zeolite minerals from Iceland Nelson, Claire J. Jacobson, Andrew D. Kitch, Gabriella D. Weisenberger, Tobias B. National Science Foundation 2021 http://dx.doi.org/10.1038/s43247-021-00274-9 https://www.nature.com/articles/s43247-021-00274-9.pdf https://www.nature.com/articles/s43247-021-00274-9 en eng Springer Science and Business Media LLC https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 CC-BY Communications Earth & Environment volume 2, issue 1 ISSN 2662-4435 General Earth and Planetary Sciences General Environmental Science journal-article 2021 crspringernat https://doi.org/10.1038/s43247-021-00274-9 2022-01-04T16:39:04Z Abstract Zeolites are secondary tectosilicates produced during the hydrothermal alteration of basalt. The minerals serve as major sinks of calcium, which readily exchanges with calcium from surrounding groundwater. However, no studies have specifically investigated the calcium isotope geochemistry (δ 44/40 Ca) of zeolites. Here, we report δ 44/40 Ca values for zeolites from East Iceland, where the minerals form during progressive burial of the lava pile. The zeolites show a δ 44/40 Ca range of 1.4‰, which strongly correlates with average mineral calcium-oxygen bond lengths. As this correlation appears most consistent with equilibrium isotope partitioning, our findings point toward developing a novel geothermometer for studying low-grade basalt metamorphism. The results also have significance for using calcium isotopes to trace basalt weathering, including its role in long-term climate regulation and application in carbon capture and storage, a leading strategy for mitigating anthropogenic climate change. Article in Journal/Newspaper Iceland Springer Nature (via Crossref) Communications Earth & Environment 2 1 |
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Springer Nature (via Crossref) |
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crspringernat |
language |
English |
topic |
General Earth and Planetary Sciences General Environmental Science |
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General Earth and Planetary Sciences General Environmental Science Nelson, Claire J. Jacobson, Andrew D. Kitch, Gabriella D. Weisenberger, Tobias B. Large calcium isotope fractionations by zeolite minerals from Iceland |
topic_facet |
General Earth and Planetary Sciences General Environmental Science |
description |
Abstract Zeolites are secondary tectosilicates produced during the hydrothermal alteration of basalt. The minerals serve as major sinks of calcium, which readily exchanges with calcium from surrounding groundwater. However, no studies have specifically investigated the calcium isotope geochemistry (δ 44/40 Ca) of zeolites. Here, we report δ 44/40 Ca values for zeolites from East Iceland, where the minerals form during progressive burial of the lava pile. The zeolites show a δ 44/40 Ca range of 1.4‰, which strongly correlates with average mineral calcium-oxygen bond lengths. As this correlation appears most consistent with equilibrium isotope partitioning, our findings point toward developing a novel geothermometer for studying low-grade basalt metamorphism. The results also have significance for using calcium isotopes to trace basalt weathering, including its role in long-term climate regulation and application in carbon capture and storage, a leading strategy for mitigating anthropogenic climate change. |
author2 |
National Science Foundation |
format |
Article in Journal/Newspaper |
author |
Nelson, Claire J. Jacobson, Andrew D. Kitch, Gabriella D. Weisenberger, Tobias B. |
author_facet |
Nelson, Claire J. Jacobson, Andrew D. Kitch, Gabriella D. Weisenberger, Tobias B. |
author_sort |
Nelson, Claire J. |
title |
Large calcium isotope fractionations by zeolite minerals from Iceland |
title_short |
Large calcium isotope fractionations by zeolite minerals from Iceland |
title_full |
Large calcium isotope fractionations by zeolite minerals from Iceland |
title_fullStr |
Large calcium isotope fractionations by zeolite minerals from Iceland |
title_full_unstemmed |
Large calcium isotope fractionations by zeolite minerals from Iceland |
title_sort |
large calcium isotope fractionations by zeolite minerals from iceland |
publisher |
Springer Science and Business Media LLC |
publishDate |
2021 |
url |
http://dx.doi.org/10.1038/s43247-021-00274-9 https://www.nature.com/articles/s43247-021-00274-9.pdf https://www.nature.com/articles/s43247-021-00274-9 |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
Communications Earth & Environment volume 2, issue 1 ISSN 2662-4435 |
op_rights |
https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1038/s43247-021-00274-9 |
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Communications Earth & Environment |
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2 |
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1 |
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1766037262451081216 |