Large-scale groundwater flow and sedimentary diagenesis in continental shelves influence marine chemical budgets

Abstract The major ion chemistry of the ocean has been assumed to be controlled by river input, hydrothermal circulation at mid-ocean ridges, carbonate production, and low-temperature alteration of seafloor basalt, but marine chemical budgets remain difficult to balance. Here we propose that large-s...

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Main Authors: Alicia M. Wilson, Andrew Osborne, Scott M. White
Format: Article
Language:English
Published: Nature Portfolio 2024-02-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/s41467-024-44919-7
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author Alicia M. Wilson
Andrew Osborne
Scott M. White
author_facet Alicia M. Wilson
Andrew Osborne
Scott M. White
author_sort Alicia M. Wilson
collection DOAJ
description Abstract The major ion chemistry of the ocean has been assumed to be controlled by river input, hydrothermal circulation at mid-ocean ridges, carbonate production, and low-temperature alteration of seafloor basalt, but marine chemical budgets remain difficult to balance. Here we propose that large-scale groundwater flow and diagenetic reactions in continental shelf sediments have been overlooked as an important contributor to major ion budgets in the ocean. Based on data synthesized from 17 passive margin basins, continental shelves contribute fluid exchanges comparable to hydrothermal circulation at mid-ocean ridges. Chemical exchange is similarly significant, indicating removal of Mg2+ from the oceans at rates similar to mid-ocean ridge convection. Continental shelves likely contribute Ca2+ and K+ to the oceans at rates that, in combination with low-temperature basalt alteration, can close current budget deficits. Flow and reaction in continental shelf sediments should be included in a new generation of studies addressing marine isotope budgets.
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spelling doaj.art-234d81d23dc14dd2974516caab868ce72024-03-05T19:36:23ZengNature PortfolioNature Communications2041-17232024-02-0115111010.1038/s41467-024-44919-7Large-scale groundwater flow and sedimentary diagenesis in continental shelves influence marine chemical budgetsAlicia M. Wilson0Andrew Osborne1Scott M. White2School of the Earth, Ocean and Environment University of South CarolinaSchool of the Earth, Ocean and Environment University of South CarolinaSchool of the Earth, Ocean and Environment University of South CarolinaAbstract The major ion chemistry of the ocean has been assumed to be controlled by river input, hydrothermal circulation at mid-ocean ridges, carbonate production, and low-temperature alteration of seafloor basalt, but marine chemical budgets remain difficult to balance. Here we propose that large-scale groundwater flow and diagenetic reactions in continental shelf sediments have been overlooked as an important contributor to major ion budgets in the ocean. Based on data synthesized from 17 passive margin basins, continental shelves contribute fluid exchanges comparable to hydrothermal circulation at mid-ocean ridges. Chemical exchange is similarly significant, indicating removal of Mg2+ from the oceans at rates similar to mid-ocean ridge convection. Continental shelves likely contribute Ca2+ and K+ to the oceans at rates that, in combination with low-temperature basalt alteration, can close current budget deficits. Flow and reaction in continental shelf sediments should be included in a new generation of studies addressing marine isotope budgets.https://doi.org/10.1038/s41467-024-44919-7
spellingShingle Alicia M. Wilson
Andrew Osborne
Scott M. White
Large-scale groundwater flow and sedimentary diagenesis in continental shelves influence marine chemical budgets
Nature Communications
title Large-scale groundwater flow and sedimentary diagenesis in continental shelves influence marine chemical budgets
title_full Large-scale groundwater flow and sedimentary diagenesis in continental shelves influence marine chemical budgets
title_fullStr Large-scale groundwater flow and sedimentary diagenesis in continental shelves influence marine chemical budgets
title_full_unstemmed Large-scale groundwater flow and sedimentary diagenesis in continental shelves influence marine chemical budgets
title_short Large-scale groundwater flow and sedimentary diagenesis in continental shelves influence marine chemical budgets
title_sort large scale groundwater flow and sedimentary diagenesis in continental shelves influence marine chemical budgets
url https://doi.org/10.1038/s41467-024-44919-7
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AT andrewosborne largescalegroundwaterflowandsedimentarydiagenesisincontinentalshelvesinfluencemarinechemicalbudgets
AT scottmwhite largescalegroundwaterflowandsedimentarydiagenesisincontinentalshelvesinfluencemarinechemicalbudgets