Significance of the terrestrial sink in the biogeochemical sulfur cycle

An imbalance in pyrite weathering and burial is regarded as one of the primary mechanisms responsible for the oxygenation of the atmosphere and oceans, but key processes governing the terrestrial sulfur cycle remain nebulous. Here, we investigate components of the terrestrial sulfur cycle in a highl...

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Main Authors: Joo, Young Ji, Sim, Min Sub, Elwood Madden, Megan, Soreghan, Gerilyn
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2022
Subjects:
Online Access:https://doi.org/10.5061/dryad.r2280gbf6
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spelling ftzenodo:oai:zenodo.org:5950263 2024-09-15T18:07:53+00:00 Significance of the terrestrial sink in the biogeochemical sulfur cycle Joo, Young Ji Sim, Min Sub Elwood Madden, Megan Soreghan, Gerilyn 2022-02-02 https://doi.org/10.5061/dryad.r2280gbf6 unknown Zenodo https://zenodo.org/communities/dryad https://doi.org/10.5061/dryad.r2280gbf6 oai:zenodo.org:5950263 info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode sulfur isotopes proglacial stream chemistry glacial sediment chemistry peat soil info:eu-repo/semantics/other 2022 ftzenodo https://doi.org/10.5061/dryad.r2280gbf6 2024-07-25T11:46:26Z An imbalance in pyrite weathering and burial is regarded as one of the primary mechanisms responsible for the oxygenation of the atmosphere and oceans, but key processes governing the terrestrial sulfur cycle remain nebulous. Here, we investigate components of the terrestrial sulfur cycle in a highly productive, glacier-fed catchment, and use a global mass balance model to put constraints on the riverine sulfur fluxes. Chemistry of stream water and plant debris in the Jostedal watershed, Norway suggests sulfur isotope discrimination is occurring in the porewater. Global models also corroborate additional, previously overlooked pyrite burial with a modest isotope fractionation (<20‰), similar to values reported from freshwater ecosystems. Collectively, our results support the notion that a significant amount of sulfate produced by weathering remains trapped in terrestrial environments. This terrestrial sulfur sink might have waxed and waned over geologic time in response to major biogeochemical events such as terrestrial afforestation. Funding provided by: National Science Foundation Crossref Funder Registry ID: http://dx.doi.org/10.13039/100000001 Award Number: EAR-1225162 Funding provided by: National Science Foundation Crossref Funder Registry ID: http://dx.doi.org/10.13039/100000001 Award Number: EAR-1418716 Funding provided by: Korea Polar Research Institute Crossref Funder Registry ID: http://dx.doi.org/10.13039/501100004230 Award Number: PE20900 Funding provided by: National Research Foundation of Korea Crossref Funder Registry ID: http://dx.doi.org/10.13039/501100003725 Award Number: 2019R1C1C1005550 Other/Unknown Material glacier Korea Polar Research Institute Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic sulfur isotopes
proglacial stream chemistry
glacial sediment chemistry
peat soil
spellingShingle sulfur isotopes
proglacial stream chemistry
glacial sediment chemistry
peat soil
Joo, Young Ji
Sim, Min Sub
Elwood Madden, Megan
Soreghan, Gerilyn
Significance of the terrestrial sink in the biogeochemical sulfur cycle
topic_facet sulfur isotopes
proglacial stream chemistry
glacial sediment chemistry
peat soil
description An imbalance in pyrite weathering and burial is regarded as one of the primary mechanisms responsible for the oxygenation of the atmosphere and oceans, but key processes governing the terrestrial sulfur cycle remain nebulous. Here, we investigate components of the terrestrial sulfur cycle in a highly productive, glacier-fed catchment, and use a global mass balance model to put constraints on the riverine sulfur fluxes. Chemistry of stream water and plant debris in the Jostedal watershed, Norway suggests sulfur isotope discrimination is occurring in the porewater. Global models also corroborate additional, previously overlooked pyrite burial with a modest isotope fractionation (<20‰), similar to values reported from freshwater ecosystems. Collectively, our results support the notion that a significant amount of sulfate produced by weathering remains trapped in terrestrial environments. This terrestrial sulfur sink might have waxed and waned over geologic time in response to major biogeochemical events such as terrestrial afforestation. Funding provided by: National Science Foundation Crossref Funder Registry ID: http://dx.doi.org/10.13039/100000001 Award Number: EAR-1225162 Funding provided by: National Science Foundation Crossref Funder Registry ID: http://dx.doi.org/10.13039/100000001 Award Number: EAR-1418716 Funding provided by: Korea Polar Research Institute Crossref Funder Registry ID: http://dx.doi.org/10.13039/501100004230 Award Number: PE20900 Funding provided by: National Research Foundation of Korea Crossref Funder Registry ID: http://dx.doi.org/10.13039/501100003725 Award Number: 2019R1C1C1005550
format Other/Unknown Material
author Joo, Young Ji
Sim, Min Sub
Elwood Madden, Megan
Soreghan, Gerilyn
author_facet Joo, Young Ji
Sim, Min Sub
Elwood Madden, Megan
Soreghan, Gerilyn
author_sort Joo, Young Ji
title Significance of the terrestrial sink in the biogeochemical sulfur cycle
title_short Significance of the terrestrial sink in the biogeochemical sulfur cycle
title_full Significance of the terrestrial sink in the biogeochemical sulfur cycle
title_fullStr Significance of the terrestrial sink in the biogeochemical sulfur cycle
title_full_unstemmed Significance of the terrestrial sink in the biogeochemical sulfur cycle
title_sort significance of the terrestrial sink in the biogeochemical sulfur cycle
publisher Zenodo
publishDate 2022
url https://doi.org/10.5061/dryad.r2280gbf6
genre glacier
Korea Polar Research Institute
genre_facet glacier
Korea Polar Research Institute
op_relation https://zenodo.org/communities/dryad
https://doi.org/10.5061/dryad.r2280gbf6
oai:zenodo.org:5950263
op_rights info:eu-repo/semantics/openAccess
Creative Commons Zero v1.0 Universal
https://creativecommons.org/publicdomain/zero/1.0/legalcode
op_doi https://doi.org/10.5061/dryad.r2280gbf6
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