Linking the lithogenic, atmospheric, and biogenic cycles of silicate, carbonate, and organic carbon in the ocean
Geochemical theory describes long term cycling of atmospheric CO 2 between the atmosphere and rocks at the Earth surface in terms of rock weathering and precipitation of sedimentary minerals. Chemical weathering of silicate rocks takes up atmospheric CO 2 , releases cations and HCO 3 − to water, and...
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ftcopernicus:oai:publications.copernicus.org:bgd1273 2023-05-15T17:52:07+02:00 Linking the lithogenic, atmospheric, and biogenic cycles of silicate, carbonate, and organic carbon in the ocean Smith, S. V. Gattuso, J.-P. 2018-09-26 info:eu-repo/semantics/application/pdf https://doi.org/10.5194/bgd-6-6579-2009 https://www.biogeosciences-discuss.net/bg-2009-161/ eng eng info:eu-repo/grantAgreement/EC/FP7/211384 doi:10.5194/bgd-6-6579-2009 https://www.biogeosciences-discuss.net/bg-2009-161/ info:eu-repo/semantics/openAccess eISSN: 1726-4189 info:eu-repo/semantics/Text 2018 ftcopernicus https://doi.org/10.5194/bgd-6-6579-2009 2019-12-24T09:57:50Z Geochemical theory describes long term cycling of atmospheric CO 2 between the atmosphere and rocks at the Earth surface in terms of rock weathering and precipitation of sedimentary minerals. Chemical weathering of silicate rocks takes up atmospheric CO 2 , releases cations and HCO 3 − to water, and precipitates SiO 2 , while CaCO 3 precipitation consumes Ca 2+ and HCO 3 − and releases one mole of CO 2 to the atmosphere for each mole of CaCO 3 precipitated. At steady state, according to this theory, the CO 2 uptake and release should equal one another. In contradiction to this theory, carbonate precipitation in the present surface ocean releases only about 0.6 mol of CO 2 per mole of carbonate precipitated. This is a result of the buffer effect described by Ψ, the molar ratio of net CO 2 gas evasion to net CaCO 3 precipitation from seawater in p CO 2 equilibrium with the atmosphere. This asymmetry in CO 2 flux between weathering and precipitation would quickly exhaust atmospheric CO 2 , posing a conundrum in the classical weathering and precipitation cycle. While often treated as a constant, Ψ actually varies as a function of salinity, p CO 2 , and temperature. Introduction of organic C reactions into the weathering-precipitation couplet largely reconciles the relationship. ψ in the North Pacific Ocean central gyre rises from 0.6 to 0.9, as a consequence of organic matter oxidation in the water column. ψ records the combined effect of CaCO 3 and organic reactions and storage of dissolved inorganic carbon in the ocean, as well as CO 2 gas exchange between the ocean and atmosphere. Further, in the absence of CaCO 3 reactions, Ψ would rise to 1.0. Similarly, increasing atmospheric p CO 2 over time, which leads to ocean acidification, alters the relationship between organic and inorganic C reactions and carbon storage in the ocean. Thus, the carbon reactions and ψ can cause large variations in oceanic carbon storage with little exchange with the atmosphere. Other/Unknown Material Ocean acidification Copernicus Publications: E-Journals Pacific |
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Copernicus Publications: E-Journals |
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English |
description |
Geochemical theory describes long term cycling of atmospheric CO 2 between the atmosphere and rocks at the Earth surface in terms of rock weathering and precipitation of sedimentary minerals. Chemical weathering of silicate rocks takes up atmospheric CO 2 , releases cations and HCO 3 − to water, and precipitates SiO 2 , while CaCO 3 precipitation consumes Ca 2+ and HCO 3 − and releases one mole of CO 2 to the atmosphere for each mole of CaCO 3 precipitated. At steady state, according to this theory, the CO 2 uptake and release should equal one another. In contradiction to this theory, carbonate precipitation in the present surface ocean releases only about 0.6 mol of CO 2 per mole of carbonate precipitated. This is a result of the buffer effect described by Ψ, the molar ratio of net CO 2 gas evasion to net CaCO 3 precipitation from seawater in p CO 2 equilibrium with the atmosphere. This asymmetry in CO 2 flux between weathering and precipitation would quickly exhaust atmospheric CO 2 , posing a conundrum in the classical weathering and precipitation cycle. While often treated as a constant, Ψ actually varies as a function of salinity, p CO 2 , and temperature. Introduction of organic C reactions into the weathering-precipitation couplet largely reconciles the relationship. ψ in the North Pacific Ocean central gyre rises from 0.6 to 0.9, as a consequence of organic matter oxidation in the water column. ψ records the combined effect of CaCO 3 and organic reactions and storage of dissolved inorganic carbon in the ocean, as well as CO 2 gas exchange between the ocean and atmosphere. Further, in the absence of CaCO 3 reactions, Ψ would rise to 1.0. Similarly, increasing atmospheric p CO 2 over time, which leads to ocean acidification, alters the relationship between organic and inorganic C reactions and carbon storage in the ocean. Thus, the carbon reactions and ψ can cause large variations in oceanic carbon storage with little exchange with the atmosphere. |
format |
Other/Unknown Material |
author |
Smith, S. V. Gattuso, J.-P. |
spellingShingle |
Smith, S. V. Gattuso, J.-P. Linking the lithogenic, atmospheric, and biogenic cycles of silicate, carbonate, and organic carbon in the ocean |
author_facet |
Smith, S. V. Gattuso, J.-P. |
author_sort |
Smith, S. V. |
title |
Linking the lithogenic, atmospheric, and biogenic cycles of silicate, carbonate, and organic carbon in the ocean |
title_short |
Linking the lithogenic, atmospheric, and biogenic cycles of silicate, carbonate, and organic carbon in the ocean |
title_full |
Linking the lithogenic, atmospheric, and biogenic cycles of silicate, carbonate, and organic carbon in the ocean |
title_fullStr |
Linking the lithogenic, atmospheric, and biogenic cycles of silicate, carbonate, and organic carbon in the ocean |
title_full_unstemmed |
Linking the lithogenic, atmospheric, and biogenic cycles of silicate, carbonate, and organic carbon in the ocean |
title_sort |
linking the lithogenic, atmospheric, and biogenic cycles of silicate, carbonate, and organic carbon in the ocean |
publishDate |
2018 |
url |
https://doi.org/10.5194/bgd-6-6579-2009 https://www.biogeosciences-discuss.net/bg-2009-161/ |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
eISSN: 1726-4189 |
op_relation |
info:eu-repo/grantAgreement/EC/FP7/211384 doi:10.5194/bgd-6-6579-2009 https://www.biogeosciences-discuss.net/bg-2009-161/ |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/bgd-6-6579-2009 |
_version_ |
1766159453451714560 |