Processes determining the marine alkalinity and calcium carbonate saturation state distributions
We introduce a composite tracer for the marine system, Alk * , that has a global distribution primarily determined by CaCO 3 precipitation and dissolution. Alk * is also affected by riverine alkalinity from dissolved terrestrial carbonate minerals. We estimate that the Arctic receives approximately...
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2014
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ftdoajarticles:oai:doaj.org/article:66f1e177be934ec99dbb9035a35213b2 2023-05-15T14:57:09+02:00 Processes determining the marine alkalinity and calcium carbonate saturation state distributions B. R. Carter J. R. Toggweiler R. M. Key J. L. Sarmiento 2014-12-01T00:00:00Z https://doi.org/10.5194/bg-11-7349-2014 https://doaj.org/article/66f1e177be934ec99dbb9035a35213b2 EN eng Copernicus Publications http://www.biogeosciences.net/11/7349/2014/bg-11-7349-2014.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 1726-4170 1726-4189 doi:10.5194/bg-11-7349-2014 https://doaj.org/article/66f1e177be934ec99dbb9035a35213b2 Biogeosciences, Vol 11, Iss 24, Pp 7349-7362 (2014) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2014 ftdoajarticles https://doi.org/10.5194/bg-11-7349-2014 2022-12-31T13:02:35Z We introduce a composite tracer for the marine system, Alk * , that has a global distribution primarily determined by CaCO 3 precipitation and dissolution. Alk * is also affected by riverine alkalinity from dissolved terrestrial carbonate minerals. We estimate that the Arctic receives approximately twice the riverine alkalinity per unit area as the Atlantic, and 8 times that of the other oceans. Riverine inputs broadly elevate Alk * in the Arctic surface and particularly near river mouths. Strong net carbonate precipitation results in low Alk * in subtropical gyres, especially in the Indian and Atlantic oceans. Upwelling of dissolved CaCO 3 -rich deep water elevates North Pacific and Southern Ocean Alk * . We use the Alk * distribution to estimate the variability of the calcite saturation state resulting from CaCO 3 cycling and other processes. We show that regional differences in surface calcite saturation state are due primarily to the effect of temperature differences on CO 2 solubility and, to a lesser extent, differences in freshwater content and air–sea disequilibria. The variations in net calcium carbonate cycling revealed by Alk * play a comparatively minor role in determining the calcium carbonate saturation state. Article in Journal/Newspaper Arctic Southern Ocean Directory of Open Access Journals: DOAJ Articles Arctic Southern Ocean Pacific Indian Biogeosciences 11 24 7349 7362 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
spellingShingle |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 B. R. Carter J. R. Toggweiler R. M. Key J. L. Sarmiento Processes determining the marine alkalinity and calcium carbonate saturation state distributions |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
We introduce a composite tracer for the marine system, Alk * , that has a global distribution primarily determined by CaCO 3 precipitation and dissolution. Alk * is also affected by riverine alkalinity from dissolved terrestrial carbonate minerals. We estimate that the Arctic receives approximately twice the riverine alkalinity per unit area as the Atlantic, and 8 times that of the other oceans. Riverine inputs broadly elevate Alk * in the Arctic surface and particularly near river mouths. Strong net carbonate precipitation results in low Alk * in subtropical gyres, especially in the Indian and Atlantic oceans. Upwelling of dissolved CaCO 3 -rich deep water elevates North Pacific and Southern Ocean Alk * . We use the Alk * distribution to estimate the variability of the calcite saturation state resulting from CaCO 3 cycling and other processes. We show that regional differences in surface calcite saturation state are due primarily to the effect of temperature differences on CO 2 solubility and, to a lesser extent, differences in freshwater content and air–sea disequilibria. The variations in net calcium carbonate cycling revealed by Alk * play a comparatively minor role in determining the calcium carbonate saturation state. |
format |
Article in Journal/Newspaper |
author |
B. R. Carter J. R. Toggweiler R. M. Key J. L. Sarmiento |
author_facet |
B. R. Carter J. R. Toggweiler R. M. Key J. L. Sarmiento |
author_sort |
B. R. Carter |
title |
Processes determining the marine alkalinity and calcium carbonate saturation state distributions |
title_short |
Processes determining the marine alkalinity and calcium carbonate saturation state distributions |
title_full |
Processes determining the marine alkalinity and calcium carbonate saturation state distributions |
title_fullStr |
Processes determining the marine alkalinity and calcium carbonate saturation state distributions |
title_full_unstemmed |
Processes determining the marine alkalinity and calcium carbonate saturation state distributions |
title_sort |
processes determining the marine alkalinity and calcium carbonate saturation state distributions |
publisher |
Copernicus Publications |
publishDate |
2014 |
url |
https://doi.org/10.5194/bg-11-7349-2014 https://doaj.org/article/66f1e177be934ec99dbb9035a35213b2 |
geographic |
Arctic Southern Ocean Pacific Indian |
geographic_facet |
Arctic Southern Ocean Pacific Indian |
genre |
Arctic Southern Ocean |
genre_facet |
Arctic Southern Ocean |
op_source |
Biogeosciences, Vol 11, Iss 24, Pp 7349-7362 (2014) |
op_relation |
http://www.biogeosciences.net/11/7349/2014/bg-11-7349-2014.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 1726-4170 1726-4189 doi:10.5194/bg-11-7349-2014 https://doaj.org/article/66f1e177be934ec99dbb9035a35213b2 |
op_doi |
https://doi.org/10.5194/bg-11-7349-2014 |
container_title |
Biogeosciences |
container_volume |
11 |
container_issue |
24 |
container_start_page |
7349 |
op_container_end_page |
7362 |
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1766329236138754048 |