Calcium distribution in the subtropical Atlantic Ocean: Implications for calcium excess and saturation horizons
7 páginas, 1 tabla, 4 figuras This study constituted the first attempt to measure dissolved calcium ([Ca2 +]meas) in the subtropical North Atlantic, during a zonal transoceanic cruise along 24.5°N (WOCE A05 section), in summer 1992. [Ca2 +]meas was obtained in 20 full-depth equidistant stations alon...
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ftcsic:oai:digital.csic.es:10261/129516 2024-02-11T10:01:28+01:00 Calcium distribution in the subtropical Atlantic Ocean: Implications for calcium excess and saturation horizons Rosón, Gabriel Fernández-Guallart, E. Pérez, Fiz F. Ríos, Aida F. Ministerio de Economía y Competitividad (España) 2016-06 http://hdl.handle.net/10261/129516 https://doi.org/10.1016/j.jmarsys.2016.01.011 https://doi.org/10.13039/501100003329 en eng Elsevier #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CTM2013-41048-P Postprint http://dx.doi.org/10.1016/j.jmarsys.2016.01.011 Sí Journal of Marine Systems 158: 45-51 (2016) 0924-7963 http://hdl.handle.net/10261/129516 doi:10.1016/j.jmarsys.2016.01.011 1879-1573 http://dx.doi.org/10.13039/501100003329 open Calcium Alkalinity Aragonite Calcite Seawater North Atlantic artículo http://purl.org/coar/resource_type/c_6501 2016 ftcsic https://doi.org/10.1016/j.jmarsys.2016.01.01110.13039/501100003329 2024-01-16T10:14:03Z 7 páginas, 1 tabla, 4 figuras This study constituted the first attempt to measure dissolved calcium ([Ca2 +]meas) in the subtropical North Atlantic, during a zonal transoceanic cruise along 24.5°N (WOCE A05 section), in summer 1992. [Ca2 +]meas was obtained in 20 full-depth equidistant stations along the section, showing that their gradients are rather sensitive to horizontal and vertical water mass distribution. Deep waters along 24.5°N systematically show a positive calcium excess of 20 ± 14 μmol·kg− 1, i.e., more [Ca2 +] than expected by CaCO3 dissolution and organic matter oxidation (estimated by total alkalinity and nitrate). CaCO3 settling and benthic dissolution accounts for 70% and the North Atlantic plus Arctic riverine inputs of HCO3− for the remaining 30%. Combining [Ca2 +]meas and CO2 data sets, carbonate mineral saturation states distributions for aragonite and calcite can be obtained. The two solubility ratios resulted, on average, 0.5% smaller than if conservative behavior for Ca2 + was assumed (an approach widely followed when [Ca2 +]meas is unknown). As a result, shallower saturation horizon depths for both carbonate states (19 dbar for aragonite and 10 dbar for calcite) are yielded if [Ca2 +]meas is taken into account instead than estimated from salinity This work has been performed under the project BOCATS (CTM2013-41048-P) supported by the Spanish Government and co-founded by the European Regional Development Fund (FEDER) Peer reviewed Article in Journal/Newspaper Arctic North Atlantic Digital.CSIC (Spanish National Research Council) Arctic Journal of Marine Systems 158 45 51 |
institution |
Open Polar |
collection |
Digital.CSIC (Spanish National Research Council) |
op_collection_id |
ftcsic |
language |
English |
topic |
Calcium Alkalinity Aragonite Calcite Seawater North Atlantic |
spellingShingle |
Calcium Alkalinity Aragonite Calcite Seawater North Atlantic Rosón, Gabriel Fernández-Guallart, E. Pérez, Fiz F. Ríos, Aida F. Calcium distribution in the subtropical Atlantic Ocean: Implications for calcium excess and saturation horizons |
topic_facet |
Calcium Alkalinity Aragonite Calcite Seawater North Atlantic |
description |
7 páginas, 1 tabla, 4 figuras This study constituted the first attempt to measure dissolved calcium ([Ca2 +]meas) in the subtropical North Atlantic, during a zonal transoceanic cruise along 24.5°N (WOCE A05 section), in summer 1992. [Ca2 +]meas was obtained in 20 full-depth equidistant stations along the section, showing that their gradients are rather sensitive to horizontal and vertical water mass distribution. Deep waters along 24.5°N systematically show a positive calcium excess of 20 ± 14 μmol·kg− 1, i.e., more [Ca2 +] than expected by CaCO3 dissolution and organic matter oxidation (estimated by total alkalinity and nitrate). CaCO3 settling and benthic dissolution accounts for 70% and the North Atlantic plus Arctic riverine inputs of HCO3− for the remaining 30%. Combining [Ca2 +]meas and CO2 data sets, carbonate mineral saturation states distributions for aragonite and calcite can be obtained. The two solubility ratios resulted, on average, 0.5% smaller than if conservative behavior for Ca2 + was assumed (an approach widely followed when [Ca2 +]meas is unknown). As a result, shallower saturation horizon depths for both carbonate states (19 dbar for aragonite and 10 dbar for calcite) are yielded if [Ca2 +]meas is taken into account instead than estimated from salinity This work has been performed under the project BOCATS (CTM2013-41048-P) supported by the Spanish Government and co-founded by the European Regional Development Fund (FEDER) Peer reviewed |
author2 |
Ministerio de Economía y Competitividad (España) |
format |
Article in Journal/Newspaper |
author |
Rosón, Gabriel Fernández-Guallart, E. Pérez, Fiz F. Ríos, Aida F. |
author_facet |
Rosón, Gabriel Fernández-Guallart, E. Pérez, Fiz F. Ríos, Aida F. |
author_sort |
Rosón, Gabriel |
title |
Calcium distribution in the subtropical Atlantic Ocean: Implications for calcium excess and saturation horizons |
title_short |
Calcium distribution in the subtropical Atlantic Ocean: Implications for calcium excess and saturation horizons |
title_full |
Calcium distribution in the subtropical Atlantic Ocean: Implications for calcium excess and saturation horizons |
title_fullStr |
Calcium distribution in the subtropical Atlantic Ocean: Implications for calcium excess and saturation horizons |
title_full_unstemmed |
Calcium distribution in the subtropical Atlantic Ocean: Implications for calcium excess and saturation horizons |
title_sort |
calcium distribution in the subtropical atlantic ocean: implications for calcium excess and saturation horizons |
publisher |
Elsevier |
publishDate |
2016 |
url |
http://hdl.handle.net/10261/129516 https://doi.org/10.1016/j.jmarsys.2016.01.011 https://doi.org/10.13039/501100003329 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic North Atlantic |
genre_facet |
Arctic North Atlantic |
op_relation |
#PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CTM2013-41048-P Postprint http://dx.doi.org/10.1016/j.jmarsys.2016.01.011 Sí Journal of Marine Systems 158: 45-51 (2016) 0924-7963 http://hdl.handle.net/10261/129516 doi:10.1016/j.jmarsys.2016.01.011 1879-1573 http://dx.doi.org/10.13039/501100003329 |
op_rights |
open |
op_doi |
https://doi.org/10.1016/j.jmarsys.2016.01.01110.13039/501100003329 |
container_title |
Journal of Marine Systems |
container_volume |
158 |
container_start_page |
45 |
op_container_end_page |
51 |
_version_ |
1790597280653377536 |