Biogenic silica recycling in sea ice inferred from Si-isotopes: constraints from Arctic winter first-year sea ice
peer reviewed We report silicon isotopic composition (d30Si vs. NBS28) in Arctic sea ice, based on sampling of silicic acid from both brine and seawater in a small Greenlandic bay in March 2010. Our measurements show that just before the productive period, d30Si of sea-ice brine similar to d30Si of...
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Springer Science & Business Media B.V.
2013
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Online Access: | https://orbi.uliege.be/handle/2268/156910 https://orbi.uliege.be/bitstream/2268/156910/1/fripiat%20et%20al_%20revised.pdf https://doi.org/10.1007/s10533-013-9911-8 |
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ftorbi:oai:orbi.ulg.ac.be:2268/156910 2024-04-21T07:48:32+00:00 Biogenic silica recycling in sea ice inferred from Si-isotopes: constraints from Arctic winter first-year sea ice Fripiat, François Tison, Jean-Louis André, Luc Notz, Dirk Delille, Bruno 2013 https://orbi.uliege.be/handle/2268/156910 https://orbi.uliege.be/bitstream/2268/156910/1/fripiat%20et%20al_%20revised.pdf https://doi.org/10.1007/s10533-013-9911-8 en eng Springer Science & Business Media B.V. http://link.springer.com/article/10.1007/s10533-013-9911-8 urn:issn:0168-2563 urn:issn:1573-515X https://orbi.uliege.be/handle/2268/156910 info:hdl:2268/156910 https://orbi.uliege.be/bitstream/2268/156910/1/fripiat%20et%20al_%20revised.pdf doi:10.1007/s10533-013-9911-8 scopus-id:2-s2.0-84900526914 open access http://purl.org/coar/access_right/c_abf2 info:eu-repo/semantics/openAccess Biogeochemistry (2013) Sea ice Nutrients Cycles Silicon Biogenic silica production Biogenic silica dissolution Physical chemical mathematical & earth Sciences Earth sciences & physical geography Physique chimie mathématiques & sciences de la terre Sciences de la terre & géographie physique journal article http://purl.org/coar/resource_type/c_6501 info:eu-repo/semantics/article peer reviewed 2013 ftorbi https://doi.org/10.1007/s10533-013-9911-8 2024-03-27T14:53:04Z peer reviewed We report silicon isotopic composition (d30Si vs. NBS28) in Arctic sea ice, based on sampling of silicic acid from both brine and seawater in a small Greenlandic bay in March 2010. Our measurements show that just before the productive period, d30Si of sea-ice brine similar to d30Si of the underlying seawater. Hence, there is no Si isotopic fractionation during sea-ice growth by physical processes such as brine convection. This finding brings credit and support to the conclusions of previous work on the impact of biogenic processes on sea ice d30Si: any d30Si change results from a combination of biogenic silica production and dissolution. We use this insight to interpret data from an earlier study of sea-ice d30Si in Antarctic pack ice that show a large accumulation of biogenic silica. Based on these data, we estimate a significant contribution of biogenic silica dissolution (D) to production (P), with a D:P ratio between 0.4 and 0.9. This finding has significant implications for the understanding and parameterization of the sea ice Sibiogeochemical cycle, i.e. previous studies assumed little or no biogenic silica dissolution in sea ice. BELCANTO Article in Journal/Newspaper Antarc* Antarctic greenlandic Sea ice University of Liège: ORBi (Open Repository and Bibliography) Biogeochemistry 119 1-3 25 33 |
institution |
Open Polar |
collection |
University of Liège: ORBi (Open Repository and Bibliography) |
op_collection_id |
ftorbi |
language |
English |
topic |
Sea ice Nutrients Cycles Silicon Biogenic silica production Biogenic silica dissolution Physical chemical mathematical & earth Sciences Earth sciences & physical geography Physique chimie mathématiques & sciences de la terre Sciences de la terre & géographie physique |
spellingShingle |
Sea ice Nutrients Cycles Silicon Biogenic silica production Biogenic silica dissolution Physical chemical mathematical & earth Sciences Earth sciences & physical geography Physique chimie mathématiques & sciences de la terre Sciences de la terre & géographie physique Fripiat, François Tison, Jean-Louis André, Luc Notz, Dirk Delille, Bruno Biogenic silica recycling in sea ice inferred from Si-isotopes: constraints from Arctic winter first-year sea ice |
topic_facet |
Sea ice Nutrients Cycles Silicon Biogenic silica production Biogenic silica dissolution Physical chemical mathematical & earth Sciences Earth sciences & physical geography Physique chimie mathématiques & sciences de la terre Sciences de la terre & géographie physique |
description |
peer reviewed We report silicon isotopic composition (d30Si vs. NBS28) in Arctic sea ice, based on sampling of silicic acid from both brine and seawater in a small Greenlandic bay in March 2010. Our measurements show that just before the productive period, d30Si of sea-ice brine similar to d30Si of the underlying seawater. Hence, there is no Si isotopic fractionation during sea-ice growth by physical processes such as brine convection. This finding brings credit and support to the conclusions of previous work on the impact of biogenic processes on sea ice d30Si: any d30Si change results from a combination of biogenic silica production and dissolution. We use this insight to interpret data from an earlier study of sea-ice d30Si in Antarctic pack ice that show a large accumulation of biogenic silica. Based on these data, we estimate a significant contribution of biogenic silica dissolution (D) to production (P), with a D:P ratio between 0.4 and 0.9. This finding has significant implications for the understanding and parameterization of the sea ice Sibiogeochemical cycle, i.e. previous studies assumed little or no biogenic silica dissolution in sea ice. BELCANTO |
format |
Article in Journal/Newspaper |
author |
Fripiat, François Tison, Jean-Louis André, Luc Notz, Dirk Delille, Bruno |
author_facet |
Fripiat, François Tison, Jean-Louis André, Luc Notz, Dirk Delille, Bruno |
author_sort |
Fripiat, François |
title |
Biogenic silica recycling in sea ice inferred from Si-isotopes: constraints from Arctic winter first-year sea ice |
title_short |
Biogenic silica recycling in sea ice inferred from Si-isotopes: constraints from Arctic winter first-year sea ice |
title_full |
Biogenic silica recycling in sea ice inferred from Si-isotopes: constraints from Arctic winter first-year sea ice |
title_fullStr |
Biogenic silica recycling in sea ice inferred from Si-isotopes: constraints from Arctic winter first-year sea ice |
title_full_unstemmed |
Biogenic silica recycling in sea ice inferred from Si-isotopes: constraints from Arctic winter first-year sea ice |
title_sort |
biogenic silica recycling in sea ice inferred from si-isotopes: constraints from arctic winter first-year sea ice |
publisher |
Springer Science & Business Media B.V. |
publishDate |
2013 |
url |
https://orbi.uliege.be/handle/2268/156910 https://orbi.uliege.be/bitstream/2268/156910/1/fripiat%20et%20al_%20revised.pdf https://doi.org/10.1007/s10533-013-9911-8 |
genre |
Antarc* Antarctic greenlandic Sea ice |
genre_facet |
Antarc* Antarctic greenlandic Sea ice |
op_source |
Biogeochemistry (2013) |
op_relation |
http://link.springer.com/article/10.1007/s10533-013-9911-8 urn:issn:0168-2563 urn:issn:1573-515X https://orbi.uliege.be/handle/2268/156910 info:hdl:2268/156910 https://orbi.uliege.be/bitstream/2268/156910/1/fripiat%20et%20al_%20revised.pdf doi:10.1007/s10533-013-9911-8 scopus-id:2-s2.0-84900526914 |
op_rights |
open access http://purl.org/coar/access_right/c_abf2 info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1007/s10533-013-9911-8 |
container_title |
Biogeochemistry |
container_volume |
119 |
container_issue |
1-3 |
container_start_page |
25 |
op_container_end_page |
33 |
_version_ |
1796950116242817024 |