231Pa and 230Th in the Arctic Ocean : Implications for boundary scavenging and 231Pa-230Th fractionation in the Eurasian Basin
231Pa, 230Th and 232Th were analyzed in filtered seawater (n=70) and suspended particles (n=39) collectedalong a shelf-basin transect from the Barents shelf to the Makarov Basin in the Arctic Ocean during GEOTRACESsection GN04 in 2015. The distribution of dissolved 231Pa and 230Th in the Arctic Ocea...
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Stockholms universitet, Institutionen för geologiska vetenskaper
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ftstockholmuniv:oai:DiVA.org:su-185828 2023-05-15T14:42:00+02:00 231Pa and 230Th in the Arctic Ocean : Implications for boundary scavenging and 231Pa-230Th fractionation in the Eurasian Basin Gdaniec, Sandra Roy-Barman, Matthieu Levier, Martin Valk, Ole van der Loeff, Michiel Rutgers Foliot, Lorna Dapoigny, Arnaud Missiaen, Lise Mörth, Carl-Magnus Andersson, Per S. 2020 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-185828 https://doi.org/10.1016/j.chemgeo.2019.119380 eng eng Stockholms universitet, Institutionen för geologiska vetenskaper Swedish Museum of Natural History, Sweden; Université Paris-Saclay, France Chemical Geology, 0009-2541, 2020, 532, orcid:0000-0003-2057-5795 http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-185828 doi:10.1016/j.chemgeo.2019.119380 ISI:000513868400001 info:eu-repo/semantics/openAccess GEOTRACES Protactinium Thorium Arctic Ocean Boundary scavenging Geochemistry Geokemi Article in journal info:eu-repo/semantics/article text 2020 ftstockholmuniv https://doi.org/10.1016/j.chemgeo.2019.119380 2023-02-23T21:44:02Z 231Pa, 230Th and 232Th were analyzed in filtered seawater (n=70) and suspended particles (n=39) collectedalong a shelf-basin transect from the Barents shelf to the Makarov Basin in the Arctic Ocean during GEOTRACESsection GN04 in 2015. The distribution of dissolved 231Pa and 230Th in the Arctic Ocean deviates from the linearincrease expected from reversible scavenging. Higher 232Th concentrations were observed at the shelf, slope andin surface waters in the deep basin, pointing at lithogenic sources. Fractionation factors (FTh/Pa) observed at theNansen margin were higher compared to FTh/Pa in the central Nansen Basin, possibly due to the residual occurrenceof hydrothermal particles in the deep central Nansen Basin. Application of a boundary scavengingmodel quantitatively accounts for the dissolved and particulate 230Th distributions in the Nansen Basin.Modelled dissolved 231Pa distributions were largely overestimated, which was attributed to the absence of incorporation of water exchange with the Atlantic Ocean in the model. 231Pa/230Th ratios of the suspended particlesof the Nansen Basin were below the 231Pa/230Th production ratio, but top-core sediments of the Nansenmargin and slope have high 231Pa/230Th-ratios, suggesting that scavenging along the Nansen margin partly actsas a sink for the missing Arctic 231Pa. GEOTRACES Article in Journal/Newspaper Arctic Arctic Ocean makarov basin Nansen Basin Stockholm University: Publications (DiVA) Arctic Arctic Ocean Makarov Basin ENVELOPE(170.000,170.000,87.000,87.000) Chemical Geology 532 119380 |
institution |
Open Polar |
collection |
Stockholm University: Publications (DiVA) |
op_collection_id |
ftstockholmuniv |
language |
English |
topic |
GEOTRACES Protactinium Thorium Arctic Ocean Boundary scavenging Geochemistry Geokemi |
spellingShingle |
GEOTRACES Protactinium Thorium Arctic Ocean Boundary scavenging Geochemistry Geokemi Gdaniec, Sandra Roy-Barman, Matthieu Levier, Martin Valk, Ole van der Loeff, Michiel Rutgers Foliot, Lorna Dapoigny, Arnaud Missiaen, Lise Mörth, Carl-Magnus Andersson, Per S. 231Pa and 230Th in the Arctic Ocean : Implications for boundary scavenging and 231Pa-230Th fractionation in the Eurasian Basin |
topic_facet |
GEOTRACES Protactinium Thorium Arctic Ocean Boundary scavenging Geochemistry Geokemi |
description |
231Pa, 230Th and 232Th were analyzed in filtered seawater (n=70) and suspended particles (n=39) collectedalong a shelf-basin transect from the Barents shelf to the Makarov Basin in the Arctic Ocean during GEOTRACESsection GN04 in 2015. The distribution of dissolved 231Pa and 230Th in the Arctic Ocean deviates from the linearincrease expected from reversible scavenging. Higher 232Th concentrations were observed at the shelf, slope andin surface waters in the deep basin, pointing at lithogenic sources. Fractionation factors (FTh/Pa) observed at theNansen margin were higher compared to FTh/Pa in the central Nansen Basin, possibly due to the residual occurrenceof hydrothermal particles in the deep central Nansen Basin. Application of a boundary scavengingmodel quantitatively accounts for the dissolved and particulate 230Th distributions in the Nansen Basin.Modelled dissolved 231Pa distributions were largely overestimated, which was attributed to the absence of incorporation of water exchange with the Atlantic Ocean in the model. 231Pa/230Th ratios of the suspended particlesof the Nansen Basin were below the 231Pa/230Th production ratio, but top-core sediments of the Nansenmargin and slope have high 231Pa/230Th-ratios, suggesting that scavenging along the Nansen margin partly actsas a sink for the missing Arctic 231Pa. GEOTRACES |
format |
Article in Journal/Newspaper |
author |
Gdaniec, Sandra Roy-Barman, Matthieu Levier, Martin Valk, Ole van der Loeff, Michiel Rutgers Foliot, Lorna Dapoigny, Arnaud Missiaen, Lise Mörth, Carl-Magnus Andersson, Per S. |
author_facet |
Gdaniec, Sandra Roy-Barman, Matthieu Levier, Martin Valk, Ole van der Loeff, Michiel Rutgers Foliot, Lorna Dapoigny, Arnaud Missiaen, Lise Mörth, Carl-Magnus Andersson, Per S. |
author_sort |
Gdaniec, Sandra |
title |
231Pa and 230Th in the Arctic Ocean : Implications for boundary scavenging and 231Pa-230Th fractionation in the Eurasian Basin |
title_short |
231Pa and 230Th in the Arctic Ocean : Implications for boundary scavenging and 231Pa-230Th fractionation in the Eurasian Basin |
title_full |
231Pa and 230Th in the Arctic Ocean : Implications for boundary scavenging and 231Pa-230Th fractionation in the Eurasian Basin |
title_fullStr |
231Pa and 230Th in the Arctic Ocean : Implications for boundary scavenging and 231Pa-230Th fractionation in the Eurasian Basin |
title_full_unstemmed |
231Pa and 230Th in the Arctic Ocean : Implications for boundary scavenging and 231Pa-230Th fractionation in the Eurasian Basin |
title_sort |
231pa and 230th in the arctic ocean : implications for boundary scavenging and 231pa-230th fractionation in the eurasian basin |
publisher |
Stockholms universitet, Institutionen för geologiska vetenskaper |
publishDate |
2020 |
url |
http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-185828 https://doi.org/10.1016/j.chemgeo.2019.119380 |
long_lat |
ENVELOPE(170.000,170.000,87.000,87.000) |
geographic |
Arctic Arctic Ocean Makarov Basin |
geographic_facet |
Arctic Arctic Ocean Makarov Basin |
genre |
Arctic Arctic Ocean makarov basin Nansen Basin |
genre_facet |
Arctic Arctic Ocean makarov basin Nansen Basin |
op_relation |
Chemical Geology, 0009-2541, 2020, 532, orcid:0000-0003-2057-5795 http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-185828 doi:10.1016/j.chemgeo.2019.119380 ISI:000513868400001 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1016/j.chemgeo.2019.119380 |
container_title |
Chemical Geology |
container_volume |
532 |
container_start_page |
119380 |
_version_ |
1766313679926591488 |