Reversible scavenging and advection – Resolving the neodymium paradox in the South Atlantic
Significant gaps in our understanding of the oceanic cycling of neodymium (Nd) and the other rare earth elements (REEs) remain despite decades of research. One important observation which has not been adequately explained is that the concentration of dissolved Nd typically increases with depth, simi...
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ftunivcam:oai:www.repository.cam.ac.uk:1810/330574 2024-01-21T10:00:44+01:00 Reversible scavenging and advection – Resolving the neodymium paradox in the South Atlantic Wang, R Clegg, JA Scott, PM Larkin, CS Deng, F Thomas, AL Zheng, XY Piotrowski, AM 2021-12-01 application/vnd.openxmlformats-officedocument.wordprocessingml.document application/pdf https://www.repository.cam.ac.uk/handle/1810/330574 https://doi.org/10.17863/CAM.78018 eng eng Elsevier http://dx.doi.org/10.1016/j.gca.2021.09.015 Geochimica et Cosmochimica Acta https://www.repository.cam.ac.uk/handle/1810/330574 doi:10.17863/CAM.78018 Attribution-NonCommercial-NoDerivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/ Neodymium isotopes Neodymium cycling Nd paradox South Atlantic GEOTRACES Article 2021 ftunivcam https://doi.org/10.17863/CAM.78018 2023-12-28T23:22:57Z Significant gaps in our understanding of the oceanic cycling of neodymium (Nd) and the other rare earth elements (REEs) remain despite decades of research. One important observation which has not been adequately explained is that the concentration of dissolved Nd typically increases with depth, similar to nutrient profiles, while Nd isotopes appear to reflect conservative water mass mixing in the intermediate and deep ocean; this has been termed the “Nd paradox”. Here we present a detailed study of the dissolved Nd isotopic composition across a section at 40°S in the South Atlantic, collected by UK GEOTRACES cruise (section GA10). The South Atlantic represents a natural laboratory for our understanding of spatial controls on ocean geochemistry, because of the large variability of inputs, spatial differences in particulate cycling, and horizontal advection and mixing at depth between major northern- and southern-sourced water masses. This variability has also made the South Atlantic a critical region subject to intense investigations that aim at reconstructing past changes in ocean processes, such as changes in biological productivity and deep ocean circulation. Our Nd isotope results from the GA10 section provide observational data show the signal of water mass mixing and reversible scavenging. In the surface ocean (0–600 m), Nd isotopic compositions are distinct between different surface ocean currents and spatially can be tied to various continental sources. In the intermediate ocean (600–2500 m), the vertical Nd isotope distribution exhibits distinct signals of different water masses by horizontal advection, including upper North Atlantic Deep Water and Antarctic Intermediate Water formed in the Atlantic Ocean or the Indian Ocean. The Nd isotope distribution also reflects influence of reversible scavenging that smears the signals downwards in the water column (i.e., offset to more radiogenic values). In the deep ocean below 2500 m, Nd isotope distribution largely follows conservative water mass mixing model. ... Article in Journal/Newspaper Antarc* Antarctic North Atlantic Deep Water North Atlantic Apollo - University of Cambridge Repository Antarctic Indian |
institution |
Open Polar |
collection |
Apollo - University of Cambridge Repository |
op_collection_id |
ftunivcam |
language |
English |
topic |
Neodymium isotopes Neodymium cycling Nd paradox South Atlantic GEOTRACES |
spellingShingle |
Neodymium isotopes Neodymium cycling Nd paradox South Atlantic GEOTRACES Wang, R Clegg, JA Scott, PM Larkin, CS Deng, F Thomas, AL Zheng, XY Piotrowski, AM Reversible scavenging and advection – Resolving the neodymium paradox in the South Atlantic |
topic_facet |
Neodymium isotopes Neodymium cycling Nd paradox South Atlantic GEOTRACES |
description |
Significant gaps in our understanding of the oceanic cycling of neodymium (Nd) and the other rare earth elements (REEs) remain despite decades of research. One important observation which has not been adequately explained is that the concentration of dissolved Nd typically increases with depth, similar to nutrient profiles, while Nd isotopes appear to reflect conservative water mass mixing in the intermediate and deep ocean; this has been termed the “Nd paradox”. Here we present a detailed study of the dissolved Nd isotopic composition across a section at 40°S in the South Atlantic, collected by UK GEOTRACES cruise (section GA10). The South Atlantic represents a natural laboratory for our understanding of spatial controls on ocean geochemistry, because of the large variability of inputs, spatial differences in particulate cycling, and horizontal advection and mixing at depth between major northern- and southern-sourced water masses. This variability has also made the South Atlantic a critical region subject to intense investigations that aim at reconstructing past changes in ocean processes, such as changes in biological productivity and deep ocean circulation. Our Nd isotope results from the GA10 section provide observational data show the signal of water mass mixing and reversible scavenging. In the surface ocean (0–600 m), Nd isotopic compositions are distinct between different surface ocean currents and spatially can be tied to various continental sources. In the intermediate ocean (600–2500 m), the vertical Nd isotope distribution exhibits distinct signals of different water masses by horizontal advection, including upper North Atlantic Deep Water and Antarctic Intermediate Water formed in the Atlantic Ocean or the Indian Ocean. The Nd isotope distribution also reflects influence of reversible scavenging that smears the signals downwards in the water column (i.e., offset to more radiogenic values). In the deep ocean below 2500 m, Nd isotope distribution largely follows conservative water mass mixing model. ... |
format |
Article in Journal/Newspaper |
author |
Wang, R Clegg, JA Scott, PM Larkin, CS Deng, F Thomas, AL Zheng, XY Piotrowski, AM |
author_facet |
Wang, R Clegg, JA Scott, PM Larkin, CS Deng, F Thomas, AL Zheng, XY Piotrowski, AM |
author_sort |
Wang, R |
title |
Reversible scavenging and advection – Resolving the neodymium paradox in the South Atlantic |
title_short |
Reversible scavenging and advection – Resolving the neodymium paradox in the South Atlantic |
title_full |
Reversible scavenging and advection – Resolving the neodymium paradox in the South Atlantic |
title_fullStr |
Reversible scavenging and advection – Resolving the neodymium paradox in the South Atlantic |
title_full_unstemmed |
Reversible scavenging and advection – Resolving the neodymium paradox in the South Atlantic |
title_sort |
reversible scavenging and advection – resolving the neodymium paradox in the south atlantic |
publisher |
Elsevier |
publishDate |
2021 |
url |
https://www.repository.cam.ac.uk/handle/1810/330574 https://doi.org/10.17863/CAM.78018 |
geographic |
Antarctic Indian |
geographic_facet |
Antarctic Indian |
genre |
Antarc* Antarctic North Atlantic Deep Water North Atlantic |
genre_facet |
Antarc* Antarctic North Atlantic Deep Water North Atlantic |
op_relation |
https://www.repository.cam.ac.uk/handle/1810/330574 doi:10.17863/CAM.78018 |
op_rights |
Attribution-NonCommercial-NoDerivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/ |
op_doi |
https://doi.org/10.17863/CAM.78018 |
_version_ |
1788703487800901632 |