Quantifying Ice-Sheet Derived Lead (Pb) Fluxes to the Ocean; A Case Study at Nioghalvfjerdsbræ
Concentrations of the toxic element lead (Pb) are elevated in seawater due to historical emissions. While anthropogenic atmospheric emissions are the dominant source of dissolved Pb (dPb) to the Atlantic Ocean, evidence is emerging of a natural source associated with subglacial discharge into the oc...
Published in: | Geophysical Research Letters |
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Language: | English |
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John Wiley and Sons Inc.
2022
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Online Access: | http://hdl.handle.net/10459.1/84452 https://doi.org/10.1029/2022GL100296 |
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ftunivlleida:oai:repositori.udl.cat:10459.1/84452 2023-05-15T13:15:51+02:00 Quantifying Ice-Sheet Derived Lead (Pb) Fluxes to the Ocean; A Case Study at Nioghalvfjerdsbræ Krisch, Stephan Huhn, Oliver Al-Hashem, Ali Hopwood, Mark J. Lodeiro, Pablo Achterberg, Eric P. 2022-12-02T10:27:10Z http://hdl.handle.net/10459.1/84452 https://doi.org/10.1029/2022GL100296 eng eng John Wiley and Sons Inc. Reproducció del document publicat a https://doi.org/10.1029/2022GL100296 Geophysical Research Letters, 2022, vol. 49, núm. 21, p. 1-13 0094-8276 http://hdl.handle.net/10459.1/84452 https://doi.org/10.1029/2022GL100296 cc-by-nc (c) Krisch et al., 2022 http://creativecommons.org/licenses/by-nc/4.0/ info:eu-repo/semantics/openAccess CC-BY-NC Arctic GEOTRACES Greenland ice sheet Lead fluxes Marine-terminating glacier Nioghalvfjerdsbrae Glaceres Plom info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2022 ftunivlleida https://doi.org/10.1029/2022GL100296 2023-01-18T00:07:25Z Concentrations of the toxic element lead (Pb) are elevated in seawater due to historical emissions. While anthropogenic atmospheric emissions are the dominant source of dissolved Pb (dPb) to the Atlantic Ocean, evidence is emerging of a natural source associated with subglacial discharge into the ocean but this has yet to be constrained around Greenland. Here, we show subglacial discharge from the cavity underneath Nioghalvfjerdsbræ floating ice tongue, is a previously unrecognized source of dPb to the NE Greenland Shelf. Contrasting cavity-inflowing and cavity-outflowing waters, we constrain the associated net-dPb flux as 2.2 ± 1.4 Mg·yr−1, of which ∼90% originates from dissolution of glacial bedrock and cavity sediments. We propose that the retreat of the floating ice tongue, the ongoing retreat of many glaciers on Greenland, associated shifts in sediment dynamics, and enhanced meltwater discharges into shelf waters may result in pronounced changes, possibly increases, in net-dPb fluxes to coastal waters. The authors thank the captain and crew of the RV Polarstern GN05 cruise, operated by the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI). The authors also like to thank Michiel Rutgers van der Loeff (AWI) for his advice upon sampling and ship time management, Takamasa Tsubouchi (University of Bergen, Norway) for the CTD control and Martin Graeve and Kai‐Uwe Ludwichowski (both AWI) who performed the macronutrient analyses. The authors are grateful for the help received from Janin Schaffer (AWI), Florian Evers (GEOMAR), Eike Köhn (GEOMAR), Nat Wilson (Woods Hole Oceanographic Institution), and Gerd Rohardt (AWI) for CTD handling and processing, to Nicola Herzberg, Jaw Chuen Yong for assistance during sampling, and to Tim Steffens (all GEOMAR) for technical assistance during HR‐ICP‐MS analyses. Manuel Colombo (WHOI) is thanked for detailed feedback on this manuscript. Stephan Krisch was financed by GEOMAR and the German Research Foundation (DFG award number . Article in Journal/Newspaper Alfred Wegener Institute Arctic glacier glacier Greenland Ice Sheet Universitat de Lleida: Repositori Obert UdL Arctic Bergen Colombo ENVELOPE(-144.733,-144.733,-76.517,-76.517) Gerd ENVELOPE(-45.750,-45.750,-60.666,-60.666) Greenland Norway Geophysical Research Letters 49 21 |
institution |
Open Polar |
collection |
Universitat de Lleida: Repositori Obert UdL |
op_collection_id |
ftunivlleida |
language |
English |
topic |
Arctic GEOTRACES Greenland ice sheet Lead fluxes Marine-terminating glacier Nioghalvfjerdsbrae Glaceres Plom |
spellingShingle |
Arctic GEOTRACES Greenland ice sheet Lead fluxes Marine-terminating glacier Nioghalvfjerdsbrae Glaceres Plom Krisch, Stephan Huhn, Oliver Al-Hashem, Ali Hopwood, Mark J. Lodeiro, Pablo Achterberg, Eric P. Quantifying Ice-Sheet Derived Lead (Pb) Fluxes to the Ocean; A Case Study at Nioghalvfjerdsbræ |
topic_facet |
Arctic GEOTRACES Greenland ice sheet Lead fluxes Marine-terminating glacier Nioghalvfjerdsbrae Glaceres Plom |
description |
Concentrations of the toxic element lead (Pb) are elevated in seawater due to historical emissions. While anthropogenic atmospheric emissions are the dominant source of dissolved Pb (dPb) to the Atlantic Ocean, evidence is emerging of a natural source associated with subglacial discharge into the ocean but this has yet to be constrained around Greenland. Here, we show subglacial discharge from the cavity underneath Nioghalvfjerdsbræ floating ice tongue, is a previously unrecognized source of dPb to the NE Greenland Shelf. Contrasting cavity-inflowing and cavity-outflowing waters, we constrain the associated net-dPb flux as 2.2 ± 1.4 Mg·yr−1, of which ∼90% originates from dissolution of glacial bedrock and cavity sediments. We propose that the retreat of the floating ice tongue, the ongoing retreat of many glaciers on Greenland, associated shifts in sediment dynamics, and enhanced meltwater discharges into shelf waters may result in pronounced changes, possibly increases, in net-dPb fluxes to coastal waters. The authors thank the captain and crew of the RV Polarstern GN05 cruise, operated by the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI). The authors also like to thank Michiel Rutgers van der Loeff (AWI) for his advice upon sampling and ship time management, Takamasa Tsubouchi (University of Bergen, Norway) for the CTD control and Martin Graeve and Kai‐Uwe Ludwichowski (both AWI) who performed the macronutrient analyses. The authors are grateful for the help received from Janin Schaffer (AWI), Florian Evers (GEOMAR), Eike Köhn (GEOMAR), Nat Wilson (Woods Hole Oceanographic Institution), and Gerd Rohardt (AWI) for CTD handling and processing, to Nicola Herzberg, Jaw Chuen Yong for assistance during sampling, and to Tim Steffens (all GEOMAR) for technical assistance during HR‐ICP‐MS analyses. Manuel Colombo (WHOI) is thanked for detailed feedback on this manuscript. Stephan Krisch was financed by GEOMAR and the German Research Foundation (DFG award number . |
format |
Article in Journal/Newspaper |
author |
Krisch, Stephan Huhn, Oliver Al-Hashem, Ali Hopwood, Mark J. Lodeiro, Pablo Achterberg, Eric P. |
author_facet |
Krisch, Stephan Huhn, Oliver Al-Hashem, Ali Hopwood, Mark J. Lodeiro, Pablo Achterberg, Eric P. |
author_sort |
Krisch, Stephan |
title |
Quantifying Ice-Sheet Derived Lead (Pb) Fluxes to the Ocean; A Case Study at Nioghalvfjerdsbræ |
title_short |
Quantifying Ice-Sheet Derived Lead (Pb) Fluxes to the Ocean; A Case Study at Nioghalvfjerdsbræ |
title_full |
Quantifying Ice-Sheet Derived Lead (Pb) Fluxes to the Ocean; A Case Study at Nioghalvfjerdsbræ |
title_fullStr |
Quantifying Ice-Sheet Derived Lead (Pb) Fluxes to the Ocean; A Case Study at Nioghalvfjerdsbræ |
title_full_unstemmed |
Quantifying Ice-Sheet Derived Lead (Pb) Fluxes to the Ocean; A Case Study at Nioghalvfjerdsbræ |
title_sort |
quantifying ice-sheet derived lead (pb) fluxes to the ocean; a case study at nioghalvfjerdsbræ |
publisher |
John Wiley and Sons Inc. |
publishDate |
2022 |
url |
http://hdl.handle.net/10459.1/84452 https://doi.org/10.1029/2022GL100296 |
long_lat |
ENVELOPE(-144.733,-144.733,-76.517,-76.517) ENVELOPE(-45.750,-45.750,-60.666,-60.666) |
geographic |
Arctic Bergen Colombo Gerd Greenland Norway |
geographic_facet |
Arctic Bergen Colombo Gerd Greenland Norway |
genre |
Alfred Wegener Institute Arctic glacier glacier Greenland Ice Sheet |
genre_facet |
Alfred Wegener Institute Arctic glacier glacier Greenland Ice Sheet |
op_relation |
Reproducció del document publicat a https://doi.org/10.1029/2022GL100296 Geophysical Research Letters, 2022, vol. 49, núm. 21, p. 1-13 0094-8276 http://hdl.handle.net/10459.1/84452 https://doi.org/10.1029/2022GL100296 |
op_rights |
cc-by-nc (c) Krisch et al., 2022 http://creativecommons.org/licenses/by-nc/4.0/ info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY-NC |
op_doi |
https://doi.org/10.1029/2022GL100296 |
container_title |
Geophysical Research Letters |
container_volume |
49 |
container_issue |
21 |
_version_ |
1766271448407605248 |