Tab. 1: Sampling date, location, ice thickness, salinity, Nd isotope compositions and REE concentrations for the sea-ice samples recovered during cruise PS80
Freshwater and sea ice in the Arctic Ocean (AO) both respond to climate forcing but changes in their distribution may in turn also significantly affect Northern Hemisphere climate. The exact mechanisms controlling their transport are, however, still subject of ongoing research. Radiogenic neodymium...
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Format: | Dataset |
Language: | English |
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PANGAEA
2017
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.883658 https://doi.org/10.1594/PANGAEA.883658 |
id |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.883658 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Arctic Ocean ARK-XXVII/3 AWI_SeaIce Cerium dissolved CTD/Rosette CTD-RO Date/Time of event Dysprosium Erbium Europium Event label Gadolinium GEOMAR Heavy rare-earth elements/Light rare-earth elements ratio Helmholtz Centre for Ocean Research Kiel Holmium ICE Ice station Ice station #3 Ice station #4 Ice station #8 incl. ice station Lanthanum Latitude of event Longitude of event Lutetium Neodymium Neodymium-143/Neodymium-144 ratio Normalized Optional event label Polarstern Praseodymium PS80/255-1 PS80/277-1 PS80/336-1 PS80/360-1 PS80 IceArc Salinity Samarium |
spellingShingle |
Arctic Ocean ARK-XXVII/3 AWI_SeaIce Cerium dissolved CTD/Rosette CTD-RO Date/Time of event Dysprosium Erbium Europium Event label Gadolinium GEOMAR Heavy rare-earth elements/Light rare-earth elements ratio Helmholtz Centre for Ocean Research Kiel Holmium ICE Ice station Ice station #3 Ice station #4 Ice station #8 incl. ice station Lanthanum Latitude of event Longitude of event Lutetium Neodymium Neodymium-143/Neodymium-144 ratio Normalized Optional event label Polarstern Praseodymium PS80/255-1 PS80/277-1 PS80/336-1 PS80/360-1 PS80 IceArc Salinity Samarium Laukert, Georgi Frank, Martin Hathorne, Ed C Krumpen, Thomas Rabe, Ben Bauch, Dorothea Werner, Kirstin Peeken, Ilka Kassens, Heidemarie Tab. 1: Sampling date, location, ice thickness, salinity, Nd isotope compositions and REE concentrations for the sea-ice samples recovered during cruise PS80 |
topic_facet |
Arctic Ocean ARK-XXVII/3 AWI_SeaIce Cerium dissolved CTD/Rosette CTD-RO Date/Time of event Dysprosium Erbium Europium Event label Gadolinium GEOMAR Heavy rare-earth elements/Light rare-earth elements ratio Helmholtz Centre for Ocean Research Kiel Holmium ICE Ice station Ice station #3 Ice station #4 Ice station #8 incl. ice station Lanthanum Latitude of event Longitude of event Lutetium Neodymium Neodymium-143/Neodymium-144 ratio Normalized Optional event label Polarstern Praseodymium PS80/255-1 PS80/277-1 PS80/336-1 PS80/360-1 PS80 IceArc Salinity Samarium |
description |
Freshwater and sea ice in the Arctic Ocean (AO) both respond to climate forcing but changes in their distribution may in turn also significantly affect Northern Hemisphere climate. The exact mechanisms controlling their transport are, however, still subject of ongoing research. Radiogenic neodymium (Nd) isotopes (expressed as eNd) and rare earth elements (REEs) have successfully been used to trace ocean circulation in the AO and can provide valuable information on the origin, transport and fate of Arctic freshwater and drifting sea ice. Here, we present first sea-ice data and discuss the applicability of these tracers to determine the pathways of Siberian freshwater and the source areas of Arctic sea ice within the Eurasian Basin. Freshwaters originating from various Siberian rivers are well mixed and diluted prior to their advection to the central AO and the Fram Strait, thereby inhibiting the assessment of the individual contributions of the different rivers for these regions. Recent investigations of seawater Nd isotope and REE distributions on the Siberian shelves now allow for a more detailed determination of the sources of transpolar freshwater transport, and suggest that freshwater from the Lena River can at least be qualitatively traced further away from the shelves. In addition, sea ice has the potential to preserve marine and riverine eNd and REE signatures of the Siberian shelf source waters transported across the AO to the Fram Strait thereby avoiding the effects of mixing. Here, we test this potential for the first time by comparing eNd and REE signatures determined from unfiltered but essentially sediment-free sea-ice samples recovered in the Eurasian Basin of the central AO in 2012 with corresponding signatures of surface seawater in the formation regions of the ice. The sampled sea ice is dominantly characterized by ?Nd values near -8, in agreement with the incorporation of radiogenic freshwater (eNd=-6) from the Yenisei and Ob rivers and its formation east of Vilkitsky Strait as identified by a ... |
format |
Dataset |
author |
Laukert, Georgi Frank, Martin Hathorne, Ed C Krumpen, Thomas Rabe, Ben Bauch, Dorothea Werner, Kirstin Peeken, Ilka Kassens, Heidemarie |
author_facet |
Laukert, Georgi Frank, Martin Hathorne, Ed C Krumpen, Thomas Rabe, Ben Bauch, Dorothea Werner, Kirstin Peeken, Ilka Kassens, Heidemarie |
author_sort |
Laukert, Georgi |
title |
Tab. 1: Sampling date, location, ice thickness, salinity, Nd isotope compositions and REE concentrations for the sea-ice samples recovered during cruise PS80 |
title_short |
Tab. 1: Sampling date, location, ice thickness, salinity, Nd isotope compositions and REE concentrations for the sea-ice samples recovered during cruise PS80 |
title_full |
Tab. 1: Sampling date, location, ice thickness, salinity, Nd isotope compositions and REE concentrations for the sea-ice samples recovered during cruise PS80 |
title_fullStr |
Tab. 1: Sampling date, location, ice thickness, salinity, Nd isotope compositions and REE concentrations for the sea-ice samples recovered during cruise PS80 |
title_full_unstemmed |
Tab. 1: Sampling date, location, ice thickness, salinity, Nd isotope compositions and REE concentrations for the sea-ice samples recovered during cruise PS80 |
title_sort |
tab. 1: sampling date, location, ice thickness, salinity, nd isotope compositions and ree concentrations for the sea-ice samples recovered during cruise ps80 |
publisher |
PANGAEA |
publishDate |
2017 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.883658 https://doi.org/10.1594/PANGAEA.883658 |
op_coverage |
MEDIAN LATITUDE: 84.893501 * MEDIAN LONGITUDE: 102.236715 * SOUTH-BOUND LATITUDE: 82.670670 * WEST-BOUND LONGITUDE: 55.102670 * NORTH-BOUND LATITUDE: 88.827670 * EAST-BOUND LONGITUDE: 130.129500 * DATE/TIME START: 2012-08-20T08:48:00 * DATE/TIME END: 2012-09-23T22:10:00 * MINIMUM ELEVATION: -4374.5 m * MAXIMUM ELEVATION: -3569.0 m |
long_lat |
ENVELOPE(55.102670,130.129500,88.827670,82.670670) |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Arctic Ocean Fram Strait lena river Polarforschung Sea ice |
genre_facet |
Arctic Arctic Arctic Ocean Fram Strait lena river Polarforschung Sea ice |
op_source |
Supplement to: Laukert, Georgi; Frank, Martin; Hathorne, Ed C; Krumpen, Thomas; Rabe, Ben; Bauch, Dorothea; Werner, Kirstin; Peeken, Ilka; Kassens, Heidemarie (2017): Pathways of Siberian freshwater and sea ice in the Arctic Ocean traced with radiogenic Neodymium isotopes and rare earth elements. Polarforschung, 87(1), 3-13, https://doi.org/10.2312/Polarforschung.87.1.3 |
op_relation |
Laukert, Georgi; Frank, Martin; Bauch, Dorothea; Hathorne, Ed C; Rabe, Benjamin; von Appen, Wilken-Jon; Wegner, Carolyn; Zieringer, Moritz; Kassens, Heidemarie (2017): Analysis of Nd isotope, REE and oxygen isotope ratios on water samples across Fram Strait. PANGAEA, https://doi.org/10.1594/PANGAEA.871520 Laukert, Georgi; Frank, Martin; Bauch, Dorothea; Hathorne, Ed C; Rabe, Benjamin; von Appen, Wilken-Jon; Wegner, Carolyn; Zieringer, Moritz; Kassens, Heidemarie (2017): Ocean circulation and freshwater pathways in the Arctic Mediterranean based on a combined Nd isotope, REE and oxygen isotope section across Fram Strait. Geochimica et Cosmochimica Acta, 202, 285-309, https://doi.org/10.1016/j.gca.2016.12.028 https://doi.pangaea.de/10.1594/PANGAEA.883658 https://doi.org/10.1594/PANGAEA.883658 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.883658 https://doi.org/10.2312/Polarforschung.87.1.3 https://doi.org/10.1594/PANGAEA.871520 https://doi.org/10.1016/j.gca.2016.12.028 |
_version_ |
1766301080559288320 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.883658 2023-05-15T14:27:22+02:00 Tab. 1: Sampling date, location, ice thickness, salinity, Nd isotope compositions and REE concentrations for the sea-ice samples recovered during cruise PS80 Laukert, Georgi Frank, Martin Hathorne, Ed C Krumpen, Thomas Rabe, Ben Bauch, Dorothea Werner, Kirstin Peeken, Ilka Kassens, Heidemarie MEDIAN LATITUDE: 84.893501 * MEDIAN LONGITUDE: 102.236715 * SOUTH-BOUND LATITUDE: 82.670670 * WEST-BOUND LONGITUDE: 55.102670 * NORTH-BOUND LATITUDE: 88.827670 * EAST-BOUND LONGITUDE: 130.129500 * DATE/TIME START: 2012-08-20T08:48:00 * DATE/TIME END: 2012-09-23T22:10:00 * MINIMUM ELEVATION: -4374.5 m * MAXIMUM ELEVATION: -3569.0 m 2017-11-30 text/tab-separated-values, 78 data points https://doi.pangaea.de/10.1594/PANGAEA.883658 https://doi.org/10.1594/PANGAEA.883658 en eng PANGAEA Laukert, Georgi; Frank, Martin; Bauch, Dorothea; Hathorne, Ed C; Rabe, Benjamin; von Appen, Wilken-Jon; Wegner, Carolyn; Zieringer, Moritz; Kassens, Heidemarie (2017): Analysis of Nd isotope, REE and oxygen isotope ratios on water samples across Fram Strait. PANGAEA, https://doi.org/10.1594/PANGAEA.871520 Laukert, Georgi; Frank, Martin; Bauch, Dorothea; Hathorne, Ed C; Rabe, Benjamin; von Appen, Wilken-Jon; Wegner, Carolyn; Zieringer, Moritz; Kassens, Heidemarie (2017): Ocean circulation and freshwater pathways in the Arctic Mediterranean based on a combined Nd isotope, REE and oxygen isotope section across Fram Strait. Geochimica et Cosmochimica Acta, 202, 285-309, https://doi.org/10.1016/j.gca.2016.12.028 https://doi.pangaea.de/10.1594/PANGAEA.883658 https://doi.org/10.1594/PANGAEA.883658 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Laukert, Georgi; Frank, Martin; Hathorne, Ed C; Krumpen, Thomas; Rabe, Ben; Bauch, Dorothea; Werner, Kirstin; Peeken, Ilka; Kassens, Heidemarie (2017): Pathways of Siberian freshwater and sea ice in the Arctic Ocean traced with radiogenic Neodymium isotopes and rare earth elements. Polarforschung, 87(1), 3-13, https://doi.org/10.2312/Polarforschung.87.1.3 Arctic Ocean ARK-XXVII/3 AWI_SeaIce Cerium dissolved CTD/Rosette CTD-RO Date/Time of event Dysprosium Erbium Europium Event label Gadolinium GEOMAR Heavy rare-earth elements/Light rare-earth elements ratio Helmholtz Centre for Ocean Research Kiel Holmium ICE Ice station Ice station #3 Ice station #4 Ice station #8 incl. ice station Lanthanum Latitude of event Longitude of event Lutetium Neodymium Neodymium-143/Neodymium-144 ratio Normalized Optional event label Polarstern Praseodymium PS80/255-1 PS80/277-1 PS80/336-1 PS80/360-1 PS80 IceArc Salinity Samarium Dataset 2017 ftpangaea https://doi.org/10.1594/PANGAEA.883658 https://doi.org/10.2312/Polarforschung.87.1.3 https://doi.org/10.1594/PANGAEA.871520 https://doi.org/10.1016/j.gca.2016.12.028 2023-01-20T09:10:02Z Freshwater and sea ice in the Arctic Ocean (AO) both respond to climate forcing but changes in their distribution may in turn also significantly affect Northern Hemisphere climate. The exact mechanisms controlling their transport are, however, still subject of ongoing research. Radiogenic neodymium (Nd) isotopes (expressed as eNd) and rare earth elements (REEs) have successfully been used to trace ocean circulation in the AO and can provide valuable information on the origin, transport and fate of Arctic freshwater and drifting sea ice. Here, we present first sea-ice data and discuss the applicability of these tracers to determine the pathways of Siberian freshwater and the source areas of Arctic sea ice within the Eurasian Basin. Freshwaters originating from various Siberian rivers are well mixed and diluted prior to their advection to the central AO and the Fram Strait, thereby inhibiting the assessment of the individual contributions of the different rivers for these regions. Recent investigations of seawater Nd isotope and REE distributions on the Siberian shelves now allow for a more detailed determination of the sources of transpolar freshwater transport, and suggest that freshwater from the Lena River can at least be qualitatively traced further away from the shelves. In addition, sea ice has the potential to preserve marine and riverine eNd and REE signatures of the Siberian shelf source waters transported across the AO to the Fram Strait thereby avoiding the effects of mixing. Here, we test this potential for the first time by comparing eNd and REE signatures determined from unfiltered but essentially sediment-free sea-ice samples recovered in the Eurasian Basin of the central AO in 2012 with corresponding signatures of surface seawater in the formation regions of the ice. The sampled sea ice is dominantly characterized by ?Nd values near -8, in agreement with the incorporation of radiogenic freshwater (eNd=-6) from the Yenisei and Ob rivers and its formation east of Vilkitsky Strait as identified by a ... Dataset Arctic Arctic Arctic Ocean Fram Strait lena river Polarforschung Sea ice PANGAEA - Data Publisher for Earth & Environmental Science Arctic Arctic Ocean ENVELOPE(55.102670,130.129500,88.827670,82.670670) |