Dissolved iron measured on water bottle samples during POLARSTERN cruise ANT-XXIV/3 ...
We report a comprehensive dataset of dissolved iron (Fe) comprising 482 values at 22 complete vertical profiles along a 1° latitudinal section at the Zero meridian. In addition a shorter high resolution (~00°09') surface section of the southernmost part of the transect (66°00' - 69°35'...
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ftdatacite:10.1594/pangaea.780271 2024-09-15T17:46:45+00:00 Dissolved iron measured on water bottle samples during POLARSTERN cruise ANT-XXIV/3 ... Klunder, Maarten B Laan, Patrick Middag, Rob de Baar, Hein J W van Ooijen, Jan C 2011 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.780271 https://doi.pangaea.de/10.1594/PANGAEA.780271 en eng PANGAEA https://research.rug.nl/en/publications/distributions-and-sources-of-dissolved-iron-in-the-polar-oceans https://dx.doi.org/10.1016/j.dsr2.2010.10.042 https://research.rug.nl/en/publications/distributions-and-sources-of-dissolved-iron-in-the-polar-oceans Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Date/Time of event Latitude of event Longitude of event Elevation of event DEPTH, water Iron, dissolved Iron, dissolved, standard deviation CTD/Rosette, ultra clean ANT-XXIV/3 Polarstern Global marine biogeochemical cycles of trace elements and their isotopes GEOTRACES International Polar Year 2007-2008 IPY Dataset dataset Supplementary Dataset 2011 ftdatacite https://doi.org/10.1594/pangaea.78027110.1016/j.dsr2.2010.10.042 2024-07-03T13:10:33Z We report a comprehensive dataset of dissolved iron (Fe) comprising 482 values at 22 complete vertical profiles along a 1° latitudinal section at the Zero meridian. In addition a shorter high resolution (~00°09') surface section of the southernmost part of the transect (66°00' - 69°35' S) is presented. Within the upper surface mixed layer the concentrations of dissolved Fe vary between 0.1 and 0.3 nM. An inverse trend versus fluorescence suggests significant Fe removal by plankton blooms. Vertical mixing and upwelling are the most important supply mechanisms of iron from deep waters to the upper surface mixed layer. At lower latitude (42°S) there is a distinct maximum of 0.6-0.7 nM in the 2000-3000 m depth range due to inflow of North Atlantic Deep Water. In one region (55°S) elevated dissolved Fe found in the surface mixed layer is ascribed to the recent deposition of aeolian dust originating from South America. Close to the Antarctic continent there is an indication of Fe supply in surface waters from ... : Data included in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ... Dataset Antarc* Antarctic International Polar Year IPY North Atlantic Deep Water North Atlantic DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Event label Date/Time of event Latitude of event Longitude of event Elevation of event DEPTH, water Iron, dissolved Iron, dissolved, standard deviation CTD/Rosette, ultra clean ANT-XXIV/3 Polarstern Global marine biogeochemical cycles of trace elements and their isotopes GEOTRACES International Polar Year 2007-2008 IPY |
spellingShingle |
Event label Date/Time of event Latitude of event Longitude of event Elevation of event DEPTH, water Iron, dissolved Iron, dissolved, standard deviation CTD/Rosette, ultra clean ANT-XXIV/3 Polarstern Global marine biogeochemical cycles of trace elements and their isotopes GEOTRACES International Polar Year 2007-2008 IPY Klunder, Maarten B Laan, Patrick Middag, Rob de Baar, Hein J W van Ooijen, Jan C Dissolved iron measured on water bottle samples during POLARSTERN cruise ANT-XXIV/3 ... |
topic_facet |
Event label Date/Time of event Latitude of event Longitude of event Elevation of event DEPTH, water Iron, dissolved Iron, dissolved, standard deviation CTD/Rosette, ultra clean ANT-XXIV/3 Polarstern Global marine biogeochemical cycles of trace elements and their isotopes GEOTRACES International Polar Year 2007-2008 IPY |
description |
We report a comprehensive dataset of dissolved iron (Fe) comprising 482 values at 22 complete vertical profiles along a 1° latitudinal section at the Zero meridian. In addition a shorter high resolution (~00°09') surface section of the southernmost part of the transect (66°00' - 69°35' S) is presented. Within the upper surface mixed layer the concentrations of dissolved Fe vary between 0.1 and 0.3 nM. An inverse trend versus fluorescence suggests significant Fe removal by plankton blooms. Vertical mixing and upwelling are the most important supply mechanisms of iron from deep waters to the upper surface mixed layer. At lower latitude (42°S) there is a distinct maximum of 0.6-0.7 nM in the 2000-3000 m depth range due to inflow of North Atlantic Deep Water. In one region (55°S) elevated dissolved Fe found in the surface mixed layer is ascribed to the recent deposition of aeolian dust originating from South America. Close to the Antarctic continent there is an indication of Fe supply in surface waters from ... : Data included in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ... |
format |
Dataset |
author |
Klunder, Maarten B Laan, Patrick Middag, Rob de Baar, Hein J W van Ooijen, Jan C |
author_facet |
Klunder, Maarten B Laan, Patrick Middag, Rob de Baar, Hein J W van Ooijen, Jan C |
author_sort |
Klunder, Maarten B |
title |
Dissolved iron measured on water bottle samples during POLARSTERN cruise ANT-XXIV/3 ... |
title_short |
Dissolved iron measured on water bottle samples during POLARSTERN cruise ANT-XXIV/3 ... |
title_full |
Dissolved iron measured on water bottle samples during POLARSTERN cruise ANT-XXIV/3 ... |
title_fullStr |
Dissolved iron measured on water bottle samples during POLARSTERN cruise ANT-XXIV/3 ... |
title_full_unstemmed |
Dissolved iron measured on water bottle samples during POLARSTERN cruise ANT-XXIV/3 ... |
title_sort |
dissolved iron measured on water bottle samples during polarstern cruise ant-xxiv/3 ... |
publisher |
PANGAEA |
publishDate |
2011 |
url |
https://dx.doi.org/10.1594/pangaea.780271 https://doi.pangaea.de/10.1594/PANGAEA.780271 |
genre |
Antarc* Antarctic International Polar Year IPY North Atlantic Deep Water North Atlantic |
genre_facet |
Antarc* Antarctic International Polar Year IPY North Atlantic Deep Water North Atlantic |
op_relation |
https://research.rug.nl/en/publications/distributions-and-sources-of-dissolved-iron-in-the-polar-oceans https://dx.doi.org/10.1016/j.dsr2.2010.10.042 https://research.rug.nl/en/publications/distributions-and-sources-of-dissolved-iron-in-the-polar-oceans |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.78027110.1016/j.dsr2.2010.10.042 |
_version_ |
1810495108500422656 |