Dataset from Evidences of strong sources of DFe and DMn in Ryder Bay, Western Antarctic Peninsula
The spatial distribution, biogeochemical cycling and external sources of dissolved iron and dissolved manganese (DFe and DMn) were investigated in Ryder Bay, a small coastal embayment of the West Antarctic Peninsula, during Austral summer (2013 and 2014). Dissolved concentrations were measured throu...
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The Royal Society
2018
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ftdatacite:10.6084/m9.figshare.6071654.v1 2023-05-15T13:37:52+02:00 Dataset from Evidences of strong sources of DFe and DMn in Ryder Bay, Western Antarctic Peninsula Bown, Johann Haren, Hans Van Meredith, Michael P. Venables, Hugh J. Laan, Patrick J. Alexander Brearley Baar, Hein J. W. De 2018 https://dx.doi.org/10.6084/m9.figshare.6071654.v1 https://rs.figshare.com/articles/Dataset_from_Evidences_of_strong_sources_of_DFe_and_DMn_in_Ryder_Bay_Western_Antarctic_Peninsula/6071654/1 unknown The Royal Society https://dx.doi.org/10.1098/rsta.2017.0172 https://dx.doi.org/10.6084/m9.figshare.6071654 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Geochemistry FOS Earth and related environmental sciences Oceanography dataset Dataset 2018 ftdatacite https://doi.org/10.6084/m9.figshare.6071654.v1 https://doi.org/10.1098/rsta.2017.0172 https://doi.org/10.6084/m9.figshare.6071654 2021-11-05T12:55:41Z The spatial distribution, biogeochemical cycling and external sources of dissolved iron and dissolved manganese (DFe and DMn) were investigated in Ryder Bay, a small coastal embayment of the West Antarctic Peninsula, during Austral summer (2013 and 2014). Dissolved concentrations were measured throughout the water column at 11 stations within Ryder Bay. The concentration ranges of DFe and DMn were large, between 0.58 and 32.7 nM, and between 0.18 and 26.2 nM, respectively, exhibiting strong gradients from the surface to the bottom. Surface concentrations of DFe and DMn were higher than concentrations reported for the Southern Ocean and coastal Antarctic waters, and extremely high concentrations were detected in deep water. Glacial meltwater and shallow sediments are likely to be the main sources of DFe and DMn in the euphotic zone, while lateral advection associated with local sediment resuspension and vertical mixing are significant sources for intermediate and deep waters. During summer, vertical mixing of intermediate and deep waters and sediment resuspension occurring from Marguerite Trough to Ryder Bay are thought to be amplified by a series of overflows at the sills, enhancing the input of Fe and Mn from bottom sediment and increasing their concentrations up to the euphotic layer.This article is part of the theme issue ‘The marine system of the West Antarctic Peninsula: status and strategy for progress in a region of rapid change’. Dataset Antarc* Antarctic Antarctic Peninsula Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Antarctic Antarctic Peninsula Austral Marguerite ENVELOPE(141.378,141.378,-66.787,-66.787) Ryder ENVELOPE(-68.333,-68.333,-67.566,-67.566) Ryder Bay ENVELOPE(-68.333,-68.333,-67.567,-67.567) Southern Ocean |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Geochemistry FOS Earth and related environmental sciences Oceanography |
spellingShingle |
Geochemistry FOS Earth and related environmental sciences Oceanography Bown, Johann Haren, Hans Van Meredith, Michael P. Venables, Hugh J. Laan, Patrick J. Alexander Brearley Baar, Hein J. W. De Dataset from Evidences of strong sources of DFe and DMn in Ryder Bay, Western Antarctic Peninsula |
topic_facet |
Geochemistry FOS Earth and related environmental sciences Oceanography |
description |
The spatial distribution, biogeochemical cycling and external sources of dissolved iron and dissolved manganese (DFe and DMn) were investigated in Ryder Bay, a small coastal embayment of the West Antarctic Peninsula, during Austral summer (2013 and 2014). Dissolved concentrations were measured throughout the water column at 11 stations within Ryder Bay. The concentration ranges of DFe and DMn were large, between 0.58 and 32.7 nM, and between 0.18 and 26.2 nM, respectively, exhibiting strong gradients from the surface to the bottom. Surface concentrations of DFe and DMn were higher than concentrations reported for the Southern Ocean and coastal Antarctic waters, and extremely high concentrations were detected in deep water. Glacial meltwater and shallow sediments are likely to be the main sources of DFe and DMn in the euphotic zone, while lateral advection associated with local sediment resuspension and vertical mixing are significant sources for intermediate and deep waters. During summer, vertical mixing of intermediate and deep waters and sediment resuspension occurring from Marguerite Trough to Ryder Bay are thought to be amplified by a series of overflows at the sills, enhancing the input of Fe and Mn from bottom sediment and increasing their concentrations up to the euphotic layer.This article is part of the theme issue ‘The marine system of the West Antarctic Peninsula: status and strategy for progress in a region of rapid change’. |
format |
Dataset |
author |
Bown, Johann Haren, Hans Van Meredith, Michael P. Venables, Hugh J. Laan, Patrick J. Alexander Brearley Baar, Hein J. W. De |
author_facet |
Bown, Johann Haren, Hans Van Meredith, Michael P. Venables, Hugh J. Laan, Patrick J. Alexander Brearley Baar, Hein J. W. De |
author_sort |
Bown, Johann |
title |
Dataset from Evidences of strong sources of DFe and DMn in Ryder Bay, Western Antarctic Peninsula |
title_short |
Dataset from Evidences of strong sources of DFe and DMn in Ryder Bay, Western Antarctic Peninsula |
title_full |
Dataset from Evidences of strong sources of DFe and DMn in Ryder Bay, Western Antarctic Peninsula |
title_fullStr |
Dataset from Evidences of strong sources of DFe and DMn in Ryder Bay, Western Antarctic Peninsula |
title_full_unstemmed |
Dataset from Evidences of strong sources of DFe and DMn in Ryder Bay, Western Antarctic Peninsula |
title_sort |
dataset from evidences of strong sources of dfe and dmn in ryder bay, western antarctic peninsula |
publisher |
The Royal Society |
publishDate |
2018 |
url |
https://dx.doi.org/10.6084/m9.figshare.6071654.v1 https://rs.figshare.com/articles/Dataset_from_Evidences_of_strong_sources_of_DFe_and_DMn_in_Ryder_Bay_Western_Antarctic_Peninsula/6071654/1 |
long_lat |
ENVELOPE(141.378,141.378,-66.787,-66.787) ENVELOPE(-68.333,-68.333,-67.566,-67.566) ENVELOPE(-68.333,-68.333,-67.567,-67.567) |
geographic |
Antarctic Antarctic Peninsula Austral Marguerite Ryder Ryder Bay Southern Ocean |
geographic_facet |
Antarctic Antarctic Peninsula Austral Marguerite Ryder Ryder Bay Southern Ocean |
genre |
Antarc* Antarctic Antarctic Peninsula Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Southern Ocean |
op_relation |
https://dx.doi.org/10.1098/rsta.2017.0172 https://dx.doi.org/10.6084/m9.figshare.6071654 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.6071654.v1 https://doi.org/10.1098/rsta.2017.0172 https://doi.org/10.6084/m9.figshare.6071654 |
_version_ |
1766098568690532352 |