Potential Sources of Particulate Iron in Surface and Deep Waters of the Terra Nova Bay (Ross Sea, Antarctica)

The distribution of particulate Fe (pFe), suspended particulate matter (SPM), and other particulate trace metals were investigated in Terra Nova Bay as part of CDW Effects on glaciaL mElting and on Bulk of Fe in the Western Ross sea (CELEBeR) and Plankton biodiversity and functioning of the Ross Sea...

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Published in:Water
Main Authors: Paola Rivaro, Francisco Ardini, Davide Vivado, Roberto Cabella, Pasquale Castagno, Olga Mangoni, Pierpaolo Falco
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
Online Access:https://doi.org/10.3390/w12123517
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spelling ftmdpi:oai:mdpi.com:/2073-4441/12/12/3517/ 2023-08-20T04:02:23+02:00 Potential Sources of Particulate Iron in Surface and Deep Waters of the Terra Nova Bay (Ross Sea, Antarctica) Paola Rivaro Francisco Ardini Davide Vivado Roberto Cabella Pasquale Castagno Olga Mangoni Pierpaolo Falco agris 2020-12-14 application/pdf https://doi.org/10.3390/w12123517 EN eng Multidisciplinary Digital Publishing Institute Oceans and Coastal Zones https://dx.doi.org/10.3390/w12123517 https://creativecommons.org/licenses/by/4.0/ Water; Volume 12; Issue 12; Pages: 3517 iron suspended particulate matter antarctica ross sea Text 2020 ftmdpi https://doi.org/10.3390/w12123517 2023-08-01T00:39:58Z The distribution of particulate Fe (pFe), suspended particulate matter (SPM), and other particulate trace metals were investigated in Terra Nova Bay as part of CDW Effects on glaciaL mElting and on Bulk of Fe in the Western Ross sea (CELEBeR) and Plankton biodiversity and functioning of the Ross Sea ecosystems in a changing Southern Ocean (P-ROSE) projects. Variable concentrations of SPM (0.09–97 mg L−1), pFe (0.51–8.70 nM) and other trace metals were found in the Antarctic Surface waters (AASW) layer, where the addition of meltwater contributed to the pool with both lithogenic and biogenic forms. The deeper layer of the water column was occupied by High Salinity Shelf Water (HSSW) and Terra Nova Bay Ice Shelf Water (TISW) encompassing glacial water as confirmed by the lightest δ18O measured values. The concentration of pFe in TISW (11.7 ± 9.2 nM) was higher than in HSSW samples (5.55 ± 4.43 nM), suggesting that the drainage of material released from glaciers surrounding the area is relevant in terms of pFe contribution. Particulate Fe/Al and Mn/Al ratios were substantially in excess compared with the mean crustal ratios. Microscopic analyses confirmed that more labile Fe oxyhydroxides and authigenic MnO2 phases were present together with biogenic sinking material. Future expected increasing melt rates of these glaciers enlarge Fe input, thus having a greater role in supplying iron and counteracting the reductions in sea ice cover around Terra Nova Bay. Text Antarc* Antarctic Antarctica Ice Shelf Ross Sea Sea ice Southern Ocean MDPI Open Access Publishing Antarctic Ross Sea Southern Ocean Terra Nova Bay The Antarctic Water 12 12 3517
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic iron
suspended particulate matter
antarctica
ross sea
spellingShingle iron
suspended particulate matter
antarctica
ross sea
Paola Rivaro
Francisco Ardini
Davide Vivado
Roberto Cabella
Pasquale Castagno
Olga Mangoni
Pierpaolo Falco
Potential Sources of Particulate Iron in Surface and Deep Waters of the Terra Nova Bay (Ross Sea, Antarctica)
topic_facet iron
suspended particulate matter
antarctica
ross sea
description The distribution of particulate Fe (pFe), suspended particulate matter (SPM), and other particulate trace metals were investigated in Terra Nova Bay as part of CDW Effects on glaciaL mElting and on Bulk of Fe in the Western Ross sea (CELEBeR) and Plankton biodiversity and functioning of the Ross Sea ecosystems in a changing Southern Ocean (P-ROSE) projects. Variable concentrations of SPM (0.09–97 mg L−1), pFe (0.51–8.70 nM) and other trace metals were found in the Antarctic Surface waters (AASW) layer, where the addition of meltwater contributed to the pool with both lithogenic and biogenic forms. The deeper layer of the water column was occupied by High Salinity Shelf Water (HSSW) and Terra Nova Bay Ice Shelf Water (TISW) encompassing glacial water as confirmed by the lightest δ18O measured values. The concentration of pFe in TISW (11.7 ± 9.2 nM) was higher than in HSSW samples (5.55 ± 4.43 nM), suggesting that the drainage of material released from glaciers surrounding the area is relevant in terms of pFe contribution. Particulate Fe/Al and Mn/Al ratios were substantially in excess compared with the mean crustal ratios. Microscopic analyses confirmed that more labile Fe oxyhydroxides and authigenic MnO2 phases were present together with biogenic sinking material. Future expected increasing melt rates of these glaciers enlarge Fe input, thus having a greater role in supplying iron and counteracting the reductions in sea ice cover around Terra Nova Bay.
format Text
author Paola Rivaro
Francisco Ardini
Davide Vivado
Roberto Cabella
Pasquale Castagno
Olga Mangoni
Pierpaolo Falco
author_facet Paola Rivaro
Francisco Ardini
Davide Vivado
Roberto Cabella
Pasquale Castagno
Olga Mangoni
Pierpaolo Falco
author_sort Paola Rivaro
title Potential Sources of Particulate Iron in Surface and Deep Waters of the Terra Nova Bay (Ross Sea, Antarctica)
title_short Potential Sources of Particulate Iron in Surface and Deep Waters of the Terra Nova Bay (Ross Sea, Antarctica)
title_full Potential Sources of Particulate Iron in Surface and Deep Waters of the Terra Nova Bay (Ross Sea, Antarctica)
title_fullStr Potential Sources of Particulate Iron in Surface and Deep Waters of the Terra Nova Bay (Ross Sea, Antarctica)
title_full_unstemmed Potential Sources of Particulate Iron in Surface and Deep Waters of the Terra Nova Bay (Ross Sea, Antarctica)
title_sort potential sources of particulate iron in surface and deep waters of the terra nova bay (ross sea, antarctica)
publisher Multidisciplinary Digital Publishing Institute
publishDate 2020
url https://doi.org/10.3390/w12123517
op_coverage agris
geographic Antarctic
Ross Sea
Southern Ocean
Terra Nova Bay
The Antarctic
geographic_facet Antarctic
Ross Sea
Southern Ocean
Terra Nova Bay
The Antarctic
genre Antarc*
Antarctic
Antarctica
Ice Shelf
Ross Sea
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Antarctica
Ice Shelf
Ross Sea
Sea ice
Southern Ocean
op_source Water; Volume 12; Issue 12; Pages: 3517
op_relation Oceans and Coastal Zones
https://dx.doi.org/10.3390/w12123517
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/w12123517
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