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Biogeochemical consequences of an oxygenated intrusion into an anoxic fjord

BACKGROUND: This paper is based on the studies of the biogeochemical structure of the water column in the anoxic Fjord Hunnbunn (south-eastern Norway) performed in 2009, 2011 and 2012. This Fjord is an enclosed basin of brackish water separated by a narrow and shallow outlet to the sea with a perman...

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Autores principales: Pakhomova, Svetlana, Braaten, Hans Fredrik Veiteberg, Yakushev, Evgeniy, Skei, Jens
Formato: Online Artículo Texto
Lenguaje:English
Publicado: BioMed Central 2014
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4036391/
https://www.ncbi.nlm.nih.gov/pubmed/24872727
http://dx.doi.org/10.1186/1467-4866-15-5
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author Pakhomova, Svetlana
Braaten, Hans Fredrik Veiteberg
Yakushev, Evgeniy
Skei, Jens
author_facet Pakhomova, Svetlana
Braaten, Hans Fredrik Veiteberg
Yakushev, Evgeniy
Skei, Jens
author_sort Pakhomova, Svetlana
collection PubMed
description BACKGROUND: This paper is based on the studies of the biogeochemical structure of the water column in the anoxic Fjord Hunnbunn (south-eastern Norway) performed in 2009, 2011 and 2012. This Fjord is an enclosed basin of brackish water separated by a narrow and shallow outlet to the sea with a permanently anoxic layer. We show how an oxygenated intrusion could lead to both positive and negative effects on the ecosystem state in Hunnbunn due to a change in the biogeochemical structure. RESULTS: During the stratified periods in 2009 and 2012 the anoxic layer amounted to approximately 10% of the total water volume in the Fjord, while dissolved oxygen (DO) was present in 80-90% of the water. In the autumn of 2011 the water chemistry structure observed in Fjord Hunnbunn was clearly affected by a recent oxygenated intrusion defined by abnormal salinity patterns. This led to a shift of the DO boundary position to shallower depths, resulting in a thicker anoxic layer comprising approximately 40% of the total water volume, with DO present only in approximately 60% of the water. The oxygenated water intrusions led to a twofold decrease of the concentrations of hydrogen sulphide, ammonia, phosphate and silicate in the deep layers with a simultaneous increase of these nutrients and a decrease of the pH level in the surface layers. The concentrations of manganese, iron, and mercury species changed dramatically and in particular revealed a significant supply of iron and methylmercury to the water column. CONCLUSIONS: Oxic water intrusions into anoxic fjords could lead not only to the flushing of the bottom anoxia, but to a dispersal of sulphidic and low oxygen conditions to the larger bottom area. The elevation of the hydrogen sulphide to the shallower layers (that can be rapidly oxidized) is accompanied by the appearance in the subsurface water of methylmercury, which is easily accumulated by organisms and can be transported to the surrounding waters, affecting the ecosystem over a larger area.
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spelling pubmed-40363912014-05-29 Biogeochemical consequences of an oxygenated intrusion into an anoxic fjord Pakhomova, Svetlana Braaten, Hans Fredrik Veiteberg Yakushev, Evgeniy Skei, Jens Geochem Trans Research Article BACKGROUND: This paper is based on the studies of the biogeochemical structure of the water column in the anoxic Fjord Hunnbunn (south-eastern Norway) performed in 2009, 2011 and 2012. This Fjord is an enclosed basin of brackish water separated by a narrow and shallow outlet to the sea with a permanently anoxic layer. We show how an oxygenated intrusion could lead to both positive and negative effects on the ecosystem state in Hunnbunn due to a change in the biogeochemical structure. RESULTS: During the stratified periods in 2009 and 2012 the anoxic layer amounted to approximately 10% of the total water volume in the Fjord, while dissolved oxygen (DO) was present in 80-90% of the water. In the autumn of 2011 the water chemistry structure observed in Fjord Hunnbunn was clearly affected by a recent oxygenated intrusion defined by abnormal salinity patterns. This led to a shift of the DO boundary position to shallower depths, resulting in a thicker anoxic layer comprising approximately 40% of the total water volume, with DO present only in approximately 60% of the water. The oxygenated water intrusions led to a twofold decrease of the concentrations of hydrogen sulphide, ammonia, phosphate and silicate in the deep layers with a simultaneous increase of these nutrients and a decrease of the pH level in the surface layers. The concentrations of manganese, iron, and mercury species changed dramatically and in particular revealed a significant supply of iron and methylmercury to the water column. CONCLUSIONS: Oxic water intrusions into anoxic fjords could lead not only to the flushing of the bottom anoxia, but to a dispersal of sulphidic and low oxygen conditions to the larger bottom area. The elevation of the hydrogen sulphide to the shallower layers (that can be rapidly oxidized) is accompanied by the appearance in the subsurface water of methylmercury, which is easily accumulated by organisms and can be transported to the surrounding waters, affecting the ecosystem over a larger area. BioMed Central 2014-04-28 /pmc/articles/PMC4036391/ /pubmed/24872727 http://dx.doi.org/10.1186/1467-4866-15-5 Text en Copyright © 2014 Pakhomova et al.; licensee BioMed Central Ltd. http://creativecommons.org/licenses/by/2.0 This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated.
spellingShingle Research Article
Pakhomova, Svetlana
Braaten, Hans Fredrik Veiteberg
Yakushev, Evgeniy
Skei, Jens
Biogeochemical consequences of an oxygenated intrusion into an anoxic fjord
title Biogeochemical consequences of an oxygenated intrusion into an anoxic fjord
title_full Biogeochemical consequences of an oxygenated intrusion into an anoxic fjord
title_fullStr Biogeochemical consequences of an oxygenated intrusion into an anoxic fjord
title_full_unstemmed Biogeochemical consequences of an oxygenated intrusion into an anoxic fjord
title_short Biogeochemical consequences of an oxygenated intrusion into an anoxic fjord
title_sort biogeochemical consequences of an oxygenated intrusion into an anoxic fjord
topic Research Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4036391/
https://www.ncbi.nlm.nih.gov/pubmed/24872727
http://dx.doi.org/10.1186/1467-4866-15-5
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