Cristin-resultat-ID: 1162545
Sist endret: 15. juni 2018, 16:39
NVI-rapporteringsår: 2014
Resultat
Vitenskapelig artikkel
2014

Biogeochemical consequences of an oxygenated intrusion into an anoxic fjord

Bidragsytere:
  • Svetlana Pakhomova
  • Hans Fredrik Veiteberg Braaten
  • Evgeny Yakushev og
  • Jens Skei

Tidsskrift

Geochemical Transactions
ISSN 1467-4866
e-ISSN 1467-4866
NVI-nivå 1

Om resultatet

Vitenskapelig artikkel
Publiseringsår: 2014
Volum: 15
Hefte: 1
Open Access

Importkilder

Scopus-ID: 2-s2.0-84901608233

Beskrivelse Beskrivelse

Tittel

Biogeochemical consequences of an oxygenated intrusion into an anoxic fjord

Sammendrag

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.

Bidragsytere

Svetlana Pakhomova

  • Tilknyttet:
    Forfatter
    ved P.P. Shirshov Instiute of Oceanology

Hans Fredrik Veiteberg Braaten

  • Tilknyttet:
    Forfatter
    ved Akvatiske miljøgifter ved Norsk institutt for vannforskning
  • Tilknyttet:
    Forfatter
    ved Kjemisk institutt ved Universitetet i Oslo

Evgeniy Yakushev

Bidragsyterens navn vises på dette resultatet som Evgeny Yakushev
  • Tilknyttet:
    Forfatter
    ved Marin biogeokjemi og oseanografi ved Norsk institutt for vannforskning
  • Tilknyttet:
    Forfatter
    ved P.P. Shirshov Instiute of Oceanology

Jens Skei

  • Tilknyttet:
    Forfatter
    ved Marin forurensning ved Norsk institutt for vannforskning
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