Biogeochemical consequences of an oxygenated intrusion into an anoxic fjord

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Geochemical Transactions Pub Date : 2014-04-28 DOI:10.1186/1467-4866-15-5
Svetlana Pakhomova, Hans Fredrik Veiteberg Braaten, Evgeniy Yakushev, Jens Skei
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引用次数: 13

Abstract

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.

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.

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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含氧入侵缺氧峡湾的生物地球化学后果
本文基于2009年、2011年和2012年对挪威东南部贫氧峡湾Hunnbunn水柱生物地球化学结构的研究。这个峡湾是一个封闭的咸淡水盆地,由一个狭窄而浅的出口与一个永久缺氧层隔开。我们展示了由于生物地球化学结构的变化,含氧入侵如何对Hunnbunn的生态系统状态产生积极和消极的影响。在2009年和2012年的分层期间,缺氧层约占峡湾总水量的10%,而溶解氧(DO)则存在于80-90%的水中。2011年秋季,Hunnbunn峡湾观测到的水化学结构明显受到最近一次含氧入侵的影响,这种入侵由异常盐度模式定义。这导致DO边界位置向较浅深度移动,导致缺氧层较厚,约占总水量的40%,而DO仅存在于约60%的水中。含氧水的侵入导致深层硫化氢、氨、磷酸盐和硅酸盐的浓度降低了两倍,同时这些营养物质的浓度增加,表层pH值降低。锰、铁和汞种类的浓度发生了巨大变化,特别是表明向水柱提供了大量的铁和甲基汞。含氧水侵入缺氧峡湾不仅会导致底部缺氧的冲刷,还会导致硫化物和低氧条件向更大的底部区域扩散。硫化氢上升到较浅层(可迅速氧化)的同时,在地下水中出现甲基汞,甲基汞很容易被生物体积累,并可运输到周围水域,影响更大范围的生态系统。
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来源期刊
Geochemical Transactions
Geochemical Transactions 地学-地球化学与地球物理
CiteScore
3.70
自引率
4.30%
发文量
2
审稿时长
>12 weeks
期刊介绍: Geochemical Transactions publishes high-quality research in all areas of chemistry as it relates to materials and processes occurring in terrestrial and extraterrestrial systems.
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