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Fjord water circulation patterns and dysoxic/anoxic conditions in a Mediterranean semi-enclosed embayment in the Amvrakikos Gulf, Greece

机译:希腊Amvrakikos海湾地中海半封闭式海湾中的峡湾水循环模式和缺氧/缺氧条件

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摘要

Oceanographic research in the Amvrakikos Gulf in Western Greece, a semi-enclosed embayment isolated from the Ionian Sea by a narrow, shallow sill, has shown that it is characterised by a fjord-like oceanographic regime. The Gulf is characterised by a well-stratified two layer structure in the water column made up of a surface layer and a bottom layer that are separated by a strong pycnocline. At the entrance over the sill, there is a brackish water outflow in the surface water and a saline water inflow in the near-bed region. This morphology and water circulation pattern makes the Amvrakikos Gulf the only Mediterranean Sea fjord. The investigations have also shown that the surface layer is well oxygenated, whereas in the pycnocline, the dissolved oxygen (DO) declines sharply and finally attains a value of zero, thus dividing the water column into oxic, dysoxic and anoxic environments. At the dysoxic/anoxic interface, at a depth of approximately 35 m, a sharp redox cline develops with Eh values between 0 and 120 mV occurring above and values between 0 and -250 mV occurring below, where oxic and anoxic biochemical processes prevail, respectively. On the seafloor underneath the anoxic waters, a black silt layer and a white mat cover resembling Beggiatoa-like cells are formed. The dysoxic/anoxic conditions appeared during the last 20 to 30 years and have been caused by the excessive use of fertilisers, the increase in animal stocks, intensive fish farming and domestic effluents. The inflicted dysoxia/anoxia has resulted in habitat loss on the seafloor over an area that makes up just over 50% of the total Gulf area and approximately 28% of the total water volume. Furthermore, anoxia is also considered to have been responsible for the sudden fish mortality which occurred in aquaculture rafts in the Gulf in February 2008. Therefore, anoxic conditions can be considered to be a potential hazard to the ecosystem and to the present thriving fishing and mariculture industry in the Gulf.
机译:在希腊西部的Amvrakikos海湾进行的海洋学研究表明,它的特征是类似峡湾的海洋学,它是一个狭窄,浅浅的槛板与爱奥尼亚海隔离开的半封闭式隔离带。海湾的特征是水柱中的层状结构十分分层,由坚固的碧萝oc隔开的表层和底层组成。在窗台上方的入口处,地表水中微咸水流出,近床层区域咸水流入。这种形态和水循环模式使Amvrakikos海湾成为唯一的地中海峡湾。研究还表明,表层被很好地氧化,而在比浓可可林中,溶解氧(DO)急剧下降,最终达到零值,因此将水柱分为有氧,低氧和无氧环境。在约35 m深度的缺氧/缺氧界面上,形成一个尖锐的氧化还原层,Eh值在0至120 mV以上,Eh值在0至-250 mV以下,分别发生有氧和无氧生化过程。 。在缺氧水之下的海底上,形成了类似于泥B样细胞的黑色淤泥层和白色垫层。缺氧/缺氧条件出现在最近的20到30年,其原因是过度使用化肥,动物种群增加,集约化养鱼和生活污水。造成的失调/缺氧已经导致海底栖息地的丧失,该区域的面积仅占海湾地区总面积的50%以上,而水的总面积约为28%。此外,缺氧也被认为是造成2008年2月海湾水产养殖筏中鱼类突然死亡的原因。因此,缺氧条件可被视为对生态系统以及目前蓬勃发展的渔业和海水养殖的潜在危害。海湾工业。

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  • 来源
    《Estuarine Coastal and Shelf Science》 |2010年第4期|p.473-481|共9页
  • 作者单位

    Laboratory of Marine Geology and Physical Oceanography, Department of Geology, University of Patras, Rio Patras 26 500, Greece;

    Laboratory of Marine Geology and Physical Oceanography, Department of Geology, University of Patras, Rio Patras 26 500, Greece;

    Laboratory of Marine Geology and Physical Oceanography, Department of Geology, University of Patras, Rio Patras 26 500, Greece;

    Laboratory of Marine Geology and Physical Oceanography, Department of Geology, University of Patras, Rio Patras 26 500, Greece;

    Laboratory of Marine Geology and Physical Oceanography, Department of Geology, University of Patras, Rio Patras 26 500, Greece;

    Laboratory of Marine Geology and Physical Oceanography, Department of Geology, University of Patras, Rio Patras 26 500, Greece;

    Prefecture of Aitoloakarnania, 30200 Messolonghi, Greece;

    Department of Biology, University of Patras, Rio Patras, Greece;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    oxygen depletion; fjord water circulation; amvrakikos gulf; Greece; mediterranean sea;

    机译:氧耗竭峡湾水循环;阿姆弗拉基科斯海湾希腊;地中海;

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