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

被引:47
|
作者
Ferentinos, George [1 ]
Papatheodorou, George [1 ]
Geraga, Maria [1 ]
Iatrou, Margarita [1 ]
Fakiris, Elias [1 ]
Christodoulou, Dimitris [1 ]
Dimitriou, Evagelos [2 ]
Koutsikopoulos, Constantin [3 ]
机构
[1] Univ Patras, Dept Geol, Lab Marine Geol & Phys Oceanog, Rion 26500, Greece
[2] Prefecture Aitoloakarnania, Mesolongion 30200, Greece
[3] Univ Patras, Dept Biol, Rion 26500, Greece
关键词
oxygen depletion; Fjord water circulation; Amvrakikos gulf; Greece; Mediterranean sea; IONIAN SEA; ESTUARINE; SEDIMENTS; HOLOCENE;
D O I
10.1016/j.ecss.2010.05.006
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
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 dine 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. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:473 / 481
页数:9
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