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首页> 外文期刊>Quaternary International >The political decision caused the drastic ecosystem shift of the Sivash Bay (the Sea of Azov)
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The political decision caused the drastic ecosystem shift of the Sivash Bay (the Sea of Azov)

机译:政治决策导致Sivash湾(亚速海)的生态系统发生了剧烈变化

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摘要

Political and economic decisions have led to more drastic changes of aquatic ecosystems, than those caused by hydrological extremes (drought, floods). Examples of this are two transformations of the Sivash Bay (Sea of Azov); a review and analyses of them are given in the paper. Sivash Bay was a hypersaline lagoon before 1963. The North Crimean Canal was built to improve water supply to the Crimean peninsula by using the waters of the Dnieper River. After the initiation of Dnieper water via the North Crimean Canal and the subsequent development of irrigated agriculture, runoff waters from the fields began draining into Bay Sivash. The salinity began to drop. Pre 1997 the average salinity in Sivash Bay was 140 g L-1; in 1997 it had dropped to 17 g L-1. A fundamentally new brackish water ecosystem gradually formed in Sivash Bay. In April 2014, Ukraine made a political decision to stop supplying Dnieper water via the North Crimean Canal. Discharge of fresh water to the bay almost ceased. Salinity began to increase, and a new transformation of the Sivash ecosystem started. Six complex expeditions were conducted in the Sivash region; their results are described and analyzed in the article. The salinity of the lagoon has now risen to 55-75 g L-1, and drastic changes have occurred in the plankton, benthos, and aquatic vegetation. (C) 2017 Elsevier Ltd and INQUA. All rights reserved.
机译:政治和经济决策导致的水生生态系统变化比水文极端事件(干旱,洪水)造成的变化更为剧烈。这方面的例子是Sivash湾(亚速海)的两次改造。本文对此进行了回顾和分析。西瓦什湾(Sivash Bay)是1963年之前的高盐湖。北克里米亚运河的建造是为了利用第聂伯河的水改善克里米亚半岛的供水。在通过北克里米亚运河启动第聂伯河水和随后的灌溉农业发展之后,田间的径流水开始排入Sivash湾。盐度开始下降。 1997年之前,Sivash湾的平均盐度为140 g L-1;在1997年,它降至17 g L-1。西瓦什湾逐渐形成了一个全新的咸淡水生态系统。 2014年4月,乌克兰作出了一项政治决定,决定停止通过北克里米亚运河供水第聂伯河。向海湾的淡水排放几乎停止了。盐度开始增加,Sivash生态系统开始了新的转型。在Sivash地区进行了六次复杂的探险;他们的结果在文章中进行了描述和分析。泻湖的盐度现已升至55-75 g L-1,浮游生物,底栖生物和水生植物发生了剧烈变化。 (C)2017爱思唯尔有限公司和INQUA。版权所有。

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