巴伦支海和鄂霍次克海流域河流中粉红鲑鱼的微量元素含量

Pub Date : 2023-12-29 DOI:10.1134/s2075111723040070
N. K. Khristoforova, A. V. Litvinenko, M. Yu. Alekseev, V. Yu. Tsygankov
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引用次数: 0

摘要

摘要测定了2019年7月流入巴伦支海的科拉半岛科拉河和图洛马河产卵的入侵粉鲑体内铅、镉、镍、铜和锌的浓度。将引入俄罗斯欧洲-北极水域的粉鲑器官和组织中的微量元素含量与2016-2018年返回萨哈林岛和伊图鲁普岛河流产卵的原产地粉鲑的微量元素含量进行了比较。结果表明,锌、铜和镍的浓度在引进的粉鲑的所有器官和组织中明显占优势,而铅和镉在鄂霍次克海粉鲑中占优势。显然,鱼体内微量元素组成的差异是由环境条件造成的。在巴伦支海,微量元素是在墨西哥湾流的影响下形成的,同时也受到科拉半岛人为因素的影响,科拉半岛的特点是提取、加工和冶炼多种金属,主要是镍和铜以及锌。在萨哈林-库里尔盆地,环境的特殊性和鲑鱼的微量元素组成是由于自然因素--火山和上升流--的影响。粉鲑鱼群在太平洋觅食和洄游时,会穿过一个由千岛海脊和千岛-堪察加洼地形成的高营养、同时具有地球化学影响的自然区域,该区域为地表水提供化学元素。在这里,鱼类体内铅的浓度增加最为明显。最近,北大西洋水域温度升高,促进了引进的粉鲑在新地区的发展,因此这里的鱼类产量将会增加。掌握粉鲑在新的觅食地的情况,摆在科学家面前的任务是监测其数量动态,并采取适当措施进行渔业管理和鱼类质量控制。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Trace Element Сontent in the Pink Salmon from the Rivers of the Basins of the Barents Sea and Sea of Okhotsk

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Trace Element Сontent in the Pink Salmon from the Rivers of the Basins of the Barents Sea and Sea of Okhotsk

Abstract

The concentrations of Pb, Cd, Ni, Cu, and Zn were determined in the invasive pink salmon that came to spawn into the Kola and Tuloma rivers of the Kola Peninsula, flowing into the Barents Sea, in July 2019. The content of trace elements in the organs and tissues of pink salmon introduced in the Euro-Arctic waters of Russia was compared to those of the pink salmon from its native range, which returned to spawn in the rivers of the Sakhalin and Iturup islands in 2016–2018. It has been established that concentrations of Zn, Cu, and Ni noticeably predominate in all organs and tissues of introduced pink salmon, whereas Pb and Cd predominate in the Sea of Okhotsk pink salmon. Obviously, the differences in the microelement composition in fish are caused by environmental conditions. In the Barents Sea, they are formed under the influence of the Gulf Stream, as well as the anthropogenic impact of the Kola Peninsula, which is characterized by the extraction, processing, and smelting of a number of metals, primarily Ni and Cu, as well as Zn. In the Sakhalin-Kuril basin, the specificity of the environment and the microelement composition of salmon are due to the influence of natural factors—volcanism and upwellings. Schools of pink salmon during feeding and migration in the Pacific Ocean cross a high-nutrient and at the same time geochemically impact natural zone formed by the Kuril Ridge and the Kuril-Kamchatka Depression, which supplies chemical elements to surface waters. Here, the concentration of Pb is most markedly increased in fish. The development of the introduced pink salmon in the new area is facilitated by the recent increase in temperature in the waters of the North Atlantic, so the amount of fish production in it will increase. The mastering of pink salmon in new feeding places sets before scientists the task of monitoring the dynamics of its abundance and taking adequate measures for fishery regulation and fish quality control.

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