鄂霍次克海还原环境中底栖生物微量元素的生物积累

S. Galkin, L. Demina
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引用次数: 1

摘要

对德林金盆地和帕拉希尔岛附近(鄂霍次克海)甲烷渗漏区底栖生物微量元素的生物积累进行了比较研究。这些数据既涉及必需元素(铁、锰、镍、钴、铬和铜),它们在一定浓度下是生物体代谢所必需的,也涉及非必需重金属(镉、铅和汞)以及砷(一种有毒的类金属)。德尤金盆地底栖动物的主要代表(海葵、蛤蜊),无论其生化性质如何,大多数元素的生物积累系数都很高(≥n103)。利用表征双壳类动物相对于其外壳在软组织中微量元素积累的系数K,使我们能够检测到生物积累特性的差异。Deryugin盆地Vesicomyidae共生双壳贝的所有微量元素均以软组织(鳃为主)为主富集(系数K > 1),其原因可能是生境的非生物因素(元素的生物有效性和水体浊度)和生物因素(营养策略)的不同影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Bioaccumulation of Trace Elements in the Organisms of Benthic Communities in the Reducing Environments of the Sea of Okhotsk
A comparative study of the bioaccumulation of trace elements in benthic organisms inhabiting the area of methane seeps in the Deryugin Basin and nearby the Paramushir Island (Sea of Okhotsk) has been performed. The data pertain to both essential elements (Fe, Mn, Ni, Co, Cr, and Cu), which are necessary in certain concentrations for the metabolism of organisms, and nonessential heavy metals (Cd, Pb, and Hg), as well as As, a toxic metalloid. Dominating representatives of the bottom fauna from the Deryugin Basin (sea anemones, clams) were characterized by high bioaccumulation coefficients of most of the elements (≥ n103), regardless of their biochemical properties. The use of the coefficient K, which characterizes the accumulation of trace elements in the soft tissues of bivalves relative to their shells, allowed us to detect differences in the bioaccumulation character. Symbiotrophic bivalves of the family Vesicomyidae from the Deryugin Basin were characterized by the accumulation of all of the trace elements mostly in soft tissues (gills, primarily) compared to the carbonate shells (coefficient K > 1). We suppose that different effect of abiotic (biological availability of elements and water turbidity) and biotic (throphic strategy) factors of the habitats may probably be a reason of such phenomenon.
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