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坎达湾(一个与白海人工分离的半咸水水体)中的微生物过程。

Microbial processes in the Kanda Bay, a meromictic water body artifically separated from the White Sea.

作者信息

Savvichev A S, Demidenko N A, Krasnova E D, Kalmatskaya O V, Kharcheva A N, Ivanov M V

机构信息

Institute of Microbiology, Academy of Sciences, Moscow, Russia.

State Oceanographic Institute, Moscow, Russia.

出版信息

Dokl Biol Sci. 2017 May;474(1):135-139. doi: 10.1134/S0012496617030103. Epub 2017 Jul 13.

Abstract

Sings of meromixis are found by means of microbiological and biogeochemical investigations in the southernn part of the Kanda Bay, an artificial water body separated front the White Sea with a railway dam. The concentration of oxygen in the bottom layer attained 1.9 mmol/L, intensity of the process of microbial sulfate reduction, 3.0 μmol of sulfur/(L day). The concentration of dissolved methane, 3.7 μmol/L. Isotopic composition of carbon in methane (δC (CH) =-79.2‰) indicates to its microbial genesis. At present, Kanda Bay is a sole in Russia man-made marine water body for which there are data on the rate of microbial processes responsible for formation of bottom water layer containing hydrogen sulfide and methane.

摘要

通过微生物学和生物地球化学调查,在坎达湾南部发现了半混合现象。坎达湾是一个人工水体,通过铁路堤坝与白海隔开。底层的氧气浓度达到1.9毫摩尔/升,微生物硫酸盐还原过程的强度为3.0微摩尔硫/(升·天)。溶解甲烷的浓度为3.7微摩尔/升。甲烷中碳的同位素组成(δC(CH)= -79.2‰)表明其为微生物成因。目前,坎达湾是俄罗斯唯一一个有关于形成含硫化氢和甲烷的底层水层的微生物过程速率数据的人造海水体。

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