黑海硫代硫酸盐和亚硫酸盐的垂直分布

IF 0.7 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY
M. N. Rimskaya-Korsakova, A. V. Dubinin
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引用次数: 0

摘要

摘要 通过对黑海水柱中的硫代硫酸盐和亚硫酸盐进行单溴比曼衍生化,首次获得了有关其垂直分布的数据。随着硫化氢的出现,硫代硫酸盐和亚硫酸盐在氧化还原界面以下出现了可检测到的数量。在大陆坡上,潜在密度为 16.40-16.80 kg/m3 的海水中亚硫酸盐的浓度达到 1.12 µM,硫代硫酸盐的浓度为 0.53 µM。在深度为 400 米(潜在密度为 16.96 千克/立方米)的深海中,亚硫酸盐和硫代硫酸盐的浓度最大值分别为 1.74 微摩尔和 0.98 微摩尔。对过滤后和未过滤情况下获得的硫代硫酸盐数据进行比较后发现,在厌氧层上部,高达 100%的硫代硫酸盐与浮游细菌有关;其比例在 600 米深处逐渐下降。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Vertical Distribution of Thiosulfate and Sulfite in the Black Sea

Vertical Distribution of Thiosulfate and Sulfite in the Black Sea

Abstract

Data on the vertical distribution of thiosulfate and sulfite by derivatization with monobromobimane in the water column of the Black Sea were obtained for the first time. Thiosulfate and sulfite appeared in detectable quantities below the redox interface along with the appearance of hydrogen sulfide. On the continental slope, the concentration of sulfite reaches 1.12 µM, and that of thiosulfate 0.53 µM in sea water with a potential density of 16.40–16.80 kg/m3. In the deep part of the sea at a depth of 400 m (potential density 16.96 kg/m3), the concentrations of sulfite and thiosulfate reach their maximum values of 1.74 and 0.98 µM, respectively. The comparison of data on thiosulfate obtained after filtration and without filtration showed that in the upper part of the anaerobic layer, up to 100% of thiosulfate is associated with bacterioplankton; its proportion gradually decreases to a depth of 600 m. These data and the correlation with sulfite and particulate organic carbon suggest that, in the upper part of the anaerobic zone, thiosulfate and sulfite obtained as a result of activity of chemoautotrophic bacteria are dominant.

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来源期刊
Doklady Earth Sciences
Doklady Earth Sciences 地学-地球科学综合
CiteScore
1.40
自引率
22.20%
发文量
138
审稿时长
3-6 weeks
期刊介绍: Doklady Earth Sciences is a journal that publishes new research in Earth science of great significance. Initially the journal was a forum of the Russian Academy of Science and published only best contributions from Russia. Now the journal welcomes submissions from any country in the English or Russian language. Every manuscript must be recommended by Russian or foreign members of the Russian Academy of Sciences.
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