Vertical distribution of thiosulfate and sulfite in the Black Sea
- 作者: Rimskaya-Korsakova M.N.1, Dubinin A.V.1
-
隶属关系:
- Shirshov Institute оf Oceanology, Russian Academy of Sciences
- 期: 卷 517, 编号 1 (2024)
- 页面: 61-67
- 栏目: GEOCHEMISTRY
- ##submission.dateSubmitted##: 31.01.2025
- ##submission.datePublished##: 13.12.2024
- URL: https://edgccjournal.org/2686-7397/article/view/650002
- DOI: https://doi.org/10.31857/S2686739724070076
- ID: 650002
如何引用文章
详细
We obtained the data on the vertical distribution of thiosulfate and sulfite by derivatization with monobromobimane in the water column of the Black Sea 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 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 of 1.74 µM and 0.98 µM, respectively. A comparison of data on thiosulfate obtained after filtration and without filtration showed that in the upper part of the anoxic layer, up to 100% of thiosulfate is associated with bacterioplankton. Microbial bound thiosulfate in the cell 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 anoxic zone, thiosulfate and sulfite are predominantly a result of the activity of chemoautotrophic bacteria.
全文:

作者简介
M. Rimskaya-Korsakova
Shirshov Institute оf Oceanology, Russian Academy of Sciences
编辑信件的主要联系方式.
Email: korsakova@ocean.ru
俄罗斯联邦, Moscow
A. Dubinin
Shirshov Institute оf Oceanology, Russian Academy of Sciences
Email: korsakova@ocean.ru
俄罗斯联邦, Moscow
参考
- Дубинин А. В., Демидова Т. П., Римская-Корсакова М. Н. и др. Определение восстановленных форм серы в воде анаэробных бассейнов // Морской гидрофизический журнал. 2019. Т. 35. № 1. С. 37–51. doi: 10.22449/0233-7584-2019-1-37-51.
- Дубинин А. В., Римская-Корсакова М. Н., Очередник О. А., Пахомова С. В. Тиосульфат в верхней части анаэробной зоны Чёрного моря // Океанология. 2023. Т. 63. № 3. С. 382–391.
- Dellwig O., Leipe T., März et al. A new particulate Mn-Fe-P-shuttle at the redoxcline of anoxic basins // Geochim. Cosmochim. Acta. 2010. V. 74. P. 7100–7115.
- Findlay A. J., Kamyshny A. Turnover Rates of Intermediate Sulfur Species (Sx2− , S0, S2O32−, S4O62−, SO32−) in Anoxic Freshwater and Sediments // Front. Microbiol. 2017. V. 8. P. 2551. doi: 10.3389/fmicb.2017.02551.
- Jørgensen B. B., Fossing H., Wirsen C. O. et al. Sulfide oxidation in the anoxic Black Sea chemocline // Deep-Sea Res. 1991. V. 38. № 2. S1083-S1103.
- Hayes M. K., Taylor G. T., Astor Y., Scranton M. I. Vertical distributions of thiosulfate and sulfite in the Cariaco Basin // Limnol. Oceanogr. 2006. V. 51. № 1. P. 280–287.
- Henkel J. V., Schulz-Vogt H. N., Dellwig O. et al. Biological manganese –dependent sulfide oxidation impacts elemental gradients in redox-stratified systems: indications from the Black Sea water column // ISME Journal. 2022. V. 16. P. 1523–1533.
- Kamyshny A., Yakushev E. V., Jost G., Podymov O. I. Role of Sulfide Oxidation Intermediates in the Redox Balance of the Oxic–Anoxic Interface of the Gotland Deep, Baltic Sea / In: E. V. Yakushev (Ed.), Chemical Structure of Pelagic Redox Interfaces: Observation and Modeling, Hdb Env Chem (2013) 22: 95–120, doi: 10.1007/698_2010_83.
- Li X., Taylor G. T., Astor Y. et al. Relationship of sulfur speciation to hydrographic conditions and chemoautotrophic production in the Cariaco Basin // Marine Chem. 2008. V. 112. P. 53–64.
- Murray J. W., Yakushev E. The suboxic transition zone in the Black sea / In: Neretin L.N. (ed.). Past and Present Water Column Anoxia. Springer, 2006. P. 105–138.
- Percy D., Li X., Taylor G. T. et al. Controls on iron, manganese and intermediate oxidation cate sulfur compounds in the Cariaco Basin // Marine Chem. 2008. V. 111. P. 47–62.
- Pimenov N. V., Neretin L. N. Composition and activities of microbial communities involved in carbon, sulfur, nitrogen and manganese cycling in the oxic/anoxic interface of the Black Sea / In: Neretin L. N.(Ed.) Past and present water column anoxia. Elsevier, 2006. P. 501–521.
- Rethmeier J., Rabenstein A., Langer M., Fischer U. Detection of traces of oxidized and reduced sulfur compounds in small samples by combination of different high-performance liquid chromatography methods // J. Chromatography A. 1997. V. 760. P. 295–302.
- Vairavamurthy A., Mopper K. Determination of sulfite and thiosulfate in aqueous samples including anoxic seawater by liquid chromatography afterderivatization with 2,2’-dithiobis(5-nitropyridine) // Environment Sci. Technol. 1990. V. 24. P. 333–337.
- Vetter R. D., Matrai E. A., Jarvor B., O’Brian J. Reduced sulfur compounds in the marine environment / In: Saltzman E. S., Cooper W. J. (Eds). Biogenic Sulfur in the Environment (ACS Symposium Series, No. 393). Washington, DC: American Chemical Society, 1989. P. 243–261.
- Volkov I. I., Neretin L. N. Hydrogen sulfide in the Black Sea / In: Kostianoy A. G., Kosarev A. N. (Eds.). The Black Sea environment. Berlin; Heidelberg; New York: Springer-Verlag, 2008. P. 309–331.
- Wakeham S. G., Amann R., Freeman K. H. et al. Microbial ecology of the stratified water column of the Black Sea as revealed by a comprehensive biomarker study // Organic Geochemistry. 2007. V. 38. P. 2070–2097.
- Zhang J-Z., Millero F. J. The chemistry of the anoxic waters in the Cariaco Trench // Deep-Sea Research. 1993. V. 40. № 5. P. 1023–1041.
- Zopfi J., Ferdelman T. G., Jørgensen B. B. et al. Influence of water column dynamics on sulfide oxidation and other major biogeochemical processes in the chemocline of Mariager Fjord (Denmark) // Marine Chemistry. 2001. V. 74. P. 29–51.
补充文件
