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Isotopic Indications of Meromixis in Separated Lakes on the White Sea Coast

Yurij K Vasil’chukMoscow State University, Moscow, RussiaA. P. LisitzinShirshov Institute of Oceanology, Russian Academy of Science, Moscow, RussiaE. D. KrasnovaMoscow State University, Moscow, RussiaNadine A BudantsevaMoscow State University, Moscow, RussiaD. A. VoronovBelozerskii Institute Of Physicochemical Biology of Moscow State University, Moscow, RussiaA. N. PantyulinMoscow State University, Moscow, RussiaJulia N ChizhovaInstitute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences, Moscow, RussiaВ. П. ШевченкоShirshov Institute of Oceanology, Russian Academy of Science, Moscow, Russia
Doklady Earth Sciencesjournal2018en
ABI

Аннотация

Studies of lakes at different stages of separation from the sea have been carried out on the northwestern coast of Kandalaksha Gulf of the White Sea. At the end of the winter period, from March 16 to 29, 2013, the lakes Kislo–Sladkoe, Trekhtzvetnoe, Nizhnee Ershovskoe, Ermolinskaya Bay and snow near the pier of Pertsov White Sea Biological Station of Moscow State University (WSBS MSU) were studied. The isotope characteristics of the water of lakes, ice and snow, the distribution of salinity, temperature, and hydrogen sulfide content were studied.

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