Reconstruction of the relative sea-level (RSL) of the Gulf of Dvina (White Sea) based on the study of lake sediments on the Onega Peninsula
DOI:
https://doi.org/10.31951/2658-3518-2020-A-4-451Ключевые слова:
lake sediments, Holocene, White Sea, sea-level change, grain-size, geochemistryАннотация
We present the preliminary results of the granulometric and geochemical analyses of lake-bottom sediments obtained from the Murmanskoe and Maloe Murmanskoe lakes. Based on the collected data, we reconstructed changes of relative sea-level (RSL) in the Gulf of Dvina (White Sea) during the Holocene. The conditions and maximum levels of two transgressions (Late Glacial and Tapes) and one Early Holocene regression were identified.
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Эта работа распространяется под международной лицензией Creative Commons Attribution-NonCommercial 4.0.