Abstract
Electron spin resonance (ESR) dating and lithostratigraphic studies of marine deposits on the TaymyrTaimyr Peninsula suggest that a marine sedimentary environment dominated during isotope Stages 4, 5, 7, 8, 9 and 15. The marine basins were predominantly cold and influenced by freshwater.
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Bolshiyanov, D., Molodkov, A. (1999). Marine Pleistocene Deposits of the Taymyr Peninsula and their Age from ESR Dating. In: Kassens, H., et al. Land-Ocean Systems in the Siberian Arctic. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-60134-7_37
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DOI: https://doi.org/10.1007/978-3-642-60134-7_37
Publisher Name: Springer, Berlin, Heidelberg
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