Abstract
Реконструкция палеотайфунов и повторяемости экстремальных паводков на юге острова Сахалин в среднем–позднем голоцене
Highlights
The geological record of extreme floods associated with the passage of the strongest typhoons in the last 6620 cal. yr. was first restored for the Sakhalin Island
The cross-section includes the peat bog with numerous loam layers which formed during the flooding of the swamp during extreme floods
The results of the ecological and taxonomic composition of diatom flora study have been presented with the aim of restoring the evolution of sedimentation environments, as well the analysis of the moisture dynamics and river activity
Summary
Reconstruction of paleotyphoons and recurrence of extreme floods in south Sakhalin Island in Middle–Late Holocene The geological record of extreme floods associated with the passage of the strongest typhoons in the last 6620 cal. Was first restored for the Sakhalin Island. The cross-section of the Holocene deposits near Dolinsk Town (the watershed in the northern part of the Susunai lowland) was chosen as a natural archive for paleotyphoon activity.
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