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Centennial- to millennial-scale climate shifts in continental interior Asia repeated between warm–dry and cool–wet conditions during the last three interglacial states: evidence from uranium and biogenic silica in the sediment of Lake Baikal, southeast Siberia

ClimatologyQuaternary PeriodSoutheast SiberiaContinental Interior AsiaEngineeringPaleoenvironmental ChangeGeographyClimate DynamicsGeochronologyPaleoclimatologySedimentologyEarth ScienceEarth's ClimateClimate ChangeLake Baikal