. . . "New environmental magnetic susceptibility data from loess-paleosol successions from the the Biya and Katun\u2019 River basins (southern Siberia) track the major climatic and environmental variations over the last glacial-interglacial cycle. Gradual transitionfrom parkland-steppe (OIS 5a) to periglacial steppe-tundra conditions (OIS 4) occurred ~75 ka BP and was replaced by parkland steppe and boreal forest during warmer intervals within OIS 3. The local LGM during the early part of OIS 2 (~25-18 ka BP) was arked by a sharp change to a dry tundra climate, confirmed by finds of typical pleniglacial loess molluscs-association (Vallonia tenuilabris, Succinea oblonga, Pupilla muscorum, Pupilla sterri a.o.) and bones of large mammals (Mammuthus primigenius," . "Late Quaternary Loess-Paleosol succesion in southern Siberia: Implications for Northern Hemispheric climatic teleconnections"@en . . "1"^^ . . "RIV/00025798:_____/03:00000096!RIV/2004/MZP/N03004/N" . "613244" . "Neuveden" . "Z(MZP:N03/98:00)" . "0"^^ . "0"^^ . "Late Quaternary Loess-Paleosol succesion in southern Siberia: Implications for Northern Hemispheric climatic teleconnections" . . "9. Kvart\u00E9r 2003 - Sborn\u00EDk abstrakt\u016F" . "7"^^ . . "N\u00FDvlt, Daniel" . . . "2"^^ . . "Late Quaternary Loess-Paleosol succesion in southern Siberia: Implications for Northern Hemispheric climatic teleconnections"@en . "Late Quaternary Loess-Paleosol succesion in southern Siberia: Implications for Northern Hemispheric climatic teleconnections" . "14-15" . . "Loess, Paleosol, Paleocliamtology, Paleoecology, Late Quaternary, Central Siberia"@en . "RIV/00025798:_____/03:00000096" . . "New environmental magnetic susceptibility data from loess-paleosol successions from the the Biya and Katun\u2019 River basins (southern Siberia) track the major climatic and environmental variations over the last glacial-interglacial cycle. Gradual transitionfrom parkland-steppe (OIS 5a) to periglacial steppe-tundra conditions (OIS 4) occurred ~75 ka BP and was replaced by parkland steppe and boreal forest during warmer intervals within OIS 3. The local LGM during the early part of OIS 2 (~25-18 ka BP) was arked by a sharp change to a dry tundra climate, confirmed by finds of typical pleniglacial loess molluscs-association (Vallonia tenuilabris, Succinea oblonga, Pupilla muscorum, Pupilla sterri a.o.) and bones of large mammals (Mammuthus primigenius,"@en . . "[CEEEE71DDDF6]" . . . "2003-01-01+01:00"^^ . . . "Brno" . "Brno" . . .