"4"^^ . . "Magnetoclimatology: Teleconnection between the Siberian loess record and North Atlantic Heinrich events"@en . "0091-7613" . "RIV/00025798:_____/03:00000434!RIV07-MZP-00025798" . "[18E49DFFF627]" . . "4"^^ . "RIV/00025798:_____/03:00000434" . . "Catto, Norm" . . "N\u00FDvlt, Daniel" . "1"^^ . . "537-540" . "614128" . . . . "Magnetoklimatologie: Vz\u00E1jemn\u00E9 vztahy mezi sibi\u0159sk\u00FDm spra\u0161ov\u00FDm z\u00E1znamem a severoatlantsk\u00FDmi Heinrichov\u00FDmi ud\u00E1lostmi"@cs . "Siberia, magnetic susceptibility, paleovclimatology, Late Pleistocene, Heinrich events"@en . "31" . "Environmental magnetic data from loess/paleosol successions from the upper reaches of the Ob River track the major climatic variations over the last glacial-interglacial cycle. The magnetic susceptibility data and stratigraphic successions confirm that the wind-vigour magnetoclimatological model is a viable alternative to the classic pedogenic model for Late Pleistocene. This interpretation must therefore consider eolian dynamics, available source materials, and transport directions, in addition to pedogenic processes. Rapid magnetic fluctuations are identified?for the first time in Siberian records?as the signature of the abrupt cold pulses responsible for the Heinrich layers in North Atlantic marine sediments. The data form a component of climatic teleconnections across the Northern Hemisphere, allowing to correlate Siberian, Chinese, European, and North American magnetic susceptibility stratigraphy, North Atlantic ice-rafted detritus, and sea-surface temperatures off the northwest coast of Africa."@en . "Geology" . . . . . . "US - Spojen\u00E9 st\u00E1ty americk\u00E9" . "Environmental magnetic data from loess/paleosol successions from the upper reaches of the Ob River track the major climatic variations over the last glacial-interglacial cycle. The magnetic susceptibility data and stratigraphic successions confirm that the wind-vigour magnetoclimatological model is a viable alternative to the classic pedogenic model for Late Pleistocene. This interpretation must therefore consider eolian dynamics, available source materials, and transport directions, in addition to pedogenic processes. Rapid magnetic fluctuations are identified?for the first time in Siberian records?as the signature of the abrupt cold pulses responsible for the Heinrich layers in North Atlantic marine sediments. The data form a component of climatic teleconnections across the Northern Hemisphere, allowing to correlate Siberian, Chinese, European, and North American magnetic susceptibility stratigraphy, North Atlantic ice-rafted detritus, and sea-surface temperatures off the northwest coast of Africa."@cs . . . "Z(MZP:N03/98:00)" . "Evans, Michael E." . "Magnetoclimatology: Teleconnection between the Siberian loess record and North Atlantic Heinrich events"@en . "Rutter, Nat W." . "Magnetoklimatologie: Vz\u00E1jemn\u00E9 vztahy mezi sibi\u0159sk\u00FDm spra\u0161ov\u00FDm z\u00E1znamem a severoatlantsk\u00FDmi Heinrichov\u00FDmi ud\u00E1lostmi"@cs . "Magnetoclimatology: Teleconnection between the Siberian loess record and North Atlantic Heinrich events" . . . "Magnetoclimatology: Teleconnection between the Siberian loess record and North Atlantic Heinrich events" . "6" . "Environmental magnetic data from loess/paleosol successions from the upper reaches of the Ob River track the major climatic variations over the last glacial-interglacial cycle. The magnetic susceptibility data and stratigraphic successions confirm that the wind-vigour magnetoclimatological model is a viable alternative to the classic pedogenic model for Late Pleistocene. This interpretation must therefore consider eolian dynamics, available source materials, and transport directions, in addition to pedogenic processes. Rapid magnetic fluctuations are identified?for the first time in Siberian records?as the signature of the abrupt cold pulses responsible for the Heinrich layers in North Atlantic marine sediments. The data form a component of climatic teleconnections across the Northern Hemisphere, allowing to correlate Siberian, Chinese, European, and North American magnetic susceptibility stratigraphy, North Atlantic ice-rafted detritus, and sea-surface temperatures off the northwest coast of Africa." .