Magnetoclimatology: Teleconnection between the Siberian loess record and North Atlantic Heinrich events

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F03%3A00000100" target="_blank" >RIV/00025798:_____/03:00000100 - isvavai.cz</a>
Alternative codes found
RIV/00025798:_____/03:00000434
Result on the web
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DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Magnetoclimatology: Teleconnection between the Siberian loess record and North Atlantic Heinrich events
Original language description
New magnetic data from loess and paleosol successions in southern Siberia, track the major climatic variations over the last glacial-interglacial cycle. Profiles of magnetic susceptibility correspond to oxygen isotope stages 1-5. Magnetic-susceptibilitydata confirm that the wind-vigour magnetoclimatological model is a viable alternative to the classic pedogenic model. These are identified?for the first time in Siberian records as the signature of the abrupt cold pulses esponsible for the Heinrich layerin North Atlantic marine sediments. The data form a component of climatic teleconnections across the Northern Hemisphere, allowing correlations to be made among: 1) Siberian magnetic susceptibility stratigraphy, 2) data recorded from other loess-paleosolsuccessions in China, European Russia, Europe, and North America, 3) North Atlantic ice-rafted detritus, and 4) sea-surface temperatures derived from molecular stratigraphy of marine sediments off the northwest coast of Africa.
Czech name
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Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Publication year
2003
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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