Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years
Dados Bibliográficos
| ID | 23375174 |
|---|---|
| Autores | Zhaolong An (0000-0002-9538-9826), Zhisheng An, George Kukla (Lamont-Doherty Earth Observatory), George J Kukla, Stephen C Porter (0000-0003-4416-5387, University of Washington), Jule Xiao |
| Ano | 1991 |
| Volume | 36 |
| Fascículo | 1 |
| Páginas | 29-36 |
| Data de publicação | 1991-07-01 |
| Peer Reviewed | Sim |
| Open Access | Sim |
| Tipo | ARTICLE |
| Periódico | Quaternary Research (JOURNAL) |
| Identificadores do periódico | ISSN: 0033-5894 • E-ISSN: 1096-0287 |
| Editora | Cambridge University Press (CUP) (PUBLISHER) |
| DOI | 10.1016/0033-5894(91)90015-w |
| OpenAlex | W2055792591 |
| Idioma | EN |
| Citações recebidas | 145 |
| Referências citadas | 13 |
The magnetic susceptibility of loess and paleosols in central China represents a proxy climate index closely related to past changes of precipitation and vegetation, and thus to summer monsoon intensity. Time series of magnetic susceptibility constructed for three loess-paleosol sequences in the southern part of the Chinese Loess Plateau document the history of summer monsoon variation during the last 130,000 yr. They correlate closely with the oxygen isotope record of stages 1 to 5 in deep-sea sediments. Soils were forming during intervals of strong summer monsoon, whereas loess units were deposited at times of reduced monsoon intensity. The Chinese loess-paleosol sequence can thus be viewed as a proxy record of Asian monsoon variability extending over the last 2.5 myr.
Climatology · East Asian Monsoon · Geochemistry · Geography · Geomorphology · Isotopes of oxygen · Loess · Loess plateau · Monsoon · Paleosol · Physical geography · Plateau (mathematics) · Proxy (statistics) · Geology · Geology and Paleoclimatology Research · Geomagnetism and Paleomagnetism Studies · Pleistocene-Era Hominins and Archaeology · Soil Science
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| Altamente citado | Sim |
| Tipos de citação | Neutras: 97 |