Journal
EARTH AND PLANETARY SCIENCE LETTERS
Volume 187, Issue 1-2, Pages 83-93Publisher
ELSEVIER SCIENCE BV
DOI: 10.1016/S0012-821X(01)00281-3
Keywords
Loess Plateau; monsoons; wind transport; upper Neogene; magnetostratigraphy; Qinghai-Xizang Plateau
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Widespread eolian red clay underlying the Plio-Pleistocene loess-palaeosol succession in northern China has been dated magnetostratigraphically back to 8.35 Ma, indicating that the East Asian monsoon started at about the same time as the Indian monsoon. An initial sedimentation rate of 11 m/Myr increased gradually to 17.5 m/Myr by 6 Ma, and then decreased to 6 m/Myr between 5 Ma and 3.5 Ma. A marked increase in sedimentation rate and grain size beginning between 3.5 Ma and 3.1 Ma indicates that the East Asian winter monsoon strengthened at this time, and intensified further after 2.6 Ma. The temporal coincidence of the stronger winter monsoon and the Pliocene uplift of northwestern Tibet just before the onset of the Northern Hemisphere glaciation indicate that the three events could be causally linked. (C) 2001 Published by Elsevier Science B.V.
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