Palynological data confirm the occurrence of forest on the Loess Plateau of central China during the Middle Quaternary (MIS13)

Author:

Wang Nannan,Tian Yanyan,Cao Xianyong,Wei Mingjian

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference97 articles.

1. Sea-surface temperature, productivity and hydrological changes in the Northern Indian Ocean (Maldives) during the interval ∼575-175 ka (MIS 14 to 7);Alonso-Garcia;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2019

2. The paleosol complex S5 in the China Loess Plateau-a record of climatic optimum during the last 1.2Ma;An;Geo. J.,1987

3. The fifth layer paleosol in the Lishi Loess and their paleoclimatic significance;An;Acta Pedol. Sin.,1980

4. Loess stratigraphy in Luochuan of China;An;Quat. Sci.,1989

5. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of Central China during the last 130,000 years;An;Quat. Res.,1991

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