joint supported by the National Natural Science Foundation of China (41401226, 41271024);the China Postdoctoral Science Foundation (2015M570865)
Marine Isotope Stage 11(MIS 11; ca. 423-362 ka) is generally considered to be the best analogue for the present interglacial(Holocene), and investigation of it will improve our understanding of current climate var...
Supported by National Natural Science Foundation of China (Grant Nos. 40772032 and 40573054);National Basic Research Program (Grant No. 2007CB815603)
The dominant magnetic minerals and carriers of magnetic signals within the Chinese Loess Plateau are magnetite, maghemite, hematite, and goethite. In this study, we investigated the provenance and evo- lution of magne...
supported by Russian Foundation for Basic Research (grants No 07-04-01146 and 06-05-65203)
Carbonate pedofeatures were studied in details in a loess-paleosol pedocomplex near Kursk, in the central part of the European Plain. The soils studied included a modern Chernozem and five Pleistocene paleosols. Carbo...
National Natural Science Foundation of China, No.40571154; No.40471119
Optically stimulated luminescence (OSL) dating for polymlneral fine-grained loess samples, collected in Laoguantai (LGT) section on the south of the Chinese Loess Plateau, was made by application of single-aliquot...
supported by the National Natural Science Foundation of China(NO:40202019,90102017,40121303);National Basic Research Program of China(2004CB720202);China Postdoctoral Fund
The widely distributed red clay sediment underlying the Chinese Loess Plateau truly records the Neogene environmental evolution, and its genesis and development are intrinsically related to the uplift processes of the...
the State Outstanding Young Scientists Foundation(Grant No.94625304)and the"Climbing Program"sponsored by the Ministry of Science and Technology(Grant No.95-yu-39)
In this paper the boron contents and boron isotopic composition ofacid-soluble phases in loess and paleosol samples are determined for the first time. The boroncontents of acid-soluble phases in the Luochuan loess sec...
This work was supportedby the National Natural Science Foundation of China (Grant Nos. 49894176, 40125001 and 49928101);the National Project for the Basic Research on Tibetan Plateau (Grant No. G1998040809).
Study on two loess sections, one located at Wu-wei near the Tengger Desert in northwestern China, another located near Ganzi at the southeast margin of the Tibetan Plateau in southwest China, reveals a coeval drying s...
This work was supported jointly by the NSFC 'Excellent Researchers' Fund' (grant No. 49928101);the National Tibetan Project (Grant No. 1998040802) ; Hundred Talents Project' ofCAS(Renjiaozi[2000]005). We thank Wu Fuli, Nie Junsheng, Wu Hongqi, Xi Xi
Loess on the northern slope of Kunlun Mountains is the synchronous deposition of the Taklimakan Desert. The paleomagnetism and climatic records of an over 80 m loess-paleosol sequence on the highest river terrace at t...
the National Natural Science Foundation of China (Grant No.49425405).
We have conducted detailed rock magnetic experiments on samples from loess unit 8 (L8) and paleosol unit 8 (S8) in Jingbian, Yichuan and Duanjiapo loess sections along an N-S transect in the Chinese Loess Plateau. Maj...
the National NaturalScience Foundation of China (Grant No. 49894170); the Key Project of the Chinese Academy of Sciences (Grant No. KZ951-A1-402).
According to the investigations of five loess sections in Shanri Province, China, it was found that the concentrations of the major greenhouse gases CO2, CH4 and N2O in loess-paleosol sequences are generally high, eve...