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Article
Adsorption experiment of water-soluble rare earth elements in atmospheric depositions and implications for source tracing in South China
The distribution patterns of rare earth elements (REEs) in fine-grained materials in various depositions were often found to be similar to those of the aeolian sediments deposited in the Loess Plateau in North...
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Article
Seasonal Variations of Uranium in Karst Waters from Northeastern Sichuan, Central China and Controlling Mechanisms
Uranium (U) (or U/Ca ratio) in speleothems has been suggested to be an indicator of soil humidity and effective rainfall in the Asian summer monsoon region. However, this argument has not yet been confirmed in...
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Article
Open AccessSpeleothem Mg, Sr and Ba records during the MIS 5c-d, and implications for paleoclimate change in NE Sichuan, Central China
Trace metals of Mg, Sr and Ba in a stalagmite (SZ2) collected from Suozi Cave in NE Sichuan, Central China, were analyzed with ICP-AES. The stalagmite was dated to have developed between 120 and 103 ka BP. Res...
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Article
Magnetic properties of sediments from the Pearl River Delta, South China: Paleoenvironmental implications
Magnetic parameters and their environmental implications of sediments in a core (PD) from the Pearl River Delta, South China, indicate that ferrimagnetic minerals with low coercivity, such as magnetite, domina...
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Article
Record of winter monsoon strength
Arising from: G. Yancheva et al. Nature 445, 74–77 (2007)10.1038/nature05431; Yancheva et al. reply
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Article
Age dating of lacustrine sediments in Lake Tianshuihai of the Tibetan Plateau by using U-series isochron method and its significance
The age of the clastic-clay sediments with varied content of carbonate in core TS95 taken from the Lake Tianshuihai in the northwest of the Tibetan Plateau was determined successfully by using the total sample...
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Article
R/S analyses of some geochemical indexes for Tianshuihai Lake core in West Kunlun Mountain and their environmental implications
With the decrease of global temperature, glacial epoch came over the earth and global climate fluctuated over a great range since the beginning of Quaternary. Paleoclimotologists of various countries have focu...
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Article
Geochemical records of palaeoclimatic changes in Weinan section since the last interglacial
Weinan section consists of Holocene soil S0, last glacial loess L1, and last interglacial soil S1, furtherly L1 can be subdivided into three layers of loess (L1–1, L1–3, and L1–5), and two layers of weakly dev...