An eolian deposit–buried soil sequence in an alpine soil on the northern Tibetan Plateau: Implications for climate change and carbon sequestration

Author:

Feng Jin-Liang,Hu Hai-Ping,Chen Feng

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Soil Science

Reference89 articles.

1. Mineral occurrence in soil environments;Allen,1989

2. Late Cenozoic Climate Change in Asia: Loess, Monsoon and Monsoon-Arid Environment Evolution;An,2014

3. Study of the eolian dust flux over the Loess Plateau: an example;An;Chin. Sci. Bull.,1990

4. Pedogenesis, permafrost, and soil moisture as controlling factors for soil nitrogen and carbon contents across the Tibetan Plateau;Baumann;Glob. Chang. Biol.,2009

5. Pedogenesis, permafrost, substrate and topography: plot and landscape scale interrelations of weathering processes on the central-eastern Tibetan Plateau;Baumann;Geoderma,2014

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