Response of humification degree to monsoon climate during the Holocene from the Hongyuan peat bog, eastern Tibetan Plateau

Palaeogeography, Palaeoclimatology, Palaeoecology

Volumn 286, Issue 3-4, 2010, Pages 171-177

  Wang, Hua ^a,b   Hong, Yetang ^b   Lin, Qinghua ^b   Hong, Bing ^b   Zhu, Yongxuan ^b   Wang, Yu ^b   Xu, Hai ^c  

^a XIHUA UNIVERSITY   (China)

^b INSTITUTE OF GEOCHEMISTRY   (China)

^c Chinese Academy of Sciences   (China)

Author keywords

Eastern Tibetan Plateau; Holocene; Humification; Monsoon; Peat

Indexed keywords

ABSORBANCE; CLIMATE VARIATION; FREEZE-THAW CYCLE; HOLOCENE; HUMIFICATION; PALEOCLIMATE; PEATLAND; TIME SERIES;

CHINA; QINGHAI-XIZANG PLATEAU;

CAREX MULIEENSIS;

EID: 75849164408     PISSN: 00310182     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.palaeo.2009.12.015     Document Type: Article

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