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Humification Degree as a Proxy Climatic Record Since the Last Deglaciation Derived from a Limnological Sequence in South China
Zhong, W (Zhong, Wei)[1]; Ma, QH (Ma, Qiaohong)[1]; Xue, JB (Xue, Jibin)[1]; Zheng, YM (Zheng, Yanming)[1]; Cai, Y (Cai, Ying)[1]; Ouyang, Y (Ouyang, Yun)[1]; Yu, XF (Yu, Xuefeng)[2]
2011-04-30
Source PublicationGEOCHEMISTRY INTERNATIONAL
Volume49Issue:4Pages:407-414
Subtype期刊论文
KeywordSwamp Dahu humification degree the Last Deglaciation East Asian monsoon South China
DOI10.1134/S0016702911040094
Indexed BySCI
Language英语
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Cited Times:2[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.ieecas.cn/handle/361006/10325
Collection加速器质谱中心
Corresponding AuthorZhong, W (Zhong, Wei)[1]
Affiliation1.School of Geography Science, South China Normal University, Guangzhou 520631, China;
2.State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS, Xi’an 710075, China
Recommended Citation
GB/T 7714
Zhong, W ,Ma, QH ,Xue, JB ,et al. Humification Degree as a Proxy Climatic Record Since the Last Deglaciation Derived from a Limnological Sequence in South China[J]. GEOCHEMISTRY INTERNATIONAL,2011,49(4):407-414.
APA Zhong, W .,Ma, QH .,Xue, JB .,Zheng, YM .,Cai, Y .,...&Yu, XF .(2011).Humification Degree as a Proxy Climatic Record Since the Last Deglaciation Derived from a Limnological Sequence in South China.GEOCHEMISTRY INTERNATIONAL,49(4),407-414.
MLA Zhong, W ,et al."Humification Degree as a Proxy Climatic Record Since the Last Deglaciation Derived from a Limnological Sequence in South China".GEOCHEMISTRY INTERNATIONAL 49.4(2011):407-414.
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