PALEOMONSOONS OF CHINA OVER THE LAST 130,000 YEARS - PALEOMONSOON RECORDS


Autoria(s): AN, ZS; WU, XH; WANG, PX; WANG, SM; DONG, GR; SUN, XJ; ZHANG, DE; LU, YC; ZHENG, SH; ZHAO, SL
Data(s)

1991

Resumo

The characteristics of the modern monsoon climate of China may be used as clues for recognizing the records of paleomonsoon climate. The present paper deals primarily with the various paleomonsoon records of the last 130,000 years in the southeast monsoon area. These records mainly come from the following three fields: (i) the historical, (ii) the geological, including loess-paleosol sequence, deserts, lakes, snowlines, timberlines, the phenomena of continental desertization and so on, and (iii) the biological, presented by vegetation a.d mammals. Among these records, the loess-paleosol sequence in the Loess Plateau reflects a climatic history characterized by alternation of two different climatic periods when the Asian winter monsoon and summer monsoon showed pronounced effects on environment, respectively.

Identificador

http://ir.qdio.ac.cn/handle/0/3851

http://www.irgrid.ac.cn/handle/1471x/166769

Fonte

AN, ZS; WU, XH; WANG, PX; WANG, SM; DONG, GR; SUN, XJ; ZHANG, DE; LU, YC; ZHENG, SH; ZHAO, SL.PALEOMONSOONS OF CHINA OVER THE LAST 130,000 YEARS - PALEOMONSOON RECORDS,SCIENCE IN CHINA SERIES B-CHEMISTRY LIFE SCIENCES & EARTH SCIENCES,1991,34(8):1007-1015

Palavras-Chave #Chemistry, Multidisciplinary
Tipo

期刊论文