Guo Zhengtang

Guo Zhengtang (Chinese: 郭正堂; pinyin: Guō Zhèngtáng; born April 8, 1964[1]) is a Chinese geologist. He is a Cenozoic geologist.[2]

This is a Chinese name; the family name is Guo.
Guo Zhengtang
Born (1964-04-08) April 8, 1964
Alma mater
Scientific career
Fields
Website

Education and early life

Guo was born in Shuozhou, Shanxi Province in 1964. He received his Bachelor of Arts degree in Geology from Peking University in 1983, and earned Ph.D. of soil science from the Pierre and Marie Curie University, France in 1990.[3]

Research and career

Guo's research mainly focuses on the eolian sediments of the Chinese Loess Plateau and ancient climate change. He was the Director-general of the Institute of Earth Environment, Chinese Academy of Sciences during 2002-2006.[4] He was a Vice-President of the INQUA Commission on Paleoclimates.[5] He and his colleagues extended the loess records in China from ~8 Ma to ~22 Ma.[6][7][8]

gollark: It's not a GC problem, they're referenced in an object.
gollark: The issue is basically that it loads Markov chains into RAM when operating on them and never clears then ever.
gollark: Maybe I need to implement a LRU cache instead of just loading all things ever into RAM?
gollark: This is due to people bad.
gollark: No, it's remarking on how few there are.

References
  1. "郭正堂" (in Chinese). Chinese Academy of Sciences. Retrieved 2 May 2017.
  2. Guo Zhengtang's publications indexed by the Scopus bibliographic database. (subscription required)
  3. http://sourcedb.igg.cas.cn/cn/zjrck/200907/t20090713_2065546.html
  4. "历任领导----中国科学院地球环境研究所".
  5. http://www.inqua.tcd.ie Archived June 23, 2010, at the Wayback Machine
  6. Guo, Z. T.; Ruddiman, W. F.; Hao, Q. Z.; Wu, H. B.; Qiao, Y. S.; Zhu, R. X.; Peng, S. Z.; Wei, J. J.; Yuan, B. Y.; Liu, T. S. (2002). "Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China". Nature. 416 (6877): 159–63. doi:10.1038/416159a. PMID 11894089.
  7. Guo, Zhengtang; Petit-Maire, Nicole; Kröpelin, Stefan (2000). "Holocene non-orbital climatic events in present-day arid areas of northern Africa and China". Global and Planetary Change. 26 (1–3): 97–103. CiteSeerX 10.1.1.562.6795. doi:10.1016/S0921-8181(00)00037-0.
  8. Yamei, H. (2000). "Mid-Pleistocene Acheulean-like Stone Technology of the Bose Basin, South China". Science. 287 (5458): 1622–1626. doi:10.1126/science.287.5458.1622. PMID 10698732.
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