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“Greatest lake period” and its palaeo-environment on the Tibetan Plateau

✍ Scribed by Li Bing-yuan; Zhu Li-ping

Publisher
SP Science Press
Year
2001
Tongue
English
Weight
699 KB
Volume
11
Category
Article
ISSN
1009-637X

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Dissolved inorganic carbon isotope (υ 13 C DIC ) is an important tool to reveal the carbon cycle in lake systems. However, there are only few studies focusing on the spatial variation of υ 13 C DIC of closed lakes. Here we analyze the characteristics of υ 13 C DIC of 24 sampled lakes (mainly closed