Diatom-inferred salinity changes from the Yushe paleolake indicate an aridification during the Pliocene–Pleistocene transition in north China
- Resource Type
- Article
- Source
- In
Palaeogeography, Palaeoclimatology, Palaeoecology 1 January 2015 417:544-553 - Subject
- Language
- ISSN
- 0031-0182