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What is Oligocene Climate Wetting in Qaidam Basin about?

The document discusses the unexpected expansion of lacustrine sedimentation in the Qaidam Basin during the Oligocene, which contradicts the prevailing notion of continuous aridification in Inner Asia. A reconstruction of hydrogen isotope records indicates significant climatic shifts, revealing a wetter climate during the Oligocene that contrasts with the arid conditions before and after this period. The study suggests that regional climatic responses to global cooling resulted in contrasting hydrological pa

Author

sknagal1

Language

EN