Intensified Central Asian aridification accompanied with strengthened Asian summer monsoons at the 400-kyr band during 4–2 Ma
Central Asian wetting has been accompanied with East Asian precipitation decrease in recent decades, but whether this is the case on longer timescales is not entirely clear. Here we present new and compiled available evidence from the Qaidam Basin of Central Asia, which shows that Central Asian arid...
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Veröffentlicht in: | Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 2024-09, Vol.649, p.112342, Article 112342 |
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