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Paleoenvironmental changes recorded in a luminescence dated loess/paleosol sequence from the Tianshan Mountains, arid central Asia, since the Penultimate Glaciation
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文摘

K-feldspar pIRIR dating can be used to date loess sample to at least ∼150 ka in ACA.

Loess in the ACA was deposited during the penultimate and last glaciation periods.

Loess deposits and stalagmite growth are comparable at glacial-interglacial cycles.

There is a climatic pattern of wet-warm (interglacials), dry-cold (glacials) in ACA.

Depositional hiatuses of over 50 kyr occur in ACA loess sequences.

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