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Variation of the Asian summer monsoon since the last glacial-interglacial recorded in a stalagmite from southwest China

<p>A high-precise 230Th dated stalagmite from southwestern China was used to reconstruct the changes of ASM and regional hydrological conditions since the last interglacial (3.6–118.1 ka BP) by the coupled δ18O and δ13C. </p>

ShareScore

36/100

Overall dataset sharing score

Score breakdown

These five areas show where the dataset supports — or may limit — practical reuse.

Stewardship: 8
Harmonization: 4
Access: 16
Reuse readiness: 8
Engagement: 0

Topics

δ18O and δ13C Stalagmite Southwest China Last glacial-interglacial period Asian summer monsoon North-South Hemispheres Local hydrological conditions