Speleothem-derived Asian summer monsoon variationsin Central China, 54–46 ka
The oxygen isotope signature (d18O) of stalagmite SI3 collected from Shizi Cave in north-east Sichuan Province provides an Asian Summer Monsoon (ASM) record in Central China for the period 54–46 ka. The SI3 d18O record clearly shows a negative d18O excursion centred around 49.4 ka, which was reporte...
Published in: | Journal of Quaternary Science |
---|---|
Main Authors: | , , , , |
Format: | Report |
Language: | English |
Published: |
2011
|
Subjects: | |
Online Access: | http://ir.ieecas.cn/handle/361006/10326 https://doi.org/10.1002/jqs.1506 |