Fig. 4: Interpolated carbonates and parent waters δ18O and Δ′17O values for speleothems from the Asian monsoon region. | Communications Earth & Environment

Fig. 4: Interpolated carbonates and parent waters δ18O and Δ′17O values for speleothems from the Asian monsoon region.

From: Variations in triple oxygen isotope of speleothems from the Asian monsoon region reveal moisture sources over the past 300 years

Fig. 4

The interpolated maps for Δ′17O values of speleothems (a) and reconstructed parent water (b), respectively. The interpolated maps for δ18O values of speleothems (c) and reconstructed parent water (d), respectively. Symbol size represents isotopic values. The interpolated maps of δ18O and Δ′17O values of speleothems were generated using inverse distance weighted (IDW) interpolation73. The locations of all sample sites are given in Fig. 1 and Supplementary Table 1.

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