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. 2022 May 13;119(20):e2200796119. doi: 10.1073/pnas.2200796119

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Copyright © 2022 the Author(s). Published by PNAS

This article is distributed under Creative Commons Attribution-NonCommercial-NoDerivatives License 4.0 (CC BY-NC-ND).

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Fig. 1. — Four-stage 4.2 ka BP paleoclimate proxies compared to KM-A speleothem δ¹⁸O, Mawmluh Cave, northeast India (4): (A) Delingha tree rings (1), (B) Dongshiya Cave speleothem (5), (C) Gol-e Zard Cave speleothem (7), (D) Mt. Logan ice core (8).