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. 2018 Aug 27;115(37):9116–9121. doi: 10.1073/pnas.1808647115

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Copyright © 2018 the Author(s). Published by PNAS.

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

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Fig. 2. — (A) Greenland: NGRIP temperature (8). (B) Southern Black Sea: TEX₈₆ sea temperature core M72-5 (10). (C) South Carpathians: AC stalagmite POM1 δ¹³C. (D) Upper Danube: Willendorf loess/paleosol profile, paleosol ages, age probability density functions (age-pdf), and stratigraphically constrained loess and gley horizons C7-2, C7-3, and C9 (22). (E) East Carpathians: TC stalagmite 1152 δ¹⁸O. (F) Eifel maar lakes, ELSA dust stack. (G) Western Massive Central: Villars Cave stalagmites δ¹³C (25). (H) Iberian Atlantic margin: TEX₈₆ sea surface temperature core MD95-2042 (17). Numbers indicate Greenland stadials at the end of the respective DO cycle. A map with locations of records is available in SI Appendix, Fig. S1.