Extended Data Fig. 3: Comparison with available terrestrial EOT geochemical proxy records.
From: Eocene to Oligocene terrestrial Southern Hemisphere cooling caused by declining pCO2
Compilation of terrestrial temperature quantitative proxy records across the Eocene/Oligocene23,24,25,43,45,56,57,58,59,60,61,62 depicting the degree of cooling for each proxy record and time span at each location. Full circles represent land-based records, while empty circles indicate records of terrestrial temperature change derived from marine sediment cores. (Map from Ocean Data View, https://odv.awi.de/).
