Extended Data Fig. 2: Cenozoic TEX86 Bayspar-derived SST compilation.
From: Enhanced ocean oxygenation during Cenozoic warm periods
SSTs are categorized in middle and low latitudes with transition and upwelling regions (a) and high latitudes (b). Grey line indicates benthic oxygen isotope compilation by Westerhold et al.8. c, Maps with core locations: modern map shows current locations of core sites. Palaeomap at 20 Ma with palaeorecords spanning 10–30 Ma and palaeomap at 50 Ma with palaeorecords spanning 40–60 Ma. Maps are adapted from the Ocean Drilling Stratigraphic Network (ODSN) Paleomap project (http://www.odsn.de/odsn/services/paleomap/paleomap.html, accessed May 2022). Palaeolatitudes for core sites are calculated after van Hinsbergen et al.52.
