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While PETM happened over the course of a few tens of thousands of years, the causes and consequences of this transition remain as hypothesis with evidence based on ancient marine sediments. With little information on how the PETM climate changed life on land, the research team used globally distributed fossil pollen preserved in ancient rocks to reconstruct how terrestrial vegetation and climate changed across this period, allowing them to reconstruct both ancient floral communities, and past climates.

United statesVera korasidisJeffrey kiehlUniversity of californiaUniversity of melbourneUs national centre for atmospheric researchDepartment of paleobiologySmithsonian national museum of natural historyNational museumNatural historyEocene thermal maximumNorthern hemisphereSouthern hemisphereAtmospheric research