Oxygen-isotope palaeothermometry of the Eocene Harudi Formation, Kutch Basin, western India: evidence for an early inception of the Middle Eocene Climatic Optimum
This study presents the first oxygen-isotope palaeothermometry of the Eocene Harudi Formation in western India, revealing high temperatures that indicate an early inception of the Middle Eocene Climatic Optimum prior to the commonly cited ~40.5 Ma.