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- W2000507899 abstract "Oxygen isotopic measurements of larger benthic foraminifers from western India suggest that the Palaeogene temperature varied between 22deg;C and 32deg;C in this region. The warm climate of the Palaeocene and the Early Eocene, hovering around 32°C, deteriorated in late Middle Eocene (corresponding to planktic zones P13-P14) when the temperature dropped by 6deg;C. With progressive cooling through the Late Eocene, the temperature reached 22deg;C during Early Oligocene times. The cooling trend set in the Middle Eocene seems to have been terminated towards the end of the Palaeogene when the temperature rose to 25°C. □Palaeotemperature, Palaeogene, oxygen isotopes, larger foraminifiers, India." @default.
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- W2000507899 date "1993-03-01" @default.
- W2000507899 modified "2023-10-16" @default.
- W2000507899 title "Palaeogene isotopic temperatures of western India" @default.
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- W2000507899 doi "https://doi.org/10.1111/j.1502-3931.1993.tb01515.x" @default.
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