Saraswati, Pratul Kumar ; Ramesh, Rengaswamy ; Navada, Suresh Vasudev (1993) Palaeogene isotopic temperatures of Western India Lethaia, 26 (1). pp. 89-98. ISSN 0024-1164
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Official URL: http://onlinelibrary.wiley.com/doi/10.1111/j.1502-...
Related URL: http://dx.doi.org/10.1111/j.1502-3931.1993.tb01515.x
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.
Item Type: | Article |
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Source: | Copyright of this article belongs to John Wiley and Sons. |
Keywords: | Palaeotemperature; Palaeogene; Oxygen Isotopes; Larger Foraminifiers; India |
ID Code: | 70273 |
Deposited On: | 18 Nov 2011 13:34 |
Last Modified: | 18 Nov 2011 13:34 |
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