| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4674790 | Procedia Earth and Planetary Science | 2015 | 4 Pages |
Abstract
The uppermost 500 cm sedimentary core from ODP sitelocated at the Eastern flank of Najareth bank in the Northern Indian Ocean has yielded altogether twenty four species of planktonic foraminifera. Among all these species, Globorotalia menardii has been found to be consistently dominant in the faunal assemblages from most of the samples. The δ18O measured on the tests of Globorotalia menardii from all levels help in precisely working out the sediment accumulation rates at different isotopic stages, and deciphering the change in climate in the Late Quaternary as well.
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