Source of a freshwater influx at the last glacial maximum in the Indian Ocean: An alternative interpretation
Abstract Recent analysis of a sediment core in the eastern Arabian Sea revealed a negative pulse of about 1% in the δ 18 O value of the planktonic Foraminifera around the last glacial maximum (LGM). This pulse has been attributed to (i) increased runoff into the Bay of Bengal from the east‐flowing s...
| Published in: | Journal of Quaternary Science |
|---|---|
| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
1992
|
| Subjects: | |
| Online Access: | http://dx.doi.org/10.1002/jqs.3390070306 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.3390070306 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3390070306 |