NDLI: Deep-sea foraminifera in a short core from the Bay of Bengal: ecological comparisons with the South China and Sulu Seas

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Deep-sea foraminifera in a short core from the Bay of Bengal: ecological comparisons with the South China and Sulu Seas

Content Provider	Springer Nature Link
Author	Rao, N. Rajeshwara Kamatchi, P. Ramesh, S.
Copyright Year	2012
Abstract	The present study encompasses a detailed investigation of downcore Holocene foraminifera and their assemblages to comprehend the ecology of the Bay of Bengal and compare it with that of the South China and Sulu Seas, at the same depth for all the three water bodies. Based on temperature and dissolved oxygen profiles, benthic foraminiferal abundance, and species diversity values, it is inferred that the Bay of Bengal is much better ventilated than either the South China or the Sulu Sea. The planktic/benthic (P/B) ratios are extremely low when compared with those reported elsewhere in the world. The absolute dominance of benthic foraminiferal species over their planktic counterparts is attributed to the effect of fragmentation and dissolution of the latter, as they are relatively more susceptible to this process. The very low P/B values are also indicative of water depth below the lysocline in this part of the Bay of Bengal.
Starting Page	3269
Ending Page	3280
Page Count	12
File Format	PDF
ISSN	18667511
Journal	Arabian Journal of Geosciences
Volume Number	6
Issue Number	9
e-ISSN	18667538
Language	English
Publisher	Springer Berlin Heidelberg
Publisher Date	2012-06-06
Publisher Place	Berlin, Heidelberg
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	Foraminifera Bay of Bengal Ecology South China Sea Sulu Sea Planktic/benthic ratio Earth Sciences
Content Type	Text
Resource Type	Article
Subject	Earth and Planetary Sciences Environmental Science

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