Climate-induced shift of deep-sea benthic foraminifera at the onset of the mid-Brunhes dissolution interval in the northeast tropical Indian Ocean

Climate-induced shift of deep-sea benthic foraminifera at the onset of the mid-Brunhes dissolution interval in the northeast tropical Indian Ocean

Abstract The mid-Brunhes dissolution interval (MBDI; Marine Isotope Stage (MIS) 13 to 7; ~ 533–191 ka) is characterized by various paleoclimatic/paleoceanographic events in the world. We investigated fossil deep-sea benthic foraminifera and sediment geochemistry at the onset of the MBDI (~ 670–440 k...

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Bibliographic Details
Main Authors: Hiroyuki Takata, Minoru Ikehara, Koji Seto, Hirofumi Asahi, Hyoun Soo Lim, Sangmin Hyun, Boo-Keun Khim
Format: Article
Language:English
Published: SpringerOpen 2024-06-01
Series:Progress in Earth and Planetary Science
Subjects:
Deep-sea biota
Sediment geochemistry
Ballasting effect
Wind-driven mixing
Indian summer monsoon
InterTropical Convergence Zone
Online Access:https://doi.org/10.1186/s40645-024-00633-y

Internet

https://doi.org/10.1186/s40645-024-00633-y

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