(Table 1) Stable carbon and oxygen isotope ratios of benthic foraminifera of ODP Hole 184-1148A

Changes in intermediate and deep ocean circulation likely played a significant role in global carbon cycling and meridional heat/moisture transport during the middle Miocene climate transition (~14 Ma). High-resolution middle Miocene (16-13 Ma) benthic foraminifer stable isotope records from the Sou...

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Bibliographic Details
Main Authors: Tian, Jun, Shevenell, Amelia E, Wang, Pinxian, Li, Qianyu, Cheng, Xinrong
Format: Dataset
Language:English
Published: PANGAEA 2009
Subjects:
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.777751
https://doi.org/10.1594/PANGAEA.777751