(Table 1) Stable carbon and oxygen isotope ratios of benthic foraminifera of ODP Hole 184-1148A, supplement to: Tian, Jun; Shevenell, Amelia E; Wang, Pinxian; Li, Qianyu; Cheng, Xinrong (2009): Reorganization of Pacific Deep Waters linked to middle Miocene Antarctic cryosphere expansion: A perspective from the South China Sea. Palaeogeography, Palaeoclimatology, Palaeoecology, 284(3-4), 375-382

• Main Authors: Tian, Jun, Shevenell, Amelia E, Wang, Pinxian, Li, Qianyu, Cheng, Xinrong
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2009
• Subjects: Sample code/label; DEPTH, sediment/rock; Cibicidoides wuellerstorfi, δ13C; Cibicidoides wuellerstorfi, δ18O; Oridorsalis spp., δ13C; Oridorsalis spp., δ18O; Drilling/drill rig; DSDP/ODP/IODP sample designation; Mass spectrometer Finnigan MAT 252; Leg184; Joides Resolution; Ocean Drilling Program ODP; Antarctic; Kennett; Pacific; Antarc*; Antarctica
• Online Access: https://dx.doi.org/10.1594/pangaea.777751; https://doi.pangaea.de/10.1594/PANGAEA.777751

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...