Proc. IODP, 317, Data report: revised Pleistocene age model based on a modified nannofossil bioevent and additional measurements of benthic foraminiferal oxygen and stable carbon isotope ratios from Hole U1352B, offshore Canterbury Basin, New Zealand

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Chapter contents Abstract Introduction Materials and methods Results Nannofossil datum reexamination Impact of new isotopic measurements Correlation with the LR04 stack and revised age model Acknowledgments References Figures F1. Selected calcareous nannofossil species. F2. N. flemingi δ¹⁸O and δ¹³C ratios. F3. δ¹⁸O comparison. F4. δ¹³C comparison. F5. δ¹⁸O variations and LR04 stack. F6. Sedimentation rates. Tables T1. Calcareous nannofossils. T2. N. flemingi δ¹⁸O and δ¹³C ratios. T3. N. flemingi and U. perigrina δ¹⁸O and δ¹³C ratios. T4. Bioevents. PDF file			Previous \| Next doi:10.2204/iodp.proc.317.210.2018 Acknowledgments This research used samples and data provided by the Integrated Ocean Drilling Program (IODP). We acknowledge the IODP Expedition 317 shipboard scientists, technical staff, and the captain and crew of the R/V JOIDES Resolution. We would like to thank Clara T. Bolton and an anonymous reviewer. This article was greatly improved by their detailed review and valuable suggestions. Oxygen and stable carbon isotopic measurements were performed under the cooperative research program of the Center for Advanced Marine Core Research (CMCR), Kochi University (Numbers 13A034, 13B028, 14A031, 14B029, 15A039, and 15B034). Funding for this research was provided by Japan Society for the Promotion of Science (JSPS Grants-in Aid for Scientific Research Number 23340154). Top of page \| Previous \| Next

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