(Table T1) Stable oxygen and carbon isotopic composition of benthic foraminifers in ODP Site 199-1218 sediments

DOI

The transition from the late Oligocene warm period into the early Miocene was marked by a series of rapid and brief episodes of cryospheric expansion and global cooling. We analyzed benthic foraminifers from nannofossil oozes recovered at Ocean Drilling Program Site 1218 to construct a stable isotope stratigraphy for the deep Pacific.

Sediment depth is given in rmcd. Foraminifers were picked from the >150 µm fraction for analyses. Analytical precision was better than 0.08 per mil.

Supplement to: Tripati, Aradhna K; Elderfield, Henry; Booth, Linda; Zachos, James C; Ferretti, Patrizia (2006): Data report: High-resolution benthic foraminiferal stable isotope stratigraphy across the Oligocene/Miocene boundary at Site 1218. In: Wilson, PA; Lyle, M; Firth, JV (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 199, 1-13

Identifier
DOI https://doi.org/10.1594/PANGAEA.777119
Related Identifier https://doi.org/10.2973/odp.proc.sr.199.221.2006
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.777119
Provenance
Creator Tripati, Aradhna K ORCID logo; Elderfield, Henry; Booth, Linda; Zachos, James C ORCID logo; Ferretti, Patrizia ORCID logo
Publisher PANGAEA
Publication Year 2006
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Language English
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 2140 data points
Discipline Earth System Research
Spatial Coverage (-135.367 LON, 8.890 LAT); North Pacific Ocean