Stable isotope ratio of G. sacculifer in sediment core MD99-2198 (0-125 ka)

DOI

Stable isotope ratios in planktic foraminifera were measured every 20 cm for the upper 0-18.5 m and every 10 cm between 18.5-22 cm (revised depth). Note that the original core depth scale in core MD99-2198 was modified by excluding two intervals (10.06-10.24 m and 13.78-14.30 m), representing episodes where the core was ripped apart, as could be concluded on the basis of large increases in porosity.

Revised depth: Intervals between 10.06-10.24 m and 13.78-14.30 m where the core was ripped apart were excluded.

Identifier
DOI https://doi.org/10.1594/PANGAEA.928986
Related Identifier https://doi.org/10.1016/j.quascirev.2021.107159
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.928986
Provenance
Creator Zhuravleva, Anastasia
Publisher PANGAEA - Data Publisher for Earth & Environmental Science
Publication Year 2021
Funding Reference German Science Foundation, TI240 8 2
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Representation
Language English
Resource Type Dataset
Format text/tab-separated-values
Size 408 data points
Discipline Earth System Research
Spatial Coverage (-61.233 LON, 12.092 LAT); Tobago basin