δ18O and δ13C and Oxcal deposition model interpolated ages of stalagmite SIB-4 from Sibaki Cave, Southwestern Iran

DOI

Samples for carbon and oxygen isotopic analysis were micromilled at 3.0 and 0.2 mm increments along the main growth axis. Approximately 3000 samples were measured using a semi-automated gas preparation and introduction system (Gasbench II) linked to a Delta V Plus isotope ratio mass spectrometer (both ThermoFisher) at the University of Innsbruck, following the methods of Spötl and Vennemann (2003). Isotope values are reported relative to the Vienna Pee Dee Belemnite (VPDB) reference. Long-term analytical precision is better than 0.1‰ (1σ) for both δ13C and δ18O.

Identifier
DOI https://doi.org/10.1594/PANGAEA.955839
Related Identifier https://doi.org/10.1594/PANGAEA.955861
Related Identifier https://doi.org/10.1002/jqs.3478
Related Identifier https://doi.org/10.25921/XPYJ-M346
Related Identifier https://doi.org/10.1002/rcm.1010
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.955839
Provenance
Creator Soleimani, Mojgan ORCID logo; Nadimi, Alireza; Koltai, Gabriella ORCID logo; Dublyansky, Yuri ORCID logo; Carolin, Stacy A ORCID logo; Spötl, Christoph ORCID logo
Publisher PANGAEA
Publication Year 2023
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 10553 data points
Discipline Earth System Research
Spatial Coverage (51.596 LON, 29.815 LAT); Fars, Iran