Uranium series isotopes and dating of stalagmite C09-2 from Closani Cave


Ages were calculated using the half-lives of Cheng et al. (2000). Correction for detrital contamination assumes a 232Th/238U weight ratio of 3.8 ± 1.9 and 230Th, 234U and 238U in secular equilibrium.Age uncertainties are quoted at the 2σ-level and do not include half-life.

DOI https://doi.org/10.1594/PANGAEA.909988
Related Identifier https://doi.org/10.1594/PANGAEA.909989
Related Identifier https://doi.org/10.1016/j.epsl.2018.07.027
Related Identifier https://doi.org/10.1016/S0009-2541(99)00157-6
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.909988
Creator Warken, Sophie F ; Fohlmeister, Jens ; Schröder-Ritzrau, Andrea ; Constantin, Silviu; Spötl, Christoph ; Gerdes, Axel ; Esper, Jan (ORCID: 0000-0003-3919-014X); Frank, Norbert ; Arps, Jennifer; Terente, Mihai; Riechelmann, Dana F C; Mangini, Augusto; Scholz, Denis
Publisher PANGAEA
Publication Year 2019
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Language English
Resource Type Dataset
Format text/tab-separated-values
Size 164 data points
Discipline Earth System Research
Spatial Coverage (22.800 LON, 45.100 LAT); Closani Cave, Romania