A comparative study of cave system Ca isotope ratios with rainfall, d13C, and trace element data: Implications for quantitative reconstructions of paleorainfall from speleothems (2023)
Attributed to:
The isotopic fingerprint of sulfidic and ferruginous environments in the sedimentary record
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.5194/egusphere-egu23-16852
Publication URI: http://dx.doi.org/10.5194/egusphere-egu23-16852
Type: Other