Differences in the 14C age, δ13C and δ18O of Holocene tufa and speleothem in the Dinaric Karst
Author:
Publisher
Elsevier BV
Subject
Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography
Reference77 articles.
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4. Carbon and oxygen isotope study of the active water−carbonate system in the karstic Mediterranean cave: Implications for paleoclimate research in semiarid regions;Bar-Matthews;Geochim. Cosmochim. Acta,1996
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