The region comprising of East Central Europe, South East Europe and Turkey contributed to
the SISAL (Speleothem Isotopes Synthesis and AnaLysis) global database with stable …

The oxygen isotope composition of speleothems is a widely used proxy for past climate
change. Robust use of this proxy depends on understanding the relationship between …

The covariance of stable hydrogen (δ 2 H) and oxygen (δ 18 O) isotopes in local
precipitation (the local meteoric water line–LMWL) serves as a benchmark in isotope …

Samples of hydrogen and oxygen stable isotopes in precipitation collected and analyzed
during the summer monsoon in 2017 and 2018 in Chengdu are reported in this paper …

Speleothems, as secondary carbonate deposits, precipitate in the cave environment from
the water originally sourced from the ocean, transferred via atmosphere through soil and …

We present the first stable isotope (δ13C and δ18O) speleothem record from continental
Croatia retrieved from two coeval stalagmites from Nova Grgosova Cave. U-Th dates …

The transmission of stable isotopes and elements/ions from the outside to the inside of a
cave and their incorporation into drip water can involve numerous biogeochemical …

Speleothems deposited from cave drip waters retain, in their calcite lattice, isotopic records
of past environmental changes. Among other proxies, δ18O is recognized as very useful for …

The study of modern cave deposits forming under near isotopic equilibrium conditions can
potentially help disentangle the processes influencing the oxygen isotope system and …

The speleothem stable carbon isotope (δ 13 C) is an important proxy for paleoclimate
reconstruction. Understanding the stable carbon isotope composition of dissolved inorganic …