“…Therefore, the growth records of tufa and speleothems may contain valuable information on the regional palaeoclimate (Geyh, 1970;Franke and Geyh, 1970;Hennig et al, 1983;Gascoyne et al, 1983;Schwarcz and Gascoyne, 1984;Baker et al, 1993;Pazdur et al, 1995). Analysis by both 14 C and uranium-series disequilibrium ( 230 Th/ 234 U; in the following text U-Th) methods has yielded dates of tufa and speleothem samples (Geyh, 1970;Franke and Geyh, 1970;Srdoč et al, 1983Srdoč et al, , 1994Hennig et al, 1983;Schwarcz and Gascoyne, 1984;Geyh and Hennig, 1986;Ford and Gospodarič, 1989;Pentecost et al, 1990;Pazdur et al, 1988Pazdur et al, , 1995Pazdur and Pazdur, 1990;Zupan, 1991;Dorale et al, 1992;Falguères et al, 1992;Baker et al, 1993). Geyh (1970) and Franke and Geyh (1970) gave the first evidence based on 69 14 C dates that speleothem growth was restricted to interglacial and interstadial periods in central Europe.…”