SPATIAL AND TEMPORAL VARIATIONS OF δD AND δ~(18)O VALUES OF CAVE DRIP WATERS: IMPLICATIONS FOR PALEOCLIMATE SIGNAL IN STALAGMITE

摘要

Circumspect isotope hydrological monitoring in karstic environment is crucial to support any future climate and/or environmental reconstruction efforts (e.g. Suric et al., 2010; Riechelmann et al., 2011), however it could be essential contribution also to ecohydrological, drinking water supply problems (Ford and Williams, 2007).