Triple isotope (dD, d17O, d18O) study on precipitation, drip water and speleothem fluid inclusions for a Western Central European cave (NW Switzerland)
Deuterium (dD) and oxygen (d18O) isotopes are powerful tracers of the hydrological cycle and have been extensively used for paleoclimate reconstructions as they can provide information on past precipitation,temperature and atmospheric circulation. More recently, the use of 17O excess derived from precise measurement of d17O and d18O gives new and additional insights in tracing the…
