First measurements of 未17O in speleothem fluid inclusions.
Triple isotope (未D, 未17O, 未18O) compared for the first time in precipitation, drip water and speleothem fluid inclusions.
New insights through 17Oexcess geochemistry in a cave environment and for precipitation.
Isotope monitoring as a prerequisite for paleoclimate reconstruction for Milandre Cave speleothems.