Triple isotope (δD, δ17O, δ18O) study on precipitation, drip water and speleothem fluid inclusions for a Western Central European cave (NW Switzerland)-Reference-Cited by-同舟云学术

Triple isotope (δD, δ17O, δ18O) study on precipitation, drip water and speleothem fluid inclusions for a Western Central European cave (NW Switzerland)

Published:2015-11 Issue: Volume:127 Page:73-89
ISSN:0277-3791
Container-title:Quaternary Science Reviews
language:en
Short-container-title:Quaternary Science Reviews

Author:

Affolter Stéphane,Häuselmann Anamaria D.,Fleitmann Dominik,Häuselmann Philipp,Leuenberger Markus

Funder

Swiss National Science Foundation

Publisher

Elsevier BV

Subject

Geology,Archeology,Archeology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Reference91 articles.

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2. Kinetic O-17 effects in the hydrologic cycle: indirect evidence and implications;Angert;Geochim. Cosmochim. Acta,2004

3. Deuterium and oxygen-18 isotope composition of precipitation and atmospheric moisture;Araguas-Araguas;Hydrol. Process,2000

4. Measurement of δ18O and δ2H values of fluid inclusion water in speleothems using cavity ring-down spectroscopy compared with isotope ratio mass spectrometry;Arienzo;Rapid Commun. Mass Sp.,2013

5. Spatial variability in the European winter precipitation delta(18)O-NAO relationship: Implications for reconstructing NAO-mode climate variability in the Holocene;Baldini;Geophys Res. Lett.,2008

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