Are oxygen isotope fractionation factors between calcite and water derived from speleothems systematically biased due to prior calcite precipitation (PCP)?
Michael Deininger, Maximilian Hansen, Jens Fohlmeister, Andrea Schröder‐Ritzrau, Yuval Burstyn, Denis Scholz
Topics & Concepts
CalciteSpeleothemIsotopes of oxygenGeologyEquilibrium fractionationCaveCarbonateKarstIsotope fractionationδ18OGeochemistryStalagmiteOxygen isotope ratio cycleStable isotope ratioMineralogyFractionationChemistryPaleontologyHoloceneArchaeologyHistoryPhysicsOrganic chemistryQuantum mechanicsKarst Systems and HydrogeologyGeology and Paleoclimatology ResearchGroundwater and Isotope Geochemistry