The influence of temperature, pH, and growth rate on the δ18O composition of inorganically precipitated calcite

Earth and Planetary Science Letters

Volumn 404, Issue , 2014, Pages 332-343

  Watkins, James M ^a   Hunt, Jonathan D ^b   Ryerson, Frederick J ^b   DePaolo, Donald J ^c,d  

^a UNIVERSITY OF OREGON   (United States)

^b LAWRENCE LIVERMORE NATIONAL LABORATORY   (United States)

^c LAWRENCE BERKELEY NATIONAL LABORATORY   (United States)

^d UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

Calcite; Carbonic anhydrase; Kinetic effects; Oxygen isotopes; Paleothermometry

Indexed keywords

ALKALINITY; CALCITE; CARBONATE MINERALS; CARBONIC ANHYDRASE; CRYSTAL GROWTH; GROWTH RATE; KINETICS; OXYGEN; TEMPERATURE;

KINETIC EFFECT; NON-EQUILIBRIUM EFFECTS; NONEQUILIBRIUM CONDITIONS; OXYGEN ISOTOPE COMPOSITION; OXYGEN ISOTOPE FRACTIONATIONS; OXYGEN ISOTOPES; PALEOTHERMOMETRY; THERMODYNAMIC EQUILIBRIA;

ISOTOPES;

CALCITE; CARBON ISOTOPE; CARBONATE; GROWTH MODELING; GROWTH RATE; ISOTOPIC COMPOSITION; ISOTOPIC FRACTIONATION; OXYGEN ISOTOPE; PALEOTEMPERATURE; PH; REACTION KINETICS; TEMPERATURE EFFECT;

EID: 84906726248     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2014.07.036     Document Type: Article

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