A Kinetic Difference Between 12C‐ and 13C‐Bound Oxygen Exchange Rates Results in Decoupled δ18O and Δ47 Values of Equilibrating DIC Solutions. (9th August 2018)

• Record Type: Journal Article
• Authors: Staudigel, Philip T.; Swart, Peter K.
• Is Part Of: Geochemistry, geophysics, geosystems. Volume 19:Number 8(2018)
• Page Start: 2371
• Page End: 2383
• Publication Date: 2018-08-09
• Subjects: clumped isotopes -- oxygen isotopes -- dissolved inorganic carbonate -- kinetic isotope effects -- paleotemperature; Geochemistry -- Periodicals; Geophysics -- Periodicals; Earth sciences -- Periodicals; 550.5
• DOI: 10.1029/2018GC007500
• Languages: English
• ISSNs: 1525-2027

Abstract

Abstract: Accurate determination of paleotemperatures using carbonate δ 18 O and Δ47 values rely upon the assumption that the minerals in question formed close to expected isotopic equilibrium with their environment. If there is insufficient time for dissolved carbonate to equilibrate with water between the production of DIC and mineralization, the mineral may preserve a disequilibrated isotopic state. The equilibrium composition and rate of DIC equilibration are related to the temperature, pH, and salinity of the solution, and these have been quantified in previous studies which investigated this via the quantitative precipitation all dissolved carbonate species (∑DIC ) as barium carbonate (BaCO3 ). Here we present a study wherein the equilibration over time of clumped isotopes (Δ47 ) is investigated at 5, 15, and 25 °C. Results show a significant non–first‐order behavior for this process, which can be explained with a kinetic isotope effect wherein oxygen bound to 12 C will exchange more rapidly than oxygen bound to 13 C. This difference in equilibration rates is minor, less than 2%; however, it results in Δ47 values paradoxically becoming initially less equilibrated during initial equilibration. The magnitude and direction of this effect is expected to vary depending on the direction from which δ 18 O values equilibrate, even in circumstances where the initial and final Δ47 values are identical. The implication of this finding is that carbonates which form rapidly can have decoupled δ 18 O and Δ47 values. This study presents a mathematical framework wherein this behavior can be described accurately to provide a predictive model for describing equilibrating aqueous systems. Plain Language Summary: A subtle <2% difference in reaction rates of oxygen bound to the heavier isotope of carbon results in an effect which can alter a commonly used paleothermometer, potentially resulting in inaccurate estimates of ancient water temperatures. By studying this process in the lab, the magnitude of this effect was measured, and a mathematical model can be used to predict the effect it may have had in a variety of natural systems. Key Points: A subtle difference in reaction rates of different isotopes of carbon has been measured in dissolved inorganic carbonate This effect results in decoupled equilibration behaviors of the δ 18 O and Δ47 paleothermometers