238U/235U measurement in single-zircon crystals: implications for the Hadean environment, magmatic differentiation and geochronology. Issue 10 (21st August 2019)

• Record Type: Journal Article
• Authors: Tissot, François L. H.; Ibanez-Mejia, Mauricio; Boehnke, Patrick; Dauphas, Nicolas; McGee, David; Grove, Timothy L.; Harrison, T. Mark
• Is Part Of: Journal of analytical atomic spectrometry. Volume 34:Issue 10(2019)
• Page Start: 2035
• Page End: 2052
• Publication Date: 2019-08-21
• Subjects: Atomic spectra -- Periodicals; Atomic absorption spectroscopy -- Periodicals; 543.0858
• DOI: 10.1039/c9ja00205g
• Languages: English
• ISSNs: 0267-9477

Abstract

Abstract : We present novel analytical methods allowing the precise determination of the uranium isotopic composition ( 238 U/ 235 U) of single zircon crystals. Abstract : Owing to the challengingly small amounts of uranium (U) they contain, the isotopic composition ( 238 U/ 235 U) of single zircon grains has never been measured. Leveraging methods we designed for analysis of small sample amounts and modern MC-ICPMS instruments, we show that precise (±0.04 to ±0.25‰) single-zircon 238 U/ 235 U measurements are now possible. We report data for 31 single grains from the Jack Hills conglomerate, and 3 reference zircon localities (FC-1, R33 and Temora). Consistent with the reducing conditions implied by the small Ce anomalies of many Hadean zircon, Jack Hills grains display only small δ 238 U variations (from −0.60 to −0.12‰). The distribution is centered on the average chondritic and bulk continental crust value, arguing against the widespread existence of Oklo-type reactors in the early Earth. The subtle δ 238 U variations in Jack Hills zircons are more plausibly explained by a small (∼0.10%) mass-dependent equilibrium isotope fractionation between at least one U-bearing accessory mineral and silicate melts, during magmatic differentiation under reducing conditions. In contrast, the large δ 238 U difference between pooled titanite and pooled zircon fractions from the Fish Canyon Tuff sample suggests larger isotope effects during igneous fractional crystallization under oxidizing conditions (∼QFM+2), with preferential removal of 235 U from the melt and into zircon, and/or other accessory phases. We estimate that ∼50% of zircon dated by the CA-ID-TIMS method would be amenable to single-grain U isotope measurements, making this method widely applicable to future studies. This would enable (i) improvements in precision and accuracy of U–Pb and Pb–Pb dates, (ii) accurate investigation of U-series disequilibrium contribution to U–Pb discordance, and (iii) accurate re-evaluation of U decay constants.