Karst-bauxite formation during the Great Oxidation Event indicated by dating of authigenic rutile and its thorium content.

ABSTRACT: Aluminium (Al)-rich palaeosols-i.e., palaeobauxite deposits-should have formed in karst depressions in carbonate sequences as a result of acidic solutions from oxidative weathering of sulfide minerals during the Great Oxidation Event (GOE), but no GOE-related karst-palaeobauxite deposits have so far been recorded. Here, we report results of in situ uranium-lead (U-Pb) dating of detrital zircon and spatially associated rutile from a metamorphosed Al-rich rock within a dolomite sequence in the Quadrilátero Ferrífero (QF) of Minas Gerais, Brazil, known as the Gandarela Formation. Rutile grains are highly enriched in thorium (Th = 3-46 ppm; Th/U ratio = 0.3-3.7) and yielded an isochron, lower-intercept age of ca. 2.12 Ga, which coincides with the final phase of the GOE-i.e., the Lomagundi even

SUBMITTER: Cabral AR 

PROVIDER: S-EPMC10224920 | biostudies-literature | 2023 May

REPOSITORIES: biostudies-literature