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C- and Sr-isotope data for marine carbonates can provide a detailed record of isotopic variations in seawater through time and have proven to be a valuable tool for interpreting biogeochemical events and correlating Neoproterozoic sedimentary successions worldwide. Negative carbon isotope excursion to values as low as −4.5‰ in the Ediacaran Polanco Limestones Formation, Uruguay has been interpreted...
The occurrence of the Vendian to lowermost Cambrian Arroyo del Soldado Group (ASG) is reported from an area located to the SW of Minas, which was formerly mapped as part of the Lavalleja Group. The Yerbal, Polanco and Cerro Espuelitas Formations of the ASG occur there as a rather continuous, microfossil-rich sedimentary cover, intruded by granites of probable Cambrian age (Minas Granite). Organic-walled...
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