Resumen

MADHAVARAJU, Jayagopal; SIAL, Alcides N.; GONZALEZ-LEON, Carlos M.  y  NAGARAJAN, Ramasamy. Carbon and oxygen isotopic variations in early Albian limestone facies of the Mural Formation, Pitaycachi section, northeastern Sonora, Mexico. Rev. mex. cienc. geol [online]. 2013, vol.30, n.3, pp.526-539. ISSN 2007-2902.

We used petrofacies analysis and stable isotope data to interpret the isotopic variations in the marine carbonate succession of the Early Cretaceous Mural Formation of northeastern Sonora (Pitaycachi section), Mexico. The petrographic study reveals a range of lithofacies from bioclastic mudstones to boundstones. Allochems consist of corals, algae, rudists, echinoids, sponge spicules, radiolarians, foraminifera and calpionellids. Samples analyzedfor stable isotope are significantly depleted with δ¹⁸O values of -15.19‰ to -6.32‰ and exhibit positive δ¹³C values ranging from 2.91‰ to 4.39‰. The lack of correlation between δ¹³C and δ¹⁸O values also supports a primary marine origin for the δ¹³C values of limestones from the Pitaycachi section. In the δ¹³C profile, the Cánova Member shows an upward increasing trend from 3.09‰ to 4.36‰ interpreted to indicate an increase in the rate of marine organic production and/or organic burial in the basin during early Albian time. The abrupt increase in carbon isotope values in the lower part of the section correlates with OAE1b. The shape of the C-isotope curve of the present study is similar to other C-isotope curves from Mexico and other continents (e.g., Vacontian basin, France) indicating that OAE1b may have been global in extent.

Palabras llave : stable isotopes; petrography; oceanic anoxic events; Pitaycachi section; Mural Formation; Sonora.

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