Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774
[email protected] Universidad Nacional Autónoma de México México Pérez Ramos, Olivia; Nestell, Merlynd Permian fusulinids from Cobachi, central Sonora, Mexico Revista Mexicana de Ciencias Geológicas, vol. 19, núm. 1, 2002, pp. 25-37 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57219103 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Revista Mexicana de Ciencias Geológicas,Permian v. 19, núm. fusulinids 1, 2002, from p. 25Cobachi,-37 central Sonora 25 Permian fusulinids from Cobachi, central Sonora, Mexico Olivia Pérez-Ramos1* and Merlynd Nestell2 1 Departamento de Geología, Universidad de Sonora Rosales y Transversal, 83000 Hermosillo, Sonora 2 Geology Department, University of Texas at Arlington, UTA 76019 *e-mail:
[email protected] ABSTRACT Upper Paleozoic rocks in the Cobachi area of central Sonora, Mexico, include the Picacho Colorado and La Vuelta Colorada formation of Carboniferous?-Permian age. A 155 m carbonate succession of the Picacho Colorado Formation, exposed on the east side of Cerro Picacho Colorado, a few kilometers southeast of Cobachi, consists of pinkish and reddish limestone, cherty limestone with some recrystallization, and bioclastic gray limestone. Crinoids, bryozoa, brachiopods and fo- raminifers are present indicating a marine shallow water shelf depositional environment. Well pre- served fusulinaceans occur near the top of the section, but are scarce, partially silicified, and poorly preserved in the middle part and the base of the section.