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This assessment of dinosaur discoveries in Mexico synthesizes present information regarding the geography and setting of the quarter in the course of the Mesozoic while it was once the western margin of the traditional continent of Pangea. The booklet summarizes learn on a number of teams, together with turtles, lepidosauromorphs, plesiosaurs, crocodyliforms, pterosaurs, and final yet no longer least, dinosaurs. furthermore, chapters concentrate on trackways and different hint fossils and on K/P boundary (the Chicxulub crater, underneath the Gulf of Mexico, has been hypothesized because the website of the boloid influence that killed off the dinosaurs). Dinosaurs and different Reptiles from the Mesozoic of Mexico is an updated, informative quantity on a space that has now not been comprehensively defined till now.
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Additional resources for Dinosaurs and Other Reptiles from the Mesozoic of Mexico
Revista Mexicana de Ciencias Geológicas 22:401–418. Vega, F. , M. del C. Perrilliat, L. DuarteTorres, G. Durán-Herrera, R. RivasGarcía, M. Aguilar-Piña, and J. F. Ventura. 2007. Eocene strata from Sabinas Basin and their bearing in sedimentary basin correlation in NE Mexico. Boletín de la Sociedad Geológica Mexicana 59:115–123. Vega-Vera, F. , L. M. Mitre-Salazar, and E. Martinez-Hernandez. 1989. Contribución al conocimiento de la estratigrafía del Grupo Difunta (Cretácico superior-Terciario) en el Noreste de México.
The orogeny was non-igneous. In northeastern Mexico, folding principally occurred along the Upper Jurassic Minas Viejas evaporite unit, using this horizon as a shear and slide zone. In this area of the SMO foldbelt, outcrops of Upper Jurassic sediments are thus found only in the center of anticlines and diapiric domes. Laramide foreland deformation in the Difunta Group was less intensive than in the SMO and also culminated through the early Paleogene. , 2000). During the Paleogene, a change in subduction style at the western active continental margin of Mexico caused magmatism in or near the Gulf coastal plain east of and parallel to the Sierra Madre Oriental.
T. Adatte, W. Stinnesbeck, M. Affolter, L. Schilli, and J. G. López-Oliva. 2002. Multiple spherule layers in the late Maastrichtian of northeastern Mexico; pp. 145–161 in C. Koeberl and K. G. ), Catastrophic Events and Mass Extinctions: Impacts and Beyond. Geological Society of America Special Paper 356. Kirkland, J. , R. P. Gates, S. Gregory, S. Nesbitt, C. I. Serrano-Brañas, and J. P. Garcia-de la Garza. 2006. Large hadrosaurine dinosaurs from the latest Campanian of Coahuila, Mexico; pp. 299–315 in S.