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The Rio Limay Subgroup is a geological unit in Neuquen, Argentina whose strata date back to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formations it contains.〔Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Cretaceous, South America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 600-604. ISBN 0-520-24209-2.〕 Having previously been considered a distinct formation, the Rio Limay Subgroup is now considered a member of the larger Neuquén Group, and itself contains several specific geological formations (from youngest to oldest): * Cerro Lisandro Formation (late Cenomanian to early Turonian) * Huincul Formation (late Cenomanian) * Candeleros Formation (early Cenomanian) ==See also== * List of dinosaur-bearing rock formations 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Rio Limay Subgroup」の詳細全文を読む スポンサード リンク
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