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Advances on Stratigraphy and Paleontology of the Muhi Quarry from the Mid-Cretaceous (Albian-Cenomanian) of Hidalgo, Central Mexico

机译:墨西哥中部伊达尔戈白垩纪中期(阿尔贝-西诺曼尼亚)穆希采石场的地层学和古生物学研究进展

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The Muhi quarry of Zimapán Hidalgo, Central México, is one of the most important Cretaceous fish localities of the country because of the great diversity of fishes, and the significance of their record in America. Here we present some advances of the stratigraphy, including a litostratigraphic description, a generalized report of the marine fauna recovered, and the depositional environment of the outcrop. The sequence consists of a light gray mudstone/biomicrite, with chert forming nodules and/or thin layers, and additional marls are intercalated; the strata are assigned to La Negra Facies of the Mid-Cretaceous (Albian-Cenomanian) El Doctor Formation from northeastern Querétaro, south-central and northwestern Hidalgo (this report). The lithology and fossils are indicative of open sea shelf to deep shelf margin Standard Facies Zones, comparable to the Standard Micro facies Types SMF 2 (microbioclastic limestone) and SMF 3 (pelagic mudstone).
机译:墨西哥中部ZimapánHidalgo的Muhi采石场是该国最重要的白垩纪鱼类产地之一,因为鱼类种类繁多,而且在美国的记录意义重大。在这里,我们介绍了地层学的一些进展,包括岩石地层学描述,关于海洋动物群的概括性报告以及露头的沉积环境。该层序由浅灰色的泥岩/生物微粒组成,石形成结节和/或薄层,并插入了其他泥灰岩。地层被分配给了东北克雷塔罗,中南部和西北伊达尔戈(Hidalgo)的白垩纪中部(阿尔伯-西诺曼尼亚)El Doctor层的La Negra相。岩性和化石是指示海陆架至深陆架缘的标准相带,与标准微相类型SMF 2(微生碎屑石灰石)和SMF 3(远洋泥岩)相当。

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