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Pennsylvanian brachiopod,fish and conodont faunas from the Caliza Masiva (San Emiliano Formation) at the Mina Profunda area,Cantabrian Zone,NW Spain
Affiliation:1. Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China;2. Cavanilles Institute of Biodiversity and Evolutionary Biology, University of Valencia, C/Catedràtic José Beltrán Martínez, 2, 46980 Paterna, Valencia, Spain;3. Chengdu Center of China Geological Survey, Chengdu 610081, China;4. State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS), Nanjing 210008, China;5. University of Bristol, Life Sciences Building, Tyndall Avenue, Bristol BS8 1TH, United Kingdom;6. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China;7. Deakin University, Geelong, School of Life and Environmental Sciences & Centre for Integrative Ecology (Burwood Campus), 221 Burwood Highway, Burwood, Victoria, 3125, Australia;8. Wuhan Center of China Geological Survey, Wuhan 430205, China
Abstract:A rock sample obtained from the Caliza Masiva of the San Emiliano Formation (Bashkirian–early Moscovian) in the Mina Profunda area (NE Villamanín) of the Bodón Nappe (Cantabrian Zone, NW Spain) has yielded numerous brachiopods and fish remains not frequently represented in the fossil record. The brachiopod assemblage comprises 13 taxa and is characterized by phosphatic (Langella, Orbiculoidea) as well as exceptionally preserved silicified calcitic elements (a small chonetid, Composita, Crurithyris, Lambdarina, and two minute terebratulids) as the main faunal components. Of special importance is the record of the microbrachiopod Lambdarina winklerprinsi nov. sp., which reduces the large Viséan–Upper Permian gap in the stratigraphic record of this genus. Conodont elements recovered from the same insoluble residue are indicative of the upper Bashkirian Idiognathoides sulcatus parvus Zone. The accompanying fish remains consist of chondrichthyan teeth and scales, an acanthodian scale and osteichthyan tooth-bearing bones, isolated teeth and isolated scales, representing the first Pennsylvanian ichthyoliths analyzed from the Cantabrian Zone. The limestone beds with selective silicification in the San Emiliano Formation provide an exceptional opportunity to improve our knowledge on the patterns of life diversity over geological time.
Keywords:Brachiopod  Ichthyolith  Conodont  San Emiliano Formation  Pennsylvanian  NW Spain
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