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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Primary terms
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Siwalik System (1)
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Neogene
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upper Miocene
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Pliocene
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middle Pliocene (1)
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Paleogene
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middle Eocene
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Suiformes
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Proboscidea
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Invertebrata
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Protista
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isotopes
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O-18/O-16 (27)
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upper Campanian (1)
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Fruitland Formation (1)
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Hell Creek Formation (1)
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Judith River Formation (1)
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Kaiparowits Formation (1)
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Maestrichtian
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lower Maestrichtian (1)
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Senonian (1)
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Two Medicine Formation (1)
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Jurassic
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Mexico
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enamel
Why the long teeth? Morphometric analysis suggests different selective pressures on functional occlusal traits in Plio-Pleistocene African suids
OXYGEN ISOTOPE PROFILES OF UPPERMOST JURASSIC VERTEBRATE TEETH AND OYSTER SHELLS: A RECORD OF PALEOENVIRONMENTAL CHANGES AND ANIMAL HABITATS
Enamel hypoplasia and dental wear of North American late Pleistocene horses and bison: an assessment of nutritionally based extinction models
STUDY OF DEFLUORIDATION OF WATER USING NATURAL CLAY MINERALS
Abstract: Pterosaur fossils are rare in the Morrison Formation, and most are poorly preserved. The Breakfast Bench Facies (BBF) at Como Bluff produces incomplete but uncrushed limbs. One proximal and two distal femora match a complete femur (BYU 17214) referred to Mesadactylus . Unexpectedly, both of the BBF distal femora possess a large intercondylar pneumatopore. BYU 17214 also possesses an intercondylar pneumatopore, but it is smaller than in the BBF femora. Distal femoral pnuematicity is previously recognized only in Cretaceous azhdarchoids and pteranodontids. A peculiar BBF jaw fragment shows strongly labiolingually compressed, incurved crowns with their upper half bent backwards; associated are anterior fangs. We suspect this specimen is a previously undiagnosed pterosaur. Additional BBF material documents a diverse pterosaur fauna including a humerus with a greatly expanded ectepicondyle possibly from a non-pterodactyloid monofenestratan.