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all geography including DSDP/ODP Sites and Legs
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South America
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fossils
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Mesozoic
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Jurassic
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Chordata
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Neusticemys neuquina
New cranial fossils of the Jurassic turtle Neusticemys neuquina and phylogenetic relationships of the only thalassochelydian known from the eastern Pacific
Diagnostic characters of Neusticemys neuquina from Tithonian levels of Va...
Neusticemys neuquina from the Titthonian level of Vaca Muerta Formation, p...
Neusticemys neuquina from Tithonian levels of Vaca Muerta Formation, photo...
Neusticemys neuquina from Tithonian levels of Vaca Muerta Formation, photo...
Neusticemys neuquina from Tithonian levels of Vaca Muerta Formation, photo...
Stratigraphic column and map showing outcrops of Vaca Muerta Formation at C...
Thalassochelydian synapomorphies on the skull and lower jaw of Neusticemys...
JPA volume 94 issue 1 Cover and Back matter
JPA volume 94 issue 1 Cover and Front matter
Jurassic marine reptiles of the Neuquén Basin: records, faunas and their palaeobiogeographic significance
Abstract The largest diversity of Jurassic marine reptiles from Gondwana has been recorded in the Neuquén Basin. Although the Early Jurassic records are limited, the records from the Middle Jurassic, especially the early Bajocian plesiosaurs and ichthyosaurs, are unique in the world. The highest abundance and taxonomic diversity is recorded from the Late Jurassic (Tithonian). Pleurodiran ( Notoemys ) and cryptodiran turtles ( Neusticemys ), ichthyosaurs ( Ophthalmosaurus, Caypullisaurus ), pliosaurs ( Pliosaurus, Liopleurodon ) and crocodilians ( Geosaurus, Metriorhynchus, Dakosaurus ) are members of this rich marine herpetofauna. Except for Notoemys, the other reptiles are pelagic. Their habits and large size ( Caypullisaurus, Liopleurodon, Dakosaurus ) suggest that they entered the sheltered Neuquén Basin occasionally, possibly for reproduction in protected areas. The model of a protected basin, open to the Pacific Ocean through gaps in an emergent by island-arc complex, fits well with the ecological requirements inferred for most of the pelagic reptiles. The Caribbean Corridor may also have played a significant role as a seaway at least during the Middle Jurassic and probably before. New findings in Tithonian and Berriasian sediments of the Neuquén Basin suggest that there was no massive extinction among the marine herpetofauna at the Jurassic–Cretaceous boundary.