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The life and times of Pteridinium simplex
INSIGHTS FROM A MONOSPECIFIC LINGULID BRACHIOPOD BED IN THE LATE DEVONIAN OF SOUTH AFRICA
An abundance- and morphology-based similarity index
8. MAN AND THE TERRESTRIAL MILIEU
Developmental change during a speciation event: evidence from planktic foraminifera
Exposure forecasting for seismic risk estimation: Application to Costa Rica
Scratching the discs: evaluating alternative hypotheses for the origin of the Ediacaran discoidal structures from the Cerro Negro Formation, La Providencia Group, Argentina
All Sizes Fit the Red Queen
Depositional processes and environmental settings in rock shelters: the case of the prehistoric Oscurusciuto site (Southern Italy)
Testing size–frequency distributions as a method of ontogenetic aging: a life-history assessment of hadrosaurid dinosaurs from the Dinosaur Park Formation of Alberta, Canada, with implications for hadrosaurid paleoecology
A nearshore Hirnantian brachiopod fauna from South China and its ecological significance
Pliocene and Late Pleistocene actinopterygian fishes from Santa Maria Island, Azores (NE Atlantic Ocean): palaeoecological and palaeobiogeographical implications
Spot the difference: Zircon disparity tracks crustal evolution: REPLY
CONCH FRITTERS THROUGH TIME: HUMAN PREDATION AND POPULATION DEMOGRAPHICS OF LOBATUS GIGAS ON SAN SALVADOR ISLAND, THE BAHAMAS
Modeling durophagous predation and mortality rates from the fossil record of gastropods
Testing for human impacts in the mismatch of living and dead ostracode assemblages at nested spatial scales in subtropical lakes from the Bahamian archipelago
Assessment of the Effect of Increasing Temperature On the Ecology and Assemblage Structure of Modern Planktic Foraminifers in the Caribbean and Surrounding Seas
Intraspecific variation in cephalopod conchs changes during ontogeny: perspectives from three-dimensional morphometry of Nautilus pompilius
The pterosaur assemblage of the Oxford Clay Formation (Jurassic, Callovian–Oxfordian) from the UK
Abstract: The Middle–Upper Jurassic Oxford Clay Formation of the UK is a highly productive fossiliferous unit, containing numerous fossils of marine and terrestrial vertebrates. Despite this abundance, pterosaurs make up only a tiny percentage of the assemblage. There are currently only seven specimens accessioned in the Oxford University Museum of Natural History and Natural History Museum, London. Of these, only one specimen (an association of material from a juvenile animal) has been named, identified as Rhamphorhynchus jessoni . Following a detailed examination, it is identified here as lacking any autapomorphies and the species R . jessoni is considered a nomen dubium . The other Oxford Clay Formation pterosaur fossils are similarly identified as indeterminate, except for an isolated scapulocoracoid which is positively identified as Rhamphorhynchus sp. The rarity of pterosaurs is attributed to a combination of the fragility of their bones and the tendency of volant animals to have low population densities at sea.