S
Stuart A. Robinson
Researcher at University of Oxford
Publications - 80
Citations - 3887
Stuart A. Robinson is an academic researcher from University of Oxford. The author has contributed to research in topics: Cretaceous & Paleogene. The author has an hindex of 29, co-authored 78 publications receiving 3073 citations. Previous affiliations of Stuart A. Robinson include University College London & University of Reading.
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Journal ArticleDOI
Terrestrial and marine extinction at the Triassic-Jurassic boundary synchronized with major carbon-cycle perturbation: A link to initiation of massive volcanism?
TL;DR: In this article, organic carbon isotope data from the UK and Greenland demonstrate that changes in flora and fauna from terrestrial and marine environments occurred synchronously with a light isotope excursion, and that this happened earlier than the Triassic-Jurassic boundary marked by ammonites in the UK.
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Cretaceous sea-surface temperature evolution: Constraints from TEX86 and planktonic foraminiferal oxygen isotopes
Charlotte L O'Brien,Stuart A. Robinson,Richard D. Pancost,Jaap S. Sinninghe Damsté,Stefan Schouten,Daniel J. Lunt,Heiko Alsenz,André Bornemann,André Bornemann,Cinzia Bottini,Simon C. Brassell,Alexander Farnsworth,Astrid Forster,Brian T. Huber,Gordon N. Inglis,Hugh C. Jenkyns,Christian Linnert,Kate Littler,Paul J. Markwick,Alison McAnena,Jörg Mutterlose,B. David A. Naafs,Wilhelm Püttmann,Appy Sluijs,Niels A. G. M. van Helmond,Johan Vellekoop,Thomas Wagner,Neil Wrobel +27 more
TL;DR: In this article, a compilation and synthesis of available planktonic foraminiferal δ18O and TEX86-SST proxy data for almost the entire Cretaceous Period is presented.
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A review of palaeoclimates and palaeoenvironments in the Levant and Eastern Mediterranean from 25,000 to 5000 years BP: setting the environmental background for the evolution of human civilisation
TL;DR: In this article, the authors conducted an extensive and up-to-date review of terrestrial and marine climatic conditions in the Levant and Eastern Mediterranean during the last 25,000 years.
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Sea-level change and facies development across potential Triassic-Jurassic boundary horizons, SW Britain
TL;DR: In this article, a sea-level lowstand surface of erosion is inferred to occur within the Cotham Member of the Lilstock Formation, a unit deposited in an environment that was often subaerially exposed.
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Evidence for global cooling in the Late Cretaceous
Christian Linnert,Stuart A. Robinson,Jackie A. Lees,Paul R. Bown,Irene Pérez-Rodríguez,Maria Rose Petrizzo,Francesca Falzoni,Kate Littler,José A. Arz,Ernest E. Russell +9 more
TL;DR: A record of SSTs for the Campanian–Maastrichtian interval from hemipelagic sediments deposited on the western North Atlantic shelf reveals that the North Atlantic was relatively warm in the earliest Campanian, but experienced significant cooling after this, suggesting that the cooling pattern was global rather than regional and, therefore, driven predominantly by declining atmospheric pCO2 levels.