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A lower Carboniferous (Visean) tetrapod trackway represents the earliest record of an edopoid amphibian from the UK
Published 2019“…We present a rare ichnological insight into early Carboniferous tetrapod diversification in the United Kingdom based on a Visean-aged specimen collected from an interdistributary trough palaeoenvironment at Hardraw Scar, Wensleydale, North Yorkshire. This specimen represents the stratigraphically oldest known tetrapod trackway from the UK. …”
Journal article -
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A potential global stratotype for the Sinemurian-Pliensbachian boundary (Lower Jurassic), Robin Hood's Bay, UK: ammonite faunas and isotope stratigraphy
Published 2000“…Robin Hood's Bay (North Yorkshire, UK) fulfils the criteria for definition as the Global Stratotype Section and Point (GSSP) for the base of the Pliensbachian Stage (Lower Jurassic). …”
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The seasonal climate of the Early-Middle Jurassic, Cleveland Basin, England
Published 1999“…Diverse aspects of the fossil floras of the Early to Middle Jurassic (Cleveland Ironstone and Dogger Formations and Ravenscar Group; Pliensbachian-Bathonian stages) of North Yorkshire, England, have been investigated in order to better define the prevailing Early-Middle Jurassic paleoclimate. …”
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Between the caves and the sea: the Late Glacial occupation of the English East Midlands
Published 2022“…Further attention has been directed towards lithic typological and technological attribute analyses of three open-air site assemblages (Farndon Fields, Nottinghamshire, Seamer Carr K, North Yorkshire, and Risby Warren, North Lincolnshire).…”
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A proposal for the Global Boundary Stratotype Section and Point (GSSP) for the base of the Pliensbachian Stage (Lower Jurassic)
Published 2003“…Wine Haven, a coastal exposure at Robin Hood's Bay (North Yorkshire, UK), fulfils the criteria indicated in the Guidelines of the International Commission on Stratigraphy (ICS) (Remane et al. 1996) for definition as the Global Stratotype Section and Point (GSSP) for the base of the Pliensbachian Stage (Early Jurassic): 1) The succession of about 30m comprises pale grey and buff-coloured sandy mudstones which very gradually pass upward into silty dark grey shales. …”
Journal article