The Lilstock Formation is a geologic formation in England. It preserves bivalve, insect and other invertebrate fossils, as well as fossil fish of Agkistracanthus mitgelensis and the basal theropod dinosaur Newtonsaurus cambrensis dating back to the Rhaetian of the Triassic period.

White Lias

The White lias is a rare, fine-grained form of limestone from the late Triassic period, occurring only in certain parts of Somerset and infrequently in Warwickshire. It gets the name ‘lias’ from the quarrymen's dialect for ‘layers’, referring to its natural state when quarried.

White lias is part of the Langport Member of the Lilstock Formation, a multi-layered bed of stone formed from shale and limestone. At its base is a bone-bed yielding ancient marine, reptilian and ammonite fossils.

White lias varies in colour from white-cream to pale grey and is traditionally used for building and flooring. Evidence of its use can be seen in manor houses, churches and cathedrals all over the UK. It is most prevalent in the Somerset towns of Midsomer Norton, Radstock, Langport and Wincanton. Bowdens quarry in Langport is the only supplier of white lias, and of the more commonly found blue lias and grey varieties.

Fossil content

Color key Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon MorphotaxonNotes Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
TaxonReclassified taxonTaxon falsely reported as presentDubious taxon or junior synonymIchnotaxonOotaxonMorphotaxon

Dinosaurs

Theropods

Theropods of the Lilstock Formation
GenusSpeciesLocationStratigraphic positionMaterialNotesImages
NewtonsaurusN. cambrensisA coelophysoid theropod

Fish

Cartilaginous Fish

Cartilaginous Fish of the Lilstock Formation
GenusSpeciesLocationStratigraphic positionMaterialNotesImage
AgkistracanthusA. mitgelensisA myriacanthid chimaeriform

See also

Further reading

  • P. B. Brodie. 1845. A History of the Fossil Insects in the Secondary Rocks of England Accompanied by a Particular Account of the Strata in which they Occur, and of the Circumstances Connected with their Preservation 1-130
  • C. J. Duffin. 1994. Myriacanthid holocephalans (Chondrichthyes) from the British Late Triassic. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen 192(1):1-16