MORTON, J.D., WHITESIDE, D.I., HETHKE, M., BENTON, M.J. 2017. Biostratigraphy and geometric morphometrics of conchostracans (Crustacea, Branchiopoda) from the Late Triassic fissure deposits of Cromhall Quarry, UK. Palaeontology, 60, 3, 349-374. DOI: 10.1111/pala.12288
Jacob D. Morton, David I. Whiteside, Manja Hethke, and Michael J. Benton- Jacob D. Morton - School of Earth Sciences University of Bristol Bristol UK (Email: jm15205.2015@my.bristol.ac.uk)
- David I. Whiteside - School of Earth Sciences University of Bristol Bristol UK (Email: david.whiteside@bristol.ac.uk)
- Manja Hethke - Institut für Geologische Wissenschaften Freie Universität Berlin Berlin Germany (Email: manja.hethke@fu-berlin.de)
- Michael J. Benton - School of Earth Sciences University of Bristol Bristol UK (Email: mike.benton@bristol.ac.uk)
- Issue published online: 26 April 2017
- Manuscript Accepted: 08 February 2017
- Manuscript Received: 27 November 2016
The enigmatic fissure deposits of south‐western England and southern Wales are famous for their unique assemblage of Late Triassic vertebrates, although their age is contentious. While recent studies of palynomorphs have dated some as Rhaetian, their conchostracan (Crustacea, Branchiopoda) assemblages have not been described in detail nor used in biostratigraphy. We find that species determination of British Late Triassic conchostracans requires detailed observations of size, shape and ornamentation. We provide evidence that although Euestheria brodieana is invariably smaller than E. minuta, with some slight differences in carapace ornamentation, the traditional view that they are very similar is upheld. The use of conchostracans as a biostratigraphical tool is here tested by application to the British Triassic fissures at Cromhall quarry where the usual stratigraphical evidence provided by superposition is absent. We find no distinction between conchostracans from bedded Rhaetian deposits of the UK and specimens collected from the fissure deposits of Cromhall Quarry, Gloucestershire, supporting a late Rhaetian age for these deposits.
Data for this study are available in the Dryad Digital Repository https://doi.org/10.5061/dryad.m17c8 Wiley Online Library