Ammonites from the Pawpaw Shale (Upper albian) in northeast Texas

The lower part of the Pawpaw Shale in northeast Texas yields an abundance of diminutive limonitic ammonites. the assemblage being: Tetragonites sp. juv., Engonoceras serpentinum (Cragin, 1900), Conlinites wrighri gen. et sp. nov., Caniabrigites wenoensis 14 (Adkins, 1920), Neophlycticeras (Neophlycticeras) sp., Neophlycticeras (Paradolphia) occidentalis sp. nov., Stoliczkaia(Stoliczkaia) clavigera Neumayr, 1875, Stoliczkaia (Lamnayella) worthense (Adkins, 1920), Stoliczkaia (Shuminaia) asiatica Matsumoto and Inoma, 1975, Enigmaticeras riceae gen. et sp. nov., Flickia simplex Pervinquiere, 1907, Ficheuria pernoni Dubourdieu, 1953, Ficheuria americana sp. nov., Anisoceras armatum (J. Sowerby, 1817), Hamites venetzianus Pictet, 1847, Mariella(Mariella) worthensis (Adkins and Winton, 1920), Mariella (Mariella) asper sp. nov., Lechites (Lechites) comanchensis (Adkins, 1920). Worthoceras worthense (Adkins, 1920). and Scaphites hilli Adkins and Winton, 1920. This assemblage is correlated with the Mortoniceras (Subschloenbachia) rostratrum Subzone of the European sequence on the basis of the occurrence of that species in the underlying Weno Limestone, in the passage beds between the Pawpaw Shale and the succeeding Main Street Limestone, and the lower part of the Main Street. Some previous authors have interpreted the diminutive limonitic ammonites of the Pawpaw as being "dwarf" or "stunted". The overwhelming majority of individuals are nuclei Of Much larger ammonites. with smaller numbers of adults of small species that occur in other facies and geographic locations. together with a smaller number still of paedomorphic dwarfs. The fauna is interpreted as a preservational one, where diagenetic pyrite formed in relatively small voids. either the early phragmocone chambers of larger ammonites, or the phragmocone and body chambers of genuinely diminutive species which oxidised to limonite during the weathering process. (C) 2004 Elsevier Ltd. All rights reserved.