Poster Number 157
See more from this Division: General Discipline Sessions
See more from this Session: Paleontology (Posters) II - Paleoecology, Taphonomy, and Traces
Abstract:
The study area is characterized by interbedded sandstone, siltstone, and mustone facies, with fine-grained clastics predominating this part of the section. Fossil assemblages in fine clastic facies are autochthonous or parautochthonous. Isolated trilobites (Symphoroides) and bivalves (cf. Grammysia) are preserved within a Cruziana ichnofacies assemblage, wherein Chondrites is common and allochthonous terrestrial plant debris is rare. Allochthonous faunal assemblages characterize all sandstone facies, representing both event and lag concentration deposits. Atrypid (Leptocoelia), strophomenid (Chronostrophiella), rhynconellid (Beachia, Rensselaeria), and spirifid (Acrospirifer, Costispirifer) brachiopods, along with archaeogastropods and tentaculitids, are preserved as casts and molds in size-sorted, fining upwards shell beds generally <0.1 m in thickness.
The outcrops preserve both in situ and transported faunal assemblages deposited in the sublittoral zone of a muddy marine shelf above storm-wave base. Coarser sandstone beds represent event concentrations of more proximal brachiopod communities. These were eroded, size-sorted, and deposited within storm-generated beds in a distal offshore setting. The occasional terrestrial plant fragments indicate proximity to a coastal environment. The influx of plant matter may have been related to high freshwater discharge events associated with storm activity that may have been responsible for shell concentrations.
See more from this Division: General Discipline Sessions
See more from this Session: Paleontology (Posters) II - Paleoecology, Taphonomy, and Traces