ASGP (2015), vol. 85: 427–432

CYLINDRICHNUS CONCENTRICUS TOOTS IN HOWARD, 1966 (TRACE FOSSIL) IN ITS TYPE LOCALITY, UPPER CRETACEOUS, WYOMING

Allan A. EKDALE & Sherie C. HARDING

Department of Geology and Geophysics, University of Utah, Room 383 FASB, 115 South 1460 East, Salt Lake City, UT 84112-0102, USA; e-mail: a.ekdale at utah.edu

Ekdale, A. A. & Harding, S. C., 2015. Cylindrichnus concentricus Toots in Howard, 1966 (trace fossil) in its type locality, Upper Cretaceous, Wyoming. Annales Societatis Geologorum Poloniae, 85: 427–432.

Abstract: Cylindrichnus concentricus is a wide spread trace fossil in shallow marine sedimentary rocks of Mesozoic and Cenozoic age. This paper clarifies the ichnotaxonomy of C. concentricus by of fering an emended diagnosis of the ichnogenus and a new diagnosis of the ichnospecies. The broad, bow-shaped architecture of C. concentricus with two openings at the sediment surface suggests that the trace maker was either a filter-feeding animal that captured suspended food particles from the water column or else a surface deposit feeder that employed tentacles or an eversible pharynx to collect nutritious sediment from the surface around one or both of the burrow openings. Although C. concentricus has been reported in a variety of different sedimentary environments around the world, in its type locality in the Cretaceous of Wyoming the trace fossilis found in low-diversity or monoichnospecific beds that exhibit hummocky cross stratification. This occurrence suggests the burrower’s tolerance (or perhaps preference) for an episodic high-energy hydrodynamic environmentre lated to major storms.

Manuscript received 18 October 2014, accepted 7 April 2015