Asteriacites is a type of five-rayed trace fossil found in marine sedimentary rocks. It records the burrows of ophiuroid and asteroid sea stars on the sea floor. Asteriacites is found in European and American rocks, from the Ordovician period onwards, and is especially numerous in the Triassic and Jurassic systems.[2][3][4]
Dense assemblages of Asteriacites ('Asteriacites beds') are considered proxies for marine settings, low bioturbation intensity, shallow tiering, high sedimentation rate and/or event-bed deposition, significant levels of hydrodynamic energy, and low predation pressure.[4]
^Mángano, M.G.; Buatois, L.A.; West, R.R.; Maples, C.G. (1999). "The origin and paleoecologic significance of the trace fossil Asteriacites in the Pennsylvanian of Kansas and Missouri". Lethaia. 32 (1): 17–30. Bibcode:1999Letha..32...17M. doi:10.1111/j.1502-3931.1999.tb00577.x.
^ abBaucon, A., Neto de Carvalho, C. 2016. Stars of the aftermath: Asteriacites beds from the Lower Triassic of the Carnic Alps (Werfen Formation, Sauris di Sopra), Italy. Palaios 31. Abstract available at http://www.tracemaker.com