Gastrochaenolites hospitium isp. nov., trace fossil by a coral-associated boring bivalve from the Eocene and Miocene of Austria

Gastrochaenolites hospitium isp. nov. is a domichnial boring showing the so-called false floors in scleractinian coral skeletons. The borings are semi-circular in mid-longitudinal section. They are produced by the mytilid Lithophaga (Leiosolenus) and keep up with further growth of their hosts for years. The false floors, being a retrusive equilibrium trace, are related to annual events.