''Gastrochaenolites'' is a trace fossil formed as a clavate (club-shaped) boring in a hard substrate such as a shell, rock or carbonate hardground. The aperture of the boring is narrower than the main chamber and may be circular, oval, or dumb-bell shaped (Kelly and Bromley, 1984). ''Gastrochaenolites'' is most commonly attributed to bioeroding bivalves such as '' Lithophaga'' and ''Gastrochaena'' (Kleeman, 1980). The fossil ranges from the

Ordovician The Ordovician ( ) is a geologic period and system, the second of six periods of the Paleozoic Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start of the Silurian Period Mya. ...

to the Recent (Taylor and Wilson, 2003; Vinn and Wilson, 2010). The first Lower Jurassic ''Gastrochaenolites'' ichnospecies is ''Gastrochaenolites messisbugi'' Bassi, Posenato, Nebelsick, 2017. This is the first record of boreholes and their producers (mytilid bivalves) in one of the larger bivalves of the globally occurring Lithiotis fauna which is a unique facies in the Lower Jurassic Tethys and Panthalassa.

References

* * * * * * {{cite journal , author = Bassi, D., Braga, J.C., Owada, M., Aguirre, J., Lipps, J.H., Takayanagi, H., Iryu, Y. , year = 2020 , title = Boring bivalve traces in modern reef and deeper water macroid and rhodolith beds , journal = Progress in Earth and Planetary Science , volume = 7 , doi = 10.1186/s40645-020-00356-w, doi-access = free

External links

''Gastrochaenolites'' systematics and diagrams (in German).
Boring fossils