| Gastrochaenolites | |
|---|---|
| Gastrochaenolites (G) andEntobia (E) in limestone cobble from the Los Banós Formation, Upper Miocene, SE Spain. | |
| Trace fossil classification | |
| Ichnofamily: | †Gastrochaenolitidae |
| Ichnogenus: | †Gastrochaenolites Leymerie, 1842 |
| Type ichnospecies | |
| Gastrochaenolites lapidicus Kelly & Bromley, 1984 | |
| Ichnospecies[1] | |
| |
| Synonyms[1] | |
| |
Gastrochaenolites is atrace fossil formed as a clavate (club-shaped) boring in a hard substrate such as a shell, rock or carbonatehardground. The aperture of the boring is narrower than the main chamber and may be circular, oval, or dumb-bell shaped.[2]Gastrochaenolites is most commonly attributed tobioeroding bivalves such asLithophaga andGastrochaena.[3] The fossil ranges from theOrdovician to the Recent.[4][5] The first Lower JurassicGastrochaenolites ichnospecies isGastrochaenolites 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.
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