| 词条 | Teredolites |
| 释义 |
Teredolites is an ichnogenus of trace fossil, characterized by borings in wood. Clavate (club-shaped) structures rimming mid-Cretaceous Burmese amber from Myanmar, previously misdiagnosed as fungal sporocarps, have recently been shown to be domichnia (crypts) of martesiine bivalves (Pholadidae: Martesiinae), comparable with Teredolites clavatus Leymerie, 1842 and Gastrochaenolites lapidicus Kelly & Bromley, 1984.[1] The substrate was not wood, but amber, hence the term Amberground was coined. See also
References1. ^{{cite journal | author = Smith, R.D.A. |author2=Ross, A.J. | year = 2018 | title = Amberground pholadid bivalve borings and inclusions in Burmese amber: implications for proximity of resin-producing forests to brackish waters, and the age of the amber | journal = Earth and Environmental Science Transactions of the Royal Society of Edinburgh | volume = 107 | issue = 2–3 | pages = 239–247 | doi = 10.1017/S1755691017000287}} External links
2 : Boring fossils|Paja Formation |
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