Marcusodictyon
| Marcusodictyon Temporal range: late Cambrian–Early Ordovician | |
|---|---|
| Scientific classification | |
| Kingdom: | Animalia |
| Phylum: | incertae sedis |
| Genus: | Marcusodictyon† Bassler 1911 |
| Species | |
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See text. | |
Marcusodictyon is a genus of problematic fossils. It has been considered the oldest bryozoan in several publications. Taylor (1984) revised the systematics of the genus and removed it from Bryozoa. The fossil constitutes a phosphatic network of low ridges that enclose polygons about 0.3–1.2 mm wide that are generally 6-sided but can be 4-, 5- or 7-sided. The internal microstructure of Marcusodictyon is composed of laminae parallel to external surfaces of ridges (Taylor 1984). Marcusodictyon occurs on late Cambrian and Tremadocian lingulate brachiopods of Baltica (Vinn 2015).
References
- Taylor, P.D. (1984). Marcusodictyon Bassler from the Lower Ordovician of Estonia: not the earliest bryozoan but a phosphatic problematicum. Alcheringa 8, 177–186.
- Vinn, O. (2015). "Rare encrusted lingulate brachiopods from the Cambrian–Ordovician boundary beds of Baltica". Alcheringa. doi:10.1080/03115518.2016.1101234. Retrieved 2015-12-15.
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