Marcusodictyon

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).

Marcusodictyon
Temporal range: late Cambrian–Early Ordovician
Scientific classification
Kingdom:
Phylum:
incertae sedis
Genus:
Marcusodictyon

Bassler 1911
Species

See text.

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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