Polysacos

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Polysacos
Temporal range: 335   Ma
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Scientific classification Red Pencil Icon.png
Kingdom: Animalia
Phylum: Mollusca
Class: Polyplacophora
Order: Multiplacophora
Genus: Polysacos
Vendrasco et al., 2004
Species:P. vickersianum
Binomial name
Polysacos vickersianum
Vendrasco et al., 2004

Polysacos is an extinct genus of multiplacophorans (chitons) known from articulated Carboniferous fossils; its seventeen shell plates are arranged in three rows, with seven iterated units. It demonstrates that multiplacophora are related to modern polyplacophora. [1] It was fringed with a ring of hollow spines resembling those of the Ordovician Echinochiton . [1]

Multiplacophora is a stem-group of chitons with a number of plates arranged in 7 rows along the body. They date to at least the Upper Cambrian, but two lower Cambrian fossils- Ocruranus and Trachyplax - may extend the range downwards.

The Carboniferous is a geologic period and system that spans 60 million years from the end of the Devonian Period 358.9 million years ago (Mya), to the beginning of the Permian Period, 298.9 Mya. The name Carboniferous means "coal-bearing" and derives from the Latin words carbō ("coal") and ferō, and was coined by geologists William Conybeare and William Phillips in 1822.</ref>

Echinochiton is an extinct genus of Ordovician chitons with hollow spines on its margins; these spines, which are unique among the chitons, have a strong organic component and show growth lines.

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References

  1. 1 2 Vendrasco, M. J.; Wood, T. E.; Runnegar, B. N. (2004). "Articulated Palaeozoic fossil with 17 plates greatly expands disparity of early chitons". Nature. 429 (6989): 288–291. Bibcode:2004Natur.429..288V. doi:10.1038/nature02548. PMID   15152250.