Polysacos vickersianum was a marine mollusc that lived during the early Carboniferous, around 345 million years ago, in what is now Indiana, USA.
It was part of a group known as multiplacophorans, which are usually considered to be close relatives of modern chitons ā but may instead represent a much earlier branch of the aculiferan lineage that convergently evolved chiton-like anatomical features.
About 2.5cm long (~1"), Polysacos had seventeen shell plates surrounded by a fringe of long spines with concave upper surfaces. Like the modern chitons it resembled it was probably a grazer that scraped up algae from hard rocky surfaces.
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References:
Sutton, Mark D., et al. "New Silurian aculiferan fossils reveal complex early history of Mollusca." Nature 637.8046 (2025): 631-636. https://doi.org/10.1038/s41586-024-08312-0
Vendrasco, Michael J., Troy E. Wood, and Bruce N. Runnegar. "Articulated Palaeozoic fossil with 17 plates greatly expands disparity of early chitons." Nature 429.6989 (2004): 288-291. https://doi.org/10.1038/nature02548
Vinther, Jakob, et al. "The origin of multiplacophoransāconvergent evolution in Aculiferan molluscs." Palaeontology 55.5 (2012): 1007-1019. https://doi.org/10.1111/j.1475-4983.2012.01180.x
Wikipedia contributors. āChitonā Wikipedia, 01 Aug. 2026, https://en.wikipedia.org/wiki/Chiton
Wikipedia contributors. āPolysacosā Wikipedia, 07 Mar. 2025, https://en.wikipedia.org/wiki/Polysacos
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