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Camptostroma

Extinct genus of marine invertebrates From Wikipedia, the free encyclopedia

Camptostroma
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Camptostroma roddyi is an extinct echinoderm from the Bonnia-Olenellus Zone of the Early Cambrian Kinzers Formation near York and Lancaster, Southeastern Pennsylvania.[2] It is the only known species in the genus Camptostroma, as other species referred to this genus "do not appear to be cogeneric."[3]

Quick facts Camptostroma Temporal range: Early Cambrian, Scientific classification ...
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Anatomy

In life, Camptostroma would have resembled a cupcake, with the mouth in the center of the upper surface, with ambulacra radiating from it in the 2-1-2 pattern common in early echinoderms. The ambulacra are straight in juveniles, but in larger adult specimens, ambulacra A, B, C, and E curve clockwise while ambulacrum D curves counter-clockwise. The anus is near the periphery between ambulacra C and D.[4]

The ambulacra may have extended beyond the upper surface on stubby arms. While this diagnosis is tentative, ongoing work appears to support it.[5]

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Classification and relationships

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Camptostroma roddyi fossil on display at the Smithsonian's National Museum of Natural History.

While initially considered to be a scyphozoan due to the fossil's medusoid shape, later investigation detected the presence of stereom plates with the calcitic cleavage pattern diagnostic of echinoderms.[2]

The Treatise on Invertebrate Paleontology accepted Durham's 1966 assignment of Camptostroma to its own class, Camptostromatoidea.[6] However, a later revision of the Treatise's classification omitted this class.[7]

Camptostroma has since been placed in a class of basal echinoderms, the Edrioasteroids,[8] although some recent authors only describe it as "edrioasteroid-like".[5]

Recent research has found weak support for the recovery of Camptostroma as the sister group of the crinoids.[9][10] However, other phylogenies are ambiguous regarding whether it is closer to the crinoids, eocrinoids, or eleutherozoans.[11]

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References

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