| Palćos: | ![]() |
Procoelomates |
| INVERTEBRATES | Coeloscleritophora |
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This
Cambrian group includes the Halkeriida.
They are characterized by having a large number of small sclerites. In
fact, most members of the group are a large number of small sclerites,
the actual body form being unknown. Where known, the body plan
includes a prominent internal cavity and restricted basal foramen -- something
like a balloon with scales.
The scales of coeloscleritophorans are distinctive in having a thin (<1µ) organic layer over the entire scale and an internal layer of aragonite fibers oriented along the long axis of the sclerite. Most, like Siphoguchites in the image (scale bar = 100µ) also have (1) bundles of external aragonite fibers inclined toward the tip which look like microscales, and (2) a rim around the base which lacks these aragonite bundles. See Porter (2005).
Recent specimens from Chenjiang suggest that the sclerites were embedded in a flexible, continuous layer of organic cuticle and stuck out "like cactus spines." In this model, both scales and cuticle were formed by an epithelilial layer of living cells. Bengston & Hou (2001). ATW051231.
| References |
Bengston, S (2004), Early skeletal fossils, in JH Lipps & BM Waggoner (eds.), Neoproterozoic-Cambrian Biological Revolutions. Pal. Soc. Papers 10: 67-77. WWW
Bengtson, S & VV Missarzhevsky (1981), Coeloscleritophora – a major group of enigmatic Cambrian metazoans. Short Pap. 2d Intn. Symp. Cambrian Syst., U.S. Geol. Surv. O.-F. Rep. 81-743: 19-21.
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