Conulariid
| Conulariida Temporal range: Upper Cambrian–Triassic |
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| Conulariid from the Mississippian of Indiana; scale in mm. | |
| Scientific classification | |
| Kingdom: | Animalia |
| Phylum: | Cnidaria |
| Class: | Scyphozoa |
| Clade: | †Conulariida |
| Genera | |
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See text. |
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See text.
Conulariida is a poorly understood fossil group that has possible affinity with the Cnidaria. Their exact position as a family or suborder of extinct scyphozoan cnidarians is highly speculative. Members of the Conulariida are commonly referred to as conulariids and appear in the fossil record from the latest Cambrian Period .
The conulariids are fossils preserved as shell-like structures made up of rows of calcium phosphate rods, resembling an ice-cream cone with fourfold symmetry, usually four prominently-grooved corners. New rods were added as the organism grew in length; the rod-based growth falsely gives the fossils a segmented appearance. Exceptional soft-part preservation has revealed that soft tentacles protruded from the wider end of the cone, and a holdfast from the pointed end attached the organisms to hard substrate. The prevailing reconstruction of the organism has it look superficially like a sea anemone sitting inside an angular, hard cone held perpendicular to the substrate. Conulariid shell is composed of francolite with carbonate ion concentration 8.1 wt%. The lattice parameters of conulariid apatite are a = 9.315(7) Å, c = 6.888(3) Å. The fine structure of their shell comprises multiple lamellae of alternately organic-rich and organic-poor layers.
Setting aside for the moment the Precambrian Vendoconularia, which may or may not be a conulariid at all, the Conulata fossil record begins with undoubted specimens in the Upper Cambrian (Hughes et al., 2000) and extends without significant break through numerous major mass extinctions. The Conulariids finally disappear from the rock record during the Lower Triassic stage of the Triassic Period (~245 million years ago).
In North America, conulariids are generally least uncommon in rocks of Ordovician and Carboniferous age.
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