| Mitrate Temporal range: | |
|---|---|
| | |
| Rhenocystis latipedunculata ventral/flat (B1) and dorsal/convex (B2) surfaces | |
| Scientific classification | |
| Kingdom: | Animalia |
| Phylum: | Echinodermata |
| Class: | † Stylophora |
| Order: | † Mitrata Jaekel, 1918 |
| Taxa | |
See Taxa | |
Mitrates are an extinct group of echinoderms, which are grouped with the cornutes and the basal Ceratocystis to form the Stylophora. Mitrates were central to the now-disproven [2] calcichordate hypothesis of chordate origins, but are now seen as either pre-radial-symmetry stem-group echinoderms, [3] or as a derived group either within the blastozoans [4] or near to the origin of crinoids. [5]
The organisms were a few millimetres long. [6] Like the echinoderms, they are covered in armour plates, each of which comprises a single crystal of calcite. This is one of the features they share with the latter group, along with a water vascular system, only discovered in 2019. [7] However, they do not display the familiar fivefold symmetry that more recent echinoderms possess, instead being close to (but not fully) bilaterally symmetrical. [6] [8]
Their heads had two sides; one, flat, was covered with large "pavement-like" [6] plates, the other, convex, bore smaller plates. [6] Their tails were long and segmented, resembling the stalk of a crinoid or the arm of a brittlestar. [6] At the opposite end was a hole which may have been mouth or anus - or both. [6]
They also bear features reminiscent of pharyngeal slits, [9] a character lost in other echinoderms but present in hemichordates. [6] This caused R.P.S. Jefferies to hold them as the ancestor of all chordates, a theory that has since been disproven. [2]
The mitrate Rhenocystis latipedunculata has been found with associated trace fossils. [10] [11] Their interpretation requires an understanding of how the animal was oriented in life; it's not agreed whether the convex side of the head was up or down, or indeed whether the "tail" was at the front or back of the organism. [6] The trace fossils suggest that they pulled themselves through the mud with their "tail", and were flat-side up. [6]
The following taxa are recognized as being included in the order Mitrata: [12]