Temporal range: Ordovician
Cothurnocystis is a genus of small, enigmatic echinoderms that lived during the Ordovician. Individual animals had a flat, boot-shaped body and a thin, rod-shaped appendage that may be a stem, or analogous to a foot or a tail. Fossils of Cothurnocystis species have been found in Nevada, Scotland, Czech Republic, France and Morocco.
The position of the Stylophora, of which Cothurnocystis is a prominent representative, has been in a state of flux. Some scientists claim to be able to see a structurally very basic notochord in the tail, and consequently consider the Stylophora to be a group of primitive chordates, calling them the "Calcichordata". Alternatively these animals are considered related to echinoderms, as the shell (or test) is similar in structure and composition to the tests of echinoderms. However, stylophoras are asymmetric organisms that lack either the radial symmetry typical of most echinoderms, or the bilateral symmetry of the chordates.
- C. americana refers to the continent where it was found.
- C. curvata is named for the curved form of its theca.
- C. elizae honors of mrs. Robbert Gray, who collected the specimens the description of this species is based upon.
- C. americana is known from the Lower Ordovician of Nevada (lowest Tremadocian, Whipple Cave Formation, near Lund, White Pine County).
- C. curvata occurs at the Upper Ordovician of Scotland (Starfish Bed of the Drummock Group, Dicellograptus anceps-zone, Thraive Glen, Girvan, Ayrshire).
- C. elizae has been collected in the Lower Ordovician of Morocco (highest Tremadocian to mid Floian, Zagora region),the Upper Ordovician of Scotland (Starfish Bed of the Drummock Group, Dicellograptus anceps-zone, Thraive Glen, Girvan, Ayrshire).
- C. fellinensis is found at the Lower Ordovician of France (Saint Chinian Formation, Montagne Noire).
The body of Cothurnocystis consists of a chalice (or theca) and a stem (tail or foot). The theca is fattened, boot-shaped and asymmetrical. The edges of the flat sides of the theca seem to consist of 14 elements, 11 defining the outline of the theca, and 3 are processes, one forming a "toe"-spike, a second a heel-spike and a third a lip-spike. The so-called "obverse"-side ("toe" pointing left), is covered with one thin integument, at the "reverse"-side the integument is interrupted by a "strut" formed by a branche of an element near the attachment of the stem, and a branche of an element at the top of the theca. Approximately from the attachment of the stem to the "toe"-spike, is a structure reminiscent of a windpipe, that has been interpreted as a series of slits in the integument. The attachment of the stem seems to consist of four sets of left and right elements, becoming narrower further from the theca. Further down single and uniform elements of the stem seem comparable to the anatomy of sealily stems. The "instep" of the boot seems to hold both the mouth and the anus.
- Ubachs, G. (1963). "Cothurnocystis Bather and Phyllocystis Thoral and an undetermined member of the order Soluta (Echinodermata, Carpoidea) in the uppermost Cambrian of Nevada". Journal of Paleontology 37 (6): 1133–1142. JSTOR 1301473.
- Bather-London, F.A. (1926). "Vortrage und diskussionen auf der Wiener Tagung der Palaeontologischen Gesellschaft im September 1923: Coturnocystus: a study in adaptation". Palaeontologische Zeitschrift 7 (1): 1–15.
- Ruta, M. (1999). "Brief review of the stylophoran debate". Evolution & Development 1 (2): 123–135. doi:10.1046/j.1525-142x.1999.99008.x. PMID 11324028.
- Lefevre, B. (2003). "Functional morphology of Stylophoran echinoderms". Palaeontology 46 (3): 511–555. doi:10.1111/1475-4983.00309.
- D. Lambert, D. Naish and E. Wyse (2001) "Encyclopedia of Dinosaurs and prehistoric life", p. 32, Dorling Kindersley Limited, London. ISBN 0-7513-0955-9
- Fossil Gallery
- Stylophora from palaeos
- Markkos taxonomy
- http://www.ayrshirehistory.org.uk/girvangeologists/Cothurnocystis.gif image
- http://www.geo-tools.com/Images/Gallery/Fossil/Big/041.jpg image
- http://www.webcitation.org/query?url=http://www.geocities.com/arturordoviciano/ordser2_arquivos/image007.jpg&date=2009-10-26+04:13:47 image
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