1973
DOI: 10.1016/s0016-6995(73)80019-1
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Les Echinodermes Cincta du Cambriende la Montagne Noire (France)

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Cited by 16 publications
(14 citation statements)
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“…The presence of a single left marginal groove that reaches M1l is a trait shared with some species of Sucocystis Cabibel, Termier & Termier, 1959; however, Protocinctus gen. nov. differs from these forms in other respects (the shape and height of the theca, the number of marginal plates, and the development of ventral swellings). The elongate thecal shape of Protocinctus gen. nov. is similar to that of Gyrocystis Jaekel, 1918, Progyrocystis Friedrich, 1993, or Elliptocinctus Termier & Termier, 1973. The arrangement of three plates in the lintel is similar to Gyrocystis , Sucocystis , and Elliptocinctus , and the absence of prominent ventral swellings is a feature shared with Trochocystoides parvus Jaekel, 1918, T. planus , S. ubaghsi , A. jaekeli , and Gyrocystis platessa Jaekel, 1918.…”
mentioning
confidence: 61%
“…The presence of a single left marginal groove that reaches M1l is a trait shared with some species of Sucocystis Cabibel, Termier & Termier, 1959; however, Protocinctus gen. nov. differs from these forms in other respects (the shape and height of the theca, the number of marginal plates, and the development of ventral swellings). The elongate thecal shape of Protocinctus gen. nov. is similar to that of Gyrocystis Jaekel, 1918, Progyrocystis Friedrich, 1993, or Elliptocinctus Termier & Termier, 1973. The arrangement of three plates in the lintel is similar to Gyrocystis , Sucocystis , and Elliptocinctus , and the absence of prominent ventral swellings is a feature shared with Trochocystoides parvus Jaekel, 1918, T. planus , S. ubaghsi , A. jaekeli , and Gyrocystis platessa Jaekel, 1918.…”
mentioning
confidence: 61%
“…Several other genera described by Cabibel et 01. (1958) and Termier and Termier (1973) appear to be synonyms. Homosteleans were apparently slow-moving, benthic detritus or suspension feeders.…”
Section: Class Homostelea (Three Genera)mentioning
confidence: 95%
“…Cinctans are confined to only a brief interval of time during the Middle Cambrian and were a component of benthic marine assemblages in Western Gondwana, Siberia and Avalonia (Barrande 1887; Termier and Termier 1973; Schröder 1973;Friedrich 1993, 1995; Sdzuy 1993; Fatka and Kordule 2001; Rozhnov 2006; Zamora and Smith 2008). Isolated plates of cinctans are very common in Middle Cambrian rocks but complete skeletons are preserved only under special conditions in specific echinoderm Lagerstätten.…”
Section: The Competing Classifications Proposed By Friedrich (1993) mentioning
confidence: 99%