Cingulochitina, PARIS, 1981

Morávek, Radek, 2009, Lower Wenlock Chitinozoa From The Bykoš Locality (Silurian, Prague Basin, Barrandian Area, Czech Republic), Acta Musei Nationalis Pragae Series B 65 (1 - 2), pp. 37-60 : 41

publication ID

https://doi.org/10.5281/zenodo.13183335

persistent identifier

https://treatment.plazi.org/id/5A608780-0A36-FFF6-A2C9-FC4778BA39CB

treatment provided by

Felipe

scientific name

Cingulochitina
status

 

Cingulochitina pitetensis VERNIERS, 1999

Pl. 2, figs. 1, 5, 5a, 6, 8; pl. 7, figs. 10-13.

1979 Linochitina aff. cingulata MARTIN et RICKARDS, p. 194,

pl. 1, fig. 7. 1981 Linochitina sp. E ; Verniers, p. 171, pl. 2, fig. 28. 1982 Cingulochitina sp. E ; Verniers, p. 26-27, pl. 6, figs.

133-137. 1999 Cingulochitina pitetensis VERNIERS, p. 374.

D e s c r i p t i o n: Cingulochitina with ovoid to conical chamber. The tubular neck is often flared. The maximal width of the vesicle is at one third of the length of the chamber. Shoulders and flexure are well developed. A ridge-like cingulum does not change the curvature of the bluntly rounded basal edge. A short narrow mucron is observed if the vesicles are not connected. Vesicle twins are common.

D i s c u s s i o n: For discussion see Cingulochitina dreyenensis .

O c c u r r e n c e: Mehaigne area, Brabant massif, Belgium (Verniers; 1981, 1982, 1999): late Llandovery to early Wenlock, Member MB3C to base of MB4.

Ithon East and Trecoed, Builth Wells district, Wales, UK

( Verniers, 1999): late lower Wenlock (middle part of the graptolite biozone riccartonensis).

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