Published November 19, 2014 | Version v1
Taxonomic treatment Open

Cyrtothyris Middlemiss 1959

  • 1. Department of Geology, University of Dayton, Dayton, OH 45469 - 2364, USA. E-mail: msandy 1 @ udayton. edu
  • 2. Natural History Museum, University of Oslo, P. O. Box 1172, NO- 0318 Oslo, Norway. & Current address: Institute of Paleobiology, Polish Academy of Sciences, ul. Twarda 51 / 55, 00 - 818 Warszawa, Poland.
  • 3. Natural History Museum, University of Oslo, P. O. Box 1172, NO- 0318 Oslo, Norway.
  • 4. School of Earth and Environment, University of Leeds, Leeds LS 2 9 JT, United Kingdom.

Description

Cyrtothyris ? sp.

Fig. 7.5–7.8

1976? v. “ Cyrtothyrismaynci new species—Owen, p. 13, pl. 2, fig. 1a–c, pl. 3, fig. 4a–c, text-fig. 7.

2011 v. partim ‘ Cyrtothyris ’ sp.—Hammer et al., p. 20, table 2.

Material and occurrence. Seep 3 (PMO 224.870, PMO 224.904?, PMO 224.919?), seep 8 (PMO 227.428?).

Description. Rounded, circular, to gently elongate outline, equibiconvex lateral profile, rectimarginate anterior commissure.

Discussion. The material from Spitsbergen reaches larger maximum dimensions than “ Cyrtothyrismaynci described from Greenland (Owen 1976). Broken ventral umbones hamper identification (e.g. Fig. 7.5–7.8) and referral to Cyrtothyris must be considered tentative. Owen commented that the Greenland form has an incipient uniplicate anterior commissure. The Spitsbergen specimens show a rectimarginate anterior commissure to possibly weakly uniplicate (Fig. 7.8, anterior commissure damaged). The Greenland material is from the Falskebugt Member (Harper et al. 2005) of Valanginian age whereas the Spitsbergen specimens are from the Upper Volgian. Cyrtothyris has not been recorded from the Upper Jurassic and these specimens may represent a new form.

Some of the Spitsbergen brachiopods are morphologically close to Cyrtothyris and Rouillieria. Species referred to these two genera may be morphologically very similar and details of the ventral umbo and profile can be important in distinguishing between them (as discussed by Middlemiss 1976). Several specimens from seep 9 are now considered to be Seductorithyris septemtrionalis; these have an erect beak and lack the produced ventral beak of Cyrtothyris, and are typically less inflated in profile than the latter. However, one specimen from seep 9 (Fig. 7.1–7.4; PMO 224.895) with a suberect ventral umbo and incipiently uniplicate anterior commissure, is referred to Cyrtothyris aff. cyrta (Walker). Middlemiss (1976) considers that this species has a rectimarginate to uniplicate anterior commissure.

Stratigraphic and geographic distribution. Upper Volgian of Spitsbergen.

Notes

Published as part of Sandy, Michael R., Hryniewicz, Krzysztof, Hammer, Øyvind, Nakrem, Hans Arne & Little, Crispin T. S., 2014, Brachiopods from Late Jurassic-Early Cretaceous hydrocarbon seep deposits, central Spitsbergen, Svalbard, pp. 501-532 in Zootaxa 3884 (6) on page 515, DOI: 10.11646/zootaxa.3884.6.1, http://zenodo.org/record/4951742

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Additional details

Biodiversity

References

  • Owen, E. F. (1976) Some Lower Cretaceous brachiopods from East Greenland. Meddelelser om GrOnland, 171 (3), 1 - 19.
  • Harper, D. A. T., Alsen, P., Owen, E. F. & Sandy, M. R. (2005) Early Cretaceous brachiopods from North-East Greenland: biofacies and biogeography. Bulletin of the Geological Society of Denmark, 52, 213 - 225.
  • Middlemiss, F. A. (1976) Lower Cretaceous Terebratulidina of northern England and Germany and their geological background. Geologisches Jahrbuch, 30, 21 - 104.