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2015 | 60 | 4 |

Tytuł artykułu

The new stem-group brachiopod Oymurania from the lower Cambrian of Siberia

Treść / Zawartość

Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
A stem-group brachiopod, Oymurania gravestocki Ushatinskaya gen. et sp. nov. is described herein from the middle Atdabanian-lower Botoman Stages (-Cambrian Stage 3) of the Siberian Platform. The fossils were extracted from limestone beds of the Emyaksin, Perekhod, and Pestrotsvet formations as assemblages of disarticulated orthoconic to cyrtoconic porous shells in apatite preservation. The originally organophosphatic shells of Oymurania are externally similar to mitral sclerites (ventral valves) of the stem-group brachiopod Micrina, although no sellate-like sclerites, nor differentiated subapical area with apophyses were recognised in our material. The range of Oymurania shells with sub-central to posteromarginal apex is similar to that of ventral valves ofMickwitzia. Oymurania is also characterised by the system of radial and orthogonal canals open in pairs or triplets in small depressions or indentations of growth lamellae in the outer shell surface. The orthogonal (Micrina-Setatella type) and radial (horizontal setigerous tubes) canals are widespread among the early Cambrian stem-group brachiopods, such as Micrina, Mickwitzia, and Setatella. In addition to these canals, Oymurania exhibits a well-developed acrotretoid columnar microstructure, also known from Setatella. A broad subapical platform in cyrtoconic shells (presumably ventral valves) of Oymurania is interpreted homologous to the deltoid area in mitrals of Micrina and pseudointerarea/interarea in ventral valves of Setatella/paterinid brachiopods. Except with probable cell imprints and openings of orthogonal canals, no morphological differentiation was, however, reflected by the shell interior of Oymurania gravestocki. Being closely related to tannuolinids and mickwitziids, Oymurania complements the picture of diversification of the early Cambrian stem-group brachiopods that occurred in parallel with radiation of paterinids and other crow-group brachiopods on the Siberian Platform and worldwide.

Wydawca

-

Rocznik

Tom

60

Numer

4

Opis fizyczny

p.963-980,fig.,ref.

Twórcy

  • Department of Palaeobiology, Swedish Museum of Natural History, Box 50007, SE-104 05 Stockholm, Sweden
autor
  • Department of Earth Sciences, Palaeobiology, Uppsala University, Villava- gen 16, SE-752 36 Uppsala, Sweden
autor
  • Department of Earth Sciences, Freie Universitat Berlin, Malteserstrasse 74-100, Haus D, Berlin, 12249, Germany
  • Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya 123, Moscow 117997, Russia

Bibliografia

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Typ dokumentu

Bibliografia

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