Email this article Shell Microstructure and Relief of the Primary Layer of the Late Jurassic Discinisca (Class Lingulata, Family Discinidae)
- Authors: Smirnova T.N.1, Ushatinskaya G.T.2, Zhegallo E.A.2, Panchenko I.V.3
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Affiliations:
- Moscow State University
- Borissiak Paleontological Institute, Russian Academy of Sciences
- “Federal State Budgetary Institution “All-Russian Research Geological Oil Institute
- Issue: Vol 53, No 5 (2019)
- Pages: 482-487
- Section: Article
- URL: https://journals.rcsi.science/0031-0301/article/view/168634
- DOI: https://doi.org/10.1134/S0031030119050113
- ID: 168634
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Abstract
The organophosphatic-shelled brachiopod Discinisca sp. is first described from the Upper Jurassic of Northwestern Siberia. Its relief and microstructure of outer and inner sides of dorsal brephic and adult valves are described. Discinisca sp. differs from other Mesozoic discinids in the primary layer with concentric relief structures.
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About the authors
T. N. Smirnova
Moscow State University
Author for correspondence.
Email: smirnovatatiana76@bk.ru
Russian Federation, Moscow, 119992
G. T. Ushatinskaya
Borissiak Paleontological Institute, Russian Academy of Sciences
Author for correspondence.
Email: gushat@paleo.ru
Russian Federation, Moscow, 117647
E. A. Zhegallo
Borissiak Paleontological Institute, Russian Academy of Sciences
Author for correspondence.
Email: ezheg@paleo.ru
Russian Federation, Moscow, 117647
I. V. Panchenko
“Federal State Budgetary Institution “All-Russian Research Geological Oil Institute
Author for correspondence.
Email: ivpanchenko89@gmail.com
Russian Federation, Moscow, 105118
