期刊
BULLETIN OF GEOSCIENCES
卷 89, 期 2, 页码 293-309出版社
CZECH GEOLOGICAL SURVEY
DOI: 10.3140/bull.geosci.1438
关键词
trilobites; ontogeny; Skryje-Tyrovice Basin; Buchava Formation; Barrandian area; Cambrian
资金
- GA UK (Grant Agency of Charles University) [656912]
- Middle Cambrian of the Barrandian
- Contact Mobility Barrande Program [MEB 021122 - PHC Barrande 24465SH]
- Prvouk [P44]
- Czech Geological Survey [334600]
Preservation of onto genetic stages of trilobites from the Cambrian of the Skryje-Tyrovice Basin (Barrandian area) has been known from several localities in the upper part of the Buchava Formation. The most complete information on exoskeletal changes during ontogeny was based on material assigned by Barrande (1852) to Sao hirsuta. Based on quantitative methods and detailed study of the morphology of the exoskeleton, we recognize three protaspid and two early meraspid instars of Sao hirsuta. We also describe the protaspid stages of two indeterminate taxa of Ptychopariida, one originally determined as the protaspides of Sao hirsuta and the other referred to by Ruzicka (1943) as Barrande's larva. Protaspides of Sao hirsuta have an adult-like morphology, and their presumed benthic mode of life is consistent with the restricted palaeogeographic distribution of this genus.
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