New Middle Ordovician hyoliths from the Ossa Morena Zone, southwestern Spain

0554808 - GLÚ 2022 RIV US eng J - Článek v odborném periodiku
Gutiérrez-Marco, J. C. - Marek, Ladislav - Malinky, J. M.
New Middle Ordovician hyoliths from the Ossa Morena Zone, southwestern Spain.
Journal of Paleontology. Roč. 96, č. 1 (2022), s. 127-142. ISSN 0022-3360. E-ISSN 1937-2337
Institucionální podpora: RVO:67985831
Klíčová slova: Hyoliths * revision * morphology * microstructure * Lagerstatte * Spain * geographical distribution * Ordovician
Obor OECD: Paleontology
Impakt faktor: 1.4, rok: 2022
Způsob publikování: Omezený přístup
https://www.cambridge.org/core/journals/journal-of-paleontology/article/abs/new-middle-ordovician-hyoliths-from-the-ossa-morena-zone-southwestern-spain/AFC3941D71CED20483F89C74459212BB

The record of Middle Ordovician (Oretanian, ca. Darriwilian 2) hyolithids from the Ossa Morena Zone of the Iberian Massif in southwestern Spain is increased with the recognition of Robardetlites sevillanus n. gen. n. sp., Andalucilites parvulus n. gen. n. sp., Pauxillites desolatus n. sp., Leolites malinkyi Marek and Gutiérrez-Marco n. sp., and Cavernolites sp. in that region. Andalucilites n. gen. and Robardetlites n. gen. are endemic whereas the other genera are known from coeval strata in the Barrandian region in central Europe, France, and Morocco, giving this assemblage a decidedly “Mediterranean province” character. The discovery of Pauxillites, Leolites, and Cavernolites in Iberia extends their geographic ranges to that region, and Leolites from this area extends its stratigraphic range downward, making its occurrence in Iberia the oldest known for that genus.
Trvalý link: http://hdl.handle.net/11104/0329455