INSUGEO   12554
INSTITUTO SUPERIOR DE CORRELACION GEOLOGICA
Unidad Ejecutora - UE
artículos
Título:
Trilobites de la Formación Volcancito (miembro Filo Azul, Cámbri, co Tardío) El Sistema de Famatina, la Rioja, Argentina
Autor/es:
TORTELLO, M.F.; ESTEBAN, SUSANA BEATRIZ
Revista:
AMEGHINIANA
Editorial:
Asociación Paleontológica Argentina
Referencias:
Lugar: Buenos Aires; Año: 2007 p. 597 - 620
ISSN:
0002-7014
Resumen:
The Filo Azul Member of the Volcancito Formation (Famatina range, La Rioja, Argentina) consists of a lower part
(30 m) of thinly laminated marls and calcareous shales with intercalations of fine-grained sandstones, a middle
part (85 m) of massive middle to thick-grained calcareous sandstones, and an upper part (50 m) of shales with
interbedded layers of fine sandstones. Previous studies on trilobites, graptolites and conodonts assigned the
section to the Upper Cambrian-Lower Ordovician. The lower portion of the member (Parabolinafrequensargentina
Biozone, lower part) contains a diverse trilobite fauna that was studied by Harrington and Leanza in the 1950s.
Since then, new collections have been obtained, which are the subject of the present study. New polymerid
trilobites, originally described on the basis of scarce material, are re-illustrated (Onychopygeriojana Harrington,
Asaphellusriojanus Harrington and Leanza, Rhadinopleuraeurycephala Harrington and Leanza, Plicatolinascalpta
Harrington and Leanza) and the assignations of several taxa are reconsidered (Angelina cf. hyeronimi (Kayser),
Parabolinella sp. 1, Parabolinella sp. 2, Pseudokainellatoselliisp. nov., Conophrys sp.) (since the agnostoids have
been recently revised, they are not included in this study). The fauna comprises several endemic species. On the
other hand, the occurrence of Parabolina(Neoparabolina)frequens (Barrande) permits the outcrop to be
correlated with other Upper Cambrian sections. The abundance of nutrients in the sea bottom must have
favoured the development of a diverse trilobite community, which included different morphotypes and feeding
habits. Several taxa were especially adapted to live under low-oxygen conditions, probably in symbiosis with
sulfur bacteria.