The PC/33b well drilled by the ENEL Company in the Monte Amiata area near Piancastagnaio (Southern Tuscany, Italy) yielded some fossiliferous layers from 3024.40 to 3028.40m. The cored interval is interpreted as belonging to the Paleozoic Basement of the Tuscan Series. The fossils identified in the cored interval belong to fragmented crinoids, gastropods, gymnocodiacean and dasycladacean algae, and to foraminifers (mainly fusulinids). Despite the strong recrystallization and metamorphism affecting the rocks, some fusulinids could be identified. They are Praeparafusulina cf. lutugini (Schellwien) (possibly reworked), Polydiexodina (Eopolydiexodina?) cf. shabalkini Leven, Yangkienia sp., Y. aff. compressa (Ozawa), Cancellina sp., Pseudodoliolina "ex.gr.' P. ozawai Yabe & Hanzawa, ?Chusenella sp., ghosts of Misellina sp. and ?Neofusulinella sp. This fusulinid association is indicative of the Cancellina Zone of Kubergandian age (Late Permian), which is recorded in Italy for the first time. -from English summary

Fusulinidi permiani nella successione metamorfica del sottosuolo del M.Amiata, Toscana meridionale (Italia) / E.PANDELI; M. PASINI. - In: RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA. - ISSN 0035-6883. - STAMPA. - 96:(1990), pp. 3-20.

Fusulinidi permiani nella successione metamorfica del sottosuolo del M.Amiata, Toscana meridionale (Italia)

PANDELI, ENRICO;
1990

Abstract

The PC/33b well drilled by the ENEL Company in the Monte Amiata area near Piancastagnaio (Southern Tuscany, Italy) yielded some fossiliferous layers from 3024.40 to 3028.40m. The cored interval is interpreted as belonging to the Paleozoic Basement of the Tuscan Series. The fossils identified in the cored interval belong to fragmented crinoids, gastropods, gymnocodiacean and dasycladacean algae, and to foraminifers (mainly fusulinids). Despite the strong recrystallization and metamorphism affecting the rocks, some fusulinids could be identified. They are Praeparafusulina cf. lutugini (Schellwien) (possibly reworked), Polydiexodina (Eopolydiexodina?) cf. shabalkini Leven, Yangkienia sp., Y. aff. compressa (Ozawa), Cancellina sp., Pseudodoliolina "ex.gr.' P. ozawai Yabe & Hanzawa, ?Chusenella sp., ghosts of Misellina sp. and ?Neofusulinella sp. This fusulinid association is indicative of the Cancellina Zone of Kubergandian age (Late Permian), which is recorded in Italy for the first time. -from English summary
1990
96
3
20
E.PANDELI; M. PASINI
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Utilizza questo identificatore per citare o creare un link a questa risorsa: https://hdl.handle.net/2158/593659
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