Marine fossils (?brachiopods, bivalves, bryozoans, crinoids) were first found in the lower part of the Late Carboniferous-Early Permian San Lorenzo Schists Formation that crops out in the Valle del Guappero type-area (Pisani Mountains, Tuscany). These sediments have so far provided only continental fossils (mainly paleofloras). The new findings modify the current reconstructions of the Late Carboniferous paleogeography and paleoenvironment in the Northern Apennines area.

Marine fossils in the Late Carboniferous metasediments of the Pisani Mountains (Tuscany, Italy) / E. PANDELI; S. DOMINICI; V. LANDI DEGL’INNOCENTI; E. CIOPPI; F. TANGOCCI. - In: BOLLETTINO DELLA SOCIETÀ GEOLOGICA ITALIANA. - ISSN 0037-8763. - STAMPA. - 127:(2008), pp. 559-565.

Marine fossils in the Late Carboniferous metasediments of the Pisani Mountains (Tuscany, Italy)

PANDELI, ENRICO;
2008

Abstract

Marine fossils (?brachiopods, bivalves, bryozoans, crinoids) were first found in the lower part of the Late Carboniferous-Early Permian San Lorenzo Schists Formation that crops out in the Valle del Guappero type-area (Pisani Mountains, Tuscany). These sediments have so far provided only continental fossils (mainly paleofloras). The new findings modify the current reconstructions of the Late Carboniferous paleogeography and paleoenvironment in the Northern Apennines area.
2008
127
559
565
E. PANDELI; S. DOMINICI; V. LANDI DEGL’INNOCENTI; E. CIOPPI; F. TANGOCCI
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Utilizza questo identificatore per citare o creare un link a questa risorsa: https://hdl.handle.net/2158/369132
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