Hasil Pencarian - FABIO MASSIMO PETTI

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  1. 1
    The Origin and Early Radiation of Archosauriforms: Integrating the Skeletal and Footprint Record.

    The Origin and Early Radiation of Archosauriforms: Integrating the Skeletal and Footprint Record. oleh Massimo Bernardi, Hendrik Klein, Fabio Massimo Petti, Martín D Ezcurra

    Diterbitkan 2015-01-01
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  2. 2
    Dinosaur diversification linked with the Carnian Pluvial Episode

    Dinosaur diversification linked with the Carnian Pluvial Episode oleh Massimo Bernardi, Piero Gianolla, Fabio Massimo Petti, Paolo Mietto, Michael J. Benton

    Diterbitkan 2018-04-01
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  3. 3
    A THEROPOD DOMINATED ICHNOCOENOSIS FROM LATE HAUTERIVIAN-EARLYBARREMIAN OF BORGO CELANO (GARGANO PROMONTORY, APULIA, SOUTHERN ITALY)

    A THEROPOD DOMINATED ICHNOCOENOSIS FROM LATE HAUTERIVIAN-EARLYBARREMIAN OF BORGO CELANO (GARGANO PROMONTORY, APULIA, SOUTHERN ITALY) oleh FABIO MASSIMO PETTI, MARIA ALESSANDRA CONTI, SIMONE D'ORAZI PORCHETTI, MICHELE MORSILLI, UMBERTO NICOSIA, PIERO GIANOLLA

    Diterbitkan 2008-03-01
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  4. 4
    LATE TRIASSIC (EARLY-MIDDLE CARNIAN) CRUROTARSAN TRACKS FROM THE VAL SABBIA SANDSTONE (EASTERN LOMBARDY, BRESCIAN PREALPS, NORTHERN ITALY)

    LATE TRIASSIC (EARLY-MIDDLE CARNIAN) CRUROTARSAN TRACKS FROM THE VAL SABBIA SANDSTONE (EASTERN LOMBARDY, BRESCIAN PREALPS, NORTHERN ITALY) oleh FABIO MASSIMO PETTI, MARCO AVANZINI, UMBERTO NICOSIA, STEFANO GIRARDI, MASSIMO BERNARDI, PAOLO FERRETTI, PAOLO SCHIROLLI, CRISTIANO DAL SASSO

    Diterbitkan 2009-11-01
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  5. 5
    MIDDLE JURASSIC - EARLY CRETACEOUS INTEGRATED BIOSTRATIGRAPHY (AMMONITES, CALCAREOUS NANNOFOSSILS AND CALPIONELLIDS) OF THE CONTRADA DIESI SECTION (SOUTH-WESTERN SICILY, ITALY)

    MIDDLE JURASSIC - EARLY CRETACEOUS INTEGRATED BIOSTRATIGRAPHY (AMMONITES, CALCAREOUS NANNOFOSSILS AND CALPIONELLIDS) OF THE CONTRADA DIESI SECTION (SOUTH-WESTERN SICILY, ITALY) oleh MARIA CONCETTA MARINO, GLORIA ANDREINI, ANGELA BALDANZA, CAROLINA D'ARPA, NINO MARIOTTI, GIOVANNI PALLINI, GUIDO PARISI, FABIO MASSIMO PETTI

    Diterbitkan 2004-03-01
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