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    <ns1:title language="it">Illustrazione della fauna triasica di Valpedena (Cadore)</ns1:title>
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    <ns1:description language="it">Descrizione della fauna triassica di Val de Pena (Lorenzago, Cadore), proveniente da una dolomia a diplopore, poco stratificata dell’Anisico al Colle Audoi. De Toni trovò delle analogie tra la fauna del Colle Audoi e la fauna della Formazione di Esino (Lombardia), con le faune della Val Badia e della Val Giudicarie, nonché con la fauna di Spiti dell’Himalaya. Attribuì la fauna al Wengen (longobardico) anche se permanevano forme anisiche e carniche.</ns1:description>
    <ns1:description language="en">Report on the Triassic fauna present in Val de Pena (Lorenzago di Cadore), from a dolomite with diplopora, slightly stratified, in the Anisicus at Colle Audoi. De Toni found similarities between the fauna of Colle Audoi and the fauna of the Formation of Esino (Lombardy), with the fauns of Val Badia and Val Giudicarie, as well as with the fauna of Spiti of the Himalayas. He attributed the fauna to the Wengen (Longobardic) even if there remained Anisical and Carnic forms. </ns1:description>
    <ns1:keyword language="it">Antonio De Toni</ns1:keyword>
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    <ns12:name_magazine language="it">Illustrazione della fauna Triasica di Valpedena (Cadore)</ns12:name_magazine>
    <ns12:pagination>86 p., VI c. di tav</ns12:pagination>
    <ns12:reihentitel>Estratto da: Memorie dell’Istituto geologico della R. Università di Padova</ns12:reihentitel>
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