Priabonian
Inte la scala dei tenpi xeolòxeghi, el Priabonian el xe è l'ultimo dei quatro piani in cui che el xe sudivixo l'Eosene, che a so volta el xe la seconda època del periodo del Paleoxene, inte l'era del Senoxòico.
El scomìnsia sirca 37,71 milioni de ani fa per concludarse 33,9 milioni di ani fa.[1][2] El xe preseduo dal Bartonian e seguio dal Rupelian, el primo piano del successivo Oligosene.[3]
Orìxene del nome
El nome el deriva da la località de Priabona, situà intel comun de Monte de Malo in provinsa de Vicenza, so i Monti Lesini Orientali (Italia), dove che i strati priaboniani i xe particolarmente caraterìsteghi
Note
- ↑ stratigraphy.org, https://stratigraphy.org/chart.
- ↑ stratigraphy.science.purdue.edu, http://stratigraphy.science.purdue.edu/gssp/.
- ↑ Gradstein, F.M.; Ogg, J.G. & Smith, A.G.; 2004: A Geologic Time Scale 2004, Cambridge University Press.
Liganbi foresti
- Museo Paleontologico di Priabonamontedimalolive.it.
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