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Priabonian
| Priabonian | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Chronology | |||||||||||||
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| Etymology | |||||||||||||
| Name formality | Formal | ||||||||||||
| Usage information | |||||||||||||
| Celestial body | Earth | ||||||||||||
| Regional usage | Global (ICS) | ||||||||||||
| Time scale(s) used | ICS Time Scale | ||||||||||||
| Definition | |||||||||||||
| Chronological unit | Age | ||||||||||||
| Stratigraphic unit | Stage | ||||||||||||
| Time span formality | Formal | ||||||||||||
| Lower boundary definition | LAD of the large acarininids and the Foraminiferan Morozovelloides crassatus | ||||||||||||
| Lower boundary GSSP | Alano section, Piave river, Venetian Prealps, Belluno, Italy 45°54′51″N 11°55′05″E / 45.9141°N 11.9180°E | ||||||||||||
| Lower GSSP ratified | February 2020[3] | ||||||||||||
| Upper boundary definition | LAD of Planktonic Foraminifers Hantkenina and Cribrohantkenina | ||||||||||||
| Upper boundary GSSP | Massignano quarry section, Massignano, Ancona, Italy 43°31′58″N 13°36′04″E / 43.5328°N 13.6011°E | ||||||||||||
| Upper GSSP ratified | 1992[4] | ||||||||||||
The Priabonian is, in the ICS's geologic timescale, the latest age or the upper stage of the Eocene Epoch or Series. It spans the time between 37.71 and 33.9 Ma. The Priabonian is preceded by the Bartonian and is followed by the Rupelian, the lowest stage of the Oligocene.[5]
Priabona, an extinct dipteran of Pipunculidae family, is named after Priabonian, the age of deposits from which this insect is known.[6]
- ^ Zachos, J. C.; Kump, L. R. (2005). "Carbon cycle feedbacks and the initiation of Antarctic glaciation in the earliest Oligocene". Global and Planetary Change. 47 (1): 51–66. Bibcode:2005GPC....47...51Z. doi:10.1016/j.gloplacha.2005.01.001.
- ^ "International Chronostratigraphic Chart" (PDF). International Commission on Stratigraphy. September 2023. Retrieved December 16, 2024.
- ^ Agnini, Claudia; Backman, Jan; Boscolo-Galazzo, Flavia; Condon, Daniel; Fornaciari, Eliana; Galeotti, Simone; Giusberti, Luca; Grandesso, Paolo; Lanci, Luca; Luciani, Valeria; Monechi, Simonetta; Muttoni, Giovanni; Pälike, Heiko; Pampaloni, Maria; Papazzoni, Cesare; Pearson, Paul; Pignatti, Johannes; Silva, Isabella; Raffi, Isabella; Rio, Domenico; Rook, Lorenzo; Sahy, Diana; Spofforth, David; Stefani, Cristina; Wade, Bridget (12 August 2020). "Proposal for the Global Boundary Stratotype Section and Point (GSSP) for the Priabonian Stage (Eocene) at the Alano section (Italy)". Episodes. 44 (2): 151–173. doi:10.18814/epiiugs/2020/020074. hdl:2158/1209925.
- ^ Silva, Isabella; Jenkins, D. (September 1993). "Decision on the Eocene-Oligocene boundary stratotype" (PDF). Episodes. 16 (3): 379–382. doi:10.18814/epiiugs/1993/v16i3/002. Retrieved 13 December 2020.
- ^ International Commission on Stratigraphy 2017
- ^ Archibald, SB; Kehlmaier, C; Mathewes, RW (2014). "Early Eocene big headed flies (Diptera: Pipunculidae) from the Okanagan Highlands, western North America". The Canadian Entomologist. 146 (4): 429–443. doi:10.4039/tce.2013.79.
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