Burdigalian
Burdigalian | |||||||||||||||||||
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Chronology | |||||||||||||||||||
The Burdigalian is, in the Ma and 15.97 ± 0.05 Ma (million years ago). Preceded by the Aquitanian, the Burdigalian was the first and longest warming period of the Miocene[4] and is succeeded by the Langhian .
Stratigraphic definitionThe name Burdigalian comes from Burdigala, the Latin name for the city of Bordeaux, France. The Burdigalian Stage was introduced in scientific literature by Charles Depéret in 1892. The base of the Burdigalian is at the first appearance of GSSP for the Burdigalian had not yet been assigned.
The top of the Burdigalian (the base of the Langhian) is defined by the first appearance of foram species Praeorbulina glomerosa and is also coeval with the top of magnetic chronozone C5Cn.1n. PaleontologyFamous Burdigalian palaeontologic localities include the Turritellenplatte of Ermingen in Germany and the Dominican amber deposits of Hispaniola .
Possible human evolutionary ancestors such as Victoriapithecus evolved during this time interval. ReferencesFootnotes
LiteratureWikisource has original works on the topic: Cenozoic#Neogene
External linksWikimedia Commons has media related to Burdigalian.
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