Langhian
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The Langhian is, in the Ma and 13.65 ± 0.05 Ma (million years ago) during the Middle Miocene.[5]
The Langhian was a continuing warming period[6] defined by Lorenzo Pareto in 1865, it was originally established in the Langhe area north of Ceva in northern Italy, hence the name. The Langhian is preceded by the Burdigalian and followed by the Serravallian Stage. Stratigraphic definitionThe base of the Langhian is defined by the first appearance of GSSP for the Langhian Stage was not yet established in 2009.
The top of the Langhian Stage (the base of the Serravallian Stage) is at the first occurrence of fossils of the nanoplankton species Sphenolithus heteromorphus and is located in magnetic chronozone C5ABr. The Langhian is coeval with the North American Land Mammal Ages,[5] with mid-Relizian to Luisian Californian regional stages (the Luisian extends barely into the early Serravallian[5]), with the early-mid Badenian Paratethys stage of Central and eastern Europe,[7] with the Tozawan stage in Japan (which runs barely into the early Serravallian[5]), with the late Batesfordian through Balcombian to early Bairnsdalian Australian stages[5] and with the mid-Cliffdenian to mid-Lillburnian New Zealand stages.[5]
PaleontologyReptiles
Cartilaginous fishSharks, rays, skates and relatives
Mammals
ClimateIn August 2021, the 6th IPCC report indicated that global temperature was 4°C– 10°C warmer during the Miocene Climatic Optimum (16.9-14.7 Ma ago) than 1850-1900.[8] See alsoReferencesFootnotes
LiteratureWikisource has original works on the topic: Cenozoic#Neogene
External links
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