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.
^Krijgsman, W.; Garcés, M.; Langereis, C. G.; Daams, R.; Van Dam, J.; Van Der Meulen, A. J.; Agustí, J.; Cabrera, L. (1996). "A new chronology for the middle to late Miocene continental record in Spain". Earth and Planetary Science Letters. 142 (3–4): 367–380. Bibcode:1996E&PSL.142..367K. doi:10.1016/0012-821X(96)00109-4.
^Edward Petuch, Ph.D. Florida Atlantic University, Department of Geosciences."FAU Department of Geosciences". Archived from the original on 2010-06-20. Retrieved 2010-05-01., Author, Cenozoic Seas: The View From Eastern North America. ISBN0-8493-1632-4