The Langhian is, in the ICS geologic timescale, an age or stage in the middle Miocene Epoch/Series.

[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 base of the Langhian is defined by the first appearance of foraminifer species Praeorbulina glomerosa and is also coeval with the top of magnetic chronozone C5Cn.1n.

The Langhian is coeval with the Orleanian and Astaracian European Land Mammal Mega Zones (more precisely: with biozones MN5 and MN6, MN6 starts just below the Langhian-Serravallian boundary[7]), with the upper Hemingfordian to mid-Barstovian 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] Sharks, rays, skates and relatives In 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.