The Lutetian is, in the geologic timescale, a stage or age in the Eocene.[4] It spans the time between 48.07 and41.03 Ma. The Lutetian is preceded by the Ypresian and is followed by the Bartonian.[5] Together with the Bartonian it is sometimes referred to as the Middle Eocene Subepoch.
Stratigraphic definition
The Lutetian was named after Lutetia, the Latin name for the city of Paris. The Lutetian Stage was introduced in scientific literature by French geologist Albert de Lapparent in 1883[6] and revised by A. Blondeau in 1981.[7]
The base of the Lutetian Stage is at the first appearance of the nanofossil Blackites inflatus, according to an official reference profile (GSSP) established in 2011.[8] Of two candidates located in Spain, the Gorrondatxe section was chosen.[9]
^Established by D.G. Jenkins and H. Luterbacher, "Paleogene stages and their boundaries (introductory remarks)" in Neues Jarhbuch fur Geologie und Paläontologie 1992.
^de Lapparent, A.A.C. (1883): Traité de Géologie, Paris.
^Blondeau (1981): "Lutetian" in Bulletin d'information des géologues du Bassin de Paris, 2, pp. 167–180.
^"The Lutetian GSSP at meter 167.85 of the Gorrondatxe section in a dark marly level where the nanofossil Blackites inflatus first appears" (working group website).