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Lutetian

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Lutetian
47.8 – 41.2Ma
Chronology
Formerly part ofTertiaryPeriod/System
Etymology
Name formalityFormal
Usage information
Celestial bodyEarth
Regional usageGlobal (ICS)
Time scale(s) usedICS Time Scale
Definition
Chronological unitAge
Stratigraphic unitStage
Time span formalityFormal
Lower boundary definitionFADof the calcareous nannofossilBlackites inflatus
Lower boundary GSSPGorrondatxe section,Western Pyrenees,Basque Country,Spain
43°22′47″N3°00′51″W/ 43.3796°N 3.0143°W/43.3796; -3.0143
Lower GSSP ratifiedApril 2011[3]
Upper boundary definitionNot formally defined
Upper boundary definition candidatesCalcareous nannofossil nearLADof theHaptophyteReticulofenestra reticulata
Upper boundary GSSP candidate section(s)Contessa highway section,Gubbio,Central Apennines,Italy

TheLutetianis, in thegeologic timescale,astageoragein theEocene.[4]It spans the time between47.8and41.2Ma.The Lutetian is preceded by theYpresianand is followed by the Bartonian.[5]Together with theBartonianit is sometimes referred to as the Middle Eocene Subepoch.

Stratigraphic definition

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The Lutetian was named afterLutetia,theLatinname for the city ofParis.The Lutetian Stage was introduced in scientific literature by French geologistAlbert de Lapparentin 1883[6]and revised by A. Blondeau in 1981.[7]

The base of the Lutetian Stage is at the first appearance of the nanofossilBlackites inflatus,according to an official reference profile (GSSP) established in 2011.[8]Of two candidates located inSpain,the Gorrondatxe section was chosen.[9]

The top of the Lutetian (the base of the Bartonian) is at the first appearance ofcalcareous nanoplanktonspeciesReticulofenestra reticulata.

The Lutetian overlaps with theGeiseltalianand lower RobiacianEuropean Land Mammal Mega Zones(The Lutetian Stage spans theMammal Paleogene zones11 through 15.[10]), the upperBridgerianandUintanNorth American Land Mammal Ages,the upperArshantanandIrdinmanhanAsian Land Mammal Ages,and theMustersanand lowerDivisaderanSouth American Land Mammal Ages.It is also coeval with the middle Johannian regional stage ofAustraliaand the upper Ulatisian and lower Nanzian regional stages ofCalifornia.

References

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  1. ^Zachos, J. C.; Kump, L. R. (2005). "Carbon cycle feedbacks and the initiation of Antarctic glaciation in the earliest Oligocene".Global and Planetary Change.47(1): 51–66.Bibcode:2005GPC....47...51Z.doi:10.1016/j.gloplacha.2005.01.001.
  2. ^"International Chronostratigraphic Chart"(PDF).International Commission on Stratigraphy.
  3. ^Molina, Eustoquio; Alegret, Laia; Apellaniz, Estibaliz; Bernaola, Gilen; Caballero, Fernando; Jaume Dinarès-Turell; Hardenbol, Jan; Claus Heilmann-Clausen; Juan C. Larrasoana; Hanspeter Luterbacher; Simonetta Monechi; Silvia Ortiz; Xabier Orue-Etxebarria; Aitor Payros; Victoriano Pujalte; Francisco J. Rodríguez-Tobar; Flavia Tori; Josep Tosquella; Alfred Uchman (2011)."The Global Stratotype Section and Point (GSSP) for the base of the Lutetian Stage at the Gorrondatxe section, Spain"(PDF).Episodes.34(2): 86–108.doi:10.18814/epiiugs/2011/v34i2/006.
  4. ^Established by D.G. Jenkins and H. Luterbacher, "Paleogene stages and their boundaries (introductory remarks)" inNeues Jarhbuch fur Geologie und Paläontologie1992.
  5. ^Gradstein, F.M.; Ogg, J.G. & Smith, A.G. (2004):A Geologic Time Scale 2004,Cambridge University Press.
  6. ^de Lapparent, A.A.C. (1883):Traité de Géologie,Paris.
  7. ^Blondeau (1981): "Lutetian" inBulletin d'information des géologues du Bassin de Paris,2,pp. 167–180.
  8. ^"The Lutetian GSSP at meter 167.85 of the Gorrondatxe section in a dark marly level where the nanofossilBlackites inflatusfirst appears "(working group website).
  9. ^See thewebsite of Eustoquio Molinafor these candidates.
  10. ^Alroy, John."Mammal Paleogene zones".p. The Paleobiology Database.Retrieved15 July2009.
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