Emsian

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Emsian
407.6 ± 2.6 – 393.3 ± 1.2 Ma
Age
Stratigraphic unitStage
Time span formalityFormal
Lower boundary definitionFAD of the conodont Polygnathus kitabicus
Lower boundary GSSPZinzil'ban Gorge, Uzbekistan
39°12′00″N 67°18′20″E / 39.2000°N 67.3056°E / 39.2000; 67.3056
Lower GSSP ratified1995[5]
Upper boundary definitionFAD of the conodont Polygnathus costatus partitus
Upper boundary GSSPWetteldorf Richtschnitt section, Wetteldorf, Eifel, Germany
50°08′59″N 6°28′18″E / 50.1496°N 6.4716°E / 50.1496; 6.4716
Upper GSSP ratified1985[6]

The Emsian is one of three

Ems river in Germany.[7] The GSSP is located in the Zinzil'ban Gorge in the Kitab State Geological Reserve of Uzbekistan, 35 centimetres (14 in) above the contact with the Madmon Formation
.

In North America the Emsian Stage is represented by Sawkill or Sawkillian time.

Biological events

Emsian-age conical mud mounds at Hamar Laghdad, Morocco

During this period, earliest known

mya).[8][9] Later agoniatitid ammonoids would die out in the Taghanic event in the upper middle Givetian. Goniatite ammonoids would give rise to further ammonoid orders, thus starting ammonoid dominance of marine fossils in further periods until their end at the Cretaceous-Paleogene mass extinction event
.

References


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