Emsium

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system series step ≈ age ( mya )
higher higher higher younger
Devon Upper Devonian Family 358.9

372.2
Frasnium 372.2

382.7
Middle Devon Givetium 382.7

387.7
Eifelium 387.7

393.3
Lower Devon Emsium 393.3

407.6
Pragium 407.6

410.8
Lochkovium 410.8

419.2
deeper deeper deeper older

The Emsium (usually shortened to Ems in German) is the highest chronostratigraphic level of the Lower Devonian series of the ( Devonian ) in geological history . Geochronologically, the stage covers the period from about 407.6 million to about 393.3 million years. The stage follows the Pragium (Devonian) and is overlaid by the Eifelium .

Naming and history

The step is named after Bad Ems in the northwest of the Taunus , where the historical type region is located. The level and name were introduced into scientific literature in 1900 by Henry de Dorlodot .

Definition and GSSP

The lower limit of the level is the first appearance of the conodont species Polygnathus kitabicus (= Polygnathus dehiscens ). The fixed and the International Commission on Stratigraphy 1996 ratified official reference profile ( english global boundary stratotype section and point , GSSP) for the base of Emsiums is the Zinzil'ban Canyon, 170 kilometers southeast of Samarkand , Uzbekistan . The upper limit of the level is defined by the first appearance of the conodont species Polygnathus costatus partitus .

Breakdown

The emsium is subdivided into five conodont biozones:

Individual evidence

  1. Evgeny A. Yolkin, AI Kim, Karsten Weddige, Jim A. Talent, Michael R. House: Definition of the Pragian / Emsian Stage boundary. Episodes. Vol. 20, No. 4, 1997, pp. 235–240 ( PDF 1.0 MB)

literature

  • Felix Gradstein, Jim Ogg & Alan Smith: A Geologic timescale. Cambridge University Press 2004, ISBN 978-0-521-78673-7 .
  • Hans Murawski & Wilhelm Meyer: Geological dictionary . 10., rework. u. exp. Ed., 278 pages, Enke Verlag, Stuttgart 1998, ISBN 3-432-84100-0 .

Web links