Asselium

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system series step ≈ age ( mya )
higher higher higher younger
Perm Lopingium Changhsingium 251.9

254.2
Wuchiapingium 254.2

259.9
Guadalupium Capitanium 259.9

265.1
Wordium 265.1

268.8
Roadium 268.8

272.3
Cisuralium Kungurium 272.3

279.3
Artinskium 279.3

290.1
Sacmarium 290.1

295.5
Asselium 295.5

298.9
deeper deeper deeper older

The Asselium is the lowest chronostratigraphic level of the Unterperm or the Cisuralium in the history of the earth . The level ranges in absolute numbers ( geochronologically ) from about 298.9 million years to about 295.5 million years. The Asselium follows the Gzhelium , the uppermost level of the Carboniferous, and is replaced by the Sacmarium .

Naming and history

The stage was separated and named in 1954 from the formerly more comprehensive Sakmar stage ( Sakmarium ) by the Soviet paleontologist, malacologist and geologist Vasily Yermolajewitsch Rushenzew ( Russian Василий Ермолаевич Руженцев , 1899–1978). The Asselium is named after the Russian-Kazakh border river Assel in the southern Urals .

Definition and GSSP

The beginning of the Asselium (and the Cisuralium ) is defined by the first appearance of the conodont species Streptognathodus isolatus . The end of the stage is reached with the first appearance of the conodont species Streptognathodus postfusus . The globally valid type locality ( GSSP = Global Stratotype Section and Point) established by the IUGS is located in the Aidaralash valley, near the city of Aqtöbe (Russian Aktyubinsk) in the southern Urals ( Kazakhstan ).

Breakdown

The Asselium can be divided into five conodont biozones:

literature

  • Felix Gradstein, Jim Ogg, Jim & Alan Smith: A Geologic timescale. Cambridge University Press 2004, ISBN 978-0-521-78673-7
  • Vladimir I. Davydov, Brian F. Glenister, Claude Spinosa, Scott M. Ritter, VV Chernykh, BR Wardlaw and WS Snyder: Proposal of Aidaralash as Global Stratotype Section and Point (GSSP) for base of the Permian System . In: Episodes. 21 (1): 11-18, Beijing 1998 ISSN  0705-3797 PDF

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