1995•EpisodesOpen access

Definition of the Eifelian- Givetian Stage boundary

Otto Heinrich Walliser, Pierre Bultynck, Karsten Weddige, R. Thomas Becker, Michael R. House

Open full text 79 citations

Abstract

he boundary for the Eifelian-Givetian Stage Global Stratotype Section and Point (GSSP) in the Middle Devonian has been ratified by the ICS and the IUGS and is placed in a section at Jebel Mech Irdane in the Tafilalt of Morocco. The position of the boundary was selected by the Subcommission on Devonian Stratigraphy in 1992 to coincide with the level at which Polygnathus pseudofoliatus changes to Polygnathus hemiansatus as described herein. The boundary corresponds closely with the base of the goniatite Maenioceras Stufe used as a Middle Devonian division, and with the entry of the dacryoconarid Nowakia otomari. Although spores are nor described from the section owing to thermal modification, the level is thought to lie below the appearance of Geminospora lemurata the entry of which has been widely used elsewhere in spore-bearing regions as a guide to the Givetian. Comments are made on the relations of the GSSP level to the associated Kačák or otomari Event.

Open-access reader

About this research paper

What this paper is about

he boundary for the Eifelian-Givetian Stage Global Stratotype Section and Point (GSSP) in the Middle Devonian has been ratified by the ICS and the IUGS and is placed in a section at Jebel Mech Irdane in the Tafilalt of Morocco. The position of the boundary was selected by the Subcommission on Devonian Stratigraphy in 1992 to coincide with the level at which Polygnathus pseudofoliatus changes to Polygnathus hemiansatus as described herein. The boundary corresponds closely with the base of the goniatite Maenioceras Stufe used as a Middle Devonian division, and with the entry of the dacryoconarid Nowakia otomari. Although spores are nor described from the section owing to thermal modification, the level is thought to lie below the appearance of Geminospora lemurata the entry of which has been widely used elsewhere in spore-bearing regions as a guide to the Givetian. Comments are made on the relations of the GSSP level to the associated Kačák or otomari Event.

Why it matters

OpenAlex reports 79 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

he boundary for the Eifelian-Givetian Stage Global Stratotype Section and Point (GSSP) in the Middle Devonian has been ratified by the ICS and the IUGS and is placed in a section at Jebel Mech Irdane in the Tafilalt of Morocco. The position of the boundary was selected by the Subcommission on Devonian Stratigraphy in 1992 to coincide with the level at which Polygnathus pseudofoliatus changes to Polygnathus hemiansatus as described herein. The boundary corresponds closely with the base of the goniatite Maenioceras Stufe used as a Middle Devonian division, and with the entry of the dacryoconarid Nowakia otomari. Although spores are nor described from the section owing to thermal modification, the level is thought to lie below the appearance of Geminospora lemurata the entry of which has been widely used elsewhere in spore-bearing regions as a guide to the Givetian. Comments are made on the relations of the GSSP level to the associated Kačák or otomari Event.

Key concepts: Stage (stratigraphy), Geology, Boundary (topology), Earth science, Mining engineering, Physical geography, Paleontology, Geography

Related papers

Back to paper searchBrowse research topicsOriginal source
Definition of the Eifelian- Givetian Stage boundary — Research Paper | ScholarLens