The Ordovician of Scandinavia: a revised regional stage classification

Author:

Nielsen Arne Thorshøj1ORCID,Ahlberg Per2ORCID,Ebbestad Jan Ove R.3ORCID,Hammer Øyvind4ORCID,Harper David Alexander Taylor5ORCID,Lindskog Anders2ORCID,Rasmussen Christian Mac Ørum6ORCID,Stouge Svend7ORCID

Affiliation:

1. Department of Geosciences and Natural Resource Management, University of Copenhagen, Øster Voldgade 10, DK-1350 Kbh K, Denmark

2. Department of Geology, Lund University, Sölvegatan 12, SE-223 62 Lund, Sweden

3. Museum of Evolution, Uppsala University, Norbyvägen 16, SE-752 36 Uppsala, Sweden

4. Natural History Museum, University of Oslo, Pb. 1172 Blindern, N-0318 Oslo, Norway

5. Palaeoecosystems Group, Department of Earth Sciences, Durham University, Durham DH1 3LE, UK

6. Globe Institute, University of Copenhagen, Øster Voldgade 5–7, DK-1350 Kbh K, Denmark

7. Natural History Museum of Denmark, University of Copenhagen, Nørre Farimagsgade 2B, DK-1350 Kbh K, Denmark

Abstract

Abstract The Ordovician of Scandinavia (i.e. Denmark, Norway and Sweden) has been investigated for over two centuries and, through time, various chronostratigraphic schemes have been introduced, facilitating regional correlation. However, a modern chronostratigraphy has never been proposed. Here, we delineate ten regional stages for the Ordovician of Scandinavia, comprising, in ascending order, the Slemmestadian, Ottenbyan, Billingenian, Volkhovian, Kundan, Segerstadian, Dalbyan, Moldåan, Jerrestadian and Tommarpian. We propose to discontinue the use of the term Hunnebergian Regional Stage despite its Scandinavian origin; this interval is included in the new Ottenbyan Stage. The base of each stage, as (re)defined here, is selected to coincide with the appearance of a characteristic fossil taxon and delimited at the top by the base of the overlying stage. The stage boundaries generally coincide with or approximate to significant changes in the depositional environment that are recognizable across Scandinavia from the carbonate platform to the foreland basin. Local efficacy has been the primary criterion for the recognition of Scandinavian stage boundaries rather than approximating to the global or East Baltic stage boundaries. It is proposed to abolish the Baltoscandian regional series and subseries, as correlation with the global series is sufficiently precise to make these higher rank regional schemes redundant.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

Reference446 articles.

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