The Ordovician of Scandinavia: a revised regional stage classification

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The Ordovician of Scandinavia : a revised regional stage classification. / Nielsen, Arne Thorshøj; Ahlberg, Per; Ebbestad, Jan Ove R.; Hammer, Øyvind; Harper, David Alexander Taylor; Lindskog, Anders; Rasmussen, Christian Mac Ørum; Stouge, Svend.

In: Geological Society, London, Special Publications, Vol. 532, 2023, p. 267-315.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Nielsen, AT, Ahlberg, P, Ebbestad, JOR, Hammer, Ø, Harper, DAT, Lindskog, A, Rasmussen, CMØ & Stouge, S 2023, 'The Ordovician of Scandinavia: a revised regional stage classification', Geological Society, London, Special Publications, vol. 532, pp. 267-315. https://doi.org/10.1144/SP532-2022-157

APA

Nielsen, A. T., Ahlberg, P., Ebbestad, J. O. R., Hammer, Ø., Harper, D. A. T., Lindskog, A., Rasmussen, C. M. Ø., & Stouge, S. (2023). The Ordovician of Scandinavia: a revised regional stage classification. Geological Society, London, Special Publications, 532, 267-315. https://doi.org/10.1144/SP532-2022-157

Vancouver

Nielsen AT, Ahlberg P, Ebbestad JOR, Hammer Ø, Harper DAT, Lindskog A et al. The Ordovician of Scandinavia: a revised regional stage classification. Geological Society, London, Special Publications. 2023;532:267-315. https://doi.org/10.1144/SP532-2022-157

Author

Nielsen, Arne Thorshøj ; Ahlberg, Per ; Ebbestad, Jan Ove R. ; Hammer, Øyvind ; Harper, David Alexander Taylor ; Lindskog, Anders ; Rasmussen, Christian Mac Ørum ; Stouge, Svend. / The Ordovician of Scandinavia : a revised regional stage classification. In: Geological Society, London, Special Publications. 2023 ; Vol. 532. pp. 267-315.

Bibtex

@article{226090739785419aa13dc3d881709a9c,
title = "The Ordovician of Scandinavia: a revised regional stage classification",
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, Mold{\aa}an, 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.",
author = "Nielsen, {Arne Thorsh{\o}j} and Per Ahlberg and Ebbestad, {Jan Ove R.} and {\O}yvind Hammer and Harper, {David Alexander Taylor} and Anders Lindskog and Rasmussen, {Christian Mac {\O}rum} and Svend Stouge",
year = "2023",
doi = "10.1144/SP532-2022-157",
language = "English",
volume = "532",
pages = "267--315",
journal = "Geological Society Special Publication",
issn = "0305-8719",
publisher = "Geological Society Publishing House",

}

RIS

TY - JOUR

T1 - The Ordovician of Scandinavia

T2 - a revised regional stage classification

AU - Nielsen, Arne Thorshøj

AU - Ahlberg, Per

AU - Ebbestad, Jan Ove R.

AU - Hammer, Øyvind

AU - Harper, David Alexander Taylor

AU - Lindskog, Anders

AU - Rasmussen, Christian Mac Ørum

AU - Stouge, Svend

PY - 2023

Y1 - 2023

N2 - 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.

AB - 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.

U2 - 10.1144/SP532-2022-157

DO - 10.1144/SP532-2022-157

M3 - Journal article

VL - 532

SP - 267

EP - 315

JO - Geological Society Special Publication

JF - Geological Society Special Publication

SN - 0305-8719

ER -

ID: 337592399