Silurian graptolite biostratigraphy of the Röstånga-1 drill core, Scania: a standard for southern Scandinavia

Jörg Maletz; Per Ahlberg; Anna Suyarkova; David Kendrick Loydell

doi:10.1080/11035897.2013.865665

Silurian graptolite biostratigraphy of the Röstånga-1 drill core, Scania: a standard for southern Scandinavia

Jörg Maletz, Per Ahlberg, Anna Suyarkova, David Kendrick Loydell

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Abstract

The Röstånga-1 core from west-central Scania provides the most complete succession of the Sandbian (Upper Ordovician) through lower Telychian (Silurian, Llandovery) strata of southern Scandinavia. The Hirnantian is identified in the Kallholn Formation by the presence of a Metabolograptus persculptus Biozone fauna. The Akidograptus ascensus, Parakidograptus acuminatus, Cystograptus vesiculosus and Monograptus revolutus biozones can be differentiated in the Rhuddanian. Following a considerable gap (Demirastrites triangulatus Biozone to a level within the Pribylograptus leptotheca Biozone), the succession resumes. The Aeronian also includes the Lituigraptus convolutus and Stimulograptus sedgwickii biozones. The Stimulograptus halli Biozone appears to be missing, but the Telychian Spirograptus guerichi to Streptograptus crispus biozones have been recognized.

Original language	English
Pages (from-to)	175-178
Journal	GFF
Volume	136
Issue number	1
Early online date	14 Jan 2014
DOIs	https://doi.org/10.1080/11035897.2013.865665
Publication status	Published - Jan 2014

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10.1080/11035897.2013.865665

Silurian graptolite biostratigraphy
This is an Accepted Manuscript of an article published by Taylor & Francis in GFF on 14/1/14, available online: http://wwww.tandfonline.com/10.1080/11035897.2013.865665
Accepted author manuscript (Post-print), 733 KB

http://www.tandfonline.com/doi/abs/10.1080/11035897.2013.865665

Cite this

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title = "Silurian graptolite biostratigraphy of the R{\"o}st{\aa}nga-1 drill core, Scania: a standard for southern Scandinavia",

abstract = "The R{\"o}st{\aa}nga-1 core from west-central Scania provides the most complete succession of the Sandbian (Upper Ordovician) through lower Telychian (Silurian, Llandovery) strata of southern Scandinavia. The Hirnantian is identified in the Kallholn Formation by the presence of a Metabolograptus persculptus Biozone fauna. The Akidograptus ascensus, Parakidograptus acuminatus, Cystograptus vesiculosus and Monograptus revolutus biozones can be differentiated in the Rhuddanian. Following a considerable gap (Demirastrites triangulatus Biozone to a level within the Pribylograptus leptotheca Biozone), the succession resumes. The Aeronian also includes the Lituigraptus convolutus and Stimulograptus sedgwickii biozones. The Stimulograptus halli Biozone appears to be missing, but the Telychian Spirograptus guerichi to Streptograptus crispus biozones have been recognized.",

author = "J{\"o}rg Maletz and Per Ahlberg and Anna Suyarkova and Loydell, \{David Kendrick\}",

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month = jan,

doi = "10.1080/11035897.2013.865665",

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T2 - a standard for southern Scandinavia

AU - Maletz, Jörg

AU - Ahlberg, Per

AU - Suyarkova, Anna

AU - Loydell, David Kendrick

N1 - This is an Accepted Manuscript of an article published by Taylor & Francis in GFF on 14/1/14, available online: http://wwww.tandfonline.com/10.1080/11035897.2013.865665

PY - 2014/1

Y1 - 2014/1

N2 - The Röstånga-1 core from west-central Scania provides the most complete succession of the Sandbian (Upper Ordovician) through lower Telychian (Silurian, Llandovery) strata of southern Scandinavia. The Hirnantian is identified in the Kallholn Formation by the presence of a Metabolograptus persculptus Biozone fauna. The Akidograptus ascensus, Parakidograptus acuminatus, Cystograptus vesiculosus and Monograptus revolutus biozones can be differentiated in the Rhuddanian. Following a considerable gap (Demirastrites triangulatus Biozone to a level within the Pribylograptus leptotheca Biozone), the succession resumes. The Aeronian also includes the Lituigraptus convolutus and Stimulograptus sedgwickii biozones. The Stimulograptus halli Biozone appears to be missing, but the Telychian Spirograptus guerichi to Streptograptus crispus biozones have been recognized.

AB - The Röstånga-1 core from west-central Scania provides the most complete succession of the Sandbian (Upper Ordovician) through lower Telychian (Silurian, Llandovery) strata of southern Scandinavia. The Hirnantian is identified in the Kallholn Formation by the presence of a Metabolograptus persculptus Biozone fauna. The Akidograptus ascensus, Parakidograptus acuminatus, Cystograptus vesiculosus and Monograptus revolutus biozones can be differentiated in the Rhuddanian. Following a considerable gap (Demirastrites triangulatus Biozone to a level within the Pribylograptus leptotheca Biozone), the succession resumes. The Aeronian also includes the Lituigraptus convolutus and Stimulograptus sedgwickii biozones. The Stimulograptus halli Biozone appears to be missing, but the Telychian Spirograptus guerichi to Streptograptus crispus biozones have been recognized.

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DO - 10.1080/11035897.2013.865665

M3 - Article

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JF - GFF

IS - 1

ER -

Silurian graptolite biostratigraphy of the Röstånga-1 drill core, Scania: a standard for southern Scandinavia

Abstract

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