Lower Ordovician (Billingenian - Kunda) conodont zonation and provinces based on sections from Horns Udde, north Öland, Sweden

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Standard

Lower Ordovician (Billingenian - Kunda) conodont zonation and provinces based on sections from Horns Udde, north Öland, Sweden. / Bagnoli, Gabriella; Stouge, Svend.

I: Bollettino della Societa Paleontologica Italiana, Bind 35, Nr. 2, 1996, s. 109-163.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Bagnoli, G & Stouge, S 1996, 'Lower Ordovician (Billingenian - Kunda) conodont zonation and provinces based on sections from Horns Udde, north Öland, Sweden', Bollettino della Societa Paleontologica Italiana, bind 35, nr. 2, s. 109-163.

APA

Bagnoli, G., & Stouge, S. (1996). Lower Ordovician (Billingenian - Kunda) conodont zonation and provinces based on sections from Horns Udde, north Öland, Sweden. Bollettino della Societa Paleontologica Italiana, 35(2), 109-163.

Vancouver

Bagnoli G, Stouge S. Lower Ordovician (Billingenian - Kunda) conodont zonation and provinces based on sections from Horns Udde, north Öland, Sweden. Bollettino della Societa Paleontologica Italiana. 1996;35(2):109-163.

Author

Bagnoli, Gabriella ; Stouge, Svend. / Lower Ordovician (Billingenian - Kunda) conodont zonation and provinces based on sections from Horns Udde, north Öland, Sweden. I: Bollettino della Societa Paleontologica Italiana. 1996 ; Bind 35, Nr. 2. s. 109-163.

Bibtex

@article{544a10483254428f8eb1d3a80a2413cb,
title = "Lower Ordovician (Billingenian - Kunda) conodont zonation and provinces based on sections from Horns Udde, north {\"O}land, Sweden",
abstract = "The Hunnebergian to Kunda conodont succession of the lower Ordovician Orthoceras Limestone on northern {\"O}land, Sweden is described. The faunal succession is based on 57563 conodont elements recorded from two representative sections: North of Horns Udde and Horns Udde quarry. The new data allow the recognition and definition of 10 successive interval zones, each characterized by a nominate species and a distinctive conodont association. The interval zones are recommended to substitute the previous assemblage zones in future references to the conodonts of the {\"O}land region. The interval zones are compared with earlier and corresponding zones of the lower Ordovician in neighbouring areas. The interval zones provide an alternative reference to former formally established zones as precise correlation across the East European Platform is possible. The fauna changed from cosmopolitan in Billingen time to provincial in Volkhov time. The fauna assemblages changed from Pandemic forms to temperate water (Precordilleran) faunas and finally were replaced by cold water (Baltic Province) conodonts of the North Atlantic Realm. The Baltic Province persisted throughout the lower Ordovician on the East European Platform. The change of fauna from Pandemic to provincial is connected with sea level changes and a shallowing of the shelf environs. One new multielement genus is recognized: Lundodus; one multielement genus has been revived: Gothodus Lindstr{\"o}m, 1955, and two multielement genera are revised: Lenodus Sergeeva, 1963 and Trapezognathus Lindstr{\"o}m, 1955. Four new species are named: Parapanderodus quietus, Protopanderodus floridus, Protopanderodus calceatus, and Scolopodus princeps, and 20 species are reported but not formally named because they are of low occurrences but with a known apparatus structure and because the number of specimens avaible was not adequate for their definition.",
keywords = "Conodont zones, Conodonts, Lower Ordovician, {\"O}land, Provincialism, Systematics",
author = "Gabriella Bagnoli and Svend Stouge",
year = "1996",
language = "English",
volume = "35",
pages = "109--163",
journal = "Societa Paleontologica Italiana. Bollettino",
issn = "0375-7633",
publisher = "Consiglio Nazionale delle Ricerche",
number = "2",

}

RIS

TY - JOUR

T1 - Lower Ordovician (Billingenian - Kunda) conodont zonation and provinces based on sections from Horns Udde, north Öland, Sweden

AU - Bagnoli, Gabriella

AU - Stouge, Svend

PY - 1996

Y1 - 1996

N2 - The Hunnebergian to Kunda conodont succession of the lower Ordovician Orthoceras Limestone on northern Öland, Sweden is described. The faunal succession is based on 57563 conodont elements recorded from two representative sections: North of Horns Udde and Horns Udde quarry. The new data allow the recognition and definition of 10 successive interval zones, each characterized by a nominate species and a distinctive conodont association. The interval zones are recommended to substitute the previous assemblage zones in future references to the conodonts of the Öland region. The interval zones are compared with earlier and corresponding zones of the lower Ordovician in neighbouring areas. The interval zones provide an alternative reference to former formally established zones as precise correlation across the East European Platform is possible. The fauna changed from cosmopolitan in Billingen time to provincial in Volkhov time. The fauna assemblages changed from Pandemic forms to temperate water (Precordilleran) faunas and finally were replaced by cold water (Baltic Province) conodonts of the North Atlantic Realm. The Baltic Province persisted throughout the lower Ordovician on the East European Platform. The change of fauna from Pandemic to provincial is connected with sea level changes and a shallowing of the shelf environs. One new multielement genus is recognized: Lundodus; one multielement genus has been revived: Gothodus Lindström, 1955, and two multielement genera are revised: Lenodus Sergeeva, 1963 and Trapezognathus Lindström, 1955. Four new species are named: Parapanderodus quietus, Protopanderodus floridus, Protopanderodus calceatus, and Scolopodus princeps, and 20 species are reported but not formally named because they are of low occurrences but with a known apparatus structure and because the number of specimens avaible was not adequate for their definition.

AB - The Hunnebergian to Kunda conodont succession of the lower Ordovician Orthoceras Limestone on northern Öland, Sweden is described. The faunal succession is based on 57563 conodont elements recorded from two representative sections: North of Horns Udde and Horns Udde quarry. The new data allow the recognition and definition of 10 successive interval zones, each characterized by a nominate species and a distinctive conodont association. The interval zones are recommended to substitute the previous assemblage zones in future references to the conodonts of the Öland region. The interval zones are compared with earlier and corresponding zones of the lower Ordovician in neighbouring areas. The interval zones provide an alternative reference to former formally established zones as precise correlation across the East European Platform is possible. The fauna changed from cosmopolitan in Billingen time to provincial in Volkhov time. The fauna assemblages changed from Pandemic forms to temperate water (Precordilleran) faunas and finally were replaced by cold water (Baltic Province) conodonts of the North Atlantic Realm. The Baltic Province persisted throughout the lower Ordovician on the East European Platform. The change of fauna from Pandemic to provincial is connected with sea level changes and a shallowing of the shelf environs. One new multielement genus is recognized: Lundodus; one multielement genus has been revived: Gothodus Lindström, 1955, and two multielement genera are revised: Lenodus Sergeeva, 1963 and Trapezognathus Lindström, 1955. Four new species are named: Parapanderodus quietus, Protopanderodus floridus, Protopanderodus calceatus, and Scolopodus princeps, and 20 species are reported but not formally named because they are of low occurrences but with a known apparatus structure and because the number of specimens avaible was not adequate for their definition.

KW - Conodont zones

KW - Conodonts

KW - Lower Ordovician

KW - Öland

KW - Provincialism

KW - Systematics

UR - http://www.scopus.com/inward/record.url?scp=0030410435&partnerID=8YFLogxK

M3 - Journal article

AN - SCOPUS:0030410435

VL - 35

SP - 109

EP - 163

JO - Societa Paleontologica Italiana. Bollettino

JF - Societa Paleontologica Italiana. Bollettino

SN - 0375-7633

IS - 2

ER -

ID: 361838323