Cambrian (Series 3 – Furongian) conodonts from the Alum Shale Formation at Slemmestad, Oslo Region, Norway

Katarina Skagestad Kleppe; Hans Arne Nakrem; Svend Stouge

doi:10.17850/njg98-1-04

Cambrian (Series 3 – Furongian) conodonts from the Alum Shale Formation at Slemmestad, Oslo Region, Norway

Katarina Skagestad Kleppe, Hans Arne Nakrem, Svend Stouge

1 Citationer (Scopus)

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Abstract

Nine samples from the Alum Shale of Slemmestad, Oslo Region, were processed for conodonts. The limestone-rich interval extending from the mid Cambrian Paradoxides paradoxissimus trilobite Zone to the Lower Ordovician Boeckaspis trilobite Zone yielded a sparse conodont fauna. The fauna is dominated by the protoconodont species Phakelodus elongatus (Zhang in An et al., 1983) and Phakelodus tenuis Müller, 1959, the paraconodont species Westergaardodina polymorpha Müller & Hinz, 1991, Westergaardodina ligula Müller & Hinz, 1991, Problematoconites perforatus Müller, 1959 and Trolmenia acies Müller & Hinz, 1991; the euconodont species Cordylodus proavus Müller, 1959 is present in the Acerocarina Superzone. The presence of the cosmopolitan Cordylodus proavus Müller, 1956 at Slemmestad provides an important tie for regional and international correlation.

Originalsprog	Engelsk
Tidsskrift	Norsk Geologisk Tidsskrift
Vol/bind	98
Sider (fra-til)	41-53
ISSN	2387-5844
DOI	https://doi.org/10.17850/njg98-1-04
Status	Udgivet - 2018

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10.17850/njg98-1-04Licens: CC BY

NJG_Vol98_Nr1_Art4_KleppeLicens: CC BY

Citationsformater

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title = "Cambrian (Series 3 – Furongian) conodonts from the Alum Shale Formation at Slemmestad, Oslo Region, Norway",

abstract = "Nine samples from the Alum Shale of Slemmestad, Oslo Region, were processed for conodonts. The limestone-rich interval extending from the mid Cambrian Paradoxides paradoxissimus trilobite Zone to the Lower Ordovician Boeckaspis trilobite Zone yielded a sparse conodont fauna. The fauna is dominated by the protoconodont species Phakelodus elongatus (Zhang in An et al., 1983) and Phakelodus tenuis M{\"u}ller, 1959, the paraconodont species Westergaardodina polymorpha M{\"u}ller & Hinz, 1991, Westergaardodina ligula M{\"u}ller & Hinz, 1991, Problematoconites perforatus M{\"u}ller, 1959 and Trolmenia acies M{\"u}ller & Hinz, 1991; the euconodont species Cordylodus proavus M{\"u}ller, 1959 is present in the Acerocarina Superzone. The presence of the cosmopolitan Cordylodus proavus M{\"u}ller, 1956 at Slemmestad provides an important tie for regional and international correlation.",

author = "Kleppe, {Katarina Skagestad} and Nakrem, {Hans Arne} and Svend Stouge",

year = "2018",

doi = "10.17850/njg98-1-04",

language = "English",

volume = "98",

pages = "41--53",

journal = "Norsk Geologisk Tiddsskrift",

issn = "0029-196X",

publisher = "Geological Society of Norway",

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TY - JOUR

T1 - Cambrian (Series 3 – Furongian) conodonts from the Alum Shale Formation at Slemmestad, Oslo Region, Norway

AU - Kleppe, Katarina Skagestad

AU - Nakrem, Hans Arne

AU - Stouge, Svend

PY - 2018

Y1 - 2018

N2 - Nine samples from the Alum Shale of Slemmestad, Oslo Region, were processed for conodonts. The limestone-rich interval extending from the mid Cambrian Paradoxides paradoxissimus trilobite Zone to the Lower Ordovician Boeckaspis trilobite Zone yielded a sparse conodont fauna. The fauna is dominated by the protoconodont species Phakelodus elongatus (Zhang in An et al., 1983) and Phakelodus tenuis Müller, 1959, the paraconodont species Westergaardodina polymorpha Müller & Hinz, 1991, Westergaardodina ligula Müller & Hinz, 1991, Problematoconites perforatus Müller, 1959 and Trolmenia acies Müller & Hinz, 1991; the euconodont species Cordylodus proavus Müller, 1959 is present in the Acerocarina Superzone. The presence of the cosmopolitan Cordylodus proavus Müller, 1956 at Slemmestad provides an important tie for regional and international correlation.

AB - Nine samples from the Alum Shale of Slemmestad, Oslo Region, were processed for conodonts. The limestone-rich interval extending from the mid Cambrian Paradoxides paradoxissimus trilobite Zone to the Lower Ordovician Boeckaspis trilobite Zone yielded a sparse conodont fauna. The fauna is dominated by the protoconodont species Phakelodus elongatus (Zhang in An et al., 1983) and Phakelodus tenuis Müller, 1959, the paraconodont species Westergaardodina polymorpha Müller & Hinz, 1991, Westergaardodina ligula Müller & Hinz, 1991, Problematoconites perforatus Müller, 1959 and Trolmenia acies Müller & Hinz, 1991; the euconodont species Cordylodus proavus Müller, 1959 is present in the Acerocarina Superzone. The presence of the cosmopolitan Cordylodus proavus Müller, 1956 at Slemmestad provides an important tie for regional and international correlation.

U2 - 10.17850/njg98-1-04

DO - 10.17850/njg98-1-04

M3 - Journal article

SN - 0029-196X

VL - 98

SP - 41

EP - 53

JO - Norsk Geologisk Tiddsskrift

JF - Norsk Geologisk Tiddsskrift

ER -

Cambrian (Series 3 – Furongian) conodonts from the Alum Shale Formation at Slemmestad, Oslo Region, Norway

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