2007
DOI: 10.1017/s0016756807003597
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A new lower Cambrian eodiscoid trilobite fauna from Swedish Lapland and its implications for intercontinental correlation

Abstract: A lower Cambrian eodiscoid trilobite fauna and an associated holmiid trilobite,Holmiasp., are described from a bioclastic limestone at the top of the Torneträsk Formation in the Luobákti section, south of Lake Torneträsk, northern Sweden. Other associated polymerid trilobites includeOrodes?lapponicaandStrenuaeva inflata. The precise age of the trilobite fauna cannot be determined, but its generic composition and stratigraphical position at the top of the lower Cambrian suggest that it was recovered from theOrn… Show more

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Cited by 21 publications
(39 citation statements)
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References 21 publications
(43 reference statements)
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“…1, area 1), northern Lapland (Føyn 1967;Ahlberg 1980;Thelander 1982;Axheimer et al 2007;Cederström et al 2011b); (2) the Laisvall mining district (Fig. 1, area 2), central Lapland (Kautsky 1945;Willdén 1980;Kulling 1982;Ahlberg 1984a;Vidal & Moczydłowska 1996;Moczydłowska et al 2001) and (3) the Lake Storuman area (Fig.…”
Section: Geological Setting and Localitiesmentioning
confidence: 99%
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“…1, area 1), northern Lapland (Føyn 1967;Ahlberg 1980;Thelander 1982;Axheimer et al 2007;Cederström et al 2011b); (2) the Laisvall mining district (Fig. 1, area 2), central Lapland (Kautsky 1945;Willdén 1980;Kulling 1982;Ahlberg 1984a;Vidal & Moczydłowska 1996;Moczydłowska et al 2001) and (3) the Lake Storuman area (Fig.…”
Section: Geological Setting and Localitiesmentioning
confidence: 99%
“…1, Torneträsk area; 2, Laisvall mining district; 3, Lake Storuman area; 4, Fånån area at Lake Sörsjön; 5, Mjøsa area, SE Norway. Based on Axheimer et al (2007, fig. 1a).…”
Section: Laisvall Mining District Swedenmentioning
confidence: 99%
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“…The top of the dentifera-plana Biozone is generally equated with the top of the Ornamentaspis? linnarssoni/"Protolenus" interval, but Axheimer et al (2007, fig. 3) depicted correlation of the latter to be either diachronous or uncertain, rising from the base of the Cephalopyge notabilis Trilobite Zone to the base of the Eoparadoxides harlani Trilobite Zone (Fig.…”
Section: Furongianmentioning
confidence: 97%