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Acritarchs from the Duolbagaisa Formation (Cambrian Series 2, Miaolingian) on the Digermulen Peninsula, Finnmark, Arctic Norway : towards a high-resolution Cambrian chronostratigraphy

Palacios, Teodoro (författare)
Univ Extremadura, Fac Ciencias, Area Paleontol, Ave Fis S-N, Badajoz 06006, Spain.
Högström, Anette E. S. (författare)
UiT Arctic Univ Norway, Arctic Univ Museum Norway, N-9037 Tromso, Norway.
Ebbestad, Jan Ove R., 1967- (författare)
Uppsala universitet,Evolutionsmuseet
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Agić, Heda, 1989- (författare)
Uppsala universitet,Paleobiologi,Univ Calif Santa Barbara, Dept Earth Sci, Santa Barbara, CA 93106 USA.
Höyberget, Magne (författare)
Rennesveien 14, N-4513 Mandal, Norway.
Jensen, Sören (författare)
Univ Extremadura, Fac Ciencias, Area Paleontol, Ave Fis S-N, Badajoz 06006, Spain.
Meinhold, Guido (författare)
Univ Gottingen, Dept Sedimentol & Environm Geol, Geosci Ctr, Goldschmidtstr 3, D-37077 Gottingen, Germany.;Keele Univ, Sch Geog Geol & Environm, Keele ST5 5BG, Staffs, England.
Taylor, Wendy L. (författare)
Univ Cape Town, Dept Geol Sci, Private Bag X3, ZA-7701 Rondebosch, South Africa.
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Univ Extremadura, Fac Ciencias, Area Paleontol, Ave Fis S-N, Badajoz 06006, Spain UiT Arctic Univ Norway, Arctic Univ Museum Norway, N-9037 Tromso, Norway. (creator_code:org_t)
CAMBRIDGE UNIV PRESS, 2020
2020
Engelska.
Ingår i: Geological Magazine. - : CAMBRIDGE UNIV PRESS. - 0016-7568 .- 1469-5081. ; 157:12, s. 2051-2066
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • New information on acritarchs from the Duolbagaisa Formation, Digermulen Peninsula, Arctic Norway, enable recognition of the three Cambrian Series 2 acritarch-based zones: the Skiagia ornata-Fimbriaglomerella membranacea, Heliosphaeridium dissimilare-Skiagia ciliosa and Volkovia dentifera-Liepaina plana Assemblage zones. Acritarchs of the Skiagia ornata-Fimbriaglomerella membranacea Zone (Cambrian Stage 3) appear near the base of the unit, close to an undetermined trilobite. In the Upper Member of the Duolbagaisa Formation, in levels with Kjerulfia n. sp. and Elliptocephala n. sp., appears an assemblage with abundant Skiagia ciliosa, indicative of the Heliosphaeridium dissimilare-Skiagia ciliosa Zone. A few metres higher appear Liepaina plana, Heliosphaeridium notatum and Retisphaeridium dichamerum, which indicate the Volkovia dentifera-Liepaina plana Zone (Cambrian Stage 4). The transition between the Duolbagaisa Formation and the overlying Kistedalen Formation is marked by the appearance of Comasphaeridium longispinosum, Multiplicisphaeridium llynense and Eliasum llaniscum, diagnostic of the Miaolingian Series. This coincides with the disappearance of Skiagia; occurrences of Skiagia in Miaolingian strata consist of reworked material related to the Hawke Bay regression at the Cambrian Stage 4-Wuliuan transition. The absence of Skiagia in higher levels of the Duolbagaisa Formation and Kistedalen Formation suggests that no unconformity formed during the Hawke Bay regression in this area. The chronostratigraphical significance of the Skiagia ornata-Fimbriaglomerella membranacea, Heliosphaeridium dissimilare-Skiagia ciliosa and Volkovia dentifera-Liepaina plana zones is critically analysed. Correlation of the Duolbagaisa Formation with peri-Gondwanan terrains of Avalonia and Iberia is established. The Digermulen Peninsula has great potential as a reference section for establishing a Cambrian chronostratigraphy based on acritarchs.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Annan geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Other Earth and Related Environmental Sciences (hsv//eng)

Nyckelord

acritarchs
Cambrian
chronostratigraphy
Hawke Bay regression
Norway
organic-walled microfossils

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