Distribution and correlation of Sabellidites cambriensis (Annelida?) in the basal Cambrian on Baltica
Sabellidites cambriensis is a tubular non-mineralized metazoan that appears as compressed ribbon-shaped imprints with transverse wrinkling, thick walls and an even tube diameter of up to 3 mm. The distribution of Sabellidites is investigated in three Ediacaran–Cambrian sections on the Digermulen Pen...
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Language: | English |
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Naturhistoriska riksmuseet, Enheten för paleobiologi
2021
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Online Access: | http://urn.kb.se/resolve?urn=urn:nbn:se:nrm:diva-4903 https://doi.org/10.1017/s0016756821001187 |
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ftnrm:oai:DiVA.org:nrm-4903 |
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Open Polar |
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Swedish Museum of Natural History: Publications (DiVA) |
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language |
English |
topic |
Sabellidites Ediacaran-Cambrian boundary biostratigraphy correlation Baltica East European Platform Other Earth and Related Environmental Sciences Annan geovetenskap och miljövetenskap |
spellingShingle |
Sabellidites Ediacaran-Cambrian boundary biostratigraphy correlation Baltica East European Platform Other Earth and Related Environmental Sciences Annan geovetenskap och miljövetenskap Ebbestad, Jan Ove R. Hybertsen, Frida Högström, Anette E. S. Jensen, Sören Palacios, Teodoro Taylor, Wendy L. Agić, Heda Høyberget, Magne Meinhold, Guido Distribution and correlation of Sabellidites cambriensis (Annelida?) in the basal Cambrian on Baltica |
topic_facet |
Sabellidites Ediacaran-Cambrian boundary biostratigraphy correlation Baltica East European Platform Other Earth and Related Environmental Sciences Annan geovetenskap och miljövetenskap |
description |
Sabellidites cambriensis is a tubular non-mineralized metazoan that appears as compressed ribbon-shaped imprints with transverse wrinkling, thick walls and an even tube diameter of up to 3 mm. The distribution of Sabellidites is investigated in three Ediacaran–Cambrian sections on the Digermulen Peninsula in Arctic Norway, spanning the Manndrapselva Member of the Stáhpogieddi Formation and the lower member of the Breidvika Formation. Here, the Ediacaran–Cambrian boundary is located in the lower part of the upper parasequence (third cycle) of the Manndrapselva Member. Specimens of Sabellidites are rare but consistently present close to the lowest level of Treptichnus pedum and upsection, whereas the taxon is common and abundant in the lower part of the lower member of the Breidvika Formation, with an upper record at c. 55 m above the base. The range is comparable with that of the GSSP section in Newfoundland, Canada, establishing Sabellidites as an index fossil for the lowermost Cambrian. In the Manndrapselva Member, Sabellidites co-occurs with the acritarch Granomarginata, indicative of the lowermost Cambrian Granomarginata Zone, whereas in the Breidvika Formation it co-occurs with Asteridium. Sabellidites is widely distributed in Baltica, through the Rovnian and Lontovan regional stages but confined to the Fortunian global stage. In its lower range, Sabellidites is associated with a Treptichnus pedum trace fossil association and a depauperate leiosphaerid acritarch assemblage, followed by a Granomarginata assemblage. In its upper range, Sabellidites co-occurs with acritarchs of the Asteridium–Comasphaeridium Zone and the tubular foraminiferan Platysolenites. In Baltica, Sabellidites is a useful index fossil. The Digermulen Early Life Research Group acknowledges funding to Anette E. S. Högström from the Norwegian Research Council (NRC, project number 231103). Travel support was given to Frida Hybertsen by the Department of Earth Sciences, Palaeobiology, Uppsala University. T. P. & S. J. acknowledge funding ... |
format |
Article in Journal/Newspaper |
author |
Ebbestad, Jan Ove R. Hybertsen, Frida Högström, Anette E. S. Jensen, Sören Palacios, Teodoro Taylor, Wendy L. Agić, Heda Høyberget, Magne Meinhold, Guido |
author_facet |
Ebbestad, Jan Ove R. Hybertsen, Frida Högström, Anette E. S. Jensen, Sören Palacios, Teodoro Taylor, Wendy L. Agić, Heda Høyberget, Magne Meinhold, Guido |
author_sort |
Ebbestad, Jan Ove R. |
title |
Distribution and correlation of Sabellidites cambriensis (Annelida?) in the basal Cambrian on Baltica |
title_short |
Distribution and correlation of Sabellidites cambriensis (Annelida?) in the basal Cambrian on Baltica |
title_full |
Distribution and correlation of Sabellidites cambriensis (Annelida?) in the basal Cambrian on Baltica |
title_fullStr |
Distribution and correlation of Sabellidites cambriensis (Annelida?) in the basal Cambrian on Baltica |
title_full_unstemmed |
Distribution and correlation of Sabellidites cambriensis (Annelida?) in the basal Cambrian on Baltica |
title_sort |
distribution and correlation of sabellidites cambriensis (annelida?) in the basal cambrian on baltica |
publisher |
Naturhistoriska riksmuseet, Enheten för paleobiologi |
publishDate |
2021 |
url |
http://urn.kb.se/resolve?urn=urn:nbn:se:nrm:diva-4903 https://doi.org/10.1017/s0016756821001187 |
long_lat |
ENVELOPE(24.083,24.083,-70.250,-70.250) ENVELOPE(11.560,11.560,64.731,64.731) ENVELOPE(28.018,28.018,70.543,70.543) |
geographic |
Arctic Breidvika Canada Digermulen Norway Stáhpogieddi |
geographic_facet |
Arctic Breidvika Canada Digermulen Norway Stáhpogieddi |
genre |
Arctic Foraminifera* Newfoundland |
genre_facet |
Arctic Foraminifera* Newfoundland |
op_relation |
Geological Magazine, 0016-7568, 2021, 159:7, s. 1262-1283 orcid:0000-0001-8769-3572 orcid:0000-0002-8219-1060 orcid:0000-0002-4917-0559 orcid:0000-0002-9899-5864 orcid:0000-0002-4002-4141 orcid:0000-0001-8375-8375 http://urn.kb.se/resolve?urn=urn:nbn:se:nrm:diva-4903 doi:10.1017/s0016756821001187 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1017/s0016756821001187 |
container_title |
Geological Magazine |
container_volume |
159 |
container_issue |
7 |
container_start_page |
1262 |
op_container_end_page |
1283 |
_version_ |
1766347167800229888 |
spelling |
ftnrm:oai:DiVA.org:nrm-4903 2023-05-15T15:16:52+02:00 Distribution and correlation of Sabellidites cambriensis (Annelida?) in the basal Cambrian on Baltica Ebbestad, Jan Ove R. Hybertsen, Frida Högström, Anette E. S. Jensen, Sören Palacios, Teodoro Taylor, Wendy L. Agić, Heda Høyberget, Magne Meinhold, Guido 2021 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:nrm:diva-4903 https://doi.org/10.1017/s0016756821001187 eng eng Naturhistoriska riksmuseet, Enheten för paleobiologi Uppsala University, Music and Museums, Museum of Evolution UiT Arctic Univ Norway, Arctic Univ Museum Norway, N-9037 Tromso, Norway Univ Extremadura, Fac Ciencias, Area Paleontol, Avenida Fis S-N, Badajoz 06006, Spain Univ Cape Town, Dept Geol Sci, Private Bag 103, ZA-7701 Rondebosch, South Africa Univ Calif Santa Barbara, Dept Earth Sci, Santa Barbara, CA 93106 USA Magne Hoyberget, Rennesveien 14, N-4513 Mandal, Norway Univ Gottingen, Geosci Ctr, Dept Sedimentol & Environm Geol, Goldschmidtstr 3, D-37077 Gottingen, Germany.;Keele Univ, Sch Geog Geol & Environm, Keele ST5 5BG, Staffs, England.;TU Bergakademie Freiberg, Inst Geol, Bernhard Von Cotta Str 2, D-09599 Freiberg, Germany Cambridge Geological Magazine, 0016-7568, 2021, 159:7, s. 1262-1283 orcid:0000-0001-8769-3572 orcid:0000-0002-8219-1060 orcid:0000-0002-4917-0559 orcid:0000-0002-9899-5864 orcid:0000-0002-4002-4141 orcid:0000-0001-8375-8375 http://urn.kb.se/resolve?urn=urn:nbn:se:nrm:diva-4903 doi:10.1017/s0016756821001187 info:eu-repo/semantics/openAccess Sabellidites Ediacaran-Cambrian boundary biostratigraphy correlation Baltica East European Platform Other Earth and Related Environmental Sciences Annan geovetenskap och miljövetenskap Article in journal info:eu-repo/semantics/article text 2021 ftnrm https://doi.org/10.1017/s0016756821001187 2022-12-08T17:17:16Z Sabellidites cambriensis is a tubular non-mineralized metazoan that appears as compressed ribbon-shaped imprints with transverse wrinkling, thick walls and an even tube diameter of up to 3 mm. The distribution of Sabellidites is investigated in three Ediacaran–Cambrian sections on the Digermulen Peninsula in Arctic Norway, spanning the Manndrapselva Member of the Stáhpogieddi Formation and the lower member of the Breidvika Formation. Here, the Ediacaran–Cambrian boundary is located in the lower part of the upper parasequence (third cycle) of the Manndrapselva Member. Specimens of Sabellidites are rare but consistently present close to the lowest level of Treptichnus pedum and upsection, whereas the taxon is common and abundant in the lower part of the lower member of the Breidvika Formation, with an upper record at c. 55 m above the base. The range is comparable with that of the GSSP section in Newfoundland, Canada, establishing Sabellidites as an index fossil for the lowermost Cambrian. In the Manndrapselva Member, Sabellidites co-occurs with the acritarch Granomarginata, indicative of the lowermost Cambrian Granomarginata Zone, whereas in the Breidvika Formation it co-occurs with Asteridium. Sabellidites is widely distributed in Baltica, through the Rovnian and Lontovan regional stages but confined to the Fortunian global stage. In its lower range, Sabellidites is associated with a Treptichnus pedum trace fossil association and a depauperate leiosphaerid acritarch assemblage, followed by a Granomarginata assemblage. In its upper range, Sabellidites co-occurs with acritarchs of the Asteridium–Comasphaeridium Zone and the tubular foraminiferan Platysolenites. In Baltica, Sabellidites is a useful index fossil. The Digermulen Early Life Research Group acknowledges funding to Anette E. S. Högström from the Norwegian Research Council (NRC, project number 231103). Travel support was given to Frida Hybertsen by the Department of Earth Sciences, Palaeobiology, Uppsala University. T. P. & S. J. acknowledge funding ... Article in Journal/Newspaper Arctic Foraminifera* Newfoundland Swedish Museum of Natural History: Publications (DiVA) Arctic Breidvika ENVELOPE(24.083,24.083,-70.250,-70.250) Canada Digermulen ENVELOPE(11.560,11.560,64.731,64.731) Norway Stáhpogieddi ENVELOPE(28.018,28.018,70.543,70.543) Geological Magazine 159 7 1262 1283 |