Miaolingian (Cambrian) trilobite biostratigraphy and carbon isotope chemostratigraphy in the Tingskullen drill core, Oland, Sweden
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F21%3AN0000131" target="_blank" >RIV/60460709:41330/21:N0000131 - isvavai.cz</a>
Result on the web
<a href="https://kirj.ee/earth-publications/?filter%5Byear%5D=2021&filter%5Bissue%5D=412&" target="_blank" >https://kirj.ee/earth-publications/?filter%5Byear%5D=2021&filter%5Bissue%5D=412&</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.3176/earth.2021.03" target="_blank" >10.3176/earth.2021.03</a>
Alternative languages
Result language
angličtina
Original language name
Miaolingian (Cambrian) trilobite biostratigraphy and carbon isotope chemostratigraphy in the Tingskullen drill core, Oland, Sweden
Original language description
The Cambrian succession of the Tingskullen drill core from northern Oland comprises Cambrian Series 2 and Miaolingian (Wulivan Stage) siliciclastic strata. The major portion of the succession is represented by the Miaolingian Borgholm Formation, which, in ascending order, is subdivided into the Mossberga, Barstad and Aleklinta members. The Aleklinta Member is barren of body fossils, whereas the Mossberga and BArstad members are moderately to highly fossiliferous and biostratigraphically reasonably well constrained. Trilobites and agnostoids from the BArstad Member are indicative of the Acadoparadoxides pin us Zone. The Mossberga Member has not yielded any zonal guide fossils but is tentatively assigned to the Eccaparadoxides insularis Zone. A delta C-13(org) curve throughout the Borgholm Formation shows a general positive trend up section without any distinctive excursion, suggesting that the Wulivan Acadoparadoxides (Baltoparadoxides) oelandicus Superzone (the Oelandicus beds) of Oland is younger than the negative Redlichiid-Olenellid Extinction Carbon isotope Excursion (ROECE), which is known from near the top of Stage 4 and close to the traditional Lower-Middle Cambrian boundary in several parts of the world.
Czech name
—
Czech description
—
Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
—
OECD FORD branch
10505 - Geology
Result continuities
Project
—
Continuities
S - Specificky vyzkum na vysokych skolach
Others
Publication year
2021
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
ESTONIAN JOURNAL OF EARTH SCIENCES
ISSN
1736-4728
e-ISSN
1736-7557
Volume of the periodical
70
Issue of the periodical within the volume
1
Country of publishing house
EE - ESTONIA
Number of pages
18
Pages from-to
18-35
UT code for WoS article
000609229300002
EID of the result in the Scopus database
2-s2.0-85099604457