Early-Middle Frasnian (Late Devonian) carbon isotope Event in the Timan-Pechora Basin (Chernyshev Swell, Pymvashor River section, North Cis-Urals, Russia)

Biostratigraphically constrained carbonate (δ13Ccarb) and organic carbon (δ13Corg) variations in the Early-Middle Frasnian boundary interval in the Pymvashor River section (Timan-Pechora Basin, Cis-Urals, in the far north of European Russia) were considered. The studied interval of section is repres...

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Autores: Kotik, Ivan S., Zhuravlev, Andrey V.|||0000-0003-4043-6303, Maydl, Tatiana V., Bushnev, Dmitriy A., Smoleva, Irina V.
Formato: artículo
Fecha de publicación:2021
País:España
Recursos:Universitat Autònoma de Barcelona
Repositorio:Dipòsit Digital de Documents de la UAB
Idioma:inglés
OAI Identifier:oai:ddd.uab.cat:250170
Acesso em linha:https://ddd.uab.cat/record/250170
https://dx.doi.org/urn:doi:10.1344/GeologicaActa2021.19.3
Access Level:acceso abierto
Palavra-chave:Late Devonian
Punctata Event
Carbon isotopes
Biomarkers
Conodonts
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spelling Early-Middle Frasnian (Late Devonian) carbon isotope Event in the Timan-Pechora Basin (Chernyshev Swell, Pymvashor River section, North Cis-Urals, Russia)Kotik, Ivan S.Zhuravlev, Andrey V.|||0000-0003-4043-6303Maydl, Tatiana V.Bushnev, Dmitriy A.Smoleva, Irina V.Late DevonianPunctata EventCarbon isotopesBiomarkersConodontsBiostratigraphically constrained carbonate (δ13Ccarb) and organic carbon (δ13Corg) variations in the Early-Middle Frasnian boundary interval in the Pymvashor River section (Timan-Pechora Basin, Cis-Urals, in the far north of European Russia) were considered. The studied interval of section is represented by the lower part of the Domanik Formation (Fm.) comprising alternations of limestones and shales. The presence of organic-rich black shales and the absence of bioturbation and benthic organisms indicate an oxygen-depleted depositional environment. Detection of isorenieratene derivatives in organic matter indicates that anoxia was present in the photic zone during deposition. The Pymvashor River section demonstrates clear manifestation of the two-fold Mid-Frasnian isotope Event in both δ13Ccarb and δ13Corg isotope records. Similarity between the Cis-Uralian and Chinese δ13Ccarb oscillations, including the two-step pattern of major positive excursions, suggests high correlative potential for the Late Devonian 'punctata Event' and minor intra-event excursions. Positive trends in carbon isotope composition of organic matter in conodont elements in the transitans-punctata interval is distinguished in the Pymvashor section. This carbon isotope pattern is similar to that of bulk δ13Corg in the Appalachian Basin and may prove to be a useful stratigraphic marker. 22021-01-0120212021-01-01Articlehttp://purl.org/coar/resource_type/c_6501VoRhttp://purl.org/coar/version/c_970fb48d4fbd8a85info:eu-repo/semantics/articleapplication/pdfhttps://ddd.uab.cat/record/250170https://dx.doi.org/urn:doi:10.1344/GeologicaActa2021.19.3reponame:Dipòsit Digital de Documents de la UABinstname:Universitat Autònoma de BarcelonaInglésengopen accesshttp://purl.org/coar/access_right/c_abf2Aquest document està subjecte a una llicència d'ús Creative Commons. Es permet la reproducció total o parcial, la distribució, la comunicació pública de l'obra i la creació d'obres derivades, sempre i quan aquestes es distribueixin sota la mateixa llicència que regula l'obra original i es reconegui l'autoria.https://creativecommons.org/licenses/by-sa/4.0/info:eu-repo/semantics/openAccessoai:ddd.uab.cat:2501702026-06-06T12:50:31Z
dc.title.none.fl_str_mv Early-Middle Frasnian (Late Devonian) carbon isotope Event in the Timan-Pechora Basin (Chernyshev Swell, Pymvashor River section, North Cis-Urals, Russia)
title Early-Middle Frasnian (Late Devonian) carbon isotope Event in the Timan-Pechora Basin (Chernyshev Swell, Pymvashor River section, North Cis-Urals, Russia)
spellingShingle Early-Middle Frasnian (Late Devonian) carbon isotope Event in the Timan-Pechora Basin (Chernyshev Swell, Pymvashor River section, North Cis-Urals, Russia)
Kotik, Ivan S.
Late Devonian
Punctata Event
Carbon isotopes
Biomarkers
Conodonts
title_short Early-Middle Frasnian (Late Devonian) carbon isotope Event in the Timan-Pechora Basin (Chernyshev Swell, Pymvashor River section, North Cis-Urals, Russia)
title_full Early-Middle Frasnian (Late Devonian) carbon isotope Event in the Timan-Pechora Basin (Chernyshev Swell, Pymvashor River section, North Cis-Urals, Russia)
title_fullStr Early-Middle Frasnian (Late Devonian) carbon isotope Event in the Timan-Pechora Basin (Chernyshev Swell, Pymvashor River section, North Cis-Urals, Russia)
title_full_unstemmed Early-Middle Frasnian (Late Devonian) carbon isotope Event in the Timan-Pechora Basin (Chernyshev Swell, Pymvashor River section, North Cis-Urals, Russia)
title_sort Early-Middle Frasnian (Late Devonian) carbon isotope Event in the Timan-Pechora Basin (Chernyshev Swell, Pymvashor River section, North Cis-Urals, Russia)
dc.creator.none.fl_str_mv Kotik, Ivan S.
Zhuravlev, Andrey V.|||0000-0003-4043-6303
Maydl, Tatiana V.
Bushnev, Dmitriy A.
Smoleva, Irina V.
author Kotik, Ivan S.
author_facet Kotik, Ivan S.
Zhuravlev, Andrey V.|||0000-0003-4043-6303
Maydl, Tatiana V.
Bushnev, Dmitriy A.
Smoleva, Irina V.
author_role author
author2 Zhuravlev, Andrey V.|||0000-0003-4043-6303
Maydl, Tatiana V.
Bushnev, Dmitriy A.
Smoleva, Irina V.
author2_role author
author
author
author
dc.subject.none.fl_str_mv Late Devonian
Punctata Event
Carbon isotopes
Biomarkers
Conodonts
topic Late Devonian
Punctata Event
Carbon isotopes
Biomarkers
Conodonts
description Biostratigraphically constrained carbonate (δ13Ccarb) and organic carbon (δ13Corg) variations in the Early-Middle Frasnian boundary interval in the Pymvashor River section (Timan-Pechora Basin, Cis-Urals, in the far north of European Russia) were considered. The studied interval of section is represented by the lower part of the Domanik Formation (Fm.) comprising alternations of limestones and shales. The presence of organic-rich black shales and the absence of bioturbation and benthic organisms indicate an oxygen-depleted depositional environment. Detection of isorenieratene derivatives in organic matter indicates that anoxia was present in the photic zone during deposition. The Pymvashor River section demonstrates clear manifestation of the two-fold Mid-Frasnian isotope Event in both δ13Ccarb and δ13Corg isotope records. Similarity between the Cis-Uralian and Chinese δ13Ccarb oscillations, including the two-step pattern of major positive excursions, suggests high correlative potential for the Late Devonian 'punctata Event' and minor intra-event excursions. Positive trends in carbon isotope composition of organic matter in conodont elements in the transitans-punctata interval is distinguished in the Pymvashor section. This carbon isotope pattern is similar to that of bulk δ13Corg in the Appalachian Basin and may prove to be a useful stratigraphic marker.
publishDate 2021
dc.date.none.fl_str_mv 2
2021-01-01
2021
2021-01-01
dc.type.none.fl_str_mv Article
http://purl.org/coar/resource_type/c_6501
VoR
http://purl.org/coar/version/c_970fb48d4fbd8a85
dc.type.openaire.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.none.fl_str_mv https://ddd.uab.cat/record/250170
https://dx.doi.org/urn:doi:10.1344/GeologicaActa2021.19.3
url https://ddd.uab.cat/record/250170
https://dx.doi.org/urn:doi:10.1344/GeologicaActa2021.19.3
dc.language.none.fl_str_mv Inglés
eng
language_invalid_str_mv Inglés
language eng
dc.rights.none.fl_str_mv open access
http://purl.org/coar/access_right/c_abf2
https://creativecommons.org/licenses/by-sa/4.0/
dc.rights.openaire.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv open access
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eu_rights_str_mv openAccess
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dc.source.none.fl_str_mv reponame:Dipòsit Digital de Documents de la UAB
instname:Universitat Autònoma de Barcelona
instname_str Universitat Autònoma de Barcelona
reponame_str Dipòsit Digital de Documents de la UAB
collection Dipòsit Digital de Documents de la UAB
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