Carbon isotope values in conodont elements from the latest Devonian–Early Carboniferous carbonate platform facies (Timan-Pechora Basin)

The δ13Corg values and their variations in conodont elements of the latest Famennian–Tournaisian species Polygnathus parapetus Druce are considered. The conodonts studied come from the latest Famennian–Tournaisian interval of the Kamenka River section (Timan-Pechora Basin). The carbon isotope compos...

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Bibliographic Details
Published in:Estonian Journal of Earth Sciences
Main Authors: Andrey V. Zhuravlev, Irina V. Smoleva
Format: Article in Journal/Newspaper
Language:English
Published: Estonian Academy Publishers 2018
Subjects:
Famennian
Tournaisian
conodonts
δ13Corg
Timan-Pechora Basin
Geology
QE1-996.5
Pechora
Online Access:https://doi.org/10.3176/earth.2018.17
https://doaj.org/article/dbac363b10a24c6bbf24abad0157722f
Description
Summary:The δ13Corg values and their variations in conodont elements of the latest Famennian–Tournaisian species Polygnathus parapetus Druce are considered. The conodonts studied come from the latest Famennian–Tournaisian interval of the Kamenka River section (Timan-Pechora Basin). The carbon isotope composition of conodont elements had an average value of –25.2‰, suggesting a low trophic level of this species. During the latest Famennian (praesulcata conodont Zone) δ13Corg shifted to more negative values (up to –30.4‰), which may be attributed to changes in the global carbon cycle and local influx of organic matter of terrestrial origin during the terminal Famennian regression.

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