Biomarker and compound-specific isotope records across the Toarcian CIE at the Dormettingen section in SW Germany

The Toarcian oceanic anoxic event (T-OAE) is associated with a prominent negative carbon isotope excursion (CIE; ~ 183 million years (Myr)). About 10-m-thick organic matter-rich sediments accumulated during the T-OAE in the Southwest German Basin (SWGB). Rock–Eval, maceral and biomarker analysis wer...

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Detalles Bibliográficos
Autores principales: Ajuaba, Stephen, Sachsenhofer, Reinhard F., Bechtel, Achim, Galasso, Francesca, Gross, Doris, Misch, David, Schneebeli-Hermann, Elke
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Berlin Heidelberg 2022
Materias:
Original Paper
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9188539/
https://www.ncbi.nlm.nih.gov/pubmed/35707060
http://dx.doi.org/10.1007/s00531-022-02196-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9188539/
https://www.ncbi.nlm.nih.gov/pubmed/35707060
http://dx.doi.org/10.1007/s00531-022-02196-z

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