1. Sedimentology and carbon isotope stratigraphy of the Rhaetian Hochalm section (Late Triassic, Austria).
- Author
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Rizzi, Małgorzata, Thibault, Nicolas, Ullmann, Clemens V., Ruhl, Micha, Olsen, Troels K., Moreau, Julien, Clémence, Marie-Emilie, Mette, Wolfgang, and Korte, Christoph
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CARBON isotopes , *CHEMOSTRATIGRAPHY , *SEDIMENTOLOGY , *STRATIGRAPHIC geology , *MASS extinctions , *ENVIRONMENTAL sciences - Abstract
The Rhaetian (~201–209 Ma, the latest stage of the Triassic) is an important time-interval for the study of environmental changes preceding the End-Triassic Mass extinction. A detailed sedimentological and chemostratigraphic study was conducted in the lower Kössen Formation at Hochalm (Austria), the type-section of the Hochalm Member (Mb). This section exposes mid-Rhaetian sediments deposited in an intraplatform shallow marine basin on the north-western margin of the Tethys. The study highlights eight apparent shallowing-upward sequences from the middle of Unit 2 to Unit 4 of the Hochalm Mb stacked within the long-term transgression that characterizes the Kössen Formation. Both the bulk carbonate and the bulk organic matter δ13C records indicate the presence of a distinct increase in carbon isotope values in the lower part of the lower Hochalm Mb. This excursion might represent a new chemostratigraphic marker that could be used for refining the Rhaetian stratigraphy and represents another important Late Triassic carbon-cycle perturbation prior to the major disturbance associated with the End Triassic biotic crisis. • Detailed paleoenvironmental model of the Hochalm Mb. • Shallowing-deepening sequences related to sea-level changes. • Carbon isotope stratigraphy in mid-Rhaetian Hochalm Mb. • Distinct increase in carbon isotopes in the lower Hochalm Mb. [ABSTRACT FROM AUTHOR]
- Published
- 2020
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