Vodrážková S, Vodrážka R, Munnecke A, Franců J, Al‐Bassam K, Halodová P, Tonarová P (2018)
Publication Language: English
Publication Type: Journal article, Online publication
Publication year: 2018
Book Volume: 52
Pages Range: 149-164
Journal Issue: 2
URI: https://onlinelibrary.wiley.com/doi/full/10.1111/let.12280
DOI: 10.1111/let.12280
Open Access Link: https://onlinelibrary.wiley.com/doi/full/10.1111/let.12280
The occurrence of wrinkle structures in Middle Devonian deep‐water siliciclastic sequences of the Prague Basin (Roblín Member, Srbsko Formation, Givetian) is reported and interpreted to be microbially induced. Current and/or gravitational forces are considered the simplest explanation of the origin of these structures. Taking into account the tectonic activity linked with ongoing Variscan orogeny, the wrinkle structures could also be interpreted as soft sediment deformation structures originating due to exposure of mat‐bearing sediment to seismic shocks. The distribution of n‐alkanes and isoprenoids suggests two types of prevailing biological sources, namely phytoplankton, representing organic material from the water column, and benthic bacteria. Judging from the sedimentary facies and lack of petrographic characteristics suggestive of light competition, the microbial mats are interpreted to be formed by non‐autotrophic bacteria.
APA:
Vodrážková, S., Vodrážka, R., Munnecke, A., Franců, J., Al‐Bassam, K., Halodová, P., & Tonarová, P. (2018). Microbially induced wrinkle structures in Middle Devonian siliciclastics from the Prague Basin, Czech Republic. Lethaia, 52(2), 149-164. https://doi.org/10.1111/let.12280
MLA:
Vodrážková, Stanislava, et al. "Microbially induced wrinkle structures in Middle Devonian siliciclastics from the Prague Basin, Czech Republic." Lethaia 52.2 (2018): 149-164.
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