Biostratigraphy and sedimentology of Upper Permian and Lower Triassic strata at Masore, Western Slovenia

@article{KolarJurkovek2018BiostratigraphyAS,
  title={Biostratigraphy and sedimentology of Upper Permian and Lower Triassic strata at Masore, Western Slovenia},
  author={T. Kolar-Jurkov{\vs}ek and B. Jurkov{\vs}ek and G. P. Nestell and D. Aljinovi{\'c}},
  journal={Palaeogeography, Palaeoclimatology, Palaeoecology},
  year={2018},
  volume={490},
  pages={38-54}
}
Abstract Upper Permian and lowermost Triassic strata of the Masore section in western Slovenia have been restudied by means of bio- and lithostratigraphy. This section is mainly characterized by a carbonate succession of the Bellerophon Formation deposited in a shallow marine ramp environment that was located in the western part of the Paleotethys. The Permian-Triassic boundary (PTB) transition is marked by laminated microbialites – stromatolites interpreted to reflect a deeper ramp environment… Expand
Permian-Triassic biofacies of the Teočak section, Bosnia and Herzegovina
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Abstract Permian–Triassic boundary (PTB) foraminifers are studied from the upper part of the Dalan Formation and the base of the Kangan Formation in four wells (A, B, E, F) on and near the Qatar Arc,Expand
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Stress-Related Evolution in Triassic Conodonts and the Middle Norian Juvenile Mortality
Conodonts are of great importance in Paleozoic and Early Triassic stratigraphy, which is proven by the large number of studies on their biostratigraphic relevance. Less emphasis was placed on theExpand
The Permian–Triassic boundary Lung Cam expanded section, Vietnam, as a high-resolution proxy for the GSSP at Meishan, China
Abstract The Lung Cam expanded stratigraphic succession in Vietnam is correlated herein to the Meishan D section in China, the GSSP for the Permian–Triassic boundary. The first appearance datum ofExpand
Suppressed competitive exclusion enabled the proliferation of Permian/Triassic boundary microbialites
  • W. Foster, K. Heindel, +9 authors J. Peckmann
  • Medicine, Geology
  • The depositional record : a journal of biological, physical and geochemical sedimentary processes
  • 2020
TLDR
It is inferred that the end‐Permian mass extinction event decreased the diversity and abundance of metazoans to the point of significantly reducing competition, allowing photosynthesis‐based microbial mats to flourish in shallow water settings and resulting in the formation of widespread microbialites. Expand

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