Published June 23, 2021
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Figure 18 in Baghuk Mountain (Central Iran): high-resolution stratigraphy of a continuous Central Tethyan Permian-Triassic boundary section
Authors/Creators
- 1. Lucyna Leda & Franziska Heuer & Hemen Moradi Salimi & Elham Farshid & Jana Gliwa & David Ware & Vachik Hairapetian & Museum für Naturkunde Berlin, Leibniz Institute for Evolution and Biodiversity Science,
- 2. Lucyna Leda & Franziska Heuer & Hemen Moradi Salimi & Elham Farshid & Jana Gliwa & David Ware & Vachik Hairapetian & Museum für Naturkunde Berlin, Leibniz Institute for Evolution and Biodiversity Science, & Elham Farshid & Geology Department, Faculty of Science, University of Isfahan, Isfahan, Iran
- 3. Amir Akbari & Department of Geology, North Tehran Branch, Islamic Azad University, Tehran, Iran
- 4. Department of Geology, Isfahan (Khorasgan) Branch, Islamic Azad University, Isfahan, Iran
- 5. Abbas Ghaderi & Marine Palynology and Paleoceanography, Utrecht University, Princetonlaan, Utrecht, the Netherlands
- 6. Ulrich Struck & Department of Geology, Faculty of Science, Ferdowsi University of Mashhad, P.O. Box 9177948974, Mashhad, Iran
- 7. Lucyna Leda & Franziska Heuer & Hemen Moradi Salimi & Elham Farshid & Jana Gliwa & David Ware & Vachik Hairapetian & Museum für Naturkunde Berlin, Leibniz Institute for Evolution and Biodiversity Science, & Vachik Hairapetian & Museum für Naturkunde, Otto-von-Guericke-Strasse 68-73, 39104 Magdeburg, Germany
Description
Figure 18. Field photographs of Early Triassic bedding surfaces with structures of possible microbial origin. (a) Flower-shaped structure in the pale-brown micritic matrix containing filaments, bivalve shell fragments, ammonoids and high-spired gastropods. (b) Kidney-shaped "twin" morphology characterized by an irregular, partly concentric structure, where micrite and sparite alternate. (c) Structures of different size, some of which grow on the margin of a previous generation. (d) Dark-grey, ovoidal, lenticular sparry calcite structure, filled by an argillaceous micrite, in pale-brown micritic matrix containing abundant filaments (probably sponge spicule remains).
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- Journal article: 10.5194/fr-24-171-2021 (DOI)
- Journal article: urn:lsid:plazi.org:pub:FFD6FFFEC1657049E56E4F63E56AFF9B (LSID)
- Journal article: https://zenodo.org/record/12763779 (URL)