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RISAge assignment of section 4 of Teichert et al. (1973) at Ali Bashi Mountains (Julfa, NW Iran)
) in Kuh-e-Ali Bashi near Julfa, northwestern Iran. This formation is comprised between the Dzhulfian (Wuchiapingian) Julfa Formation (below) and the uppermost Changhsingian (Dorashamian) to lowermost Triassic Elikah Formation (above) and contains a...
Pre–mass extinction decline of latest Permian ammonoids
The devastating end-Permian mass extinction is widely considered to have been caused by large-scale and rapid greenhouse gas release by Siberian magmatism. Although the proximate extinction mechanisms are disputed, there ...
Stable carbon and nitrogen isotopes of Permian-Triassic Boundary sections in the regions of Julfa (NW Iran) and Abadeh (Central Iran)
The Permian-Triassic (P-Tr) boundary sections in the regions of Julfa (NW Iran) and Abadeh (Central Iran) have high potential for the study of the most dramatic extinction event in Earth’s history. As part of a multidisciplinary project, we have...
Early Triassic microbialites and carbonate factory changes across the Permian-Triassic boundary near Julfa (NW Iran) and Abadeh (Central Iran)
Permian-Triassic boundary sections in the regions of Julfa (NW Iran) and Abadeh (Central Iran) display three characteristic rock units: (1) the Paratirolites Limestone (4-5 m thick) with the mass extinction horizon (P-Tr extinction event) at the top...
Lithostratigraphy and carbonate microfacies across the Permian-Triassic boundary near Julfa (NW Iran) and Abadeh (Central Iran)
Permian-Triassic boundary sections in the regions of Julfa (NW Iran) and Abadeh (Central Iran) display three characteristic rock units: (1) the Paratirolites Limestone (4-5 m thick) with the mass extinction horizon (P-Tr extinction event) at the top...