12 citations as recorded by crossref.

1. The Permian–Triassic boundary section at Baghuk Mountain, Central Iran: carbonate microfacies and depositional environment F. Heuer et al. 10.1007/s12549-021-00511-1
2. Abrupt warming in the latest Permian detected using high-resolution in situ oxygen isotopes of conodont apatite from Abadeh, central Iran J. Chen et al. 10.1016/j.palaeo.2020.109973
3. Middle Triassic Nautilida from the Besano Formation of Monte San Giorgio, Switzerland V. Pieroni 10.1186/s13358-022-00263-1
4. Baghuk Mountain (Central Iran): high-resolution stratigraphy of a continuous Central Tethyan Permian–Triassic boundary section D. Korn et al. 10.5194/fr-24-171-2021
5. Sponge Takeover from End-Permian Mass Extinction to Early Induan Time: Records in Central Iran Microbial Buildups A. Baud et al. 10.3389/feart.2021.586210
6. Isotopic time-series (δ13C and δ18O) obtained from the columnar layer of Permian brachiopod shells are a reliable archive of seasonal variations C. Garbelli et al. 10.1016/j.palaeo.2022.111264
7. Depositional environment and sequence stratigraphy architecture of continuous Upper Permian and Lowermost Triassic deep marine deposits in NW and SW Iran S. Arefifard & A. Baud 10.1016/j.palaeo.2022.111187
8. Ostracods from the end‐Permian mass extinction in the Aras Valley section (north‐west Iran) J. Gliwa et al. 10.1002/spp2.1330
9. Decoupling of morphological disparity and taxonomic diversity during the end-Permian mass extinction J. Wan et al. 10.1017/pab.2020.57
10. Calibrating the late Smithian (Early Triassic) crisis: New insights from the Nanpanjiang Basin, South China X. Dai et al. 10.1016/j.gloplacha.2021.103492
11. Exceptions to the temperature–size rule: no Lilliput Effect in end‐Permian ostracods (Crustacea) from Aras Valley (northwest Iran) P. Nätscher et al. 10.1111/pala.12667
12. Gradual warming prior to the end‐Permian mass extinction J. Gliwa et al. 10.1111/pala.12621