12 citations as recorded by crossref.

1. The Middle Eocene Seeb Formation of Oman: An Investigation of Acyclicity, Stratigraphic Completeness, and Accumulation Rates in Shallow Marine Carbonate Settings S. Beavington-Penney et al. https://doi.org/10.2110/jsr.2006.109
2. Microfacies and biofabric of nummulite accumulations (Bank) from the Eocene deposits of Western Alborz (NW Iran) M. Hadi et al. https://doi.org/10.1016/j.jafrearsci.2016.09.012
3. Stratigraphy of the Alveolina elliptica group from the Middle Eocene of Iran: Calibration with calcareous nannofossils biozones and description of Alveolina ozcani n. sp. M. Hadi et al. https://doi.org/10.1016/j.jop.2023.11.002
4. Fossil indicators of nutrient levels. 2: Evolution and extinction in relation to oligotrophy M. Brasier https://doi.org/10.1144/GSL.SP.1995.083.01.08
5. Microfacies analysis of Eocene Ziarat Formation (eastern Alborz zone, NE Iran) and paleoenvironmental implications M. Hadi et al. https://doi.org/10.1080/27669645.2021.1956175
6. A quantitative and statistical discrimination of morphotaxa within the Ediacaran genus Palaeopascichnus J. Hawco et al. https://doi.org/10.1002/spp2.1290
7. Reclassification of Glomalveolina subtilis as a distinct species within Glomalveolina genus: new record from the Iranian platform in the Central Neo-Tethys M. Hadi et al. https://doi.org/10.1017/jpa.2026.10220
8. Alveolinids from the Lower Indus Basin, Pakistan (Eastern Neo‐Tethys): Systematic and biostratigraphic implications M. Rahman et al. https://doi.org/10.1002/gj.4119
9. Why do lower plants and animals biomineralize? M. Brasier https://doi.org/10.1017/S0094837300013750
10. The geographic, environmental and phylogenetic evolution of the Alveolinoidea from the Cretaceous to the present day M. BouDagher-Fadel & G. Price https://doi.org/10.14324/111.444/ucloe.000015
11. Functional anatomy of fusulinids (foraminifera): Significance of the polar torsion illustrated inTriticites andSchwagerina (Schwagerinidae) U. Leppig https://doi.org/10.1007/BF02989476
12. New species of larger benthic foraminifera from the Maastrichtian deposits of the southern margin of the Neotethys (Zagros Foreland Basin) H. Ghanbarloo et al. https://doi.org/10.1016/j.jop.2024.10.003