The assessment of REE patterns and 143 Nd/144 Nd ratios in fish remains. Earth and Planetary Science Letters, 84(2/3), 181–196
DOI: 10.1016/0012-821X(87)90084-7
A new selachian fauna from the Late Maastrichtian of Texas (Upper Cretaceous/Navarro Group; Kemp Formation). Münchner Geowissenschaftliche Abhandlungen Reihe A, Geologie und Paläontologie, 34, 131–189, 10 fig., 15 pl.
Late Paleocene to Early Eocene marine vertebrates from the Uppermost Aruma Formation (northern Saudi Arabia): Implications for the K-T transition. Comptes Rendus de l'Académie des Sciences, Series IIA – Earth and Planetary Science, 329(12), 905–912
DOI: 10.1016/S1251-8050(00)88504-3
Late Cretaceous elasmobranchs from the Mahajanga Basin of Madagascar. Cretaceous Research, 22(4), 491–496
DOI: 10.1006/cres.2001.0269
Marine vertebrate faunas from the Maastrichtian phosphates of Benguérir (Ganntour Basin, Morocco): Biostratigraphy, palaeobiogeography and palaeoecology. Palaeogeography, Palaeoclimatology, Palaeoecology, 409, 217–238
DOI: 10.1016/j.palaeo.2014.04.020
Frequency, taxonomy and morphology of diffrent shark taxa of Lower Paleogene and Upper Cretaceous from Morocco, North Arfica. Pluralidade, 3(3), 54–68
Multispecies shark feeding in the trans-saharan seaway: evidence from late cretaceous dyrosaurid (Crocodyliformes) fossils from northeastern Mali. Palaios, 30(7), 589–596
DOI: 10.2110/palo.2014.109
Climate cooling and clade competition likely drove the decline of lamniform sharks. Proceedings of the National Academy of Sciences of the United States of America, 116(41), 20584–20590
DOI: 10.1073/pnas.1902693116
Feeding ecology has shaped the evolution of modern sharks. Current Biology, 31(23), 5138–5148
DOI: 10.1016/j.cub.2021.09.028
Global impact and selectivity of the Cretaceous-Paleogene mass extinction among sharks, skates, and rays. Science, 379, 802–806
DOI: 10.1126/science.abn2080
The Upper Cretaceous elasmobranch fauna from Senegal. Cretaceous Research, 146, Article 105480
DOI: 10.1016/j.cretres.2023.105480