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, 2018. Early evolution of colonial animals (Ediacaran Evolutionary Radiation–Cambrian Evolutionary Radiation–Great Ordovician Biodiversification Interval). Earth-Science Reviews 178, 105-135. doi:10.1016/j.earscirev.2018.01.013
, 2019. Revised Cambrian stratigraphy in the Franconian Forest (Frankenwald), Germany, reveals typical West Gondwanan succession in the Saxothuringian belt. Newsletters on Stratigraphy 52, 377-433. doi:10.1127/nos/2019/0495
, 2019. Comment on: \ Alvaro, J. J., Esteve, J. \& Zamora, S. 2019. Morphological assessment of the earliest paradoxidid trilobites (Cambrian Series 3) from Morocco and Spain. Geological Magazine 156, 1691-1707. doi:10.1017/S0016756818000961
, 2019. RE: Overused “greenhouse climate” paradigm: consequence for ancient climate synthesis. Science Advances
, 2022. Trans-Avalonian green–black boundary (early Middle Cambrian): transform fault-driven epeirogeny and onset of 26 m.y. of shallow marine anoxia in Avalonia (Rhode Island–Belgium) and Baltica. Canadian Journal of Earth Sciences doi:10.1139/cjes-2022-0065
, 2022. Discussion of ‘Reply to “Uppermost Cambrian carbon chemostratigraphy: the HERB and undocumented TOCE events are not synonymous”’Abstract. Geological Magazine 159, 173-176. doi:10.1017/S001675682100090X
, 2023. Cambrian microfossils from the High Atlas, Morocco: Taxonomic, biostratigraphic, palaeobiogeographic, and depositional significance of the Brèche \ a Micmacca limestone beds. Journal of African Earth Sciences 197, 104751. doi:10.1016/j.jafrearsci.2022.104751
, 2023. U-Pb zircon dates from North American and British Avalonia bracket the Lower–Middle Cambrian boundary interval, with evaluation of the Miaolingian Series as a global unit. Geological Magazine , 1-27. doi:10.1017/S0016756823000729
