“…Large (>1,000 kg) herbivorous dinosaurs (=megaherbivores) dominated terrestrial North American communities for the last ∼98 Myr of the Mesozoic Era both in diversity and abundance ( O’Gorman & Hone, 2012 ; Codron et al, 2012 ; Codron, Carbone & Clauss, 2013 ; Brown et al, 2013a ). Between the Late Jurassic and Late Cretaceous, a major change in megaherbivore faunal composition is observed: previously dominant sauropods are replaced by ‘duck-billed’ hadrosaurids and ‘horned’ ceratopsids, stegosaurs become extinct and armoured ankylosaurs experience an increase in diversity ( Zanno & Makovicky, 2011 ; Barrett, 2014 ; Nesbitt et al, 2019 ; Holtz, 2021 ). The decline and decrease in sauropod diversity (herein the ‘sauropod decline’) occurred between the Cenomanian and Campanian/Maastrichtian—much later than the complete loss of stegosaurs that appears to have occurred between the Tithonian and Albian ( Williamson & Weil, 2008 ; D’Emic, Wilson & Thompson, 2010 ; Mannion & Upchurch, 2011 ; D’Emic & Foreman, 2012 ).…”