“…The global Paleocene fossil record is even poorer than that of the Maastrichtian, both in terms of number of known sites, but also in terms of recorded biodiversity and, in most cases, quality of preservation ( Patterson, 1964 ; Thomas et al, 1999 ; Cavin, 2002 ; Friedman & Johnson, 2005 ; Parris, Smith-Grandstaff & Gallagher, 2007 ; Schwarzhans & Milàn, 2017 ; Capobianco, Foreman & Friedman, 2019 ). The Danian neritic sites near Palenque, Mexico, constitute notable exceptions from this rule ( Alvarado-Ortega et al, 2015 ; Cantalice & Alvarado-Ortega, 2016 ; Cantalice, Alvarado-Ortega & Bellwood, 2020 ), yielding well-preserved and diverse shallow water actinopterygian assemblages comprising typical Paleogene (e.g., marine osteoglossomorphs) as well as derived faunal elements (including aulostomoids, pomacentrids and other percomorphs), which foreshadow the more modern-like, acanthomorph-dominated assemblages from the early Eocene of Turkmenistan and the Kabardino-Balkaria ( Bannikov & Parin, 1997 ; Bannikov & Carnevale, 2012 ; Bannikov et al, 2017 ), Bolca, the London Clay and other localities ( Arambourg, 1967 ; Daniltshenko, 1962 ; Eastman & Grande, 1991 ; Bannikov, 1993 ; Bonde, 1997 ; Afsari et al, 2014 ; Davesne, 2017 ; Beckett et al, 2018 ; Friedman & Carnevale, 2018 ).…”