“…The southern Pyrenean basins were located at tropical latitudes during the Paleogene (e.g., Hay et al, 1999; Silva-Casal et al, 2019) and, in the Eocene, formed part of an elongated gulf that connected in the west to the Bay of Biscay and was limited in the north to the axial zone of the Pyrenees (see Plaziat, 1981; Garcés et al, 2020). These basins rank among the most complete records of Eocene marine sedimentary successions in Europe, with decapod crustacean taxa described from several outcrops (e.g., Via, 1969, 1973; Artal and Castillo, 2005b; Artal et al, 2006, 2013; Ossó et al, 2014; Dominguez and Ossó, 2016; López-Horgue and Bodego, 2017; Artal and Van Bakel, 2018a, b, 2020; Ferratges et al, 2019, 2020). These successions document a wide range of depositional settings, from proximal alluvial to shallow marine in the east to slope and deep-marine and abyssal plains in the west (e.g., Garcés et al, 2020).…”