“…11A to E), Ireland (Mienis et al ., 2009a,b; van der Land et al ., 2014; Fig. 11F), Gulf of Cadiz (Wienberg et al ., 2009), Mediterranean (Freiwald et al ., 2009), Morocco (Foubert et al ., 2008; Hebbeln et al ., 2019), Mauritania (Wienberg et al ., 2018), Namibia (Hanz et al ., 2019), north‐west Atlantic (Mienis et al ., 2014), Florida (Grasmueck et al ., 2006; Correa et al ., 2012; Mulder et al ., 2012; Lüdmann et al ., 2016), Gulf of Mexico (Mienis et al ., 2012; Hebbeln et al ., 2014), Brazil (Viana et al ., 1998; Pires et al ., 2014), Uruguay (Carranza et al ., 2012) and Argentina (Muñoz et al ., 2012); (ii) the Indian Ocean (Maldives; Reolid et al ., 2017) and Australia (Coral Sea; Beaman et al ., 2016); and (iii) the Pacific (Hawaii; Long & Baco, 2014; British Columbia; Neves et al ., 2014; Alaska; Etnoyer & Morgan, 2005; Stone, 2006). The position and growth history of the coral mounds may vary through time depending on their response to climate changes and associated variations in ocean circulation and water mass distribution.…”