“…Hence, the greatest likelihood to discover soft parts of ammonoids or nautilids is given in such Konservat-Lagerstätten (= conservation deposits; Seilacher, 1970), where soft parts became quickly phosphatised or pyritised and aragonite shells were dissolved. There are records of cephalopod soft parts and there is some potential for such preservation in, e.g., the Ordovician Soom Shale in South Africa (Gabbott, 1999), the Devonian Hunsrück Slate in Germany (De Baets et al, 2013;Stilkerich et al, 2017), the Devonian Hangenberg Black Shale in Morocco (Klug & Vallon, 2019;Klug et al, 2016a), the Carboniferous of Bear Gulch (Doguzhaeva et al, 2007;Landman et al, 2010;Mapes et al, 2019), the Carboniferous of the Itararé-Formation in Uruguay (Closs, 1967;Lehmann et al, 2015), the Triassic Thaynes Group in the USA (Doguzhaeva et al, 2018), the Jurassic of Christian Malford and Dorset (Hart et al, 2020;Wilby et al, 2004Wilby et al, , 2008, the Jurassic of Eichstätt, Nusplingen, Painten and Solnhofen (e.g., Dietl & Schweigert, 2011;Fuchs, 2006a;Klug et al, , 2016bKlug et al, , 2021aKlug et al, , 2021bSchweigert, 2009Schweigert, , 2021, the Cretaceous of Germany Klug et al, 2012), and, last but not least, the Cretaceous of Lebanon (Engeser & Reitner, 1986;Fuchs & Larson, 2011a, 2011bFuchs, 2006aFuchs, , 2006bJattiot et al, 2015;Klug et al, 2020Klug et al, , 2021aLukeneder & Harzhauser, 2004;Roger, 1946;Wippich & Lehmann, 2004;Woodward, 1883…”