“…A variety of reagents have been employed to remove bone mineral and increase access to remaining organic fractions, such as hydrochloric acid (HCl) (Buckley, 2013; Buckley, 2015; Buckley et al, 2009; Buckley et al, 2010; Buckley, Larkin & Collins, 2011; Buckley & Wadsworth, 2014; Cleland, Schroeter & Schweitzer, 2015; Cleland, Voegele & Schweitzer, 2012; Ostrom et al, 2000; Wadsworth & Buckley, 2014; Welker et al, 2015), sodium ethylenediaminetetraacetic acid (EDTA) (Buckley et al, 2008; Cappellini et al, 2012; Cleland, Voegele & Schweitzer, 2012; Humpula et al, 2007; Nielsen-Marsh et al, 2002; Nielsen-Marsh et al, 2005; Ostrom et al, 2006; Schweitzer et al, 2007; Schweitzer et al, 2009), and ammonium EDTA (Ostrom et al, 2000). Reagents used to solubilize bone proteins for subsequent mass spectrometry (MS) and immunological applications are equally diverse, and have included (among others) ammonium bicarbonate (ABC) (Buckley et al, 2009; Buckley et al, 2010; Buckley, Larkin & Collins, 2011; Cappellini et al, 2012; Cleland, Schroeter & Schweitzer, 2015; Cleland, Voegele & Schweitzer, 2012), and guanidine hydrochloride (GuHCl) (Buckley, 2015; Buckley & Wadsworth, 2014; Cleland, Voegele & Schweitzer, 2012; Schweitzer et al, 2007; Schweitzer et al, 2009; Wadsworth & Buckley, 2014). However, these methods have not been consistently employed across fossil studies, which may hamper direct comparisons of preserved protein content between fossil specimens, as these reagents have been shown to vary in efficacy when used to extract bone proteins for enzyme-linked immunosorbent assay (ELISA) and sodium dodecyl sulfate polyacrylamide gel electrophoresis (SDS-PAGE) (Cleland, Voegele & Schweitzer, 2012).…”