“…In any case, samples must be selected with extreme care in order to assure contemporaneity (see , for the major factors for consideration when using this approach). There are a number of MRE studies that have employed the paired sample methodology to determine ΔR corrections (e.g., Albero et al, 1986;Dettman et al, 2015;Facorellis, 1998;Hadden & Cherkinsky, 2017;Head et al, 2016;Latorre et al, 2017;Nakamura, 2007;Owen, 2002;Southon et al, 1995;Southon & Fedje, 2003). The atmospheric counterpart of marine samples in these studies is generally charcoal, but recent work has been done employing land snail shells (see Macario, Alves, Chanca, et al, 2016)-it has been shown that some species are reliable proxies for the atmospheric carbon reservoir (see Macario, Alves, Carvalho et al, 2016)-and terrestrial mammal bones (see, e.g., Ascough, Cook, Church, et al, 2007;Ascough, Cook, Dugmore, & Scott, 2007) for that purpose.…”