“…Remagnetizations can occur in any environment in which secondary magnetic minerals form, including oxic (e.g., van der Voo and Torsvik, 2012), sulphidic (e.g., Roberts and Weaver, 2005), and methanic environments (e.g., Weaver et al, 2002;Larrasoaña et al, 2007), or at moderate (e.g., Aubourg and Pozzi, 2010;Kars et al, 2012Kars et al, , 2014 carbonates, together with stable SD particles, produces characteristic wasp-waisted hysteresis behaviour (Jackson 1990;Roberts et al, 1995;Tauxe et al, 1996) that contrasts with that of nonremagnetized carbonates (e.g., Roberts et al, 2013a). Such hysteresis signatures have been argued to provide a fingerprint for carbonate remagnetization (Jackson, 1990;McCabe and Channell, 1994;Channell and McCabe, 1994;Jackson and Swanson-Hysell, 2012;van der Voo and Torsvik, 2012).…”