Figure F5. A. Linear correlation coefficients for slopes of natural remanent magnetization (NRM) versus anhysteretic remanent magnetization (ARM) during alternating-field demagnetization (red) and NRM demagnetization versus ARM acquisition (ARMAQ) (blue) that constitute the RPI proxies. B. Component inclination of NRM. C. Benthic δ18O record (red) correlated to the Lisiecki and Raymo (2005) stack (blue) by Hodell et al. (2008). Glacial MIS are labeled. D. Slopes of NRM/ARM (red) and NRM/ARMAQ (blue) for the 20–60 mT demagnetization and acquisition interval that constitute RPI proxies. Figure from Channell et al. (2008).
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