Fig. 10From: The effects of meteoric diagenesis on the geochemical composition and microstructure of Pliocene fossil Terebratalia coreanica and Laqueus rubellus brachiopod shells from northeastern JapanCross-plots of isotopic composition versus AFR or AF-PCR (a, b, e, and f) and of isotopic composition versus MCLI (c, d, g, and h) . The gray bar on the y-axis indicates a range of δ13C or δ18O values of the modern brachiopod shell (OTTCo or SGLR)Back to article page