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Did changes in terrigenous components of deep-sea cherts across the end-Triassic extinction relate to Central Atlantic magmatic province volcanism?
Further provenance analyses will be needed to clarify CAMP volcanism and associated environmental changes recorded in the pelagic deep-sea succession! It is noteworthy that the migration of biogenic Si from proto-shale intervals to adjacent proto-chert intervals during the diagenetic transformation from opal-A to opal-CT (Tada, 1991) suggests that SiO2/Al2O3 ratios in shales tend to be similar to those of eolian dust, while those in cherts reflect the biogenic Si content within a chert and adjacent shale beds per terrigenous material content in the proto-chert interval (e.g., Ikeda et al., 2017).Ikedacho Sexual Massage
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