Oxygen isotopic evidence for late Triassic monsoonal upwelling in the northwestern Tethys
The oxygen isotopic composition of conodonts from the Pizzo Mondello section in the Sicani Basin (Sicily, Italy), on the northwestern Tethys margin, has been used to reconstruct regional paleoseawater conditions. The δ18Ophos values (21‰-21.9‰) measu
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