In arctic Siberia, time-series δ 13 C values show a decreasing trend from near +6‰ in the Maastakh and basal Khatyspyt formations, and then an oscillation between −5 and +4‰ through the overlying reaches of the interval 25 , 26 , 35 before stabilizing near 0‰ in dolostones of the lower Turkut Formation.
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