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Fig. 3
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Phare d’Ailly core lithology compared to the δ13C of bulk OM and n-alkane C27 and C29 δ13C and δ2H isotopic composition. Shaded areas: extension of CIE 1 and 2 and a possible CIE3. See Figure 2 for Peaks P1 and P2. Pal. = Paleocene.
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