Figure F12. Chronostratigraphic correlation of Holes U1307A and U1307B based on calcareous nannofossils, diatoms, planktonic foraminifers, and dinocysts. Relationship to magnetostratigraphy is shown in the left panel. Bar at 56–62 mcd indicates tentatively identified hiatus. MIS = marine isotope stage, LO = last occurrence, FO = first occurrence.
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