Figure F2. PETM on Shatsky Rise. Onset of event is recognized by major changes in lithology, carbonate content, foraminiferal preservation, and the presence of bulk sediment CIE. PETM at Site 1208 is recognized by preservational change and confirmed by bulk sediment carbon isotope stratigraphy. Sites are organized by present (and paleo) water depth.

Figure F2. PETM on Shatsky Rise. Onset of event is recognized by major changes in lithology, carbonate content, foraminiferal preservation, and the presence of bulk sediment CIE. PETM at Site 1208 is recognized by preservational change and confirmed by bulk sediment carbon isotope stratigraphy. Sites are organized by present (and paleo) water depth.