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r MAR) at 39 Ma may be an artifact of a change in sedimentation rate that is not resolved in the extended age model (10) but is possibly indicated by other proxy records (33). However, the occurrence of the peak at 39 Ma appears to be part of a cycle of high- and low-productivity intervals observed at this location (14).
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note
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This manuscript benefited from discussions with P. Barker, S. Blair, S. Bohaty, D. Hodell, A. Piotrowski, and J. Smellie; laboratory assistance from A. Heatherington and R. Thomas; and thoughtful reviews by three anonymous referees. This study was supported by NSF grant OCE-962970 to E.E.M. Samples used in this study were provided by the ODP.
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