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Although ocean-transferred signals do in general propagate more slowly than atmospheric signals, they can nevertheless move rapidly enough to preclude their resolution within millennial. and possibly even centennial scale records. For instance, Haine et al. (23) have used chlorofluorocarbons as tracers to demonstrate that Antarctic Bottom Water from the Weddell Sea traveled more than 8500 km toward New Zealand in only 23 years.
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We thank J. Tian. K. Pahnke, W. Prell, W. Howard, J. McManus, and D. Oppo for providing data used in the preparation of Figs. 2 to 4 and the accompanying discussion; R. Wust, L Carter, and two referees for their constructive criticism of the manuscript; and the scientific, drilling and ship's staff of drilling Leg 181 and the staff of ODP-Texas A&M University for the hardworking contributions they made toward collecting, describing, archiving and sampling the core materials from Site 1119. This research used samples provided by the ODP, which is sponsored by NSF and participating countries under management of the Joint Oceanographic Institutions. Financial support was provided by the Australian Research Council (grant no. DP0344080) and by the University of Adelaide.
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