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1991) J. Phys. Oceanogr. 21, 1058–1061. 68. Shea, D. , Trenberth, K. E. & Reynolds, R. W. (1992) J. Clim. 5, 987–1001. 69. Broecker, W. , Ledwell, J. , Weiss, R. , Jahne, B. & Munnich, K. O. (1986) J. Geophys. Res. 91, 10517–10527. 70. Wanninkhof, R. (1992) J. Geophys. Res. 97, 7373–7382. 71. Liss, P. S. & Merlivat, L. (1986) in The Role of Air-Sea Exchange in Geochemical Cycling, ed. Buat-Menard, P. (Reidel, Hingham, The Netherlands), pp. 113–127. 72. Esbensen, S. K. & Kushnir, Y. , Corvalis, OR), Climatic Research Institute Report 29.

33. Watson, A. , Robertson, J. , Williams, P. J. le B. & Fasham, M. J. R. (1991) Nature (London) 350, 50–53. 34. Weiss, R. , van Woy, F. A. & Salameh, P. K. (1992) Surface Water and Atmospheric Carbon Dioxide and Nitrous Oxide Observations by Shipboard Automated Gas Chromatography: Results from Expeditions Between 1977 and 1990 (Scripps Inst. of Oceanography, La Jolla, CA), SIO Report 92-11, ORNL/CDIAC-59, NPD-044. 35. Japan Meteorological Agency (1994) WMO World Data Center for Greenhouse Gases, Sample Issue, CD-ROM (Japan Meteorological Agency, Tokyo).

The degree to which deep Atlantic circulation is involved is an open question. In the northern Atlantic where these events have their strongest expression in surface water properties, deep water paleochemical signals can be small even for extrema such as the LGM (18, 53), and benthic foraminifera are often scarce and sporadic, making it hard to construct a continuous high-resolution time series at these sites. Curry and Oppo (68) has evidence suggesting that at least the larger of these events influences the carbon isotope composition of benthic foraminifera from the tropical Atlantic.

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