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Department of Earth Sciences, Oxford University, South Parks Road, Oxford, OX1 3PR, ENGLAND, gideonh@earth.ox.ac.uk
Lamont-Doherty Earth Observatory of Columbia University, Route 9W, Palisades, New York, 10964, USA, boba@ldeo.columbia.edu
| The first 20% of the full text of this article appears below. |
| 1. INTRODUCTION |
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As in other applications of the U-series, those in paleoceanography rely on fractionation of the nuclides away from secular equilibrium. In the oceanic setting, this fractionation is generally due to differences in the solubility of the various nuclides. The behavior of the U-series nuclides in the ocean environment was widely researched in the middle decades of the twentieth century. This work established knowledge of the concentrations of the nuclides in the various compartments of the ocean system, and of their fluxes between these compartments. Such understanding was comprehensively summarized in the Ivanovich and Harmon U-series volume (1992), particularly by Cochran (1992). Understanding of the behavior of the U-series nuclides has not advanced very dramatically in the decade since that summary but a major theme of research has been the use of this geochemical understanding to develop U-series tools to assess the past environment (Table 1
).
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