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- W1619674886 abstract "This chapter reviews the major geochemical methods used to reconstruct past ocean circulation. The carbon isotopic composition and trace metal concentrations in the calcite tests of benthic foraminifera are used to reconstruct the nutrient content of deep water masses. These water mass tracers reflect both biological cycling and physical circulation and mixing in the oceans. Conservative water mass tracers which reflect circulation and mixing alone are also discussed. These tracers include both the isotopic and chemical composition of the benthic foraminifera as well as information from sediment pore waters. Methods for inferring the rates of past ocean circulation are also examined, including radiocarbon, the accumulation of the decay products of uranium in sediments, and geostrophic shear estimates. Finally, the ocean circulation inferred for the Last Glacial Maximum based on these techniques is discussed." @default.
- W1619674886 created "2016-06-24" @default.
- W1619674886 creator A5005219457 @default.
- W1619674886 date "2014-01-01" @default.
- W1619674886 modified "2023-09-30" @default.
- W1619674886 title "Tracers of Past Ocean Circulation" @default.
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