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- W2323417146 abstract "ABSTRACT There is a general consensus that the global chemistry of ocean water has not changed markedly during the Phanerozoic. Nevertheless, significant changes have occurred in the geochemical cycles of some elements and patterns of change have been reconstructed, in various forms, through consideration of the isotope ratios 13 C/ 12 C, 34 S/ 32 S, 87 Sr/ 86 Sr and 143 Nd/ 144 Nd. There have also been attempts to constrain variations in the isotopic composition of sea water itself through measurements of D/H and 18 O/ 16 O, the latter both directly and indirectly. Dissolved constituents in seawater display secular changes in isotopic composition as a consequence of quite different driving mechanisms. δ 13 C and δ 34 S variations are broadly correlated and linked by carbon and sulphur exogenic cycle interaction through redox reactions (the “free oxygen cycle”). The 87 Sr/ 86 Sr trend is determined by the balance among different Sr inputs to the oceanic pool, which vary in their isotopic composition (limestones, old granitic material and young basaltic material). Neodymium isotope variations are not globally synchronous. Changes in 143 Nd/ 144 Nd are influenced by local erosion products from continental landmasses and can therefore be different for coexisting palaeocean basins." @default.
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- W2323417146 date "1989-01-01" @default.
- W2323417146 modified "2023-09-23" @default.
- W2323417146 title "The isotopic geochemistry of ocean waters through time" @default.
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- W2323417146 doi "https://doi.org/10.1017/s0263593300028613" @default.
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