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- W4385285427 abstract "Secular variations in the major ion chemistry and isotopic composition of seawater on multimillion-year time scales are well documented, but the causes of these changes are debated. Fluid inclusions in marine halite indicate that the Li concentration in seawater [Li + ] SW declined sevenfold over the past 150 million years (Ma) from ~184 μmol/kg H 2 O at 150 Ma ago to 27 μmol/kg H 2 O today. Modeling of the lithium geochemical cycle shows that the decrease in [Li + ] SW was controlled chiefly by long-term decreases in ocean crust production rates and mid-ocean ridge and ridge flank hydrothermal fluxes without requiring changes in continental weathering fluxes. The decrease in [Li + ] SW parallels the 150 Ma increase in seawater Mg 2+ /Ca 2+ and 87 Sr/ 86 Sr, and the change from calcite to aragonite seas, KCl to MgSO 4 evaporites, and greenhouse to icehouse climates, all of which point to the importance of plate tectonic activity in regulating the composition of Earth’s hydrosphere and atmosphere." @default.
- W4385285427 created "2023-07-27" @default.
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- W4385285427 date "2023-07-28" @default.
- W4385285427 modified "2023-10-16" @default.
- W4385285427 title "Seafloor hydrothermal systems control long-term changes in seawater [Li <sup>+</sup> ]: Evidence from fluid inclusions" @default.
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- W4385285427 doi "https://doi.org/10.1126/sciadv.adf1605" @default.
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