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• W2023476844 abstract "A geologically driven model for evaporative deposition of marine sulfate and other sulfur fluxes roughly reproduces the observed stratigraphic record of Paleozoic global evaporite depositional rates and the observed age curve. Erosional and depositional fluxes in this model are controlled by areas available for erosion and deposition, which are in turn controlled by sea level, global hypsography, and plate tectonic movement of the continents through low-latitude evaporite belts. Sea level also provides the record of seafloor-spreading rates needed to determine fluxes at mid-ocean ridges. The success of this geologically driven model, as opposed to geochemical models dependent on isotopic compositions or reservoir contents to determine fluxes, suggests the possibility of modeling fluxes of elements that have no useful isotopic record. It also suggests that variability of the stratigraphic record of evaporite deposition is not entirely the result of accidents of erosion and preservation, but instead may reflect major changes in fluxes to and from seawater. The model's dependence on sea level to replicate the age curve implies that sea level has been a major ultimate control on changing of seawater." @default.
• W2023476844 created "2016-06-24" @default.
• W2023476844 creator A5041424674 @default.
• W2023476844 date "1992-05-01" @default.
• W2023476844 modified "2023-10-17" @default.
• W2023476844 title "A Geological Numerical Model for Paleozoic Global Evaporite Deposition" @default.
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• W2023476844 doi "https://doi.org/10.1086/629631" @default.
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