calcium and strontium isotope systematics in the lagoon estuarine environments of south australia: implications for water source mixing carbonate fluxes and fish migration
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This, thusly, has suggestions for the neighborhood carbonate cycle and carbon-carbon ponders that demonstrates that the South fills in as an unadulterated sink for DIC.
The isotope information from the hardyhead angle gathered in the theta demonstrates that δ is principally controlled by organic procedures, as opposed to the piece of the isotope Ca of neighborhood water consumption.
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