Paleosalinity (or palaeosalinity) is the salinity of the global ocean or of an ocean basin at a point in geological history. == Importance == From Bjerrum plots, it is found that a decrease in the salinity of an aqueous fluid will act to increase the value of the carbon dioxide-carbonate system equilibrium constants, (pK*).
Paleosalinity (or palaeosalinity) is the salinity of the global ocean or of an ocean basin at a point in geological history. == Importance == From Bjerrum plots, it is found that a decrease in the salinity of an aqueous fluid will act to increase the value of the carbon dioxide-carbonate system equilibrium constants, (pK*).
Source: Wikipedia "Paleosalinity" · CC BY-SA 4.0
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