The presence of dissolved salts gives seawater its characteristic salty taste and high density compared to freshwater. The salinity of seawater is usually measured in parts per thousand (ppt) and varies depending on the location, evaporation, precipitation, and freshwater inputs from rivers and glaciers. The average salinity of ocean water is approximately 35 ppt, meaning that there are about 35 grams of dissolved salts in every kilogram of seawater.
The dissolved salts in marine ecosystems play vital roles in maintaining the ecological balance and supporting the diverse organisms that inhabit these environments. They influence water density, affect the buoyancy of marine organisms, regulate osmotic pressure, and provide essential nutrients for various species. The intricate interactions between dissolved salts and other physical and biological factors shape the unique characteristics and biodiversity of marine ecosystems.