How did the sea become salty?
Rain water falling on the land has a part in the weathering (breakdown) of rocks and the erosion (transport) of weathered rock fragments.
Rivers carry:
Larger rock fragments as bed load (rolling along the bottom of the stream),
Smaller rock fragments and mineral grains as suspended load (within the water column),
Ions or dissolved "salts" from the chemical weathering of rocks and minerals as dissolved load.
Feldspars are the most abundant minerals in the Earth's crust. Through a type of chemical weathering called hydrolysis, feldspars are altered to form clays, and their ions (Ca, K, and Na) are released to be carried in solution by running water, eventually making their way to the sea.
The weathering of other minerals and rocks also provides salts to the sea. For example, the calcite in limestone dissolves in slightly acidic natural waters, yielding Ca and CO3.
Rivers carry an estimated 4 billion tons of dissolved "salts" to the seas each year.
Some of these dissolved solids will be deposited as sediment, so yearly gains may roughly balance sediment deposition.
Salts have become concentrated in the sea (compared with freshwater) because the sun's heat causes the evaporation of water, leaving the salts behind.
The early sea's may have had a lowwer specific gravity but overall it's stable