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Well crustaceans make their shells from calcium carbonate, and when they die it puts extra calcium into the environment.

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What is sources of calcium and sodium in oceans?

The primary sources of calcium in oceans are from the weathering of rocks on land and underwater volcanic activity. Sodium in oceans mainly comes from the weathering of rocks on land and dissolution of minerals in oceanic crust. Both calcium and sodium are essential elements for marine organisms and play crucial roles in various biological processes.


Compare the nitrogen carbon and oxygen cycles.?

The nitrogen cycle involves the movement of nitrogen between the atmosphere, living organisms, and the soil. The carbon cycle involves the movement of carbon between the atmosphere, living organisms, oceans, and the Earth's crust. The oxygen cycle involves the movement of oxygen between the atmosphere, living organisms, and the oceans through processes such as photosynthesis and respiration.


Do all oceans have the same amount of salt?

No, the amount of salt in oceans can vary due to factors such as evaporation rates, precipitation, and inflow of freshwater from rivers. The Atlantic Ocean is generally saltier than the Pacific Ocean due to differences in these factors.


What is the residence time of sodium in millions of years if the total amount of sodium in the oceans is 1.5x1022g and it supplies to the ocean at a rate of 2.2 x 1014 grams per year?

The residence time of sodium in the oceans is calculated by dividing the total amount of sodium in the oceans by the rate at which it is supplied. In this case, the residence time of sodium in millions of years would be (1.5x10^22 g) / (2.2x10^14 g/year) = 6.8x10^7 years.


What is the chemical equation for carbonate rock formation?

The chemical equation for carbonate rock formation involves the precipitation of calcium carbonate (CaCO3) from dissolved bicarbonate ions (HCO3-) in water. This process typically occurs in oceans or lakes where calcium ions (Ca2+) and bicarbonate ions are present, leading to the formation of carbonate rocks like limestone or dolomite.