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Actually, the pH of the ocean is slightly basic, in the pH range of 8 but it varies depending on location. And CO2 does get tied up with alkali metal salts in cold water to remain in solution (calcium bicarbonate or magnesium bicarbonate) but when those salts are carried to warmer regions by ocean currents, the bicarbonates decompose to calcium (or magnesium) carbonate and release the other molecule of CO2 back in the atmosphere. If the Calcuim cabonate forms in warm shallow seas, it will be the start of making limestone which is a really permanent sequester of the carbon dioxide. Just look at the Grand Canyon, you see 600 million odd years of carbonate sequestration right before your eyes if the vertical limestone cliffs. Isn't it amazing how mother nature uses warm water to sequester CO2?

From: Panelists agree state to see 3- to 5-foot increase in sea level within 100 years

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