Effects of increased seawater pCO2 on early development of the 2025

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pH is a measure of how many free hydrogen ions are in the seawater. The more carbon dioxide in the ocean, the more these free agents are created, causing lower pH (more acidic).
Ocean acidification is a consequence of increasing carbon dioxide (CO2) emissions, a greenhouse gas driving climate change. The ocean absorbs around one third of all human induced CO2, causing a change in seawater chemistry called ocean acidification.
Because of human-driven increased levels of carbon dioxide in the atmosphere, there is more CO2 dissolving into the ocean. The oceans average pH is now around 8.1 , which is basic (or alkaline), but as the ocean continues to absorb more CO2, the pH decreases and the ocean becomes more acidic.
The excess carbon dioxide currently in our atmosphere has meant that absorption has increased. This lowers the pH, making the water more acidic. Marine species can cope with short-term variations to ocean pH. However, ocean acidification is ongoing, which may reduce the ability of some organisms to adapt.
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