Ocean Acidification: Chemistry and Marine Life Effects

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CO2 Basics
Ocean Chemistry
Acidification Impact
Climate Links

CO2 Basics

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    Atmosphere is 78% nitrogen, 21% oxygen, and 0.04% CO2.

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    CO2 sources include respiration, decay, fossil fuels, and volcanoes.

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    Land plants and oceans each absorb about 25% of atmospheric CO2.

The concept of the pH scale and the chemical characteristics of acids, bases, and buffer systems.
The global carbon cycle, specifically how carbon dioxide is exchanged between the atmosphere and surface oceans.
Basic chemical reactions and equilibrium, particularly how carbon dioxide dissolves in water to form carbonic acid.
The basic anatomy and biology of calcifying marine organisms, such as corals and shellfish, which rely on calcium carbonate.
The synergistic impacts of ocean warming, deoxygenation, and acidification combined on marine food webs.
Socioeconomic consequences of declining marine populations on global fisheries, aquaculture industries, and coastal tourism.
Mitigation and adaptation strategies, including ocean alkalinity enhancement, blue carbon sequestration, and selective breeding of resilient species.
International environmental policies, climate agreements, and conservation efforts focused on reducing carbon emissions to protect marine habitats.
43.6K views249likes7:08@teacherspet1898Original Release: 2021-05-13

Ocean acidification occurs when atmospheric carbon dioxide dissolves in seawater, forming carbonic acid that releases hydrogen ions; these hydrogen ions compete with calcium to bind with carbonate ions, reducing the availability of carbonate ions needed by marine organisms to build shells and skeletons, thereby threatening ocean ecosystems and creating ripple effects throughout marine food webs.