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(The Gist of Science Reporter) Turning Ocean Waters Acidic Threatening Marine Life [APRIL-2020]

(The Gist of Science Reporter) Turning Ocean Waters Acidic Threatening Marine Life

[APRIL-2020]

Turning Ocean Waters Acidic Threatening Marine Life

Seawater to be alkaline. Yet, our oceans are becoming more and more acidic. In fact, they are currently 26% more acidic is salty, and as such one would expect it than they were before the world became industrialized, with the rate of acidification increasing faster than we have ever witnessed before.
Atmospheric Carbon Dioxide (CO2) continues to rise due to anthropogenic CO2 emissions which are released when fossil fuels are burned.
This CO2 doesn’t just waft away into space, some of it remains in the atmosphere where it acts as a greenhouse gas that traps heat, making the planet warmer; and about 30% of it is absorbed by the oceans, where it changes the chemistry of seawater, making it more acidic.
Yet, while this does reduce the amount of carbon dioxide in the atmosphere — which is currently 40% higher than it was before the industrial revolution — it is the primary cause of ocean acidification.

There are two other potential causes of acidification:

Acidification of coastal waters due to runoff containing nitrogen and phosphates from land-based sources;
Release of carbon stored in frozen methane hydrates found in the ocean sediments, which can potentially be released due to ocean warming — a process that would not be reversible.

Oceans Act as Carbon Sink:

The oceans play a key role in the natural carbon cycle, with carbon dioxide moving from the atmosphere into the oceans across the ocean-atmosphere interface.
As carbon dioxide is found in higher concentrations in the atmosphere, it is readily absorbed by the oceans, which traditionally act as a carbon sink.
When carbon dioxide dissolves in seawater it enters the carbonate system where it occurs in one of three forms: dissolved carbon dioxide, carbonate ions (CO32−) or bicarbonate ions (HCO3−).
When carbon dioxide is absorbed into the oceans from the atmosphere it can chemically react with seawater to form carbonic acid (H2CO3), which slowly releases hydrogen ions (H+). Some of these hydrogen ions bond with carbonate ions present in seawater to form bicarbonate.
Consequently, as more and more carbon dioxide is absorbed by the oceans, the concentration of carbonate decreases while the concentrations of hydrogen and bicarbonate increase, resulting in a decrease in pH (potential of hydrogen — the scale used to measure the concentration of hydrogen).
The more hydrogen ions are present in seawater (or any solution), the more acidic it is, and therefore the lower the pH.

Effects of Ocean Acidification:

Impact on Marine Life: Dissolved carbon dioxide is assimilated by phytoplankton during the process of photosynthesis, and carbonate ions (calcium carbonate, CaCO3) are synthesized by zooplankton and other marine organisms, such as snails, shellfish and corals to build shells and skeletons.
While high concentrations of CO2 may be beneficial to photosynthesizing phytoplankton, fleshy algae and seagrasses if sunlight and nutrients are freely available, it can be detrimental to other marine life.
Carbonic acid can reduce the concentration of calcium carbonate needed by zooplankton and other calcium builders to build and maintain their shells and skeletons.
This can affect development, growth, and survival of a wide range of species – from tiny zooplankton to mollusks, coral, urchins and to a lesser degree, even crustaceans such as crabs.
Coral reefs provide essential ecosystem services: they provide food and shelter for a wide range of marine species and are important breeding habitat and nursery grounds for commercial fishery species.
They also offer coastal protection from storm surges and are an important source of tourism revenue.
Their demise would have substantial ecosystem, economic and social implications.
Impact on Marine Ecosystems: With some species, such as phytoplankton and seagrass expected to fare better in acidic waters than others, we are likely to see shifts in the species composition of various marine ecosystems.
This will lead to changes in food webs, where predators will have to find alternative food sources in order to survive. Those that are unable to adapt are likely to disappear.
Impact on Society: With severe implications to marine food webs, ocean acidification ultimately poses a severe threat to ecosystem health and diversity and to both subsistence and commercial fisheries, as well as coral reef tourism.
The demise of these income-generating sectors could have substantial social and economic ramifications.

Solutions:

A number of mitigating solutions have been proposed to reduce ocean acidification.
Reducing CO2 Emissions: As anthropogenic CO2 emissions are the primary cause of ocean acidification, the most realistic and feasible mitigation solution is to reduce the amount of CO2 in the atmosphere by reducing CO2 emissions. To achieve this, we ultimately need to reduce the amount of fossil fuels that are burned to produce power.
Removing CO2 from the Atmosphere: While removing CO2 from the atmosphere using geoengineering methods seems a tad far-fetched and is likely to be expensive, it can easily be accomplished naturally by implementing appropriate land use practices that promote the absorption of atmospheric CO2 by plants and soil — for example, tree planting initiatives, reforestation, and wetland restoration programs.
Reducing Coastal Pollution: Reducing nutrient pollution of coastal zones could be an important mitigation measure in areas where pollution from terrestrial sources is a key driver of acidification. This is particularly relevant in areas where calcifying marine organisms contribute significantly to the local economy, for example, coral reef tourism or shellfish aquaculture.
Improving Ecosystem Resilience: While building ecosystem resilience in itself will not reduce ocean acidification, mechanisms such as marine protected areas can serve as tools to help ecosystems become more resilient to the impacts of ocean acidification and other stressors.
Using Additives: The addition of alkaline mineral rocks to the ocean to act as a buffering agent to reduce acidity, as has been used in freshwater lakes, would only be economically feasible and effective in coastal areas on a small scale. Scaling this up for the entire ocean would simply not be effective; nor would it be economically viable. This option could potentially have negative environmental impacts that are still unknown.
Adapting Human Activities: Human activities that depend on the oceans, such as commercial aquaculture and fisheries, may need to adapt to changes in ocean acidity as our knowledge and understanding improve through research. This may lead to affected industries evolving in line with changes and impacts if they wish to survive. For example, hatchery managers can farm species that have a higher tolerance of acidification, they can relocate their operation, or they can limit pumping of water into tanks/ponds when pH levels are not too low.
Reducing Atmospheric Warming: Reducing other greenhouse gases and using geoengineering methods, such as solar irradiation, that target atmospheric warming rather than atmospheric CO2 are not likely to be beneficial in the short term. However, they may play a role over larger time scales by preventing carbon stored in methane hydrates from being released into the oceans due to melting hydrates.
While some of the above solutions are indeed creative, the only truly feasible and effective way to reduce atmospheric CO2 and ultimately ocean acidification is to reduce the amount of CO2 emitted into the atmosphere in the first place. The most effective way to do this would be to replace dirty fossil fuels with cleaner sources of energy. The technology is available, we just need the political will to push ahead with this.