Sunday, April 22, 2012

Ocean Acidification Research

Ocean Acidification Causes and Solutions

Causes:


The acidification of the world’s ocean has increased at a rapid rate following the Industrial Revolution. The main cause of ocean acidification is the increase in carbon emissions since this time. Oceans have become more acidic at such a rapid rate, that calcifying organism has been unable to evolve to meet this change. This is especially troubling as calcifying microorganism form the basis of marine food webs throughout the ocean. These microorganisms need these shells for protection from other microorganism. When microorganism finally succumbs to the acidification, all other populations within the marine food web will also be devastated. Ocean acidification is a truly international issue, as it is a threat to global biodiversity. The United States is in a unique position to take a stand on ocean acidification because it is the largest producer of the underlying cause; carbon emissions. This endemic will only continue to become more global as developing nations continue to industrialize and release carbon into the atmosphere.
The root of ocean acidification is carbon dioxide emission. Carbon dioxide emission comes from a variety of source such as cars, industrial pollution, electric generated emission, petroleum, natural gas, coal, fossil fuels and much more. From the carbon dioxide that is emitted, the ocean absorbs a quarter of the carbon dioxide. When the carbon dioxide is absorbed, a chemical change occurs; the carbon dioxide + water + carbonate ion à 2 bicarbonate ions. This chemical change results in making the ocean more acidic and lowers the pH of the ocean.
Ocean acidification affects all aspects of ocean life, especially the shelled (calcifying) organisms. The lowering of the pH level affects mussels and oysters shells, causing a direct decline in their populations. This occurs because a lowering of pH causes the shells to dissolve in turn making shelled organisms vulnerable to dissolution. Statistics and tests show that there is a 25- 45% decrease in calcification and there are also clear signs of structural damage in their shell. Pteropods are small winged snails that are the basis of the food chain for much of the commercial fishing. Recent studies have showed the dissolution to their shells if exposed to the carbonate content of the ocean in the next 50 years.
Coral reefs are very sensitive to temperature and if the carbon dioxide levels in the atmosphere cause even a 1-2 degree change in the water that could cause bleaching of the coral. Bleaching of corals is when the coral expels their vital algal symbionts, leaving the coral looking translucent. An example of this was in 1998 when a single bleaching event led to the loss of almost 20% of the world’s living coral. And it is thought that by 2050 more reefs will be disappearing from erosion then we can build due to the combination of warm waters and reduced calcification due to acidification. Another danger to reefs is the higher carbon dioxide concentrate in the water, leading to lowered calcification rates. These lower rates affect the reef’s ability to grow its carbonate skeleton. If this is to happen then the coral will grow much slower and will be much more fragile leading to quicker erosion.
The effects of the increase in carbonate in the oceans could drastically damage humans as well. This is because nearly 500 million people depend on healthy reefs for sustenance, resources, and protection, and with an estimated 30 million people depending on reefs entirely for food. Challenges faced by the coral reefs in the future are directly temperature change.
Ocean acidification will affect different areas of the ocean at different times, for instance areas of higher latitude where the natural carbonate levels are lowest are more susceptible. Also areas to be greatly affected are cold water coral communities which often grow at depths of hundreds of meters and already grow at slow rates and are also fragile. They are thought to be important for many nursery habitats, they are also a hotspot for biodiversity, other benthic ecosystems and organisms such as mollusks, star fish and sea urchins are expected to be hit early due to their already low carbonate concentrations in their deep environments.

Solutions:
Numerous previous solutions exist to solve the problem of increasing carbon emissions and ocean acidification. Alternate energy solutions have been developed to generate electricity in more environmentally friendly methods. Solar and wind powered electrical generation systems have become more prevalent in their appropriate regions in recent years. The main limitation of alternate “green” energy producing solutions is that they cannot be utilized in all regions of our nation. Therefore, the current consensus is that only a combination of solutions will allow the nation to transition from its dependence on fossil fuels. Efforts are also underway to reduce the amount of carbon emissions produced in the transportation of people and commodities. Government regulations have and will continue to improve the fuel efficiency of consumer vehicles well into the future. Automobile manufacturers have recently embraced electric, natural gas, and hybrid vehicles due to rising fuel costs. The main obstacle of reducing transportation related carbon emissions are the American consumer. The commercial transportation industry will certainly shift to “green” sources of energy as fuel prices increase in order to maintain profits. However, consumers may not be willing to purchase smaller, fuel efficient vehicles that are presumed to be less safe. These combustion methods will not be able to proliferate until its supporting infrastructure becomes economical and readily-available. Public mass transportation in metropolitan areas also helps reduce carbon emissions.
The solution to ocean acidification is simply to reduce carbon emissions. Several working solutions have already been developed and utilized throughout the nation. Although increasing awareness would be detrimental to the effort, this course of action is limited as most people are already aware of global climate change and have not attempted to change their carbon footprints. Unfortunately, government intervention may be required to stop the rising trend of carbon emissions. It is clear that the majority of citizens will only adapt clean energy solutions when they become economically advantageous. One solution that seems practical is the process of geologic sequestration. This term refers to the injection of carbon emissions into deep underground reservoirs. However, this solution is also has be met with disagreements. It is agreeable that ocean acidification is impossible to get rid of. Even though public awareness may be overlooked as previously stated, increasing public awareness can always be a positive. It might seem that promoting public awareness is useless now, but in the long run, it will have served its purpose.  

 Sources:
Dr. Hood, M., Dr. Hans-Otto, P., Dr. Fabry, V., Dr. Gattuso, J., & Dr. Reibesell, U. (n.d.). Ocean acidification network. Retrieved from http://www.ocean-acidification.net/FAQeco.html
EPA. (2011, April 14). U.S environmental protection agency. Retrieved from
http://www.epa.gov/climatechange/emissions/co2_human.htm
Natural resources defence council. (2009, September 17). Retrieved from
http://www.nrdc.org/oceans/acidification
Pmel carbon organization. (n.d.). Retrieved from http://www.pmel.noaa.gov/co2/story/What is Ocean Acidification?

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