Introduction Over the last decade, there has been much focus in the ocean science community on studying the potential impacts of ocean acidification (OA). Ocean acidification describes a change in the ocean’s carbon chemistry which is an emerging global problem. Oceans cover nearly 70 percent of the planet’s surface and play a crucial role in regulating atmospheric carbon dioxide through the interaction of physical, chemical, and biological processes (Orr, Fabry, Aumont, Bopp, Doney, Feely, ... & Key, 2005). As a result of anthropogenic emissions from fossil fuels, cement manufacturing, changes in land use and other human activities, carbon dioxide levels have built up in the atmosphere (Orr et al., 2005). Excess levels of CO2 then dissolve …show more content…
Research shows corrosive properties of water with lower pH levels can be harmful for calcifying marine organisms that depend on specific levels of carbonate minerals to form protective shells, such as plankton, oysters, clams, and crab, will ultimately threaten their ability to reproduce and survive (Doney et al., 2009). Higher ocean acidity is also harmful because it alters habitat development for seagrass, kelp, and coralline algae (Doney et al., 2009). Although scientists claim adult fish appear to be less sensitive to OA, some species may be adversely affected during early development stages or indirectly through the loss of other key species in their respective food webs (Ishimatsu, Hayashi, & Kikkawa, 2008). Alaskan’s face the greatest risk from OA because subsistence and commercial fishing occupations rely heavily on the health of these lower food chain creatures which have become vulnerable to ocean chemistry changes (Doney et al., …show more content…
Computer model projections demonstrate that even with optimistic scenarios, an additional reduction in pH of 0.2-0.3 is predicted by the end of the century (Caldeira & Wickett, 2005). While the chemical processes of OA are largely understood, a considerable research gap exists with regard to the biological and socio-economic consequences of these changes (Brandner, Narita, Rehdanz, & Tol, 2014). The urgency of addressing this issue increased significantly following scientist’s discovery of regions identified as “ocean acidification hotspots” where changes in pH are now occurring at an accelerated rate (NOAA PMEL Carbon Group,
G., Cong-Qiang, L., WeiDong, Z., Minella, M., Vione, D., Kunshan, G., & ... Hiroshi, S. (2016). Reviews and Syntheses: Ocean acidification and its potential impacts on marine ecosystems. Biogeosciences, 13(6), 1767. doi:10.5194/bg-13-1767-2016
Projected changes of pH over the next 100 years due to Ocean acidification effects phytoplankton-doubling time.
Ocean acidification is where the ocean water becomes more acidic due to the amount of carbon dioxide in the water. Humans use fossil fuels such as coal, oil, and natural gas that release large amounts of carbon dioxide into the atmosphere. Oceans absorb about one quarter of the carbon dioxide released each year, and since the amount of carbon dioxide in the water increases, it becomes more acidic (Ocean Acidification, NOAA). More acid in the water means that it will be lower on the pH scale and will release more hydrogen ions. This is in comparison to having more base in the water, where it will be higher on the pH scale and will release more hydroxyl ions. The pH scale rates the concentration of hydrogen in water, and acidic water releases more hydrogen ions than basic water. The scale goes from zero to fourteen, where a pH of seven is neutral, a pH less than seven is acidic, and a pH greater than seven is basic. Oceans have an average pH of 8.16, but that number is predicted to decrease
The ocean is a very delicate ecosystem in which the slightest change of pH or chemical composition will result in devastating results. Between 25 and 40% of anthropogenic carbon emissions have entered the marine area since the industrial age (Sabine et
Ocean Acidification is a process that occurs everyday and majorly affects our planet, but most people don’t even realize it exists. Though it can technically be argued that Ocean Acidification has some benefits for the planet, most of the time the effects of this process are very poor and negatively affect the entire world around us. Human evolution has played a major role in contributing to Ocean Acidification. Whenever humans use energy we release Carbon Dioxide into the atmosphere or also known as CO2. This can be in the form of burning fossil fuels from the ground or the removal of national forest by burning. CO2 is a greenhouse gas, which means whenever we can emit it in large quantities or unnatural amounts it can have negative effects on the atmosphere. These high levels of CO2 in the atmosphere result in climate change and more specifically Ocean Acidification. Ocean Acidification occurs when excess Carbon Dioxide is absorbed into the ocean. When this process takes place it can completely disturb the chemical balances of the water. For example, it can reduce pH levels, Biodiversity, and the abundance of calcifying species.
Ocean acidification is the mean decrease in the pH of the earth oceans. Between 1751 and 2004 ocean pH have decreased from 8.25 to 8.14 (Jacobson 2005). The ocean will absorb nearly a quarter of carbon dioxide from the atmosphere every year. Carbon dioxide in seawater increases the hydrogen ion concentration of the seawater, thus lowering the pH of the seawater. A higher concentration of carbon dioxide will lead to bleaching responses to coral reefs. When coral reefs got bleached will damage marine ecosystem. Coral reefs provide shelter, fish and marine life can raise their offspring to form a complete ecological environment. The pH in ocean acidification is the key factor that led coral reefs to fade out and calcification rate increase rapidly. Because increased acidity of the oceans is the production of shell and skeleton plates
Atmospheric CO2 levels are projected to reach 730 to 1090 ppm by 2100 due to rising anthropogenic CO2 inputs (IPCC 2007, Joos et al., 2001, Meehl et al., 2005, Wigley 2004, Wigley and Raper 2001). Oceanic uptake of CO2 is raising marine pCO2 and lowering pH as the dominant dissolved carbonate species in sea water shift from CO32- and HCO3- towards HCO3- and H2CO3, a process known as ocean acidification (OA) (Qu?r? et al., 2012). Declines in pH and ?aragonite associated with emerging changes in carbonate chemistry due to OA will impact diverse marine biota (Doney et al., 2009).
Ocean acidification is the decrease in the acidity levels of the Earth 's oceans, caused by the intake of carbon dioxide emitted in to the environment and atmosphere. Since the industrial revolution, fossil fuel-powered machines have increased human technology and advancement. However, this has caused the emissions, large amounts of carbon dioxide, deforestation, and other greenhouse gases into the atmosphere. Ocean acidification, in turn, has created a benefit to us by slowing down climate change by absorbing the emissions in the water that have remained in the air. However, studies are now starting to show that the massive amounts of carbon dioxide in the water bodies are altering the water chemistry and affecting the biodiversity and life cycles of many marine organisms, especially those at the lower end of the food chain. Other organisms living off the food chain would be part of a symbiotic relationship involving nutrient cycling: where all other organisms are feeding off of the larger one, yet are providing some benefit to the overall host.
Ocean acidification means an ongoing decrease in the pH of the Earth’s oceans, caused by the uptake of carbon dioxide from the atmosphere. Around 30-40% of the CO2 released by humans into the atmosphere dissolves into oceans, rivers and lakes.
Both climate change and ocean acidification, consequences of changes in water lifer cycle due to the absorption of anthropogenic CO2 in our atmosphere. The carbonic acid that gets formed decreases the PH and concentration of carbonate ion, building blocks of the shells and skeletons for many marine organisms. This is tipping the balance of biodiversity and ecosystems. Time-series records of ocean carbon chemistry over the past 25 years show clear trends of increasing ocean carbon and decreasing pH in lockstep with
The world we live in is so vast and exciting. Seventy percent of our world is liquid water we call the ocean. In the ocean there are many creatures that each are unique in their own way. However, it is possible that in our lifetime, many marine organisms will become endangered or possibly extinct. The loss of these mejestic marine creatures will be caused mainly because of human advancements in which fossil fuels are used to produce energy. Biodiversity is greatly affected by this increase in acidity. As the ocean acidifies, multiple social and economic issues arise. As humans, we rely on the ocean for almost everything. Much of our food, clothing, cleaning products and cosmetics come from the ocean. With the loss of
A burden which lays on the shoulders of today’s man is that of climate change, namely, global warming. However, this evil has many ignored byproducts, some which are equally detrimental. In this thesis, we will write about the effects of one of the greatest of this, ocean acidification, known as “global warming’s equally evil twin”.
Ocean Acidification is, excess carbon dioxide (CO2) in the atmosphere. All of ocean acidification happens underwater; that is why it is unseeable and unfeelable. When coal, oil, and gas release carbon dioxide (CO2) into the atmosphere, it dissolves into the ocean. The ocean has absorbed approximately, 525 billion tons of carbon dioxide (CO2) from the atmosphere. Scientists once believed that, when the carbon dioxide (CO2) entered the atmosphere and dispersed into the ocean, it left less carbon dioxide (CO2) in the air to warm planet Earth. But, they quickly learned that the ocean's chemistry was changing.
Over the past couple of years, no other issue has received more attention in the marine community than ocean acidification. Marine biologists have been constantly working towards solving this issue and are hoping to see improvement’s very soon. Ocean acidification refers to the relentless growth in acidity of the Earth’s oceans. This on-going acidity has attributed to an important element; a constant rise of carbon dioxide levels in the Earth. The number one reason this issue is still happening is because of burning fossil fuels. In addition to burning fossil fuels, it has come to a point where it has enlarged a large amount of carbon dioxide by releasing it into the atmosphere. Chemists have taken this issue into attention that carbon enters the ocean and combines with seawater to fallout acid, which boosts the level of acidity. This process is known as ocean acidification.
Ocean acidification has the ability to affect the growth of sea life shells due to the decrease of density of carbonate ions. These shelled creatures are an important part of the ocean ecosystem due to the structures they create, water purification, and they are also food for predators. (Gazeau 2207).