Climate Change : The Effects Of Climate Change On Coral Reefs

Some of the carbon dioxide is being combined with our oceans to make up carbonic acid. Thus decreasing the PH of the oceans, and with this acidification it is known to be dangerous for many reason. Many of the large animals are losing key nutrition, it is hindering photosynthesis and is even wiping out existing ecosystems. The one key group that is harmed the most is creatures that are classified as Calcifiers. They are one of the most common animals in the sea, which means that, if the acidity of the oceans continue to rise, a significant chunk will die out or have to adapt rapidly to the environmental change. The reason they are in the most danger is because with the ocean becoming more acidic it is eroding the shells off of the sea

Currently there is no saturation level above four in the world. If current trends continue, by 2060, there will be no location above 3.5 and by 2100, no place above 3. The negative trends are extremely concerning as the changing water levels are making the reefs’ survival more unlikely. The energy required for calcification increase, and thus calcification rates decrease. Because of the lack of growth, coral diversity plunges. Over half a million species have spent their life on coral reefs. Coral reefs are intricate exchange bazaars that pass nutrients to various animals. Without the reefs, this exchange would not be possible and the abating of the reefs contributes to the disappearance of the ecosystem as a whole. While ocean acidification is not the only reason for the withering reefs, it is the most detrimental. The effect of ocean acidification extends beyond just the coral reefs. This process affects marine animals’ tightly regulated internal chemistry such as metabolism, enzyme activity, and protein function. Ocean acidification alters the presence of key nutrients such as iron and nitrogen essential to animals. It will also make the ocean noisier (Kolbert 136-141). The implications of ocean acidification are interminable. Human realization is imperative to slow the rate at which ocean saturation is declining. The less carbon emissions released in the air, the less carbon dioxide is absorbed by the ocean which will inadvertently prove beneficial to the coral reefs, but also many other species dependent on the

The rate of natural extinction occurs at a rate of one to five species every year. According to Joanna Zelmen, from The Huffington Post, there are over 2,500 species of coral alone, and they could all be threatened by the year 2050. Humans uphold the biggest influence on the diminishing reefs through overfishing, construction, and pollution, but we can also have the biggest impact to help these strange yet beautiful animals.

Global temperatures are steadily rising due to anthropogenic causes; this increase in temperature is causing changes to ocean properties that can impact the organisms that call this medium their home. One of the most evident impacts of climate change on the world’s oceans is the resulting raise in ocean surface temperatures. Rising ocean temperatures can directly affect biogenic reef building organisms like corals which produce some of the most diverse and productive ecosystems in the world. Previous studies within this field have determined that climate change is a notable stressor for these corals causing large scale bleaching events; where they release their photosynthetic symbionts. Once the symbionts of these organisms are released corals begin to starve and ultimately die resulting in

coral survival, growth and reproduction leaving corals bright white. Furthermore, climate change alters the carbon dioxide concertation within the ocean causing variation of pH level through which ocean become more acidic. This event is referred to as ocean acidification. When this occurs, the corals are unable to absorb calcium carbonate needed for skeletal maintenance (Freiwald, et al., 2004). In addition, human population dynamics have increased through the 21th

“Since the beginning of the industrial era, the ocean has absorbed some 525 billion tons of CO2 from the atmosphere, presently around 22 million tons per day” (Ocean Portal, n.d). This number is expected to increase forevermore as atmospheric carbon dioxide levels increase and the effects of Climate Change worsen. At first, the idea of our oceans absorbing carbon dioxide from the atmosphere may sound great, however, scientists have been quick to learn otherwise. High concentrations of carbon dioxide in oceans can have detrimental effects on the ocean chemistry and marine ecosystems (Hardt; Safina, 2008). Marine ecosystems are greatly complex and depend on every marine organism to function properly, any change can put the whole ecosystem at risk. For example, the increase of carbon dioxide in our oceans is responsible for the dissolving of “brittle star” skeletal parts, which has in effect caused food scarcity for many fish, crabs, shrimp, and other starfish (Leu, 2013). Furthermore, these marine ecosystems are very important to humans- being the primary food source for millions around the world and having an economic market worth trillions of dollars (Hardt; Safina, 2008). Part of keeping these ecosystems safe is to understand how they work and how projected changes can harm marine organisms.

Not only does this increase in ocean acidity result in shell degradation, but it has also been shown to breakdown existing coral reefs, as well as limit the building of new coral reef structures all over the planet. Corals, like calcifying species, rely on a steady supply of calcium carbonate in order to build and maintain it 's strong structures. This preventable destruction would not only be breaking down some of the most ancient ecosystems, but also some of the most diverse ecosystems on the planet. Occupying less than one percent of the ocean floor, coral reefs are home to more than twenty-five percent of marine life. Thanks to their diversity, coral reefs provide millions of people with food, medicine, protection from storms, and revenue from fishing and

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

This increase in oceanic inorganic carbon has offset the seawater carbonate chemistry by causing increasing concentrations of CO2 and bicarbonate, while causing decreasing concentrations of carbonate and pH levels (Dedmer 2013). Rost and colleagues (2008) express that emissions of fossil fuel have caused an immense increase in the levels of atmospheric CO2, which are then deposited into the surface water of oceans. This increase in carbonic acid is in turn decreasing the pH balance, which poses a threat to marine organisms.

The map above shows a depiction of aragonite saturation, a form of calcium carbonate that many marine species also rely on to build their protective shells. It is anticipated that a high volume of species relying on carbonate ions to form outer layers and exoskeletons will be negatively affected by the changing chemistry of seawater. Even a slight drop in pH levels will mean higher concentrations of hydrogen ions will be available to bond with carbonate ions, forming more bicarbonate than normal. Marine calcifying species are this put at a higher risk for predation. Ocean researchers and marine biologists are hopeful that some marine species that calcify for survival will be able to adapt to the changing pH levels in the oceans. Others are not so optimistic, and expect that an acidic oceanic environment may result in mass extinction and serious disruptions to aquatic food chains.

Consequently, Climate change has a major impact on The Great Barrier Reef such as; increasing sea temperatures, warmer waters that are causing corals to become bleached and stressed. Sea levels rising, extreme weather conditions (like storms and cyclone that-re breaking up the coral reefs). Furthermore, increasing flooding therefore polluting the reef, and fishes moving to cooler waters and leaving bird

Anthropogenic activity has led to greatly increased emissions of greenhouses gases. Increased temperatures, acidification and stratification are all affected by increased carbon dioxide (CO2) concentrations. These symptoms of climate change have direct and indirect effects on to marine ecosystems, all of which start at the major primary producers of the oceans: phytoplankton.

Carbon dioxide is a greenhouse gas that we exhale in our daily lives. Plants use carbon dioxide to create oxygen that all mammals use. However, carbon dioxide can also change the chemistry of the ocean, this is often referred to as ocean acidification. The excess carbon dissolves into oxygen in the water, producing a chemical called carbonic acid. This acid causes the ocean to become more acidic. In the eighteenth century, the pH was 8.07 which was slightly basic. Currently, the pH is around 8.01 this is about a twenty-five percent increase in acidity. (National geographic) While this slight change may not seem outrageous, it is causing multiple marine life struggles. The acid melts the shells of pteropods causing a low supply of food that would support larger fish.

Atmospheric carbon dioxide is a greenhouse gas, meaning it traps solar radiation in the atmosphere. This is done by either absorbing or reflecting infra-red waves, thereby trapping them in the Earth’s atmosphere for longer, contributing to global warming. Rising sea surface temperature has a large effect on coral, due to their low range of tolerance of 23°–29°Celsius. Large-scale bleaching events can occur from a temperature change as little as 1-2°Celsius (Brown 1997). Bleaching is the loss of colour from the coral and can be due to two reasons, the symbiotic zooxanthellae plankton either leave the coral

The effects of global warming touch every human, animal, plant, ocean, landmass, and atmosphere level on this planet. The numerous effects of global warming are mixes of "good" and "bad" results, depending on how your definition of "good" results and "bad" results are. A "good" effect, a person could say, would be for regions with normally cold temperatures to receive warmer temperatures for their normal. Yet, there are more "bad" effects that seem to out weight the "good" effects. Some of the effects would include increases of flooding, severe storm systems, and rising sea-levels. One major consequence would be an increase of temperature globally. This would