Effect of Stratospheric Ozone Depletion on Aquatic Ecosystems

Phytoplankton are microscopic photosynthesising organisms which live in water. In favourable environmental conditions they have a very high rate of reproduction. They are eaten by microscopic animals called zooplankton. In an investigation, samples of water were removed from a lake at intervals over a twelve-month period and the biomasses of these organisms were determined. The results are shown in the graph.

The oceans need to be protected because it is where life began and if not taken care of, life as we know it will end. The well-being of the ocean is constantly being threatened and needs to stop. When dangerous substances go into the ocean, ecosystems suffer and become endangered along with the lives of people and marine life. The importance of protecting and preserving the quality and biodiversity of the world 's coasts must be recognized because they are truly irreplaceable. If humans are not educated , and become careless about what is thrown on the ground or sprayed on lawns, disastrous effects follow when it comes to the condition of the ocean’s ecosystems, which can endanger life itself, leading to a problem only we can correct. There is historical evidence of ocean pollution, although the problem still shadows us today.

Oceans cover approximately 75% of Earth 's surface and are vital to this planet and the people who inhabit it. Oceans provide food, natural resources, and recreation for nearly everyone in this world. Unfortunately Oceans have been receiving mass amount of pollutants including oil spills, toxic waste dumping, and industrial dumping. These pollutants will have negative impacts on the wildlife in the ocean, as we are seeing already with the Coral Reefs, and soon enough it will begin to affect our lives as well.

Since early 1998, climate change has been demonstrating its effects in increasing the ocean 's temperature (West & Salm, 2003). Warm water stress corals causing the phenomenon known as coral bleaching, by which expulsion of colourful symbiotic algae the zooxanthellae, vital for

Six abiotic factors that affect the organisms living in the ecosystem are sunlight, temperature, the density, the buoyancy level, the salinity level, and the penetration of light. The sunlight entering the ecosystem allows the process of photosynthesis to continue. This process provided nutrients, food, and energy to the plants and animals in the area, allowing the food chain to be secure. The temperature of the water should be between 68 to 82 degrees Fahrenheit. If the temperatures go lower than the range, or higher, some organisms who use the coral reef as a habitat may not be able to adapt or survive in the new conditions. The density of the coral reef affects the communities of animals and other biotic factors since some of them can only survive between certain depths of the water. The buoyancy level of the water in the coral reef contributes to the ability to move for the animals. Buoyancy is the force that supports an organism’s weight. The salinity level in a coral reef is greater than the salinity in a freshwater ecosystem. If the salinity levels

“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.

UV radiation, such as that from the sun can be very harmful. It has been shown to cause many different mutations within cells, leading to issues for the organism such as death or disease. One of the most prevalent sources of UV radiation for humans is the sun. It’s very important for us to know the extent of cellular damage that can be caused by this radiation, as to know how harmful the sun’s rays are to us as humans. One way that the damage caused by the suns radiation can be tested is through the model organism yeast. For this lab, we exposed two different strains of yeast to UV radiation to test its affects. One strain was able to self-repair, while one was genetically altered so that it could not. Observations were recorded at

How do CFCs or chlorofluorocarbons affect Canada’s Ozone layer. To answer this question we first have to understand chlorofluorocarbons and the earth's ozone layer. Chlorofluorocarbons are chemical compounds made up of three chlorine atoms. One fluorine atom and 1 carbon atom. There were many uses for CFCs ranging from, being used as coolants in refrigerants to propellants for aerosols to being used as solvents for dry cleaning. As CFCs are non- flammable and not very toxic we thought they were a revolutionary compound, but unfortunately CFCs were one of the leading causes for the depletion of our ozone layer. ozone is a type of oxygen, an ozone molecule consists of three oxygen atoms whereas a regular oxygen molecule only consists of two.

The Ocean. Commonly known, as the big blue is one of the most ecologically diverse habitats on earth. It is home to 7000,000 million different species, all of which directly rely on the stability and natural habitats, which exist around the globe. In fact, over two thirds of the species living in the ocean are unknown (DNews). The industrial revolution changed the world for the better; the industrial revolution introduced hundreds of new products, which changed the way humans live. Throughout this paper we will discuss the causes and solutions to environmental degradation in the ocean.

Floras and microbes are additional main biotic mechanisms of many oceanic ecosystems. Microbes act as decomposers for oceanic ecosystems, and they break defunct living matter and transforms it into vitality that is used by other existing organisms in the oceanic ecosystem. Detrivores, which are a type of animal, also eat deceased or putrefying plants and animal matter. Algae, which are autotrophs, appear as the head herbal vivacity and primary producers in oceanic ecosystems. The sunlight transforms the light into energy for nourishment for marine plants. Heat and light are focal abiotic factors discovered in essentially all oceanic ecosystems, consequently oceanic ecosystems has some broaden abiotic mechanisms, comprising viscosity and many more. The power that the bulk of an organism is called buoyancy. The durability of the drive of seawater is called viscosity. These abiotic factors source to the drive of all organisms in oceanic systems. Sunlight pierces the sea exterior only about 65 feet. As there is more salt in the Great Barrier Reef than in other oceanic ecosystems the marine holds less oxygen than the

In 1988, the National Aeronautics and Space Administration had conclusive proof products adding to the output of carbon dioxide and methane gases in the atmosphere were causing the earth to warm; and, if not stopped will make it inhabitable for human life. In the 1970’s the United States had conclusive proof that products releasing Chlorofluorocarbons into the atmosphere were causing the ozone layer to deplete; and, that if continued would be dangerous for human life. The United States took international global action, by joining the Montreal Protocol, to phase out the products producing chlorofluorocarbon and the ozone layer has been successfully replenished .

These increasing ocean temperatures, which result in global warming, are mostly due to the amount of CO2 released in the air, therefore threatening the existence of the coral reef systems (Cole, Pratchett and Jones). The reduction of the coral reef ecosystems are attributed to the climate induced bleaching from the past decade. The loss of coral reef environments has direct affects to the habitat of an organism within the reefs (Cole, Pratchett and Jones), leading to a decrease in biodiversity (Coker, Pratchett and Munday).

(Principle number 3). The ocean contains many organisms and ecosystems that contribute to our life on land. These ecosystems function by transferring energy between different trophic levels. Trophic levels are the positions in which organisms are within an ecosystem. The order for this is 1. Autotrophs – things that can create their own food, 2. Herbivores – organisms that eat plants. 3. Carnivores – organisms that eat other organisms and finally 4. Decomposers – organisms which decompose organic material. For example, plants are at the very beginning of the trophic levels. They are labeled as autotrophs since they make their own food with photosynthesis, which we all knew already. This is the same for plants that lay on the bottom of the ocean, they take in the CO2 emissions we create in the atmosphere and take in sunlight to create

It has been proven that the Earth’s atmosphere blocks 98.7 percent of the sun’s UV rays. The other 2.3 percent that we are exposed to, have both beneficial and harmful effects. We do need to focus on the benefits, because we have way more of them. The only harm it does to our body is skin cancer, which by being more careful we can protect from. The

Scientists all over the world have been widely researching to find out ways in which the ozone layer is being destroyed through human actions. The ozone layer is gradually being destroyed by ozone depleting chemicals. These chemicals include chlorofluorocarbons (CFCs), hydroflourocarbons (HFCs), methyl bromide, halons, methyl chloroform and carbon tetrachloride among others (Ryding 173). These chemicals are used locally in coolants, fire extinguishers, solvents, pesticides, aerosol propellants and foaming agents.