The Effects Of Bleaching On Coral Reefs

As atmospheric carbon dioxide levels continue to rise, global warming will increase ocean temperatures and, along with that, the frequency and severity of bleaching events. In 2010, one of the hottest years in recorded human history, reefs bleached throughout the Caribbean and the Indian Ocean and off the coasts of Thailand, Cambodia, Malaysia and the Philippines. Without the necessary reduction in the production of emissions, the death of the Great Barrier Reef will result in 6 billion dollars less in the economy and the loss of more than 50,000 jobs, If the oceans' corals were to collapse, the whole food chain will

Coral bleaching is a somewhat recent phenomenon that has prompted many communities and countries around the world to enact policies and legislation that deal with their dying coral reefs. In early 1998, a mass coral bleaching event took place on the Australian Great Barrier Reef, and broad scale aerial surveys confirmed that most of the inland reefs had experienced at least some bleaching (Lally 1999). The following analysis of the Great Barrier Reef will illustrate that a successful policy process must incorporate the people who live, work, and depend on the fragile environment into the decision-making about

Coral reefs are found in shallow tropical waters along the shores of islands and continents. Coral bleaching is a topic that gets left in the dust. Not many people really pay attention or show much interest in it. Widespread bleaching, involving major coral reef regions and resulting in mass coral mortality has raised concerns about linkage of the events to global phenomenons including global warming or climate change and increased UV radiation from ozone depletion. Corals provide a lot not just for us humans but for marine life as well. Marine Biology provides information about how bleaching happens and how it affects the coral. Buchheims’ article is full of logos and a few pathos while the other source is full of ethos. In The Nature Conservancy’s director Stephanie Wear provides us with lots of professional opinions

Coral bleaching is normally characterized by the expulsion of the zooxanthellae algae, loss of algal pigmentation, or both. Coral bleaching events have had serious effects on corals and reefs worldwide. What is crucial to the understanding of zooxanthellae expulsion and bleaching is how the density of zooxanthellae within the coral is changing, if at all, under the prevailing range of environmental conditions (Gates and Edmunds, 1999). Over the last twenty years, there has been a dramatic increase in both the frequency and intensity of coral bleaching events. Sixty major bleaching events have been reported between 1960 and 1979, whereas only nine were reported prior to 1979 (Huppert and Stone, 1998). Given the dependence of the coral on this symbiotic algae, it is important to determine the cause of these bleaching events. According to Helvarg (2000, p.12):

Consisting of less than 1% of the world oceans, the coral reefs are ancient animals comprising of thin calcium carbonate deposits within the photic layer. Aside from its biologically diverse ecosystems, coral reefs are major source of food for millions and provides habitats and nursery areas for many marine organisms. Coral reefs also act as a physical buffer to protect the coastlines from tropical storms and erosion. In addition, many local communities rely on coral reefs to generate an income through activities such as fishing and diving. However, 75% of the coral reefs are under threat from induced impacts of humans and climate change (Burke, et al., 2011). This essay looks at the human impacts constantly being inflicted on coral reefs.

Coral bleaching usually occurs when the surface of a sea with coral in it becomes too warm for the coral. When the water heats to as little as one degree higher than normal, coral expels the algae living in its tissue, which causes it to turn completely white. The rise in temperature of the sea surface has been linked mainly to global warming. Other causes of coral bleaching include oxygen starvation caused by an increase in zooplankton, increased solar irradiance, increased sedimentation, bacterial infections, changes in salinity, herbicides, low tide and exposure, cyanide fishing and elevated sea levels. Bleaching events in 2016 were unprecedented, nearly 90% of the coral in the Great

In 1980, NOAA’s marine biologist started noticing the coral bleaching. There has been three important coral reef bleaching events in the history. The first global bleaching event “El Niño” was in 1998, it was a “huge underwater heatwave killed 16% of the corals on reefs around the world” . The second bleaching event was in 2010 and was called La Niña. This event affected especially areas near Palau and Micronesia in the Pacific. In October of 2015, NOAA announced the third global bleaching event in which has already become the longest event recorded, affecting coral reefs for consecutive years.

The bleaching of coral reefs is when warm water forces algae to leave the reef. Once the algae disappear, the coral goes from a vibrant color to a pale white. As one marine biologist said, “You go from a vibrant, three-dimensional structure teeming with life, teeming with color, to a flat pavement...” This bleaching makes the coral more vulnerable to diseases and a greater risk of death. The biggest bleaching events to have occurred in

A hypothesis created by a group of scientists determined that the cause for bleaching was due to stress (Brown and Ogden). This stress is closely linked to salinity changes, exposure to ultraviolet radiation in excessive amounts, huge climate changes and most importantly the increase in warm waters (Douglas ). Corals can survive in water that is between 25˚ and 29˚C. Any water temperature above that will result in the death of algae (Brown and Ogden). High ocean temperatures mixed with solar radiation are attributed to current large-scale bleaching events leading to global climate change, such as El Niño (Douglas ).

The Great Barrier Reef in Australia is experiencing bleaching. According to France-Presse, bleaching of a reef is “coral...that has been stressed by the heat” (France-Presse). When a coral has been “stressed by heat,” (France-Presse) the coral discards the algae that lives within itself which causes the coral to be more susceptible to disease. It can take up to several decades for a coral to recover from bleaching. Because of that fact that most coral does not have enough time to recover, it dies.

Coral bleaching may seem new and a strange topic, but it has been around and wreaking havoc for many of years. Bleaching starts to happen when the water temperatures rise slightly above average temps for more than several days, which then kills the vibrant coral (“Global Warming”). The coral reefs get their vivid color from algae and other small organisms. They are found in the coral’s tissue. Algae helps supply food for the reef through carbohydrates. The algae creates the carbohydrates through photosynthesis (“Coral Reefs”). Coral bleaching

One particularly visible sight that brings climate change to the attention of the public is the series of large tracts of bleached coral on the Great Barrier Reef resulting from unusually warm summers. The Great Barrier Reef is an Australian icon, symbolic of the wealth of Australia's biological diversity. It is the nursery to fishing industries and is visited by thousands of tourists each year, bringing hundreds of millions of dollars into our community. While the high visibility of coral bleaching has made us aware of this impact of climate change we should be equally concerned

When people think of bleaching they might think about bleaching their hair which is damaging if repeated often or perhaps accidentally spilling bleach on a shirt and ruining it. But there is another type of bleaching that a lot of people don’t know about, and that’s coral bleaching. It affects a large majority of the Great Barrier Reef which is a primitive host of living things. The Great Barrier Reef is desperate for attention and it’s up to us to try and save it and prevent more damage from being done.

Coral reefs are threatened by global warming. They can only live in waters between 18 C and 30 C. Therefore, with the increase in temperature of the surrounding water, there has been an unprecedented increase in the number of coral bleaching events during the past 2 decades (which have had some of the warmest years in history). When ocean temperatures get too high, coral polyps lose the symbiotic algae inside them, causing them to turn white, or "bleach," and eventually die.

Coral reefs contain symbiotic algae called zooxanthellae which gives the coral its healthy brownish color. The algae "utilizes sunlight and the coral animal's respired CO2 to produce energy rich compounds that feed the coral host" (AIMS, 2003). When stress factors such as "heat, solar radiation, pollution, reduced salinity and changes in oxygenation" occur around the coral, bleaching can begin (Dennis). When bleaching occurs, the algae, which create nutrients for the coral to feed from, is released due to stresses to the reef. Thus the coral starves and its white calcium carbonate skeleton of the coral becomes visible (AIMS, 2003). But one of the main stresses that contributes to the lifeless white appearance of the coral is the warmer temperatures of the sea surface water.