Coral reefs are geological structures formed from collections of living organisms called coral polyps. Coral reefs consist of calcium carbonate skeletons built by coral polyps that interact with zooxanthellae algae. They are found in shallow tropical and subtropical waters, rich in sunlight, warm temperatures, and have high levels of calcium carbonate.
Coral polyps are small animals belonging to the cnidaria group, which also includes jellyfish and sea anemones. They have a cylindrical body with a mouth in the middle and tentacles surrounding the mouth. Coral polyps have the ability to expand their calcium carbonate skeleton through a process called calcification.
The calcification process occurs when coral polyps secrete enzymes that convert carbon dioxide and calcium ions in water into calcium carbonate that settles and forms the skeleton of coral reefs. This process lasts for a long time and gradually forms a solid coral reef structure.
Coral reefs have a variety of colors influenced by various factors, namely:
Chlorophyll present in zooxanthellae gives green-blue or brown color to coral reef tissue. This color provides protection against excessive sunlight and helps coral reefs to survive in shallow waters where light intensity is very high.
In addition, zooxanthellae also help in the formation of calcium carbonate skeletons that form the physical structure of coral reefs. Zooxanthellae provide calcium carbonate produced from their photosynthesis to coral reefs, which is used for growth and formation of strong shells.
During the process of photosynthesis, zooxanthellae also release oxygen as a byproduct. This oxygen is important for coral reefs and other organisms that live around them. Differences in zooxanthellae species and their concentrations in coral reefs can lead to color variations.
The combination of these factors creates beauty and color diversity in coral reefs. This diversity of colors is important for the visual and ecological appeal of coral reefs, as well as providing shelter and food for the various species that live in them.
Coral reef whitening is a phenomenon that occurs when coral reefs lose color or experience damage so that they turn white and colorless as normal. Some factors that can cause coral reefs to turn white:
Coral bleaching is a sign of extreme stress on coral reefs and can threaten their survival. If there is no rapid recovery, bleached coral reefs may die, leaving behind fragile coral reefs and reduced biodiversity in coral reef ecosystems.
During El Niño periods, there is an increase in sea and ocean surface temperatures even reaching 35°C. Based on predictions by the National Oceanic and Athmosphere Administration Coral Reef Watch, coralbleaching is predicted to occur more frequently and evenly, in line with rising sea surface temperatures due to climate change. The world is on the verge of a fourth mass coral bleaching event that can be seen from most of the dead tropical reefs including parts of Australia's Great Barrier Reef. Long El Niño periods or their high intensity can lead to more serious and widespread bleaching of coral reefs. Once the El Niño period is over, surviving coral reefs can recover if no other significant stresses occur. However, if coral reefs continue to experience stress or are exposed to other stresses such as pollution or physical damage, their recovery can be hampered.
Therefore, coral reef protection and efforts to reduce greenhouse gas emissions are very important in maintaining the health and sustainability of coral reef ecosystems.
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