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Reef

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A reef is a ridge or shoal of rock, coral, or other stable material beneath the water.

Nusa Lembongan Reef
Nusa Lembongan Reef

Reefs are vital to the health of our oceans and our coastlines. They can form through abiotic processes, which are non-living events like sand deposition or wave erosion. However, many of the most famous reefs are biotic. This means they are created by living organisms. Corals and coralline algae are the primary builders of these massive structures.

Great-Barrier-Reef-2018-Luka-Peternel
Great-Barrier-Reef-2018-Luka-Peternel

Some reefs are even man-made, known as artificial reefs. These can be intentional structures or accidental shipwrecks.

Living reefs grow through a complex biological process. Corals and calcareous algae grow on top of one another. This builds a three-dimensional, macroscopic skeletal framework.

Nusa Lembongan Reef
Nusa Lembongan Reef

This framework is constantly modified by other organisms and inorganic processes. Some reefs, called mounds, differ from these skeletal frameworks. Mounds are built by microorganisms that lack large skeletons. For example, cyanobacteria can encourage the accumulation of calcium carbonate. This creates distinct sediment bodies on the seafloor. These microbial mounds, like stromatolites, were very common before large shelled organisms evolved.

Reefs are classified by their origin, location, depth, and topography. They also take different shapes based on their relation to land. A fringing reef is attached directly to a landmass. A barrier reef forms a calcareous barrier around land, creating a lagoon between the shore and the reef. An atoll is a ring-shaped reef that exists with no land present at all. In these systems, the reef front facing the ocean is a high-energy area. The internal lagoon is a lower-energy area with fine-grained sediments.

The history of reef building spans millions of years. During the Cambrian Period, extinct organisms called Archaeocyatha built reefs with tubular skeletons. In the Cretaceous Period, molluscs known as rudist bivalves were major reef builders. The corals we recognize today are called Scleractinia. They arose after the Permian–Triassic extinction event. These corals have become increasingly important throughout the Mesozoic Era. They differ from older rugose corals because their skeletons are made of aragonite rather than calcite.

Coral reefs are incredibly significant to marine life and human safety. They serve as a resource for one-third of all marine populations. Animals use them for habitat, protection, and spawning grounds. Reefs also act as a physical barrier for coastlines. They block forceful waves and storms from hitting the shore. Without them, storms could cause extreme damage to buildings and people. The Great Barrier Reef in Australia is the largest coral reef system on Earth. It reaches a length of over 2,300 kilometers.

Today, reefs face a major threat called coral bleaching. This occurs when corals experience high-stress events. Common stressors include temperature changes, sun exposure, or changes in nutrient availability. When stressed, corals expel the zooxanthellae algae living in their tissues. These algae are essential because they produce energy for the coral. Without them, the coral becomes colorless, or bleached.

Bleached coral
Bleached coral

If the stress does not stop, the coral will eventually die. This impacts the entire marine ecosystem that relies on the coral.

We are currently seeing massive global bleaching events. The 4th major global bleaching event was classified by the NOAA and ICRI. Significant bleaching was observed from February 2023 until April 2024. This event was seen in at least 83 different countries. During this recent event, 84% of the world's reefs were affected. This is a huge increase from the 1st global event in 1998, when only 21% of reefs were impacted. Organizations like the GCRMN and NOAA work to monitor these changes.

Conservation efforts are focused on protecting these underwater worlds. Scientists work to identify high-risk areas to allow for quick emergency responses. One way to help is by improving water quality. Another method is the repopulation of coral to revive damaged areas. People also create artificial reefs to help marine life. These can be made by sinking oil rigs through the Rigs-to-Reefs program. They can also be purpose-built objects like reef balls. These structures provide stable surfaces for algae and invertebrates to attach to.

Vanatinai, Louisiade Archipelago
Vanatinai, Louisiade Archipelago

This creates a home for many different fish species.

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🖼️ Images & Media (7)
File:Nusa Lembongan Reef.jpg
Nusa Lembongan Reef.jpg
File:PamalicanAfterLiftOff.jpg
PamalicanAfterLiftOff.jpg
File:Reef.jpg
Reef.jpg
File:Vanatinai, Louisiade Archipelago.jpg
Vanatinai, Louisiade Archipelago.jpg
File:Bleached_coral.jpg
Bleached_coral.jpg
File:Great-Barrier-Reef-2018-Luka-Peternel.jpg
Great-Barrier-Reef-2018-Luka-Peternel.jpg
File:Fossil Reef Windley Key 1.jpg
Fossil Reef Windley Key 1.jpg
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