- Fringing reefs form near the continental shelf and stay adjacent to the coastline.
- A shallow lagoon separates these reefs from the coast.
- Reefs such as these are prevalent throughout the world.
- Offshore on the continental shelf, barrier reefs can be found. They normally run for some distance parallel to the beach. Between the beach and the barrier reef lies a deep and vast lagoon.
- Atolls form along mid-ocean ridges. They are round or elliptical, bordered on all four sides by oceans, and feature shallow waters in the middle known as a lagoon.
- Shallow water
- The surface that is semi-hard or hard
- Sediments free water
- Warm water (temperature~27 degrees)
- A plentiful supply of nutrients
- The oceans are becoming more acidic due to global warming, posing a threat to the coral ecology.
- Furthermore, glaciers are melting, causing sea levels to rise. Rising sea levels bury coral reefs and deprive them of sunshine, causing them to develop slowly.
- Marine contamination in plastic waste and other activities has starved the corals. Coral reefs require air and room to survive.
- We may lose them sooner than we imagined because of increased levels of marine pollution.
- When the waters get warmer than the desired temperature, coral bleaching occurs.
- Corals become stressed due to their low-temperature tolerance and discharge symbiotic algae in reaction.
- When they run out of algae, they lose their life supply and cease to exist.