This article was automatically translated from the original Turkish version.
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The Epipelagic Zone, the uppermost layer of the World oceans, extends to a depth of approximately 200 meters below the surface. This region is also known as the "sunlight zone" because it is the layer where sun light penetrates the ocean most intensely. The majority of oceanic photosynthesis events occur in this zone, making it of great importance for sea life.

Layers of the ocean
The epipelagic zone is distinctly different from other ocean layers in its physical and chemical characteristics. Thanks to the penetration of sunlight, its temperature is high and it is in constant mixture motion due to surface currents.
This layer is the deepest into the ocean where sunlight reaches most effectively. However, as depth increases, light intensity decreases. Beyond approximately 100 to 150 meters, light weakens significantly and becomes insufficient for photosynthesis. Phytoplankton, the primary producers in this zone, play a major role in oxygen production.
The temperature of the epipelagic zone varies by region. Near Equator, surface temperatures can reach up to 30°C, while in polar regions they can drop to 0°C. These temperature differences play a key role in the formation of ocean currents.
The salinity in the epipelagic zone averages around 3.5 percent but can vary due to regional factors such as rainfall, evaporation, and sweet freshwater inputs. Because of photosynthetic organisms and continuous gas exchange with the atmosphere, this is the zone with the highest oxygen levels.
This zone is the ocean layer with the greatest biological diversity. Due to the abundance of nutrients, a large proportion of marine life resides here.
In this zone, commercially important fish such as tuna, mackerel, swordfish, sardines and anchovies are common. Additionally, dog fish, barracudas and marlins are also predatory fish that hunt here. Flying fish also live in this zone.

Flying fish Exocoetus volitans

Green sea turtle Cheloniidae
One of the most important ecosystems in the epipelagic zone is coral reefs. Corals are found in shallow, sunlit areas and provide shelter for many marine organisms. However, climate change and ocean acidification are causing coral bleaching and widespread harm of coral reefs.
This zone is critically important for the carbon cycle, oxygen production and food chain.
The epipelagic zone faces numerous threats due to human activities:
The Epipelagic Zone is one of the most critical regions of the ocean ecosystem. This layer, where sunlight reaches, is an ecosystem where photosynthetic organisms live, oxygen is produced, and many species find habitat. However, threats such as global warming, overfishing and pollution are endangering this delicate ecosystem. Protecting this zone is vital not only for marine life but for the ecological balance of the entire planet.

Physical and Chemical Properties of the Epipelagic Zone
Light Availability and Photosynthesis
Temperature
Salinity and Oxygen Levels
Organisms Living in the Epipelagic Zone
Phytoplankton and Zooplankton
Fish Species
Mammals and Sea Turtles
Coral Reefs
The Role of the Epipelagic Zone in the Ecosystem
Threats to the Epipelagic Zone