The deep zone
The epipelagic ocean zone is most habitable.
The water in the deep zone (abyssal zone) of the ocean would be most dense due to the high pressure and low temperature, causing water to become more compact and denser compared to surface waters.
The ocean floor is the most anaerobic zone in the ocean.
The neritic zone is the relatively shallow part of the ocean above the drop off of the continental shelf. The neritic zone is also known as the coastal water, coastal ocean or the sublittoral zone.
The neritic zone is the relatively shallow part of the ocean above the drop off of the continental shelf. The neritic zone is also known as the coastal water, coastal ocean or the sublittoral zone.
The aphotic zone is located in the ocean below the depth of sunlight penetration. It is a deep, dark layer where sunlight cannot reach, resulting in very low to no light levels. Organisms in this zone have adapted to survive in complete darkness.
The epipelagic ocean zone is most habitable.
The deep-water zone is the region of the ocean that is located below the sunlight zone, extending from approximately 200 meters to the ocean floor. This zone is characterized by low temperatures, high pressure, and complete darkness, and is inhabited by different species of fish, cephalopods, and other deep-sea creatures. Seabed features such as abyssal plains, trenches, and hydrothermal vents can be found in the deep-water zone.
Most plants and animals live in the Sunlit Zone.
The epipelagic ocean zone is most habitable.
The epipelagic zone of the ocean is where most life lives.
In the ocean...hahaha