In the ocean, the aphotic zone is sometimes referred to as the
dark ocean. Depending on how it is defined, the aphotic zone of the ocean begins between depths of about to and extends to the
ocean floor. The majority of the ocean is aphotic, with the average depth of the sea being deep; the deepest part of the sea, the
Challenger Deep in the
Mariana Trench, is about deep. The depth at which the aphotic zone begins in the ocean depends on many factors. In clear, tropical water sunlight can penetrate deeper and so the aphotic zone starts at greater depths. Around the poles, the angle of the sunlight means it does not penetrate as deeply so the aphotic zone is shallower. If the water is turbid, suspended material can block light from penetrating, resulting in a shallower aphotic zone. Temperatures can range from roughly to . The aphotic zone is further divided into the
mesopelagic,
bathyal,
abyssal, and
hadal zones. The mesopelagic zone extends from to . The bathyal zone extends from to . The abyssal zone extends from to or , depending on the authority. The hadal zone refers to the greatest depths, deeper than the abyssal zone. Some twilight occurs in the mesopelagic zone, but creatures below the mesopelagic must be able to live in complete darkness. ==Life in the aphotic zone==