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The disphotic zone is a layer within the ocean's photic zone where sunlight penetrates but is insufficient for photosynthesis. This zone extends from the base of the euphotic zone (where photosynthesis occurs) down to about 200 meters. While light is present, the rate of respiration exceeds photosynthesis in this region. The depth of the disphotic zone can vary based on factors like cloud cover, water turbidity, and ocean surface conditions. Organisms in this zone may migrate to the photic zone at night, while others are adapted to live permanently in darkness.12

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