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The neritic zone is the relatively shallow part of the ocean above the drop-off of the continental shelf, approximately 200m in depth.〔anon. (n.d). Ocean Regions: Blue Water - Characteristics. Available: http://www.onr.navy.mil/focus/ocean/regions/bluewater1.htm. Last accessed 15 May 2014.〕〔Rizk, F. (n.d). MARINE ENVIRONMENT AND PRIMARY PRODUCTIVITY. Available: http://faculty.scf.edu/rizkf/OCE1001/OCEnotes/chap11.htm. Last accessed 15 May 2014.〕 From the point of view of marine biology it forms a relatively stable and well-illuminated environment for marine life, from plankton up to large fish and corals, while physical oceanography sees it as where the oceanic system interacts with the coast. == Definition (marine biology), context, extra terminology == In marine biology, the neritic zone, also called coastal waters, the coastal ocean or the sublittoral zone,〔(Advanced Learner's Dictionary of Botany )〕 refers to that zone of the ocean where sunlight reaches the ocean floor, that is, where the water is never so deep as to take it out of the photic zone. It extends from the low tide mark to the edge of the continental shelf, with a relatively shallow depth extending to about 200 meters (110 fathoms or 667 feet). Above the neritic zone lie the intertidal (or eulittoral) and supralittoral zones; below it the continental slope begins, descending from the continental shelf to the abyssal plain and the pelagic zone. Within the neritic, marine biologists also identify the following: * The infralittoral zone is the algal dominated zone to maybe five metres below the low water mark. * The circalittoral zone is the region beyond the infralittoral, which is dominated by sessile animals such as oysters. * The subtidal zone is sometimes defined as the shallower region of the neritic zone close to the shore. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「neritic zone」の詳細全文を読む スポンサード リンク
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