Ocean water is always in motion due to the impact of tides, caused by the gravitational pull of the Moon and the Sun to the Earth, waves and currents caused by the effects of wind. Compensatory currents arise due to water shortages. For example, the water of the Mediterranean is very strongly evaporated, a few rivers and streams pour in, so the water has high salinity and a large density. Deep water flowing from the Mediterranean to the Atlantic creates a shortage, so a surface current flows from the Atlantic into the Mediterranean to make up for that shortage.

Due to its 71% surface cover, the oceans have a great influence on the biosphere. The evaporation of the oceans determines most of the precipitation that Earth receives, the ocean’s water temperature also largely determines the Earth’s climate and wind patterns. Life in the ocean has an evolutionary history that took place about 3 billion years before the movement of plants and animals on land. The amount of life and distance from the coast (the sterility factor) influence the main distribution of marine biomes. Organisms such as algae, algae, and moss that live in tidal areas (where the mainland meets the sea) fix them to the rock so they are not washed away by the tides. The ocean is also inhabited by many species and can be divided into several zones (zones, floors) such as the high seas, the bottom areas, the illuminated areas, the underexposed areas, etc.

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