Ocean Zones 5-3 and 5-4 Notes

Ocean Zones: Intertidal Zone ● Organisms that live in the rocky intertidal zone must be able to tolerate the pounding of the waves and changes in both salinity and temperature. ● They must also withstand periods of being underwater and periods of being exposed to the air. Rocky Shores ● The constantly changing water level along a rocky shore in the Intertidal zone creates different habitats. ● The highest rocks, above the highest high-tide line are never completely covered with water, but get wet as the waves break against the rocks. ● A stripe of black algae indicates the highest high-tide line. ● The rocks below this level are covered with barnacles. Barnacles can close up their hard shells. In Tide Pools: ● When the tide goes out, some water remains in depressions among the rocks called tide pools. ● As the water in a tide pool is warmed by the sun, the water begins to evaporate. ● The remaining water becomes saltier. If it rains, however, the salinity quickly decreases. ● Organisms in the tide pool must be able to withstand these changes in temperature and salinity. ● Tide-pool organisms must also withstand the force of the waves when the tide comes in again. Where River Meets Ocean ● Estuaries are coastal inlets or bays where fresh water from rivers mixes with the salty ocean water. Water that is partly salty and partly fresh is brackish. Neritic Zone ● The shallow water over the continental shelf receives sunlight and a steady supply of nutrients washed from the land into the ocean. The light and nutrients enable large plantlike algae to grow. These algae serve as a food source and shelter for other organisms. ● In many parts of the neritic zone, upwelling currents bring additional nutrients from the bottom to the surface. ● These nutrients support large numbers of plankton, which form the base of ocean food webs. Open-Ocean Zone ● The open ocean differs from the neritic zone in two important ways. ● First, only a small part of the open ocean receives sunlight. ● Second, the water has fewer nutrients. ● As a result, the open ocean supports fewer organisms. Surface Zone: ● The surface zone is the only part of the open ocean that receives enough sunlight to support the growth of algae. Transition Zone: ● The water here is darker and colder than in the surface zone. Deep Zone: ● In the deep zone, the water is even darker and colder than in the transition zone. ● Because of its harsh conditions, the deep ocean is often compared to a desert. ● Few organisms live in the deep zone, compared to other ocean and land environments. ● Finding food in the darkness is a challenge. Many deep-sea fishes produce their own light. ● The production of light by living things is called bioluminescence. Chemical reactions in the cells of organisms produce bioluminescence. ● However, there is one kind of deep-zone environment—a hydrothermal vent—that supports organisms of an unusual number, variety, and size. ● At a hydrothermal vent, hot water rises out of cracks in the ocean floor. This rising water has been heated by hot rock magma beneath the ocean floor and is full of nutrients. ● These vents are located along ocean ridges, where the plates are moving apart and new ocean floor is forming. Review Questions: 1. What are conditions like in the rocky intertidal zone? - Pounding waves, changes in salinity and water temperature, and exposure to sunlight and air. 2. What type of water might you find in an estuary? - A mixture of salt and fresh water. 3. Describe the physical conditions in the neritic zone. - Shallow water, sunlight, steady supply of nutrients. 4. Explain how the neritic zone conditions support the growth of plankton. - Plankton depend on the sunlight and rich nutrient supplies found in the neritic zone. 5. How do conditions in the open ocean and neritic zone differ? - The neritic zone receives sunlight throughout and has high amounts of nutrients. In the open-ocean zone, sunlight penetrates only a short distance and the water has few nutrients. 6. Describe a hydrothermal vent. - Hot water rises out of cracks in the ocean floor that has been heated by hot rock magma in the Earth’s crust.