Page 215 - (DK) Ocean - The Definitive Visual Guide
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CYCLES OF LIFE AND ENERGY            213


             Productivity                                                                 Upwelling

             Throughout the world’s oceans, the abundance of                              The open-ocean surface water can become
             marine life varies dramatically. The ocean is more                           impoverished, as nutrients are constantly absorbed
             productive in some places and at some times than                             by phytoplankton and fall with detritus to the sea
             others. The amount of sunlight is a major influence                          floor. Nutrient-rich water can be restored to the
             on productivity and changes with latitude and time                           surface on a large scale by vertical ocean currents
             of year. The supply of nutrient-rich water from the                          in a process called upwelling (see p.60).
             sea floor and light for photosynthesis is affected by                          Near land, coastal upwelling is caused by surface
             changing water movements and day length, affecting                           currents, such as the Humboldt Current off South
             plankton levels. Temperature also affects productivity                       America (see p.58). In the equatorial waters of the
             as it influences the rate                                                    Pacific and Atlantic, mid-ocean upwelling occurs
             of photosynthesis.                                                           when water masses are driven north and south by
                                                                                          the trade winds, and cooler, nutrient-rich water
             CLEAR, TROPICAL OCEAN                                                        rises to take their place. Polar upwelling can
             Tropical waters are not mixed                                                happen where winter storms cause intense water
             seasonally, so few nutrients are                  RICH, MURKY TEMPERATE SEA  movement. When upwelling occurs and there is
             returned to the surface, and little               In coastal and temperate areas, water
             plankton growth is possible. Here, a              turbulence circulates nutrient-rich water   sufficient sunlight, phytoplankton multiply rapidly
             solitary turtle cruises in crystal-clear          that supports a variety of algae, such    to support a vast number of organisms, creating
             surface waters near Hawaii.                       as this kelp forest in the Pacific.  the most productive ocean waters in the world.

                                                                                                  NUTRIENT-RICH WATERS
                                                                                                  Where there is upwelling, large numbers of small
                                                                                                  fish gather to feed on the plankton. They, in turn,
                                                                                                       attract larger predators like these copper
                                                                                                         sharks feeding on sardines off the coast
                                                                                                          of South Africa.               OCEAN LIFE
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