Prentice HallEARTH SCIENCE  Tarbuck    Lutgens
Chapter   Ocean Water and          Ocean Life13    S6E3.c Describe the composition, location, and    subsurface topography...
15.1 The Composition of Seawater   Salinity     Salinity is the total amount of solid material      dissolved in water.  ...
15.1 The Composition of Seawater   Salinity     Sources of Sea Salt      • Chemical weathering of rocks on the continents...
Salts in Seawater
15.1 The Composition of Seawater   Salinity     Processes Affecting Salinity      • Processes that decrease salinity:    ...
Natural Processes Affecting Salinity
15.1 The Composition of Seawater   Ocean Temperature Variation     The ocean’s surface water temperature      varies with...
Variations in OceanSurface Temperature
Variations in OceanWater Temperature
15.1 The Composition of Seawater   Ocean Density Variation     Density is defined as mass per unit volume.      It can be...
15.1 The Composition of Seawater   Ocean Density Variation     Density Variation with Depth      • The pycnocline is the ...
Variations in Ocean   Water Density
15.1 The Composition of Seawater   Ocean Layering     Oceanographers generally recognize a      three-layered structure i...
15.1 The Composition of Seawater   Ocean Layering     Transition Zone      • Between surface layer and deep zone      • T...
Ocean Zones
15.2 The Diversity of Ocean Life   Classification of Marine Organisms     Marine organisms can be classified      accordi...
Plankton
15.2 The Diversity of Ocean Life   Classification of Marine Organisms     Nekton      • Nekton include all animals capabl...
Nekton
Benthos
15.2 The Diversity of Ocean Life   Marine Life Zones     Three factors are used to divide the ocean      into distinct ma...
15.2 The Diversity of Ocean Life   Marine Life Zones     Distance from Shore      • The intertidal zone is the strip of l...
Marine Life Zones
15.2 The Diversity of Ocean Life   Marine Life Zones     Water Depth      • The pelagic zone is open zone of any depth.  ...
15.2 The Diversity of Ocean Life   Marine Life Zones     Hydrothermal Vents      • Here seawater seeps into the ocean flo...
Hydrothermal Vents
Tube Worms Found Along   Hydrothermal Vents
15.3 Oceanic Productivity   Primary Productivity     Primary productivity is the production of      organic compounds fro...
Productivity in the Barents Sea
15.3 Oceanic Productivity   Primary Productivity     Productivity in Polar Oceans      • The low availability of solar en...
Water Layers in the Tropics
15.3 Oceanic Productivity   Primary Productivity     Productivity in Temperate Oceans      • In temperate regions, which ...
Productivity in Northern Hemisphere,         Temperate Oceans
15.3 Oceanic Productivity   Primary Productivity     Productivity in Temperate Oceans      • Spring        - Spring bloom...
15.3 Oceanic Productivity   Oceanic Feeding Relationships     Trophic Levels      • A trophic level is a nourishment leve...
15.3 Oceanic Productivity   Oceanic Feeding Relationships     Food Chains and Food Webs      • A food chain is a sequence...
Food Chains and Webs
Oceans2012[1]
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  • Oceans2012[1]

    1. 1. Prentice HallEARTH SCIENCE Tarbuck  Lutgens
    2. 2. Chapter Ocean Water and Ocean Life13 S6E3.c Describe the composition, location, and subsurface topography of the world’s oceans.
    3. 3. 15.1 The Composition of Seawater Salinity  Salinity is the total amount of solid material dissolved in water.  Because the proportion of dissolved substances in seawater is such a small number, oceanographers typically express salinity in parts per thousands.  Most of the salt in seawater is sodium chloride, common table salt.
    4. 4. 15.1 The Composition of Seawater Salinity  Sources of Sea Salt • Chemical weathering of rocks on the continents is one source of elements found in seawater. • The second major source of elements found in seawater is from Earth’s interior.
    5. 5. Salts in Seawater
    6. 6. 15.1 The Composition of Seawater Salinity  Processes Affecting Salinity • Processes that decrease salinity: - Precipitation - Sea ice melting - Icebergs melting - Runoff from land • Processes that increase salinity: - Evaporation - Formation of sea ice
    7. 7. Natural Processes Affecting Salinity
    8. 8. 15.1 The Composition of Seawater Ocean Temperature Variation  The ocean’s surface water temperature varies with the amount of solar radiation received, which is primarily a function of latitude.  Temperature Variation with Depth • The thermocline is the layer of ocean water between about 300 meters and 1000 meters where there is a rapid change of temperature with depth. • The thermocline is a very important structure because it creates a barrier to marine life.
    9. 9. Variations in OceanSurface Temperature
    10. 10. Variations in OceanWater Temperature
    11. 11. 15.1 The Composition of Seawater Ocean Density Variation  Density is defined as mass per unit volume. It can be thought of as a measure of how heavy something is for its size.  Factors Affecting Seawater Density • Seawater density is influenced by two main factors: salinity and temperature.
    12. 12. 15.1 The Composition of Seawater Ocean Density Variation  Density Variation with Depth • The pycnocline is the layer of ocean water between about 300 meters and 1000 meters where there is a rapid change of density with depth.
    13. 13. Variations in Ocean Water Density
    14. 14. 15.1 The Composition of Seawater Ocean Layering  Oceanographers generally recognize a three-layered structure in most parts of the open ocean: a shallow surface mixed zone, a transition zone, and a deep zone.  Surface Zone • Shallow (300 to 450 meters) • Zone of mixing • Sun-warmed zone
    15. 15. 15.1 The Composition of Seawater Ocean Layering  Transition Zone • Between surface layer and deep zone • Thermocline and pycnocline  Deep Zone • Sunlight never reaches this zone. • Temperatures are just a few degrees above freezing. • Constant high-density water
    16. 16. Ocean Zones
    17. 17. 15.2 The Diversity of Ocean Life Classification of Marine Organisms  Marine organisms can be classified according to where they live and how they move.  Plankton • Plankton include all organisms—algae, animals, and bacteria—that drift with ocean currents. • Phytoplankton are algal plankton, which are the most important community of primary producers in the ocean. • Zooplankton are animal plankton.
    18. 18. Plankton
    19. 19. 15.2 The Diversity of Ocean Life Classification of Marine Organisms  Nekton • Nekton include all animals capable of moving independently of the ocean currents, by swimming or other means of propulsion.  Benthos • Benthos describes organisms living on or in the ocean bottom.
    20. 20. Nekton
    21. 21. Benthos
    22. 22. 15.2 The Diversity of Ocean Life Marine Life Zones  Three factors are used to divide the ocean into distinct marine life zones: the availability of sunlight, the distance from shore, and the water depth.  Availability of Sunlight • The photic zone is the upper part of the ocean into which sunlight penetrates.
    23. 23. 15.2 The Diversity of Ocean Life Marine Life Zones  Distance from Shore • The intertidal zone is the strip of land where the land and ocean meet and overlap, or the zone between high and low tides. • The neritic zone is the marine-life zone that extends from the low-tide line out to the shelf break. • The oceanic zone is the marine-life zone beyond the continental shelf.
    24. 24. Marine Life Zones
    25. 25. 15.2 The Diversity of Ocean Life Marine Life Zones  Water Depth • The pelagic zone is open zone of any depth. Animals in this zone swim or float freely. • The benthic zone is the marine-life zone that includes any sea-bottom surface regardless of its distance from shore. • The abyssal zone is a subdivision of the benthic zone characterized by extremely high pressures, low temperatures, low oxygen, few nutrients, and no sunlight.
    26. 26. 15.2 The Diversity of Ocean Life Marine Life Zones  Hydrothermal Vents • Here seawater seeps into the ocean floor through cracks in the crust. • At some vents, water temperatures of 100oC or higher support communities of organisms found nowhere else in the world.
    27. 27. Hydrothermal Vents
    28. 28. Tube Worms Found Along Hydrothermal Vents
    29. 29. 15.3 Oceanic Productivity Primary Productivity  Primary productivity is the production of organic compounds from inorganic substances through photosynthesis or chemosynthesis.  Photosynthesis is the use of light energy to convert water and carbon dioxide into energy-rich glucose molecules.  Chemosynthesis is the process by which certain microorganisms create organic molecules from inorganic nutrients using chemical energy.
    30. 30. Productivity in the Barents Sea
    31. 31. 15.3 Oceanic Productivity Primary Productivity  Productivity in Polar Oceans • The low availability of solar energy limits photosynthetic productivity in polar areas.  Productivity in Tropical Oceans • Productivity in tropical regions is limited by the lack of nutrients.
    32. 32. Water Layers in the Tropics
    33. 33. 15.3 Oceanic Productivity Primary Productivity  Productivity in Temperate Oceans • In temperate regions, which are found at mid- latitudes, a combination of these two limiting factors, sunlight and nutrient supply, controls productivity. • Winter - Low productivity - Days are short and sun angle is low.
    34. 34. Productivity in Northern Hemisphere, Temperate Oceans
    35. 35. 15.3 Oceanic Productivity Primary Productivity  Productivity in Temperate Oceans • Spring - Spring bloom of phytoplankton is quickly depleted. - Productivity is limited. • Summer - Strong thermocline develops so surface nutrients are not replaced from below. - Phytoplankton population remains relatively low.
    36. 36. 15.3 Oceanic Productivity Oceanic Feeding Relationships  Trophic Levels • A trophic level is a nourishment level in a food chain. Plant and algae producers constitute the lowest level, followed by herbivores and a series of carnivores at progressively higher levels.  Transfer Efficiency • The transfer of energy between trophic levels is very inefficient.
    37. 37. 15.3 Oceanic Productivity Oceanic Feeding Relationships  Food Chains and Food Webs • A food chain is a sequence of organisms through which energy is transferred, starting with the primary producer. • A food web is a group of interrelated food chains. • Animals that feed through a food web rather than a food chain are more likely to survive because they have alternative foods to eat should one of their food sources diminish or disappear.
    38. 38. Food Chains and Webs
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