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   Diatoms
     Photosynthetic
      algae
     Diatomaceous
      earth
   Radiolarians
     Protozoans
     Use external
      food

                     © 2011 Pearson Education, Inc.
   Tests from diatoms
    and radiolarians
    generate siliceous
    ooze.




                     © 2011 Pearson Education, Inc.
   Coccolithophores
       Also called
        nannoplankton
       Photosynthetic algae
       Coccoliths –
        individual plates
        from dead organism
       Rock chalk
         Lithified coccolith-
         rich ooze


                                 © 2011 Pearson Education, Inc.
   Foraminifera
     Protozoans
     Use external
      food
     Calcareous ooze




                   © 2011 Pearson Education, Inc.
   Depends on three processes:
       Productivity
       Destruction
       Dilution




                       © 2011 Pearson Education, Inc.
   Dominated by lithogenous sediment, may
    contain biogenous sediment
   Carbonate Deposits
     Carbonate minerals containing carbon trioxide (CO3 )
     Marine carbonates primarily limestone – CaCO3
     Most limestones contain fossil shells
         Suggests biogenous origin
       Ancient marine carbonates constitute 25% of all
        sedimentary rocks on Earth.




                            © 2011 Pearson Education, Inc.
   Stromatolites
     Fine layers of
      carbonate
     Warm, shallow-
      ocean, high salinity
     Cyanobacteria




                             © 2011 Pearson Education, Inc.
© 2011 Pearson Education, Inc.
© 2011 Pearson Education, Inc.
   Minerals precipitate directly from
    seawater
     Manganese nodules
     Phosphates
     Carbonates
     Metal sulfides
   Small proportion of marine
    sediments
   Distributed in diverse environments
                  © 2011 Pearson Education, Inc.
   Fist-sized lumps of
    manganese, iron, an
    d other metals
   Very slow
    accumulation rates
   Grows ~1 centimeter
    over several million
    years
   Many commercial
    uses

                      © 2011 Pearson Education, Inc.
   Phosphates
       Phosphorus-bearing
       Occur beneath areas in surface ocean of very high
        biological productivity
       Economically useful as fertilizer

   Carbonates
     Aragonite and calcite
     Oolites


                           © 2011 Pearson Education, Inc.
   Metal sulfides
       Contain:
           Iron
           Nickel
           Copper
           Zinc
           Silver
           Other metals
       Associated with hydrothermal vents


                           © 2011 Pearson Education, Inc.
   Evaporites
     Minerals that
      form when
      seawater
      evaporates
     Restricted open
      ocean circulation
     High
      evaporation rates
     Halite (common
      table salt) and
      gypsum
                     © 2011 Pearson Education, Inc.
   Macroscopic
    meteor debris
   Microscopic iron-
    nickel and silicate
    spherules (small
    globular masses)
       Tektites
       Space dust
   Overall, insignifica
    nt proportion of
    marine sediments


                      © 2011 Pearson Education, Inc.
© 2011 Pearson Education, Inc.
   Energy resources
       Petroleum
         Mainly from continental shelves
       Gas hydrates
   Sand and gravel (including tin, gold, and so
    on)
   Evaporative salts
   Phosphorite
   Manganese nodules and crusts

                        © 2011 Pearson Education, Inc.
© 2011 Pearson Education, Inc.
© 2011 Pearson Education, Inc.

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Marine Sediments Types (Detailed)

  • 1. Diatoms  Photosynthetic algae  Diatomaceous earth  Radiolarians  Protozoans  Use external food © 2011 Pearson Education, Inc.
  • 2. Tests from diatoms and radiolarians generate siliceous ooze. © 2011 Pearson Education, Inc.
  • 3. Coccolithophores  Also called nannoplankton  Photosynthetic algae  Coccoliths – individual plates from dead organism  Rock chalk  Lithified coccolith- rich ooze © 2011 Pearson Education, Inc.
  • 4. Foraminifera  Protozoans  Use external food  Calcareous ooze © 2011 Pearson Education, Inc.
  • 5. Depends on three processes:  Productivity  Destruction  Dilution © 2011 Pearson Education, Inc.
  • 6. Dominated by lithogenous sediment, may contain biogenous sediment  Carbonate Deposits  Carbonate minerals containing carbon trioxide (CO3 )  Marine carbonates primarily limestone – CaCO3  Most limestones contain fossil shells  Suggests biogenous origin  Ancient marine carbonates constitute 25% of all sedimentary rocks on Earth. © 2011 Pearson Education, Inc.
  • 7. Stromatolites  Fine layers of carbonate  Warm, shallow- ocean, high salinity  Cyanobacteria © 2011 Pearson Education, Inc.
  • 8. © 2011 Pearson Education, Inc.
  • 9. © 2011 Pearson Education, Inc.
  • 10. Minerals precipitate directly from seawater  Manganese nodules  Phosphates  Carbonates  Metal sulfides  Small proportion of marine sediments  Distributed in diverse environments © 2011 Pearson Education, Inc.
  • 11. Fist-sized lumps of manganese, iron, an d other metals  Very slow accumulation rates  Grows ~1 centimeter over several million years  Many commercial uses © 2011 Pearson Education, Inc.
  • 12. Phosphates  Phosphorus-bearing  Occur beneath areas in surface ocean of very high biological productivity  Economically useful as fertilizer  Carbonates  Aragonite and calcite  Oolites © 2011 Pearson Education, Inc.
  • 13. Metal sulfides  Contain:  Iron  Nickel  Copper  Zinc  Silver  Other metals  Associated with hydrothermal vents © 2011 Pearson Education, Inc.
  • 14. Evaporites  Minerals that form when seawater evaporates  Restricted open ocean circulation  High evaporation rates  Halite (common table salt) and gypsum © 2011 Pearson Education, Inc.
  • 15. Macroscopic meteor debris  Microscopic iron- nickel and silicate spherules (small globular masses)  Tektites  Space dust  Overall, insignifica nt proportion of marine sediments © 2011 Pearson Education, Inc.
  • 16. © 2011 Pearson Education, Inc.
  • 17. Energy resources  Petroleum  Mainly from continental shelves  Gas hydrates  Sand and gravel (including tin, gold, and so on)  Evaporative salts  Phosphorite  Manganese nodules and crusts © 2011 Pearson Education, Inc.
  • 18. © 2011 Pearson Education, Inc.
  • 19. © 2011 Pearson Education, Inc.