G131 HOME
INFORMATION
SCHEDULE
RESOURCES
EXERCISES
NOTES
Links to summaries of key issues for each topic
PREAMBLE
Introduction
History

PART I
Water Planet
Plate Tectonics
Sea Floor
Review 1
Physical Prop.
Chemistry
Ocean Stuct.

PART II
Atmosphere
Currents
Waves
Tides

PART III
Coasts/Beaches
Environ. for Life
Production
Plankton
Nekton
Benthos
Environ. Issues



VISUALS

Links to images employed in lectures on a topic-by-topic basis

TEXT
Link to chapter outlines at online learning center at McGraw Hill.
NOTES
Links to summaries of key issues for each topic

 
Sea Floor and Sediments (contd.)

Notes on Topic:

  • The notes represent summaries of key issues for each topic
  • They emphasize the terminology used to describe the various phenomena.

  •  3. Sediments:
    Learning Objectives: 
    • Characteristics and global occurrence of different sediment types.
    • Sources for sediment: lithogenous, biogenous, hydrogenous, cosmogenous. 
    Sediment Particles:
    • Three different major sources 
    • Lithogenous (rock fragments)
      • formed by physical weathering processes on land (terrigenous)
      • from volcanism (e.g. ashes) 
      • often altered by chemical weathering
    • Biogenous (biogenic), or ooze: 
      • hard skeletal parts, shells (tests), bones, teeth of marine organisms
    • Hydrogenous: 
      • formed chemically.
    Hydrogenous Sediments: 
    • Formed as particles or coatings
    • Manganese (Mn, Fe, Co, Cu, Ni) nodules grow slowly (1 - 10 mm/Ma) 
      • may form on teeth, etc. where sediments accumulate slowly
    • Also, carbonates, evaporites (salt), phosphorites.
    Cosmogenous Sediments:
    • Particles from space, 
      • dust, tektites and meteorite fragments (3 x 1010g/a),
      • characterized by chemistry (Fe, or Fe-rich) 
    Biogenous Ooze:
    • Biological material from surface waters
      • comprises >30% of sediment
      • diluted by other particles
      • calcareous or siliceous
      • deep ocean undersaturated in calcite and silica
    • Carbonate dissolves in deep ocean at low temperatures and high pressures
      • carbonate compensation depth (CCD ~4km), or lysocline
    • Calcareous oozes dominate shallower regions of open ocean
      • absent in deep ocean basins
      • Formed from foraminifera, (microscopic animals), pteropods (snails)
      • coccolithophores (calcareous plants), coccoliths of microscopic plants.
    • Silica dissolves slowly
      • Diatomaceous oozes from diatoms (plants) under nutrient-rich waters
        • N. Pacific and Antarctica
      • Radiolarian oozes from radiolaria (microscopic animals)
        • equatorial Pacific.
    Red Clay:
    • Very fine oxidized, lithogenous sediment
      • deep waters of Pacific.


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