1 part in 2000 of light reaching the Earth's surface is captured for photosynthesis
Chemosynthesis
Production of usable energy directly from energy rich inorganic molecules
Available in the environment not from the sun
Very few organism carry out chemosynthesis
Only simple forms of life
Primary Productivity
Synthesis of organic material from inorganic material
Expressed in grams of carbon bound into organic material per square meter of ocean surface area per year
Diatom
Single celled phytoplankton
Most abundant
Made of silicon
Autotrophs
Make their own food
Heterotrophs
Eat other things to obtain energy
TrophicPyramid
Physical Factors Affecting Marine Life
Light
Temperature
Dissolved nutrients
Salinity
Dissolved gases
Acid-base balance
Hydrostatic Pressure
Light
Most sunlight approaching at a low angle reflects off of the water surface
Blue light penetrates the deepest
Red light is absorbed near the surface
Light energy absorbed by water turns to heat
# of particles affects amount of penetrating light
Photic Zone
Uppermost layer of seawater lit by sun (approx 100m/330ft)
Aphotic Zone
Permanently dark layer of seawater beneath the photic zone
Euphotic Zone
Upper most part of the photic zone (70m/230ft)
Disphotic zone
Where light is present but not bright enough to allow photosynthesis
Temperature
Rate of chemical reactions in living organisms is dependent on heat
Metabolic rate is the rate at which energy releasing reactions proceed within an organism
The metabolic rate approximately doubles with a 10 oC (18 oF) temperature rise
Ectotherms
Cold Blooded organisms
Have internal temperature that stays close to their surroundings
Endotherms
Warm Blooded organisms
Have stable, high internal temperatures
Dissolved Nutrients
Nutrient is a compound required for the production of organic matter
Nitrogen in form of nitrate (NO3-) and Phosphorus as phosphate (PO43-) are main inorganic nutrients for primary productivity
Salinity
Changing salinity can cause physical damage of membranes, Alter protein structure, Affect specific gravity, density and buoyancy of organism
Most simple marine organisms are isotonic i.e. salinity inside their bodies is equal to salinity of the seawater
Dissolved Gases
Marine organisms primarily require oxygen and carbon dioxide to stay alive
Oxygen is not easily dissolved in seawater
Carbon dioxide is more soluble and essential to primary productivity
Acid-Base Balance
Seawater is slightly alkaline at pH 8
Dissolved substances in seawater act as a buffer
Acids or bases distort the shapes of enzymes/proteins
Hydrostatic Pressure
Pressure is maintained inside and outside an organism
Same in ocean and at bottom of atmosphere
Marine organisms do not need heavy shells to keep from being crushed
At great depths high pressure makes gases more soluble, Inactivates some enzymes, Metabolic rates for similar temperatures are higher
Classifications of Marine Environment
Divided into zones based on homogeneous physical features like Light, Temperature, Salinity, Depth, Latitude, Water Density, Location (primary division between water and ocean bottom)
Community
Assemblage of all interacting species of organisms in an area
Population
A group of organisms of the same species in a specific area
Ecosystem
System of all interacting organisms, including their non-living surroundings
Habitat
Space an organism inhabits; defined by biological requirements of each particular organism
Niche
Includes all ways an organism affects organisms with which it interacts as well as how it modifies its physical surroundings
Competitive Exclusion Principle
No two species can occupy the same ecological niche in the same place at the same time
Less fit species must evolve into a slightly different niche
Communities can modify the physical aspects of their environment
Coral reefs alter current patterns, ocean temperature, and change proportion of dissolved gases
Climax Community is a long established, stable community