Primary Production
1/2 of total photosynthesis occurs in the ocean*
Primary production is important to study because it is the base of the food web
Carbon Cycle
- Photosynthesis takes up CO2 to make organic carbon molecules of the phytoplankton cell (algae)
- The Global Carbon cycle is closely related to the Global Warming cycle
- Respiration produces CO2 gas from organisms
Global Carbon Cycle
- Photosynthesis produces oxygen
- 1/2 oxygen comes from ocean
Section II: Requirements for Growth
- Phytoplankton grow because of light and nutrients
- Plankton are small organisms that drift with ocean currents
- Phytoplankton: small cells that contain chlorophyll and drift with ocean currents
- Photosynthesis: Chemical reaction that uses H2O and CO2 and energy from sunlight to produce glucose and oxygen.
- Net Primary production is the difference between the amount of CO2 consumed by photosynthesis and amount of CO2 produced by respiration
- NPP is positive when photosynthesis is greater than respiration
- NPP is negative when respiration is greater than photosynthesis
- When CO2 is consumed by photosynthesis it creates organic phytoplankton cells
- 1/3 of the CO2 produced in industrial age are consumed by the ocean (largely through carbon pump)
Major phytoplankton Groups
- Diatomes are made up of silica which is heavy
- Flagellates avoid sinking
- Photosynthetic bacteria are the main photosynthesizers and are able to grow with low nutrients
Light dependency of Phytoplankton Growth
- Compensation light level is the light intensity where NPP=0
- Photosynthesis compensates for respiration loss
- Light limited region has low photosynthesis
- Light saturated regions has max photosynthesis
- Protoinhibited is too light to photosynthesize
4 Phyotoplankton nutrients
- Nitrogen
- Silica (for diatomes)
- Phosphorous
- Iron
Nutrient-Dependency Theory
- Growth advantage is with small phytoplankton because it needs less nutrients
- Deep ocean=light limited and Surface ocean=nutrients limited
As we warm the surface layer of the ocean and leave the deep layer cold, does that strengthen or weaken the thermocline? Answer: Strengthens because mixing decreases
Iron Limitation
- Southern Ocean is iron limited
- Iron is a micronutrient
- The main source of Iron is dust
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