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Learn about primary productivity in the oceans, its measurement techniques, carbon fixing, and nutrient cycling. Explore plankton nets, chlorophyll extraction, and more. Prepare for study questions with detailed explanations.
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Textbook HW read p214-221Answer the following questions Why is Detritus important ? Explain Nutrient Regeneration? How is primary production measured? What types of bacteria perform nitrogen fixation? What is a tertiary consumer?
Homework • The Oceans Primary Productivity • Study questions 1-14 • Page 4-13
Primary Productivity • The rate of carbon fixation under a square meter of sea surface in a unit of time • Which means how much glucose is made in a set area during a set time.
What is Carbon Fixing Mean??? Carbon is “fixed” (built into an organic molecule) through the process of photosynthesis Carbon is added to hydrogen and oxygen to produce C6H12O6 aka_ glucose
Photosynthesis • Fixes carbon into glucose using the energy of sunlight • 6CO2 + 6H2O + sunlight C6H12O6 + 6O2
Chemosynthesis • Fixes carbon into glucose using energy from chemical compounds found at hydrothermal vents (especially hydrogen sulfide) • Base of food chain that doesn’t require sunlight
Respiration • The breakdown of glucose in the presence of oxygen to release Energy for life processes • C6H12O6 + 6O2 6CO2 + 6H2O + energy
Gross vs Net • Gross primary productivity – total primary production (carbon fixed) • Net primary productivity – amount of primary production minus the amount used by respiration = amount available to support other trophic levels Trophic level ------ a feeding level
Biomass and Standing Crop • Biomass = the organic matter that is produced…Many times expressed as a weight • Standing crop = the total amount of plant biomass present in a given volume of water at a given instant • This helps us determine how much life can the area support –Remember Carrying Capacity?
Figure 14.4 Water column stability = less nutrients therefore less BIOMASS Note: Plenty of solar energy little nutrients – tropical location
Plankton Net • A fine mesh net used to collect samples of microscope Plankton Extra Credit Make a Plankton Net – 20 points
Plankton Net in Tow Plankton net is towed in water. Volume of water is calculated Plankton is collected in tube and is counted. How do they count it? Amount of plankton found in one ml or cc is compared with volume of water
Measure standing crop • 3 ways • Filtration of cells – plankton tow • Chlorophyll extraction • Chlorophyll fluorescence – satellite imagery • Drawbacks • Patchy distribution
Satellite Imagery One way to measure productivity Measures chlorophyll concentration per square meter of sea surface Only measures top meter of water Limited because blue light penetrates 100 m. That means ONLY1% of possible water column production is measured
Compensation depth • Depth where the rate of respiration = the rate of photosynthesis • Net productivity will be ZERO
Compensation depth decreases with phytoplankton growthMore Production! Result = reservoir of nutrients below compensation depth
The area in the water column where production equals consumption • Biomass • Standing Crop • Compensation depth • Photosynthesis
The total amount of plant biomass present in a given volume of water at a given instant • Biomass • Standing Crop • Compensation Depth • Water Column Stability
More Productivity in the Nertic Zones is a result of • Nutrient Runoff • More Light • Less Bacteria • Less Light
At Compensation Depth Net Productivity will be • 90% • 10% • 1% • 0
What percentage of water column productivity is measured in Satellite Imaging • 100% • 99% • 1% • 0%
Carbon fixing results in the production of • Carbon Dioxide • Methane • Glucose • Nitrates
Factors that affect primary productivity Light Nutrient availability Water column stability
Nutrients are brought by • Runoff (from land) OR • WITHIN THE WATER COLUMN THROUGH: • Upwelling (bottom water wells up as surface water moves away) • Overturn (denser sinks, less dense rises) • Mixing (wind stirs up water column)
How to access deep nutrient reservoir • Overturn • But strong winds may mix plankton too deep for photosynthesis • Upwelling • Ekman spiral • Divergence zones
Generalized cycle Available Nutrients Decomposition Producers Consumers
Nitrogen cycle (Again) Bacteria heavily involved Ammonia nitrite nitrate for use by producers N2 fixed for use by producers
Limiting Nutrient The nutrient that runs out first and will limit growth Usually Nitrogen “N” N and P occur in similar concentrations, but producers need more N In Our fish tanks no fish = no nitrates = no algae
Redfield Ratio The elemental composition of marine organic matter (dead and living) is fairly constant. The ratios of carbon to nitrogen to phosphorus remaines the same from coastal (Neritic) to open ocean (Oceanic) regions. C :N :P = 106 : 16: 1 Carbon: Nitrogen : Phosphorus (This is molar ratio.)
Nutrient Profile versus distance from shore more nutrients less shore open ocean
M nutrients Nutrient Profile versus water depth Surface
Eutrophication Excess nutrients (N and P) from fertilizers, sewage, etc., cause bloom in producers. As nutrients are depleted, bloom dies all at once. Massive decomposition depletes oxygen fish kills
Alive, healthy and Diverse Dead- Algae covered
What controls productivity by latitude? • Polar – light limits – 6 months of light or darkness • Mid latitudes – light and nutrients limit as they vary over the year • Tropics/ subtropics – nutrients limit
Figure 14.3 Peak points of both Nutrients and Solar energy = Peak Production