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Critical and Compensation Depths Spring bloom and seasonal cycle
Geographic variation Atlantic vs. Pacific Latitudinal variation
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Light Intensity / Irradiance
Diatoms Dinoflagellates Coccolithophores Cyanobacteria High Low Nutrients Low High Light Intensity / Irradiance Narrow Broad Light Spectrum Temperature Deep water / Winter Shallow water / Summer
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Competition for nutrients
μmax1 = μmax2 Ks1<Ks2 μmax2 > μmax1 Equal Ks Species 1 Species 2 Specific Growth Rate μ Max growth rate (a constant) Half-saturation constant Nutrient Concentration N
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Keep in mind the physics & chemistry of the mixed layer
Wind Light & Heat Nutrients
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Draw the mixed layer here
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Photosynthesis requires light, Respiration does not
Depth Depth + biomass - biomass (Requires light) (Independent of light)
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Compensation Depth P = R Compensation depth R P Depth P>R
Biomass increases P = R Compensation depth P<R Biomass decreases Depth
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Critical Depth GPP=ΣR Net Primary Production (NPP) = 0 Critical depth
R P Gross Primary Production (GPP) Sum of Respiration (ΣR) Depth GPP=ΣR Net Primary Production (NPP) = 0 Critical depth
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If critical depth > mixed layer depth, GPP>ΣR, NPP >0
R P Gross Primary Production (GPP) Sum of Respiration (ΣR) Depth Bottom of mixed layer Critical depth
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If critical depth < mixed layer depth, GPP<ΣR, NPP<0
R P Gross Primary Production (GPP) Sum of Respiration (ΣR) Depth Critical depth Bottom of mixed layer
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Critical depth concept is critical!
Respiration Photosynthesis Understand why R is a straight line Understand why P is an exponential curve Know the difference between: critical depth and compensation depth Depth
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Can you explain why production peaks where it does?
Production is a rate e.g. [g C m-2 y-1] Biomass is a concentration e.g. [g C m-2]
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Spring bloom in satellite images
NASA/Goddard Space Flight Center, The SeaWiFS Project and GeoEye, Scientific Visualization Studio. NOTE: All SeaWiFS images and data presented on this web site are for research and educational use only. All commercial use of SeaWiFS data must be coordinated with GeoEye ( Data provided by: Norman Kuring (NASA/GSFC)
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Need to add zooplankton to understand seasonal cycles
Phytoplankton Physical mixing processes Nutrients Irradiance Zooplankton
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Definitions Phytoplankton Phyto- (plant) and planktos (drifter) drifting single-celled algae Zooplankton Zoo- (animal) and planktos (drifter) Small drifting animals
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Definitions Autotrophs get their carbon and energy from inorganic sources. Phytoplankton are autotrophs because they get their carbon from CO2 and energy from light. Heterotrophs get their carbon and energy from pre-formed organic matter. Zooplankton are heterotrophs because they get carbon and energy by eating phytoplankton (or zooplankton).
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Some marine heterotrophs (Zooplankton)
Protists - single cells Size range: 1 to 1000 μm Life span: days to ~week Crustaceans Size range: 0.01 to 10 cm Life span: weeks to years Gelatinous animals Size range: mm to m Life span: months to ~year ciliates dinoflagellates Copepods are the most numerous multicellular marine animals! krill copepods Greek roots: “auto” =self “hetero”=other “troph”=nutrition or to feed jellyfish salps
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Generation times differ
Phytoplankton Reproduce by dividing ~ hours to days Limited by: Nutrients, light, temperature Zooplankton Several life stages ~2-4 weeks Limited by: Food availability, temperature
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Seasonal evolution of mixed layer
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Annual cycle in N. Atlantic
Nutrients Light Temperature Mixing Mixing Relative increase Stratified
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Annual cycle in N. Atlantic
Nutrients Light Temperature Mixing Mixing Stratified Relative increase Spring bloom Fall mini- Phytoplankton biomass Zooplankton biomass This mechanism of bloom formation is described by Sverdrup’s “Critical Depth” hypothesis.
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Draw seasonal cycle of temperate and light profiles with critical depth here
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Primary production and its seasonal cycle vary greatly in space
Chl a from SeaWIFS satellite Nutrient sources to surface waters are: rivers and land runoff upwelling atmosphere The most productive regions of the oceans are the coastal regions because this is where upwelling is strongest and where river and land runoff meet the sea. Here nutrients result in high productivity rates, which in turn result large fisheries.
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Atlantic Ocean is saltier than Pacific Ocean
The surface N. Atlantic is saltier than the surface N. Pacific, making surface water denser in the N. Atlantic at a given temperature. This difference is because on average N. Atlantic is warmer than N because local heating from the Gulf Stream. Warmer water evaporates faster, leaving higher-salinity water.
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Mixed layer is deeper in Atlantic than in Pacific
Atlantic Ocean Depth (m) South pole Equator North Pole Pacific Ocean The surface N. Atlantic is saltier than the surface N. Pacific, making surface water denser in the N. Atlantic at a given temperature. This difference is because on average N. Atlantic is warmer than N because local heating from the Gulf Stream. Warmer water evaporates faster, leaving higher-salinity water. Depth (m) South pole Equator North Pole Temperature
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Nutrient limitation varies among oceans
Mixed layer is deeper and more nutrient-limited in Atlantic than in Pacific Remineralized nutrients accumulate in deep water, transported by ocean conveyer belt
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Atlantic vs. Pacific mixed layer depths
Time (month) Dcr Dm (Atl.) Dm (Pac.) NPP>0 NPP>0
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Atlantic vs. Pacific spring bloom
Winter: Deep mixed layer, Production shuts down Spring: Phytoplankton bloom Zooplankton - slow to catch up Winter: Shallower mixed layer, Continuous low production Spring: Phytoplankton bloom Zooplankton - right there to eat the bloom! Phytoplankton biomass Zooplankton biomass
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Latitudinal variation in seasonal cycles driven by variation in irradiance
[Also Irradiance] 90oN = N. Pole 60oN ~Anchorage,AK 30oN ~N. Florida 0oN = Equator
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Seasonal cycle varies with latitude
Nutrients Light [Nutrient] Latitude Light Winter Spring Summer Autumn Winter Lalli & Parsons
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Annual cycles in other regions
Phytoplankton biomass Zooplankton biomass Try this on your own: Draw the vertical profiles of temperature and light and the critical depth for each region as we did in class for the North Atlantic.
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This time watch the Arctic and equator
NASA/Goddard Space Flight Center, The SeaWiFS Project and GeoEye, Scientific Visualization Studio. NOTE: All SeaWiFS images and data presented on this web site are for research and educational use only. All commercial use of SeaWiFS data must be coordinated with GeoEye ( Data provided by: Norman Kuring (NASA/GSFC)
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