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1 Primary Production and Energy Flow Chapter 18 NEVER FORGET!!! ENERGY FLOWS: solar (or nuclear) input heat output NUTRIENTS RECYCLE: mass conservation.

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Presentation on theme: "1 Primary Production and Energy Flow Chapter 18 NEVER FORGET!!! ENERGY FLOWS: solar (or nuclear) input heat output NUTRIENTS RECYCLE: mass conservation."— Presentation transcript:

1 1 Primary Production and Energy Flow Chapter 18 NEVER FORGET!!! ENERGY FLOWS: solar (or nuclear) input heat output NUTRIENTS RECYCLE: mass conservation inorganic ↔ organic

2 2 http://antwrp.gsfc.nasa.gov/apod/image/9709/solprom1_eit_big.jpg

3 3 Focus Areas: Trophic Levels Terrestrial 1º Production Controls:  Actual evapotranspiration (AET)  Precipitation  Soil fertility  Consumers Aquatic 1º Production Controls:  Nutrients  Light  Consumers

4 4 Introduction Trophic Level: Position in a food web determined by number of energy transfers from primary producers to current level:  Primary producers occupy first level.  Primary consumers occupy second level.  Secondary consumers occupy third level.  Tertiary consumers occupy fourth level.

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8 8 Introduction Primary production: Fixation of energy by autotrophs in an ecosystem.  Rate of primary production: Amount of energy fixed over a given period of time.  Gross primary production: Total amount of energy fixed by autotrophs.  Net primary production: Amount of energy leftover after autotrophs have met their metabolic needs.

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10 10 Primary Production Controls Bottom-Up Controls  Influences of physical and chemical factors of an ecosystem. Top-Down Controls  Influences of consumers.

11 11 Actual Evapotranspiration and Terrestrial Primary Production Rosenzweig estimated influence of moisture and temperature on rates of primary production by plotting relationship between annual net primary production and annual actual evapotranspiration (AET).  AET: Annual amount of water that evaporates and transpires off a landscape.  Cold dry ecosystems tend to have low AET.

12 12 Evapotranspiration and Terrestrial Primary Production

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14 14 Soil Fertility and Terrestrial Primary Production Significant variation in terrestrial primary production can be explained by differences in soil fertility.  Shaver and Chapin found arctic net primary production was twice as high on fertilized plots as unfertilized plots.  Bowman suggested N is main nutrient limiting net primary production in a dry tundra meadow, and N and P jointly limit production in a wet meadow.

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16 16 Primary Production on the Serengeti McNaughton estimated Serengeti grazers consume an average of 66% of annual primary production.  Rate of primary production in the Serengeti is positively correlated with rainfall quantity.

17 17 Primary Production in the Serengeti Found grazers can increase primary production.  Increased growth rate.  Compensatory Growth  Lower respiration rate due to lower biomass.  Reduced self-shading.  Improved water balance due to reduced leaf area.

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19 19 Patterns of Aquatic Primary Production Several studies have found quantitative relationship between phosphorus and freshwater phytoplankton biomass. Several studies support generalization that nutrient availability controls rate of primary production in freshwater ecosystems.

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21 21 Lake 226

22 22 Global Patterns of Marine Primary Production

23 23 Lake Primary Production Carpenter proposed piscivores and planktivorous fish can cause significant deviations in primary productivity.  Carpenter and Kitchell proposed the influence of consumers on lake primary productivity propagate through food webs.  Trophic Cascade Hypothesis

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