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8.2 Energy Flow Through Ecosystems

  • Learning objectives
    • Describe the strategies organisms use to acquire and use energy.
    • Explain how changes in energy availability affect populations and ecosystems.
    • Explain how the activities of autotrophs and heterotrophs enable the flow of energy within an ecosystem.

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Changes in energy availability can result in …

  • changes in population size.
  • disruptions to an ecosystem
  • affects in the number and size of the trophic levels.

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Dynamics of an Ecosystem

  • biotic components of an ecosystem are living organisms can be categorized according to their food source
    • Autotrophs
    • Heterotrophs
  • abiotic components of an ecosystem are the nonliving, inorganic properties of the environment
    • Chemical elements
    • Sunlight
    • Water

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Autotrophs

  • capture energy (e.g., sunlight) using inorganic nutrients
  • produces organic compounds
    • Producers
  • possess chlorophyll and carry on photosynthesis
    • photosynthesizes
      • Green plants
      • Algae
      • Blue-green bacteria

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Chemoautotrophs

  • bacteria that obtain energy from the oxidation of inorganic compounds
    • ammonia
    • nitrites
    • Sulfides
  • synthesize carbohydrates
  • found in cave communities
  • ocean depths & volcanic vents

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Heterotrophs

  • need a source of preformed organic nutrients and consume tissues of other organisms
    • consumers
  • herbivores
  • carnivores
  • omnivores
  • decomposers
  • detritivores

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Herbivores

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Carnivores

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Decomposers

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Energy Flow

  • major ecosystems are dependent upon solar energy flow and finite pools of nutrients
    • most cannot exist without a continual supply of solar energy
  • Energy flow in an ecosystem is a consequence of two fundamental laws of thermodynamics:
    • The first law of thermodynamics states energy can neither be created nor destroyed; it can only be changed from one form of energy to another.
    • The second law of thermodynamics states when energy is transformed from one form to another, there is always some loss of energy from the system, usually as low grade heat.

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Energy Balances

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Food Webs are Examples of Energy Flow

  • complex trophic (feeding) relationships that exist in nature
    • grazing food web begins with leaves, stems, and seeds eaten by herbivores and omnivores
    • detrital food web begins with detritus, followed by decomposers (including bacteria and fungi)
      • connected to a grazing food chain when consumers of a grazing food chain feed on the decomposers of the detrital food chain
      • some ecosystems, more energy may move through the detrital food web than moves through the detritus food web

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Grazing & Detrital Food Web

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Trophic Levels

  • feeding level of one or more populations in a food web
    • a food chain represents a single path sequence of organisms that form links
  • organisms of an ecosystem counted in the number of steps in a food chain away from input energy (most likely sunlight)

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Trophic Levels

  • First trophic level
    • primary producers
  • Second trophic level
    • all the primary consumers
      • herbivores & omnivores
  • Third trophic level
    • secondary consumers, etc.
      • carnivores and detritivores

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10% Energy movement

  • about 10% of the energy at a particular trophic level is incorporated into the next trophic level
    • 1,000 kg of plant material converts to 100 kg of herbivore tissue, which converts to 10 kg of first carnivores, which can support 1 kg of second level carnivores
  • rapid loss of energy is the reason food chains have from three to four links, rarely five
    • few large carnivores in ecosystems

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Ecological Pyramid

  • trophic structure of an ecosystem
  • base of the pyramid represents the producer trophic level
  • apex representing the highest consumer trophic level

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Types of Ecological Pyramids

Pyramid of Energy

Pyramid of Biomass

Pyramid of Numbers

energy content of each trophic level in a food web

number of organisms in each trophic level

weight (biomass) of organisms at each trophic level at one time

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Biogeochemical Cycles

  • pathways by which chemicals circulate through the biotic and abiotic components of an ecosystem
  • cycles are primarily gaseous cycles (carbon and nitrogen); others are sedimentary cycles, (phosphorus)
  • reservoir is that portion of Earth that acts as a storehouse for the element
  • exchange pool is the portion of the environment from which producers take chemicals, such as the atmosphere or soil
  • biotic community is the pathway through which chemicals move through food chains

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Water Cycle

  • freshwater evaporates and condenses on Earth
    • also hydrologic cycle
      • evaporation
      • condensation
      • precipitation
      • transpiration

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Carbon Cycle

  • photosynthesis removes CO2 from the atmosphere
  • respiration then returns CO2 to the atmosphere.
  • CO2 from the air combines with water to produce bicarbonate (HCO3), which is a source of carbon for aquatic producers, primarily protists.
  • the reservoir for the carbon cycle is largely composed of organic matter
    • calcium carbonate in shells
    • Limestone
    • fossil fuels
      • Burning fossil fuels increases the CO2
      • More CO2 is entering the atmosphere than being placed into reservoirs
      • CO2 is a greenhouse gas climate change due to global warming

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Nitrogen Cycle

  • atmospheric reservoir of nitrogen
    • N2 is 78% of the atmosphere
    • nitrogen deficiency can limit plant growth
  • Nitrogen fixation occurs when N2 is converted to a form that plants can use
    • nitrogen-fixing bacteria living in nodules on the roots of legumes make nitrogen compounds for plants
  • Denitrification is conversion of NO3- to nitrous oxide (N2O) and N2
  • Human activity through inorganic fertilizers upsets the natural balance in aquatic systems
    • causes algal blooms

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Phosphorus Cycle

  • weathering rock makes phosphate ions (PO4 and HPO42-) available to plants that take up phosphate from the soil
    • Some of this phosphate runs off into aquatic ecosystems where algae incorporate it into organic molecules before it is entrapped in sediments
    • Phosphate that is not taken up by algae is incorporated into sediments in the oceans.
  • phosphate taken up by producers is incorporated into a variety of organic compounds
    • animals eat producers and incorporate some of the phosphate into phospholipids, ATP, and nucleotides of DNA
    • decay of organisms and decomposition of animal wastes eventually makes phosphate ions available again
  • available phosphate is generally taken up quickly; it is usually the limiting nutrient in most ecosystems.
  • Humans impact natural ecosystems using phosphate fertilizers causing algal blooms

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