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Chapter 54
Ecosystems
Ecosystems
Ecosystem - consists of all the organisms living in a community as well as all the abiotic factors with which they interact.
Trophic structure - all the feeding relationships within an ecosystem.
Trophic levels - divides the species of an ecosystem by what their main source of nutrition is.
Trophic Relationships in Ecosystems Primary Producers - 1st trophic level
consisting of autotrophs; “the base” (photosynthesize)
Primary Consumers - herbivores Secondary Consumers - carnivores that
eat herbivores Tertiary Consumers - carnivores that eat
other carnivores
Trophic Relationships in Ecosystems (con’t) Quarternary Consumers - high order
carnivores that consume larger carnivores
Detritovores - derive energy by consuming dead organic material such as leaves, feces, and dead organisms from all trophic levels.
Food Chains and Food Webs
Food Chain - pathway by which food energy is passed from trophic level to trophic level– Example
• dandelion - grasshopper - mouse - snake - hawk (terrestrial)
• phytoplankton - zooplankton - small fish - medium sized fish - large fish (marine)
Food Webs - elaborate feeding relationships between all trophic levels
Food Chains and Food Webs (con’t)
Ecosystem Processes
Production - rate of incorporation of energy and materials into bodies of organisms
Consumption - metabolic use for growth and reproduction of assimilated organic materials
Decomposition - breakdown of organic material into inorganic material– bacteria, fungi, and some animals
– links all trophic levels recycling nutrients back into the abiotic environment
Energy Flow in Ecosystems
An ecosystem’s energy budget depends on the amount of primary productivity.– the amount of light energy converted to
chemical energy (organic compounds) Biomass - term used to describe primary
productivity– the amount of new vegetation added to the
ecosystem in terms of dry weight per unit time
Productivity of Different Ecosystems
Energy Flow through Ecosystems
Most of the energy is lost as it flows through each trophic level due to heat.– metabolic rate of the organism
Secondary Productivity - rate at which consumers convert chemical energy into their own new biomass.– Herbivores can only eat a fraction of the plant
biomass produced, and can only digest a fraction of what they eat.
Energy Partitioning in a Caterpillar
lost as heat
converted to biomass
recycled by detritovores
Energy Flow through Ecosystems (con’t) Ecological efficiency - percentage of energy
transferred from one trophic level to the next (~10% is transferred)
Pyramid of Productivity - food chain is diagrammatically represented using blocks where the primary producers form the base
Biomass pyramid - representation of the standing crop biomass in a trophic level
Pyramid of Net Productivity
Primary Producers only convert ~1% of light energy into biomass.
Consumers convert ~10% of chemical energy into biomass.
Biomass Pyramid
Biogeochemical Cycles
Water cycle Carbon cycle Nitrogen cycle Phosphorus cycle
Biological Magnification
Biological magnification - concentration of toxins at successive trophic levels– top-level carnivores tend to be the
organisms most severely affected . These toxins, such as DDT and PCBs,
are pesticides that may accumulate in tissues after ingestion. (fat tissue)
Biological Magnification of DDT in a Food Chain
Food Chain Concentration of DDT in A Long Island Marsh sprayed for Mosquito Control 1967
ppm
Water .00005
Plankton .04
Silverside Minnow .23
Sheephead Minnow .94
Pickerel 1.23
Needlefish 2.07
Heron 3.57
Tern 3.91
Osprey 13.8
Merganser 22.8
Cormorant 26.4
Human Impact-Ozone Depletion Ozone (O3) - bottom layer of the stratosphere that
protects Earth from UV radiation. Depletion since 1975 is due to CFC’s,
chlorflourocarbons, chemicals used in refrigerators, aerosol, and styrofoam.
Chlorine reacts with the O3 molecules reducing them to O2 molecules
Reactions allow the chlorine to dissociate from the O2 molecules allowing the chlorine to react with more ozone.
Human Impact-Ozone Depletion (con’t)
Ozone is constantly produced and destroyed, however, atoms, such as Cl & Br, siphon ozone away faster than
it is being produced.
Ozone Depletion - Antarctica