Ecosystem Ecology Chapter 3.

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Presentation transcript:

Ecosystem Ecology Chapter 3

You should know: Ecosystem Biotic/abiotic Producer/autotroph Consumer/heterotroph Photosynthesis/cellular respiration Trophic levels Primary consumer/secondary consumer/tertiary consumer Food chain/food web Herbivore/carnivore/omnivore Scavenger/detritivore/decomposer

Energy flow in ecosystems ONE WAY! Laws of thermodynamics always apply: Energy cannot be created or destroyed, only converted from 1 form to another Whenever energy is converted from 1 form to another, some of the energy is lost as heat Simplified version: food chain Detailed version: food web Energy input  autotroph  heterotroph Note that the  shows the direction of energy flow

Ecological pyramids Used to compare trophic levels Types: Pyramid of numbers Pyramid of biomass Pyramid of energy

Ecosystem productivity GPP = gross (total) energy captured during photosynthesis Plants use some of this energy during cellular respiration NPP = net (remaining) energy NPP = GPP – plant respiration

Productivity… Influenced by lots of factors: See table 3.8 p. 64 Type of plants Available solar radiation, nutrients, water Maturity of the community Human impacts See table 3.8 p. 64

Bioaccumulation As substances move through a food chain, some are not passed on These substances can be stored in the bodies of organisms in the food chain – bioaccumulation Fat-soluble toxins tend to build up in higher levels of a food chain – biological magnification Example – DDT pesticide and Bald Eagle

Biogeochemical cycles Not one way! Earth is a closed system – matter cannot escape Law of conservation of matter: Matter cannot be created or destroyed, it can only be changed from one form to another.

Water (hydrologic) cycle Necessary for life: Provides a medium for chemical reactions, transports material throughout bodies, and moderates temperatures Important processes: Precipitation Evaporation, transpiration Runoff

Carbon cycle C is in organic compounds: proteins, nucleic acids, lipids, carbohydrates CO2 is stored in the atmosphere (and in some rocks) Important processes: Photosynthesis Respiration, decomposition, combustion Human impact on carbon cycle – increased combustion has increased amount of CO2 in atmosphere

Nitrogen cycle N is found in proteins, nucleic acids, and chlorophyll 78% of atmosphere is N, but this is not in a form that can be absorbed by living things Nitrogen fixation – converts atmospheric N into nitrates and nitrites - forms that can be used by plants: combustion, volcanic action, lightning, and nitrogen-fixing bacteria Nitrogen-fixing bacteria – live in nodules on the roots of plants called legumes Nitrogen is returned to the atmosphere during decomposition

Phosphorus cycle P is found in nucleic acids, ATP and phospholipids found in cell membranes P is not found as a gas in the atmosphere It cycles from the soil, into the food chain and back Phosphorus is a limiting factor in many aquatic ecosystems Sudden input into an ecosystem can cause rapid growth of algae – algal bloom When algae begins to die and decompose, the oxygen in the system is consumed, resulting in hypoxic conditions