Energy Flow Through Ecosystems
Ecosystem: the sum of all the organisms living in a given area and the abiotic factors they interact with
Biotic factors: living, or once living, components of an environment
Abiotic factors: nonliving (physical and chemical properties of the environment)
1st law of thermodynamics: energy can neither be created nor destroyed, only transferred
Law of conservation of mass: chemical elements are continually recycled in the environment
2nd law of thermodynamics: exchanges of energy increase the entropy of the universe
A net gain in energy results in energy storage or growth of an organism
A net loss of energy results in loss of mass and eventual death of an organism
Organisms use different strategies to regulate body temperature
Endotherms: use thermal energy from metabolism to maintain body temperatures
Ectotherms: use external sources (ie sun/shade or other organisms) to regulate their body temperature
Metabolic rate: the total amount of energy an animal uses in a unit of time
Can be measured in calories, heat loss, or by the amount of oxygen consumed (or CO2 produced)
Oxygen is used in cellular respiration and CO2 is produced as a by-product
An animal’s metabolic rate is related to its body mass
Smaller organisms = higher metabolic rate
Larger organisms = lower metabolic rate
Semelparity
Big-bang reproduction
Many offspring produced at once
Individual often dies afterwards
Less stable environments
Iteroparity
Repeated reproduction
Few, but large offspring
More stable environments
Species can be grouped into trophic levels based upon their mains source of nutrition and energy
Unlike mass, energy CANNOT be recycled
The sun constantly supplies energy to ecosystems
Primary producers (autotrophs): use light energy to synthesize organic compounds
Plants, algae, photosynthetic plankton
Some organisms are chemosynthetic (vs photosynthetic) meaning they produce food using the energy created by chemical reactions
Ie some bacteria and archaea organisms
Heterotrophs: rely on autotrophs because they cannot make their own food
Primary consumers: herbivores
Secondary consumers: carnivores that eat herbivores
Tertiary consumers: carnivores that eat other carnivores
Decomposers: get energy from detritus (nonliving organic material; leaves, wood, dead organisms)
Include fungi and many prokaryotes
Important for recycling chemical elements
The trophic structures of a community are determined by the feeding relationships between organisms
Food chain: the transfer of food energy up the trophic levels
Food webs: linked food chains
Any changes to the availability of energy can disrupt ecosystems
For example:
If energy resources change, so can the number and size of trophic levels (Increase energy, increase trophic levels/size; decrease energy, decrease trophic levels/size)
A change at the producer level can affect the number and size of the remaining trophic levels
Primary production: the amount of light energy that is converted to chemical energy
Primary producers set a “spending limit” for the entire ecosystems energy budget
Gross primary production (GPP): total primary production in an ecosystem
Net primary production (NPP): the GPP minus the energy used by the primary producers for respiration (Ra)
Satellite images show that different ecosystems have varying NPP
Secondary production: the amount of chemical energy in a consumer’s food that is converted to new biomass
The transfer of energy between trophic levels is at around 10% efficiency
Biomass: the total weight of dry matter (dry weight) present in the ecosystem at any one time; the total mass of organisms at a trophic level.
With less energy at higher trophic levels, there are usually fewer organisms as well.
Organisms tend to be larger in size at higher trophic levels, but their smaller numbers result in less biomass.
Unlike energy, matter cycles through ecosystems
Matter is found in limited amounts, unlike solar energy
Biogeochemical cycles: nutrient cycles that contain both biotic and abiotic factors
Water, carbon, nitrogen, and phosphorus cycle
Biological importance of the water cycle: water is essential for all life and influences the rate of ecosystem processes
Biological importance of the carbon cycle: carbon is essential for life and required in the formation of organic compounds
Biological importance of the nitrogen cycle: nitrogen is important for the formation of amino acids, proteins, and nucleic acids
Biological importance of the phosphorous cycle: phosphorus is important for the formation of nucleic acids, phospholipids, and ATP (energy)
Ecosystem: the sum of all the organisms living in a given area and the abiotic factors they interact with
Biotic factors: living, or once living, components of an environment
Abiotic factors: nonliving (physical and chemical properties of the environment)
1st law of thermodynamics: energy can neither be created nor destroyed, only transferred
Law of conservation of mass: chemical elements are continually recycled in the environment
2nd law of thermodynamics: exchanges of energy increase the entropy of the universe
A net gain in energy results in energy storage or growth of an organism
A net loss of energy results in loss of mass and eventual death of an organism
Organisms use different strategies to regulate body temperature
Endotherms: use thermal energy from metabolism to maintain body temperatures
Ectotherms: use external sources (ie sun/shade or other organisms) to regulate their body temperature
Metabolic rate: the total amount of energy an animal uses in a unit of time
Can be measured in calories, heat loss, or by the amount of oxygen consumed (or CO2 produced)
Oxygen is used in cellular respiration and CO2 is produced as a by-product
An animal’s metabolic rate is related to its body mass
Smaller organisms = higher metabolic rate
Larger organisms = lower metabolic rate
Semelparity
Big-bang reproduction
Many offspring produced at once
Individual often dies afterwards
Less stable environments
Iteroparity
Repeated reproduction
Few, but large offspring
More stable environments
Species can be grouped into trophic levels based upon their mains source of nutrition and energy
Unlike mass, energy CANNOT be recycled
The sun constantly supplies energy to ecosystems
Primary producers (autotrophs): use light energy to synthesize organic compounds
Plants, algae, photosynthetic plankton
Some organisms are chemosynthetic (vs photosynthetic) meaning they produce food using the energy created by chemical reactions
Ie some bacteria and archaea organisms
Heterotrophs: rely on autotrophs because they cannot make their own food
Primary consumers: herbivores
Secondary consumers: carnivores that eat herbivores
Tertiary consumers: carnivores that eat other carnivores
Decomposers: get energy from detritus (nonliving organic material; leaves, wood, dead organisms)
Include fungi and many prokaryotes
Important for recycling chemical elements
The trophic structures of a community are determined by the feeding relationships between organisms
Food chain: the transfer of food energy up the trophic levels
Food webs: linked food chains
Any changes to the availability of energy can disrupt ecosystems
For example:
If energy resources change, so can the number and size of trophic levels (Increase energy, increase trophic levels/size; decrease energy, decrease trophic levels/size)
A change at the producer level can affect the number and size of the remaining trophic levels
Primary production: the amount of light energy that is converted to chemical energy
Primary producers set a “spending limit” for the entire ecosystems energy budget
Gross primary production (GPP): total primary production in an ecosystem
Net primary production (NPP): the GPP minus the energy used by the primary producers for respiration (Ra)
Satellite images show that different ecosystems have varying NPP
Secondary production: the amount of chemical energy in a consumer’s food that is converted to new biomass
The transfer of energy between trophic levels is at around 10% efficiency
Biomass: the total weight of dry matter (dry weight) present in the ecosystem at any one time; the total mass of organisms at a trophic level.
With less energy at higher trophic levels, there are usually fewer organisms as well.
Organisms tend to be larger in size at higher trophic levels, but their smaller numbers result in less biomass.
Unlike energy, matter cycles through ecosystems
Matter is found in limited amounts, unlike solar energy
Biogeochemical cycles: nutrient cycles that contain both biotic and abiotic factors
Water, carbon, nitrogen, and phosphorus cycle
Biological importance of the water cycle: water is essential for all life and influences the rate of ecosystem processes
Biological importance of the carbon cycle: carbon is essential for life and required in the formation of organic compounds
Biological importance of the nitrogen cycle: nitrogen is important for the formation of amino acids, proteins, and nucleic acids
Biological importance of the phosphorous cycle: phosphorus is important for the formation of nucleic acids, phospholipids, and ATP (energy)