An ecosystem consists of all the organisms living in matter an area, aswell as the abiotic factors with which they interact.
The arctic fox was introduced on subarctic islands around 1900 to establish populations for the fur trade
surprising outcome: the conversion of grassland to tundra in many places on the island
Arctic terns, a prey source for the foxes, and major guano generators that provide nutrients for grasslands
Ecosystem dynamics involve two main processes: energy flow and chemical cycling.
Energy flows through ecosystems, while chemicals cycle within ecosystems.
Ecologists study the transformations of energy and matter in an ecosystem and map the movements of chemical elements.
The first law of thermodynamics states that energy cannot be created or destroyed, only transferred or transformed.
Energy enters an ecosystem as solar radiation, is conserved, and is lost from organisms as heat.
The second law of thermodynamics states that every exchange of energy increases the entropy of the universe.
In an ecosystem, energy conversions are not completely efficient; some energy is always lost as heat.
The law of conservation of mass states that matter cannot be created or destroyed.
Chemical elements are continually recycled within ecosystems.
Ecosystems are open systems, absorbing energy and mass and releasing heat and waste products.
Energy and nutrients pass from primary producers (autotrophs) to primary consumers (herbivores) to secondary consumers (carnivores) to tertiary consumers (carnivores that feed on other carnivores).
Detritivores, or decomposers, are heterotrophs that derive their energy from detritus, nonliving organic matter.
Prokaryotes and fungi are the main decomposers in ecosystems.
In most ecosystems, primary production is the amount of light energy converted to chemical energy by autotrophs during a given time period.
The amount of solar radiation reaching Earth’s surface limits the photosynthetic output of ecosystems.
Only a small fraction of solar energy actually strikes photosynthetic organisms, and even less is of a usable wavelength. Only about 1% of light striking photosynthetic organisms is converted to chemical energy.
Total primary production is known as the ecosystems gross primary production (GPP).
GPP is measured as the conversion of energy from light (or chemicals) to the chemical energy of organic molecules per unit time.
Net primary production (NPP) is GPP minus energy used by autotrophs for respiration (Ra).
NPP equation
aerobic cellular respiration equation
photosynthesis equation
NPP is the amount of new biomass added in a given time period, not the total biomass of autotrophs.
Satellite data indicate that ecosystems vary greatly in their NPP and contribution to the total NPP on Earth.
Net ecosystem production (NEP) is a measure of the total biomass accumulation during a given period.
NEP is gross primary production minus the total respiration of all organisms (RT) in an ecosystem.
NEP equation
NEP is estimated by comparing CO2 and O2 entering or leaving an ecosystem. If more CO2 enters than leaves, the system is storing carbon.
In marine and freshwater ecosystems, both light and nutrients control primary production.
Depth of light penetration affects primary production in the photic zone of an ocean or lake.
More than light, nutrients limit primary production in most oceans and lakes.
Nitrogen and phosphorous are the nutrients that most often limit marine production.
In lakes, phosphorus limits cyanobacterial growth more often thannitrogen. This has led to the use of phosphate-free detergents.
In terrestrial ecosystems, temperature and moisture affect primary production on a large scale.
NPP increases with precipitation.
Increasing temperature and solar energy also increase NPP.
Soil nutrients can limit primary production in terrestrial ecosystems.