Carbon Cycle Flashcards
Carbon’s Importance
an essential element of life
- part of organic molecules of living organisms
– makes up 20% of total body weight
- basis of long chains of organic molecules that form membranes and walls of cells, constitute backbone of proteins, fats, carbohydrates & store energy for later use
Carbon cycle
- movement of carbon from nonliving environment into living things & back (movement of carbon around the biosphere).
Carbon Sinks (contain large quantities of matter)
atmosphere - carbon dioxide ocean - carbonate & bicarbonate rocks - coal & limestone oil & natural gas peat
Flow Definition
- Processes that move matter between pools are known as flows.
Fast components of the Carbon Cycle
- Involves processes that are associated with living organisms - biotic components
Slow components of the Carbon Cycle
- involves carbon that is held in rocks, in soils, or as petroleum hydrocarbons (fossil fuels) – can be stored for millions of years - abiotic components
Photosynthesis (by autotrophs)
Plants take in CO2 & incorporates carbon into their tissues
CO2 is converted into sugars
Producers convert CO2 in the atmosphere into carbohydrates during photosynthesis
Respiration
- Returns CO2
- Sugars converted back into CO2
- Consumers obtain carbon from carbohydrates in the producers they eat
- During cellular respiration, some carbon is released back into the atmosphere as CO2 (fluxes)* this is measurable
Respiration - Decomposition
- When organisms die, carbon that was part of the live biomass pool becomes part of the dead biomass pool
decomposers break down dead matter which returns CO2 to water or air via respiration - Carbon stored in bodies of organisms as fat, oils, or other molecules, may be released into soil or air when organisms dies
Exchange
- CO2 in atmosphere & CO2 dissolved in water are constantly exchanged
- Basically an equal exchange of carbon
Sedimentation
- Slow
_ Calcium carbonate precipitates out of water as sediments, when dissolved, CO2 combines with calcium ions in water it becomes calcium carbonate
largest carbon pool in slow part of carbon cycle - Some carbon is stored in limestone, forming one of the largest “carbon sinks” on Earth.
Burial or fossil fuel pools
Some carbon can be buried
Small fraction of organic carbon in dead biomass pool is buried & incorporated into ocean sediments before it can decompose into its constituent elements
Extraction
- Human extraction of fossil fuels brings carbon to Earth’s surface, where it can be combusted
- These molecules may form deposits of coal, oil, or natural gas, which are known as fossil fuels
- Fossil fuels store carbon left over from bodies of organisms that died millions of years ago
Combustion
- fossil fuels & plant matter are converted into CO2
by humans & natural combustion by fires or volcanoes - release carbon into atmosphere as CO2 or into soils as ash
Human Effect - Combustion
- The best-known & most significant human alteration of the carbon cycle is the combustion of fossil fuels
- The excess CO2 in atmosphere acts to increase the retention of heat energy in the biosphere
results in global warming - an increase in temperature of Earth