4.3 Carbon cycling Flashcards
Autotrophs absorb CO2 from the atmosphere and convert it into
organic compounds.
Reduces the concentration of CO2 in the atmosphere (approximately 0.039% or 390 micromoles/mole)
Some CO2 will directly dissolve
in water (soluble), but most will combine with water to become carbonic acid.
Carbonic acid can dissociate to
form H+ and HCO3- (bicarbonate/ hydrogen carbonate)
H+ ions explains how carbon dioxide reduces
pH of water.
Both dissolved carbon dioxide and hydrogen carbonate ions are absorbed by
aquatic plants and other autotrophs that live in water.
Photosynthesis uses CO2 keeping the
concentration of CO2 inside the leaf low,
maintains concentration gradient of CO2
CO2 from outside the leaf diffuses down the concentration gradient into
the leaf
CO2 moves through the
stomatal pores in the leaves of land plants
In many aquatic plants diffusion happens directly through the surface tissues.
CO2 is a
waste product of aerobic cell respiration
Methanogens
are archaean microorganisms that produce methane as a metabolic byproduct in anaerobic respiration (methane is produced from carbon dioxide)
Methanogens are found in a variety of anaerobic environments:
Wetlands (paddies, swamps and mangroves)
Digestive tracts of animals (cows, humans, termites)
Marine & freshwater sediments (mud in lakebeds)
Landfill sites (in which organic matter has been buried)
Measurements indicate that the levels of atmospheric methane are
increasing
It is estimated that, on average, methane persists in the atmosphere for
12 years (naturally oxidized in the stratosphere)
The most important process of methane removal is
oxidation by hydroxyl radicals.
methane + hydroxyl radical → carbon dioxide + water
Partially decomposed organic matter can be compressed to form
brown soil-like peat