The initial source of energy for almost all communities is sunlight
Light is absorbed and converted into usable chemical energy (ATP) via the process of photosynthesis
This energy is used to make organic compounds (e.g. glucose) from inorganic molecules (CO2 and H2O)
The organic compounds can be used as building blocks to create a range of macromolecules needed by the cells and tissues
All green plants are photosynthetic, along with certain algae (e.g. seaweeds) and prokaryotes (e.g. cyanobacteria)
Photosynthesis Equation
Some communities can derive energy from oxidation reactions involving inorganic compounds
These inorganic sources may include ammonia, hydrogen gas, hydrogen sulfide or iron oxide
Such communities may be located near deep sea hydrothermal vents or in underground caves where no light can penetrate
The specific chemical processes deployed by these organisms may vary depending on the inorganic chemical used as an energy source
Iron-oxidising bacteria found in the soil are an example of a chemoautotroph – they use the electrons from iron (oxidation) to produce ATP
Chemosynthesis Example
Organisms undertake cell respiration to release the chemical energy stored in organic compounds
Carbohydrates (glucose) serve as the primary fuel source, but other compounds (lipids, proteins) may be used
The organic compounds can either be produced by the organism itself (autotrophy) or obtained from other organisms (heterotrophy)
Cell respiration can occur anaerobically (no oxygen = low ATP yield) or aerobically (oxygen = high ATP yield)
The release of energy involves oxidation reactions (high energy electrons are used in the production of ATP)
Cell Respiration Equation