Prokaryote, relatively simple unicellular
organism, such as a bacterium, characterized by the absence of a nucleus and
other specialized cell structures. Scientists distinguish prokaryotes from
eukaryotes, which are more complex organisms with cells that contain a nucleus,
such as plants and animals.
Structure
of prokaryotes
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Reproduction
of Prokaryotes
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Nutrition
Like most organisms, prokaryotes
require carbon and energy to create nutrients such as carbohydrates, proteins,
lipids, and nucleic acids. Prokaryotes obtain carbon and energy from a variety
of sources. Certain prokaryotes use carbon dioxide as their carbon source.
Called autotrophs, these prokaryotes derive energy from different sources, such
as photosynthesis or inorganic molecules.
Photoautotrophs, including the
cyanobacteria and the green sulfur and purple sulfur archaebacteria, derive
their energy from light. Chemoautotrophs, such as the soil bacteria Nitrobacter
and Nitrosomonas, derive their energy from inorganic compounds such as
hydrogen sulfide, ammonia, and iron. Heterotrophs are organisms that rely on
ready-made organic compounds such as glucose or alcohol for their carbon
source. Heterotrophs obtain energy by degrading organic molecules, such as
plant or animal matter. A small group of bacteria, the photoheterotrophs, use
light as their energy source, while chemo heterotrophs use organic compounds
for both their carbon and energy sources.
Importance of Prokaryotes
Prokaryotes play significant
roles in our daily lives. In a process called nitrogen fixation, many species
of cyanobacteria convert atmospheric nitrogen to nitrogenous compounds that
other organisms use as food sources. Moreover, the photosynthesis occurring in
cyanobacteria still contributes substantial amounts of oxygen to the atmosphere
and stores the Sun’s energy in carbohydrate molecules. Cyanobacteria are the
foundation for aquatic ecosystems, providing food for protozoa and other
aquatic organisms. Cyanobacteria are threatened, however, by ultraviolet
radiation, which penetrates the atmosphere as a result of the thinning ozone
layer.
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