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[Prev] | [Next]DNA-dependent RNA polymerases in bacteria and archaea are different from each other. The primary RNA polymerase of all organisms is responsible for creating messenger RNA that is then translated into proteins at the ribosome. Bacterial RNA polymerase is relatively simple, containing 4 different proteins. In contrast, RNA polymerase from methanogens and halophiles (both Archaea) contains 8 proteins. In hyperthermophiles (Archaea) RNA polymerase is even more complex, containing 10 proteins. None of the archaeal RNA polymerases are affected by the antibiotic rifampicin, a known inhibitor of the bacterial RNA polymerase. The eukaryotic RNA polymerase responsible for most mRNA transcription (termed RNA polymerase II) contains 12 proteins and is similar to the RNA polymerase in the archaea.
RNA polymerases from all organisms recognize a variety of start sequences or promoters. A promoter for mRNA transcription in bacteria is recognized by the (sigma) protein and has two recognition zones about 10 and 35 bases before the transcription start site. The exact sequence recognized by RNA polymerase depends upon the σ factor that has bound to the enzyme, and cells have different numbers of σ factors that bind to different types of promoter sequences. This allows regulation of mRNA expression by changing the levels of σ factors inside the cell. In archaea and eukaryotes the transcription recognition sequence is a TATA sequence (termed the TATA box) and transcription is regulated by various protein transcription factors that bind to regions near the TATA box and then recruit RNA polymerase.

The best-studied bacteria have promoters at two positions upstream of the transcription start site that are recognized by the σ factors associated with RNA polymerase. The transcriptional control elements in the archaea are much more like those found in eukaryotes, where RNA polymerase is recruited to a promoter by interaction with protein regulatory factors, and transcription begins downstream of a TATA box.
The structural make-up of the ribosomes of bacteria and archaea are similar in many respects. The ribosomes of archaea and bacteria are of the same size (70S) and are smaller than those of eukaryotes (80S). However, most of the ribosomal proteins, translation factors and tRNAs of archaea more closely resemble their counterparts in eukaryotes. In fact, mixing experiments with ribosomes from E. coli (Bacteria), Sulfolobus (Archaea) and yeast (Eukarya) have shown functional substitution between Archaea and Eukarya. Specifically, when the small subunit from a yeast ribosome was mixed with the large subunit from Sulfolobus, the hybrid ribosome was capable of translation in vitro. When the small subunit from yeast was mixed with the large subunit of E. coli, translation did not occur. Also, in all organisms translation begins at a start codon (typically an AUG in the mRNA). In bacteria, this codon causes the insertion of formylmethionine, while in archaea and eukaryotes, it results in insertion of an unmodified methionine.
Archaeal membranes have features unlike those found in either eukaryotes or bacteria. The lipids in archaea have a different chemical make-up in the following way. Remember that lipids in bacteria are amphipathic molecules (i.e. having both hydrophobic and hydrophilic portions) containing a backbone of glycerol connected to a hydrophilic head group and two hydrophobic long-chain fatty acids. In eukaryotes and bacteria the fatty acids are attached to the glycerol backbone by ester bonds, while in archaea ether linkages are used. Also, the stereochemistry of lipids from archaea is primarily of the S form, while that of bacteria and eukaryotes is of the R form. In some archaea the hydrophobic chains attached to the glycerol backbone are twice normal length and pass completely through the membrane, attaching to a second backbone on the opposite side. This adds extra stability to the membrane and these dual lipids are often found in archaea living in extreme environments.

Archaea have an ether linkage between their fatty acids and the glycerol backbone, which is in contrast to the ester linkage seen in bacteria and eukaryotes. (A) An ether-linked lipid show as the chemical structure and a space-filling model. (B) A tetraether lipid, showing a general chemical structure. An example of a tetraether lipid from the thermophilic archaeal species Thermoplasma acidophilium is shown as a space-filling model.
As we have discussed, almost all bacteria have cell walls. These walls contain peptidoglycan, with N-acetyl muramic acid being the signature molecule for the presence of peptidoglycan. Archaea are considerably more diverse in the composition of their cell walls. They lack peptidoglycan, but some contain pseudomurein that has a similar structure as shown in Figure 2-54. N-acetylalosaminuronic acid replaces N-acetylmuramic acid in the backbone of the molecule and each glycan unit is linked together using 1,3 glycosidic bonds, instead of the 1,4 glycosidic bonds seen in peptidoglycan. Many archaea do not contain a peptidoglycan molecule in any form, instead covering the outside of the membrane with proteins, glycoproteins or polysaccharides. Scientists refer to these cell walls as S-layers. In any case the function of the cell wall remains the same, containing the cytoplasm and giving the microbe its shape.

Archaea have several different types of cell wall. Some contain a structure reminiscent of peptidoglycan called pseudomurein. The chemical formula is pictured on the left. Other microbes will have a surface layer (S-layer) composed of repeating units of one or a few proteins, glycoproteins or sugar. These crystal lattices serve to protect the cell. The micrograph on the right shows the surface of Methanospirillum hungatei cells. Note the regular repetition of the pattern on the outside surface. (Source: M. Firtel, et al. 1993. J. Bacteriol. 175:7550-7560)
These various differences between archaea, bacteria and eukaryotes indicate major differences between these life forms, and phylogenetic analysis bears out this conclusion. It is clear that the archaea are more divergent from bacteria than we are from an amoeba. This in turn indicates that the common progenitor of these groups existed very early in evolution. Analysis and classification of the archaea has fundamentally changed how biologists think about organismal diversity.
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