Pre_GI: SWBIT SVG BLASTN

Query: NC_003030:303812 Clostridium acetobutylicum ATCC 824, complete genome

Lineage: Clostridium acetobutylicum; Clostridium; Clostridiaceae; Clostridiales; Firmicutes; Bacteria

General Information: This strain was isolated in 1924 from garden soil in Connecticut, USA, by E. Wyer and L. Rettger. It is one of the best studied solventogenic clostridia. Solvent-producing bacterium. This genus comprises about 150 metabolically diverse species of anaerobes that are ubiquitous in virtually all anoxic habitats where organic compounds are present, including soils, aquatic sediments and the intestinal tracts of animals and humans. This shape is attributed to the presence of endospores that develop under conditions unfavorable for vegetative growth and distend single cells terminally or sub-terminally. Spores germinate under conditions favorable for vegetative growth, such as anaerobiosis and presence of organic substrates. It is believed that present day Mollicutes (Eubacteria) have evolved regressively (i.e., by genome reduction) from gram-positive clostridia-like ancestors with a low GC content in DNA. This organism is a benign saccharolytic and proteolytic soil bacterium capable of producing a number of organic solvents (solventogenic bacterium) through fermentation of various organic compounds. acetobutyricum were isolated by Chaim Weizman during the World War I and used to develop industrial starch-based acetone, butanol and ethanol fermentation processes.

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BLASTN Alignment.txt

Subject: NC_010003:2029416 Petrotoga mobilis SJ95, complete genome

Lineage: Petrotoga mobilis; Petrotoga; Thermotogaceae; Thermotogales; Thermotogae; Bacteria

General Information: Petrotoga mobilis SJ95 (DSM 10674) is an anaerobic thermophile, isolated from the production waters of a North Sea oil reservoir. This organism, a member of the Thermotogales, has the characteristic morphology of one or more cells contained in a sheath-like envelope which extends beyond the cell wall. Petroleum reservoirs are a unique subsurface environment characterized by high temperatures, moderate to high salt concentrations, and abundant organic matter.