Saccharomyces cerevisiae mating type a cells enlarged and elongated when exposed to a-factor, a sex pheromone produced by mating-type a cells. This morphogenesis required exogenous 1)-glucose, nitrogen, and phosphate, and cells in exponential phase responded better than stationary-phase cells. Morphogenesis was blocked by cycloheximide and by inhibitors of cell wall biosynthesis such as 2-deoxy-D>glucose, 2-deoxy-2-fluoro-D>glucose, and 2-deoxy-2-fluoro-D-mannose, but not by polyoxin D. One to two hours after addition of pheromone, a cells became more susceptible to lysis by glucanases, a change that was dependent on the dose of a-factor and was blocked by drugs that block morphogenesis. On the other hand, treatment with a-factor did not increase susceptibility to attack by trypsin, subtilisin, or exoa-mannanase. Radioactive label, incorporated into cell wall polysaccharides during treatment with a-factor, was not secreted into the medium during morphogenesis. Analysis of the labeled wall polymers showed that a-factor-treated cells contain more glucan and less mannan than control cells, and that the mannan of treated cells contains an increased proportion of shorter side chains and unsubstituted backbone mannose units. Thin-section electron microscopy oftreated cells revealed that the cell wall possesses a diffuse outer layer in the extension and is thinner at the tip.

We report the detection of living colonies of nano-organisms (nanobes) on Triassic and Jurassic sandstones and other substrates. Nanobes have cellular structures that are strikingly similar in morphology to Actinomycetes and fungi (spores, filaments, and fruiting bodies) with the exception that they are up to 10 times smaller in diameter (20 nm to 1.0 m). Nanobes are noncrystalline structures that are composed of C, O, and N. Ultra thin sections of nanobes show the existence of an outer layer or membrane that may represent a cell wall. This outer layer surrounds an electron dense region interpreted to be the cytoplasm and a less electron dense central region that may represent a nuclear area. Nanobes show a positive reaction to three DNA stains, [4Ј,6-diamidino-2 phenylindole (DAPI), Acridine Orange, and Feulgen], which strongly suggests that nanobes contain DNA. Nanobes are communicable and grow in aerobic conditions at atmospheric pressure and ambient temperatures. While morphologically distinct, nanobes are in the same size range as the controversial fossil nannobacteria described by others in various rock types and in the Martian meteorite ALH84001.

SummaryA variety of adhesive support-®lms were tested for their ability to adhere various biological specimens for transmission electron microscopy. Support ®lms primed with 3-amino-propyl triethoxy silane (APTES), poly-L-lysine, carbon and ultraviolet-B (UV-B)-irradiated carbon were tested for their ability to adhere a variety of biological specimens including axenic cultures of Bacillus subtilis and Escherichia coli and wild-type magnetotactic bacteria. The effects of UV-B irradiation on the support ®lm in the presence of air and electrostatic charge on primer deposition were tested and the stability of adhered specimens on various surfaces was also compared. APTES-primed UV-Birradiated Pioloform TM was consistently the best adhesive, especially for large cells, and when adhered specimens were UV-B irradiated they became remarkably stable under an electron beam. This assisted the acquisition of in situ phase-contrast lattice images from a variety of biominerals in magnetotactic bacteria, in particular metastable greigite magnetosomes. Washing tests indicated that specimens adhering to APTES-primed UV-B-irradiated Pioloform TM were covalently coupled. The electron beam stability was hypothesised to be the result of mechanical strengthening of the specimen and support ®lm and the reduced electrical resistance in the specimen and support ®lm due to their polymerization and covalent coupling.

SummaryWe report biogenic magnetite whiskers, with axial ratios of 6 : 1, elongated in the [1 1 1], [1 1 2] and [1 0 0] directions, resembling the magnetite whiskers detected in the Martian meteorite ALH84001 by Bradley et al., and interpreted by those authors as evidence of vapour-phase (abiogenic) growth. Magnetosomal whiskers with extended defects consistent with screw dislocations and magnetosomes resembling flattened twinned platelets, as well as other twinning phenomena and other structural defects, are also reported here. Magnetosomes with teardrop-shaped, cuboidal, irregular and jagged structures similar to those detected in ALH84001 by McKay et al., coprecipitation of magnetite possibly with amorphous calcium carbonate, coprecipitation of magnetite possibly with amorphous silica, the incorporation of titanium in volutin inclusions and disoriented arrays of magnetosomes are also described. These observations demonstrate that the structures of the magnetite particles in ALH84001, their spatial arrangement and coprecipitation with carbonates and proximity to silicates are consistent with being biogenic. Electron-beam-induced flash-melting of magnetosomes produced numerous screw dislocations in the {1 1 1}, {1 0 0} and {1 1 0} lattice planes and induced fusion of platelets. From this, the lack of screw dislocations reported in the magnetite particles in ALH84001 (McKay et al., and Bradley et al.) indicates that they have a low-temperature origin.