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R P Blakemore

Publications and source records attributed to R P Blakemore.

14 recordsLinked to original sources
PubMed1991

Electroporation and conjugal plasmid transfer to members of the genus Aquaspirillum.

Electroporation methods and conjugal matings were used to transfer several plasmid vectors to Aquaspirillum dispar and Aquaspirillum itersonii. The incompatibility P class plasmid RP4 was conjugally transferred from Escherichia coli HB101 to these spirilla, and the transconjugants subsequently donated the molecule to plasmid-free E. coli and A. dispar strains via conjugal matings. High-voltage electrotransformation was used to transfer plasmids pUCD2, pSa151 and RP4 to A. dispar and A. itersonii, at efficiencies as high as 3 x 10(4) transformants per micrograms plasmid DNA. RP4 DNA isolated from spirillum hosts, but not RP4 from E. coli cells was successfully transferred to A. dispar and A. itersonii by electrotransformation, suggesting that modification and/or restriction activity may be present in these Aquaspirillum species.

Bacteria↗
PubMed1991

Phylogenetic analysis of Aquaspirillum magnetotacticum using polymerase chain reaction-amplified 16S rRNA-specific DNA.

The 16S rRNA gene of the magnetotactic magnetogen Aquaspirillum magnetotacticum MS1 was amplified by a polymerase chain reaction, using two eubacterial consensus oligodeoxynucleotide primers flanking the majority of the 16S rRNA gene, cloned, and sequenced. Phylogenetic analysis revealed that A. magnetotacticum MS1 belongs to the alpha-group of proteobacteria. This assignment offers perspective on the biochemical properties of A. magnetotacticum, since this organism is expected to have the general properties that are common to this phylogenetic group.

Base Sequence↗
PubMed1989

Magnetite and magnetotaxis in microorganisms.

Magnetotactic bacteria from freshwater and marine sediments orient and navigate along geomagnetic field lines. Their magnetotactic response is based on intracellular, single magnetic domains of ferrimagnetic magnetite, which impart a permanent magnetic dipole moment to the cell.

Animals↗
PubMed1989

Periplasmic superoxide dismutases in Aquaspirillum magnetotacticum.

Aquaspirillum magnetotacticum MS-1 cells cultured microaerobically (dissolved O2 tension 1% of saturation), expressed proteins with superoxide dismutase (SOD) activity. The majority (roughly 95%) of total cell superoxide dismutase activity was located in the cell periplasm with little or no activity in the cell cytoplasm. Iron-type SOD (FeSOD) contributed 88% of the total activity activity detected, although a manganese-type SOD (MnSOD) was present in the periplasm as well. Cells cultured at a higher dissolved O2 tension (10% of saturation) expressed increased activity of the MnSOD relative to that of the FeSOD.

Catalase↗
PubMed1988

Characterization of the bacterial magnetosome membrane.

Intact magnetosomes of Aquaspirillum magnetotacticum were purified from broken cells by a magnetic separation technique. Electron microscopic and chemical analyses revealed the magnetite to be enclosed by a lipid bilayer admixed with proteins. Lipids were recovered in fractions expected to contain (i) neutral lipids and free fatty acids, (ii) glycolipids and sulfolipids, and (iii) phospholipids (in a weight ratio of 1:4:6). Phospholipids included phosphatidylserine and phosphatidylethanolamine. Two of the numerous proteins detected in the magnetosome membrane were not found in other cell membranes or soluble fractions.

Bacteria↗
PubMed1986

Hydroxamate production by Aquaspirillum magnetotacticum.

Spent culture fluids from Aquaspirillum magnetotacticum MS-1 grown at high (20 microM) but not low (5 microM) iron concentration contained material yielding a positive hydroxamate test. Cells possessed six major outer membrane proteins. Three outer membrane proteins ranging from 72,000 to 85,000 daltons were coordinately produced at iron concentrations conducive to hydroxamate production. A 55,000-dalton iron-repressible outer membrane protein was also present in strain MS-1 cultured at low but not high ferric quinate concentration. Culture fluids from strain MS-1 which were hydroxamate positive augmented growth of a Salmonella typhimurium siderophore-deficient (enb-7) mutant in low-iron medium, suggesting a role of hydroxamate in uptake of iron by the cell.

Bacteria↗
PubMed1986

Iron respiration-driven proton translocation in aerobic bacteria.

Washed cell suspensions of Aquaspirillum magnetotacticum MS-1, A. itersonii E12639, Bacillus subtilis 6633, and Escherichia coli CSH27 translocated protons in response to the added oxidant O2 or NO3-, with triphenylmethylphosphonium bromide as the permeant ion. Iron respiration-driven proton translocation was observed in A. magnetotacticum MS-1, B. subtilis, and E. coli but not in a nonmagnetic strain of A. magnetotacticum (strain NM-1A) or with A. itersonii. Proton translocation to Fe3+ was totally inhibited by 500 microM NaN3 or 0.5 microM carbonyl cyanide m-chlorophenylhydrazone.

Aerobiosis↗
PubMed1984

Magnetosome dynamics in magnetotactic bacteria.

Diffusive motions of the magnetosomes (enveloped Fe3O4 particles) in the magnetotactic bacterium Aquaspirillum magnetotacticum result in a very broad-line Mössbauer spectrum (T approximately 100 mm/s) above freezing temperatures. The line width increases with increasing temperature. The data are analyzed using a bounded diffusion model to yield the rotational and translational motions of the magnetosomes as well as the effective viscosity of the material surrounding the magnetosomes. The results are [theta 2] l/2 less than 1.5 degrees and [x2] 1/2 less than 8.4 A for the rotational and translational motions, respectively, implying that the particles are fixed in whole cells. The effective viscosity is 10 cP at 295 K and increases with decreasing temperature. Additional Fe3+ material in the cell is shown to be associated with the magnetosomes. Fe2+ material in the cell appears to be associated with the cell envelope.

Bacterial Physiological Phenomena↗
PubMed1980

Ultrastructure of a magnetotactic spirillum.

The ultrastructure of a magnetotactic bacterium (strain MS-1) was examined by transmission, scanning, and scanning-transmission electron microscopy. The organism resembled other spirilla in general cell morphology, although some differences were detected at the ultrastructural level. Electron-dense particles within magnetotactic cells were shown by energy-dispersive X-ray analysis to be localizations containing iron. A non-magnetotactic variant of strain MS-1 lacked these novel bacterial inclusion bodies. A chain of these particles traversed each magnetotactic cell in a specific arrangement that was consistent from cell to cell, seemingly associated with the inner surface of the cytoplasmic membrane. Each particle was surrounded by an electron-dense layer separated from the particle surface by an electron-transparent region. The term "magnetosome" is proposed for the electron-dense particles with their enveloping layer(s) as found in this and other magnetotactic bacteria.

Cell Membrane↗
PubMed1979

Isolation and pure culture of a freshwater magnetic spirillum in chemically defined medium.

A bipolarly flagellated magnetotactic spirillum containing intracellular chains of single domain-sized magnetite crystals was isolated by applying a magnetic field to sediments from a freshwater swamp. The organism was cultured in a chemically defined medium containing ferric quinate and succinate as sources of iron and carbon, respectively. Nonmagnetic variants of this isolate were maintained in chemically defined medium lacking ferric quinate. In contrast to magnetic cells, these had less iron and lacked measurable magnetic remanence and the intracytoplasmic crystals. In other respects, including moles percent guanine plus cytosine content, growth characteristics, nutrition, and physiology, the two types were similar. The isolate reduced nitrate without accumulating nitrite and produced ammonia during growth. Nitrate or ammonium ions served as a nitrogen source. The organism was microaerophilic and did not grow anaerobically with nitrate in the medium. In chemically defined medium, cells synthesized magnetite only if the initial O2 concentration in the atmosphere of sealed cultures was 6% (vol/vol) or less.

Crystallization↗
PubMed1976

Arginine catabolism by Treponema denticola.

Treponema denticola, an anaerobe commonly present in the human mouth, ferments various amino acids and glucose. Amino acid analyses indicated that substrate amounts of arginine were utilized by T. denticola growing in a complex, serum-containing medium. Cell suspensions metabolized L-arginine to citrulline, NH3, CO2, proline, and small amounts of ornithine. CO2, NH3, ornithine, and proline were produced from L-citrulline by cell suspensions. Determinations of radioactivity in products formed from L-[U-14C]ornithine indicated that cell suspensions converted this amino acid to proline. Furthermore, proline was excreted by cells growing in a complex, arginine-containing medium. Arginine iminohydrolase (deiminase) and ornithine carbamoyltransferase activities were detected in T. denticola cell extracts. Carbamoylphosphate dissimilation by extracts yielded adenosine triphosphate. The data indicate that T. denticola derives energy by dissimilating L-argine via the arginine iminohydrolase pathway. However, unlike some of the other bacteria that utilize this pathway, T. denticola converts to proline much of the ornithine derived from L-arginine.

Arginine↗