Anaerobic dechlorination of 2,4-dichlorophenol in freshwater sediments in the presence of sulfate.

In the presence of added sulfate, 2,4-dichlorophenol and 4-chlorophenol were transformed stoichiometrically to 4-chlorophenol and phenol, respectively, in anaerobic freshwater lake sediments between 18 and 40 degrees C. The concomitantly occurring sulfate reduction reduced the initial sulfate concentration from 25 mM to about 6 to 8 mM and depressed methane formation.     

Studies on dissimilatory sulfate-reducing bacteria that decompose fatty acids

Gliding motility, ultrastructure and nutrition of two newly isolated filamentous sulfate-reducing bacteria, strains 5ac10 and 4be13, were investigated. The filaments were always attached to surfaces. Growth was supported by addition of insoluble aluminium phosphate or agar as substrata for gliding movement. Electron microscopy of ultrathin sections revealed cell walls characteristic of Gramnegative bacteria; the undulated structure of the outer membrane may pertain to the translocation mechanism. Intracytoplasmic membranes were present. Acetate, higher fatty acids, succinate or fumarate served as electron donors and carbon sources. Strain 5ac10 grew also with lactate, but not with benzoate that was used only by strain 4be13. Strain 5ac10 was able to grow slowly on H₂ plus CO₂ or formate in the presence of sulfate without additional organic carbon source. The capacity of complete oxidation was shown by stoichiometric measurements with acetate plus sulfate. Both strains contained b- and c-type cytochromes. Desulfoviridin was detected only in strain 5ac10. The two filamentous gliding sulfate reducers are described as new species of a new genus, Desulfonema limicola and Desulfonema magnum.     

Fossile Reptil-Eischalen (Chelonia,Crocodilia, Dinosauria) aus dem unteren Barremium von Galve (Provinz Teruel,SE-Spanien)

The Lower Cretaceous vertebrate bearing sediments of Galve (province of Teruel, SE Spain) have yielded some hundred fossil eggshell fragments, all slightly diagenetically altered. Concerning their microstructure, an assignment of the material to different taxa of reptiles was possible. The eggshell assemblage of Galve consists of a-c) three types of chelonian eggshells, one of them probably representing the subfamily Batagurinae, which would extend this taxon back into the Lower Cretaceous, d) the oldest known crocodilian eggshells, with lacunae systems on the outer surface, comparable to Recent taxa, and e-f) two different types of dinosaurian eggshells. In correspondence to the suggested fluviatile paleoenvironment of Galve, the fossil eggshells described herein are fragmented and represent mostly turtles and crocodiles.     

Comparison of phylogenetic relationships based on phospholipid fatty acid profiles and ribosomal RNA sequence similarities among dissimilatory sulfate-reducing bacteria

Abstract Twenty-five isolates of dissimilatory sulfate-reducing bacteria were clustered based on similarity analysis of their phospholipid ester-linked fatty acids (PLFA). Of these, 22 showed that phylogenetic relationships based on the sequence similarity of their 16S rRNA directly paralleled the PLFA relationships. Desulfobacter latus and Desulfobacter curvatus grouped with the other Desulfobacter spp. by 16S rRNA comparison but not with the PLFA analysis as they contained significantly more monoenoic PLFA than the others. Similarly, Desulfovibrio africanus clustered with the Desulfovibrio spp. by 16S rRNA but not with them when analyzed by PLFA patterns because of higher monoenoic PLFA content. Otherwise, clustering obtained with either analysis was essentially congruent. The relationships defined by PLFA patterns appeared robust to shifts in nutrients and terminal electron acceptors. Additional analyses utilizing the lipopolysaccharide-lipid A hydroxy fatty acid patterns appeared not to shift the relationships based on PLFA significantly except when completely absent, as in Gram-positive bacteria. Phylogenetic relationships between isolates defined by 16S rRNA sequence divergence represent a selection clearly different from the multi-enzyme activities responsible for the PLFA patterns. Determination of bacterial relationships based on different selective pressures for various cellular components provides more clues to evolutionary history leading to a more rational nomenclature.     

Hyperostotic fish bones (“Tilly bones”) from presumably Pliocene phosphorites of the Lake Manyara area,northern Tanzania

PalZ - Hyperostotic fish bones from the presumable Pliocene phosphate-bearing deposits along Lake Manyara, Tanzania, are described. In contrast to marine occurrences of this kind, the pathological...     

Structure and dynamics of the complex of single stranded DNA binding protein of Escherichia coli with circular single stranded DNA of filamentous phages

We have analyzed the equilibrium and nonequilibrium properties of the complex of the single stranded DNA binding protein of Escherichia coli (EcoSSB) and circular single stranded DNA of filamentous phages M13mp8 and F1 using static and dynamic light scattering, analytical ultracentrifugation and electron microscopy. Upon binding to the single stranded DNA the EcoSSB tetramer replaces an equivalent volume of water trapped within the coiled single stranded DNA and hinders the folding of the single stranded DNA into secondary structures at all salt concentrations. The salt dependent compaction of the stoichiometric complex can be described assuming a flexible polyelectrolyte chain. The solution structure of the macromolecular complex is a random coil and in the electron microscope a beaded flexible structure of the complex with a bead diameter of 6 nm appears at all salt concentrations used. The internal motions of the stoichiometric complex can be described by the Rouse-Zimm model of polymer dynamics. The segmental mobility of the complex can be correlated with changes in the binding site size of the EcoSSB tetramer; it indicates the presence of interactions between EcoSSB tetramers bound to single stranded DNA.     

Anaerobic biodegradation of 2,4-dichlorophenol in freshwater lake sediments at different temperatures.

Anaerobic degradation of 2,4-dichlorophenol (2,4-DCP) between 5 and 72 degrees C was investigated. Anaerobic sediment slurries prepared from local freshwater pond sediments were partitioned into anaerobic tubes or serum vials, which then were incubated separately at the various temperatures. Reductive 2,4-DCP dechlorination occurred only in the temperature range between 5 and 50 degrees C, although methane was formed up to 60 degrees C. In sediment samples from two sites and at all tested temperatures from 5 to 50 degrees C, 2,4-DCP was transformed to 4-chlorophenol (4-CP). The 4-CP intermediate was subsequently degraded after an extended lag period in the temperature range from 15 to 40 degrees C. Adaptation periods for 2,4-DCP transformation decreased between 5 and 25 degrees C, were essentially constant between 25 and 35 degrees C, and increased in the tubes incubated at temperatures between 35 and 40 degrees C. The degradation rates increased exponentially between 15 and 30 degrees C, had a second peak at 35 degrees C, and decreased to about 5% of the peak activity by 40 degrees C. In tubes from one sediment sample, incubated at temperatures above 40 degrees C, an increase in the degradation rate was observed following the minimum at 40 degrees C. This suggests that at least two different organisms were involved in the transformation of 2,4-DCP to 4-CP. Storage of the original sediment slurries for 2 months at 12 degrees C resulted in increased adaptation times, but did not affect the degradation rates.     

In situ distribution of EcoRI methylase and restriction endonuclease in cells of Escherichia coli Bs 5

Specific IgG antibodies were raised in rabbits against purified EcoRI methylase and restriction endonuclease. Post embedding labeling experiments, using the protein A-gold technique, were made with paraformaldehyde-glutaraldehyde fixed cells, embedded in Lowicryl K4M resin at low temperatures. Labeling with methylase-specific antibodies showed 60-70% of gold particles in the cytoplasm and 30-40% at the cell envelope, whereas the use of restriction enzyme-specific antibodies led to a distribution of 10-30% in the cytoplasm and 70-90% in the cell envelope. The results coincide with the proposed function of the enzymes: in the cytoplasm methylase protects the cells' own DNA from self-destruction, and the restriction endonuclease cuts foreign DNA when entering the cell.