Insights Into the Mineralogy and Surface Chemistry of Extracellular Biogenic S0 Globules Produced by Chlorobaculum tepidum.

Elemental sulfur (S0) is produced and degraded by phylogenetically diverse groups of microorganisms. For Chlorobaculum tepidum, an anoxygenic phototroph, sulfide is oxidized to produce extracellular S0 globules, which can be further oxidized to sulfate. While some sulfur-oxidizing bacteria (e.g., Allochromatium vinosum) are also capable of growth on commercial S0 as an electron donor, C. tepidum is not. Even colloidal sulfur sols, which appear indistinguishable from biogenic globules, do not support the growth of C. tepidum. Here, we investigate the properties that make biogenic S0 globules distinct from abiotic forms of S0. We found that S0 globules produced by C. tepidum and abiotic S0 sols are quite similar in terms of mineralogy and material properties, but the two are distinguished primarily by the properties of their surfaces. C. tepidum's globules are enveloped by a layer of organics (protein and polysaccharides), which results in a surface that is fundamentally different from that of abiotic S0 sols. The organic coating on the globules appears to slow the aging and crystallization of amorphous sulfur, perhaps providing an extended window of time for microbes in the environment to access the more labile forms of sulfur as needed. Overall, our results suggest that the surface of biogenic S0 globules may be key to cell-sulfur interactions and the reactivity of biogenic S0 in the environment.

Chlorobaculum tepidum growth on biogenic S(0) as the sole photosynthetic electron donor.

The green sulfur bacteria, the Chlorobi, are phototrophic bacteria that oxidize sulfide and deposit extracellular elemental sulfur globules [S(0)]. These are subsequently consumed after sulfide is exhausted. S(0) globules from a Chlorobaculum tepidum mutant strain were purified and used to show that the wild-type strain of Cba. tepidum can grow on biogenic S(0) globules as the sole photosynthetic electron donor, i.e. in medium with no other source of reducing power. Growth yields and rates on biogenic S(0) are comparable with those previously determined for Cba. tepidum grown on sulfide as the sole electron donor. Contact between cells and S(0) was required for growth. However, only a fraction of the cell population was firmly attached to S(0) globules. Microscopic examination of cultures growing on S(0) demonstrated cell-S(0) attachment and allowed for the direct observation of S(0) globule degradation. Bulk chemical analysis, scanning electron microscopy, secondary ion mass spectrometry and SDS-PAGE indicate that Cba. tepidum biogenic S(0) globules contain carbon, oxygen and nitrogen besides S and may be associated with specific proteins. These observations suggest that current models of S(0) oxidation in the Chlorobi need to be revised to take into account the role of cell-S(0) interactions in promoting S(0) degradation.

Comparative Genomic Insights into Ecophysiology of Neutrophilic, Microaerophilic Iron Oxidizing Bacteria.

Neutrophilic microaerophilic iron-oxidizing bacteria (FeOB) are thought to play a significant role in cycling of carbon, iron and associated elements in both freshwater and marine iron-rich environments. However, the roles of the neutrophilic microaerophilic FeOB are still poorly understood due largely to the difficulty of cultivation and lack of functional gene markers. Here, we analyze the genomes of two freshwater neutrophilic microaerophilic stalk-forming FeOB, Ferriphaselus amnicola OYT1 and Ferriphaselus strain R-1. Phylogenetic analyses confirm that these are distinct species within Betaproteobacteria; we describe strain R-1 and propose the name F. globulitus. We compare the genomes to those of two freshwater Betaproteobacterial and three marine Zetaproteobacterial FeOB isolates in order to look for mechanisms common to all FeOB, or just stalk-forming FeOB. The OYT1 and R-1 genomes both contain homologs to cyc2, which encodes a protein that has been shown to oxidize Fe in the acidophilic FeOB, Acidithiobacillus ferrooxidans. This c-type cytochrome common to all seven microaerophilic FeOB isolates, strengthening the case for its common utility in the Fe oxidation pathway. In contrast, the OYT1 and R-1 genomes lack mto genes found in other freshwater FeOB. OYT1 and R-1 both have genes that suggest they can oxidize sulfur species. Both have the genes necessary to fix carbon by the Calvin-Benson-Basshom pathway, while only OYT1 has the genes necessary to fix nitrogen. The stalk-forming FeOB share xag genes that may help form the polysaccharide structure of stalks. Both OYT1 and R-1 make a novel biomineralization structure, short rod-shaped Fe oxyhydroxides much smaller than their stalks; these oxides are constantly shed, and may be a vector for C, P, and metal transport to downstream environments. Our results show that while different FeOB are adapted to particular niches, freshwater and marine FeOB likely share common mechanisms for Fe oxidation electron transport and biomineralization pathways.

Interannual dynamics of viriobenthos abundance and morphological diversity in Chesapeake Bay sediments.

Despite significant implications of viral activity in sediment ecosystems, there are limited data describing how sediment viral assemblages respond to broader ecosystem changes. To document this, the spatial and temporal dynamics of viral and bacterial abundance (BA) and changes in the morphological distribution of viruses were examined within three salinity regions over 2 years. Viral abundances (VA) ranged from 0.2 to 17 × 10(10) viruses mL(-1) sediment while direct bacterial counts ranged from 3.8 to 37 × 10(8) cells mL(-1) sediment. Peaks and valleys in the abundance of extracted viruses and bacteria from surface sediments occurred simultaneously, with lows in February 2004 and highs in April 2003. Across all samples, viral and BA were positively correlated (P < 0.001). Vertical profiles showed a decrease in viral and BA with depth in sediments. Based on transmission electron microscopy results, viruses with diminutive capsids (20-50 nm) and from the Myoviridae and Podoviridae viral family types were dominant within surface sediments. The most morphologically diverse viral assemblages occurred in autumn samples from the sandy, polyhaline station and spring samples from the mesohaline station. Seasonal changes showed an average 72% decrease in VA from spring to winter. These observations support the view that viriobenthos assemblages are responsive to seasonal environmental changes and that viral processes have significant implications for the biogeochemical processes mediated by bacterial communities within Bay sediments.

In vivo time-lapse documentation using confocal and multi-photon microscopy reveals the mechanisms of invasion into the Arabidopsis root vascular system by Fusarium oxysporum.

Fusarium oxysporum, a major soil-borne fungal pathogen, causes vascular wilt, damping-off, and root rot diseases on over 100 cultivated plant species. Mechanisms of root colonization by F. oxysporum in Arabidopsis thaliana were studied through in planta 3-dimensional time-lapse documentation using confocal and multi-photon microscopy. Data from individual encounter sites were acquired repeatedly over a several day period without physical manipulation or retrieval from the growth chamber. In vivo observations were facilitated by transformation of F. oxysporum for constitutive cytoplasmic expression of the fluorescent protein ZsGreen, and host responses were monitored using autofluorescence or GFP-tagged endoplasmic reticulum. Penetration into the vascular system occurred primarily in the meristematic region of primary and lateral roots. Fungal hyphae may release phytotoxin(s) that compromise host cells not directly in contact with hyphae. This novel approach was essential for visualizing the dynamic interactions between F. oxysporum and A. thaliana from both the host and pathogen sides.