Revisiting Plant Plasma Membrane Lipids in Tobacco: A Focus on Sphingolipids

The lipid composition of plasma membrane (PM) and the corresponding detergent-insoluble membrane (DIM) fraction were analyzed with a specific focus on highly polar sphingolipids, so-called glycosyl inositol phosphorylceramides (GIPCs). Using tobacco (Nicotiana tabacum) ‘Bright Yellow 2’ cell suspension and leaves, evidence is provided that GIPCs represent up to 40 mol % of the PM lipids. Comparative analysis of DIMs with the PM showed an enrichment of 2-hydroxylated very-long-chain fatty acid-containing GIPCs and polyglycosylated GIPCs in the DIMs. Purified antibodies raised against these GIPCs were further used for immunogold-electron microscopy strategy, revealing the distribution of polyglycosylated GIPCs in domains of 35 ± 7 nm in the plane of the PM. Biophysical studies also showed strong interactions between GIPCs and sterols and suggested a role for very-long-chain fatty acids in the interdigitation between the two PM-composing monolayers. The ins and outs of lipid asymmetry, raft formation, and interdigitation in plant membrane biology are finally discussed.Eukaryotic plasma membranes (PMs) are composed of three main classes of lipids, glycerolipids, sphingolipids, and sterols, which may account for up to 100,000 different molecular species (Yetukuri et al., 2008; Shevchenko and Simons, 2010). Overall, all glycerolipids share the same molecular moieties in plants, animals, and fungi. By contrast, sterols and sphingolipids are different and specific to each kingdom. For instance, the plant PM contains an important number of sterols, among which β-sitosterol, stigmasterol, and campesterol predominate (Furt et al., 2011). In addition to free sterols, phytosterols can be conjugated to form steryl glycosides (SG) and acyl steryl glycosides (ASG) that represent up to approximately 15% of the tobacco (Nicotiana tabacum) PM (Furt et al., 2010). As for sphingolipids, sphingomyelin, the major phosphosphingolipid in animals, which harbors a phosphocholine as a polar head, is not detected in plants. Glycosyl inositol phosphorylceramides (GIPCs) are the major class of sphingolipids in plants, but they are absent in animals (Sperling and Heinz, 2003; Pata et al., 2010). Sphingolipidomic approaches identified up to 200 plant sphingolipids (for review, see Pata et al., 2010; Cacas et al., 2013).Although GIPCs belong to one of the earliest classes of plant sphingolipids that were identified in the late 1950s (Carter et al., 1958), only a few GIPCs have been structurally characterized to date because of their high polarity and a limited solubility in typical lipid extraction solvents. For these reasons, they were systematically omitted from published plant PM lipid composition. GIPCs are formed by the addition of an inositol phosphate to the ceramide moiety, the inositol headgroup of which can then undergo several glycosylation steps. The dominant glycan structure, composed of a hexose-GlcA linked to the inositol, is called series A. Polar heads containing three to seven sugars, so-called series B to F, have been identified and appeared to be species specific (Buré et al., 2011; Cacas et al., 2013; Mortimer et al., 2013). The ceramide moiety of GIPCs consists of a long-chain base (LCB), mainly t18:0 (called phytosphingosine) or t18:1 compounds (for review, see Pata et al., 2010), to which is amidified a very-long-chain fatty acid (VLCFA), the latter of which is mostly 2-hydroxylated (hVLCFA) with an odd or even number of carbon atoms. In plants, little is known about the subcellular localization of GIPCs. It is assumed, however, that they would be highly represented in the PM (Worrall et al., 2003; Sperling et al., 2005), even if this remains to be experimentally proven. The main argument supporting such an assumption is the strong enrichment of trihydroxylated LCB (t18:n) in detergent-insoluble membrane (DIM) fractions (Borner et al., 2005; Lefebvre et al., 2007), LCB being known to be predominant in GIPC’s core structure as aforementioned.In addition to this chemical complexity, lipids are not evenly distributed within the PM. Sphingolipids and sterols can preferentially interact with each other and segregate to form microdomains dubbed the membrane raft (Simons and Toomre, 2000). The membrane raft hypothesis suggests that lipids play a regulatory role in mediating protein clustering within the bilayer by undergoing phase separation into liquid-disordered and liquid-ordered phases. The liquid-ordered phase, termed the membrane raft, was described as enriched in sterol and saturated sphingolipids and is characterized by tight lipid packing. Proteins, which have differential affinities for each phase, may become enriched in, or excluded from, the liquid-ordered phase domains to optimize the rate of protein-protein interactions and maximize signaling processes. In animals, rafts have been implicated in a huge range of cellular processes, such as hormone signaling, membrane trafficking in polarized epithelial cells, T cell activation, cell migration, and the life cycle of influenza and human immunodeficiency viruses (Simons and Ikonen, 1997; Simons and Gerl, 2010). In plants, evidence is increasing that rafts are also involved in signal transduction processes and membrane trafficking (for review, see Mongrand et al., 2010; Simon-Plas et al., 2011; Cacas et al., 2012a).Moreover, lipids are not evenly distributed between the two leaflets of the PM. Within the PM of eukaryotic cells, sphingolipids are primarily located in the outer monolayer, whereas unsaturated phospholipids are predominantly exposed on the cytosolic leaflet. This asymmetrical distribution has been well established in human red blood cells, in which the outer leaflet contains sphingomyelin, phosphatidylcholine, and a variety of glycolipids like gangliosides. By contrast, the cytoplasmic leaflet is composed mostly of phosphatidylethanolamine, phosphatidylserine, phosphatidylinositol, and their phosphorylated derivatives (Devaux and Morris, 2004). With regard to sphingolipids and glycerolipids, the asymmetry of the former is established during their biosynthesis and that of the latter requires ATPases such as the aminophospholipid translocase that transports lipids from the outer to the inner leaflet as well as multiple drug resistance proteins that transport phosphatidylcholine in the opposite direction (Devaux and Morris, 2004). This ubiquitous scheme encountered in animal cells could apply in plant cells as proposed (Tjellstrom et al., 2010). Indeed, the authors showed that there is a pronounced transverse lipid asymmetry in root at the PM. Phospholipids and galactolipids dominate the cytosolic leaflet, whereas the apoplastic leaflet is enriched in sphingolipids and sterols.From such a high diversity of the plant PM thus arises the question of the respective contribution of lipids to membrane suborganization. Our group recently tackled this aspect by characterizing the order level of liposomes prepared from various plant lipids and labeled with the environment-sensitive probe di-4-ANEPPDHQ (Grosjean et al., 2015). Fluorescence spectroscopy experiments showed that, among phytosterols, campesterol exhibits the strongest ability to order model membranes. In agreement with these data, spatial analysis of the membrane organization through multispectral confocal microscopy pointed to the strong ability of campesterol to promote liquid-ordered domain formation and organize their spatial distribution at the membrane surface. Conjugated sterols also exhibit a striking ability to order membranes. In addition, GIPCs enhance the sterol-induced ordering effect by emphasizing the formation and increasing the size of sterol-dependent ordered domains.The aim of this study was to reinvestigate the lipid composition and organization of the PM with a particular focus on GIPCs using tobacco leaves and cv Bright Yellow 2 (BY-2) cell cultures as models. Analyzing all membrane lipid classes at once, including sphingolipids, is challenging because they all display dramatically different chemical polarity, from very apolar (like free sterols) to highly polar (like polyglycosylated GIPCs) molecules. Most lipid extraction techniques published thus far use a chloroform/methanol mixture and phase partition to remove contaminants, resulting in the loss GIPCs, which remain in the aqueous phase, unextracted in the insoluble pellet, or at the interphase (Markham et al., 2006). In order to gain access to both glycerolipid and sphingolipid species at a glance, we developed a protocol whereby the esterifed or amidified fatty acids were hydrolyzed from the glycerol backbone (glycerolipids) or the LCB (sphingolipids) of membrane lipids, respectively. Fatty acids were then analyzed by gas chromatography-mass spectrometry (GC-MS) with appropriate internal standards for quantification. We further proposed that the use of methyl tert-butyl ether (MTBE) ensures the extraction of all classes of plant polar lipids. Our results indicate that GIPCs represent up to 40 mol % of total tobacco PM lipids. Interestingly, polyglycolyslated GIPCs are 5-fold enriched in DIMs of BY-2 cells when compared with the PM. Further investigation led us to develop a preparative purification procedure that allowed us to obtain enough material to raise antibodies against GIPCs. Using immunogold labeling on PM vesicles, it was found that polyglycosylated GIPCs cluster in membrane nanodomains, strengthening the idea that lateral nanosegregation of sphingolipids takes place at the PM in plants. Multispectral confocal microscopy was performed on vesicles prepared using GIPCs, phospholipids, and sterols and labeled with the environment-sensitive probe di-4-ANEPPDHQ. Our results show that, despite different fatty acid and polar head compositions, GIPCs extracted from tobacco leaves and BY-2 cells have a similar intrinsic propensity of enhancing vesicle global order together with sterols. Assuming that GIPCs are mostly present in the outer leaflet of the PM, interactions between sterols and sphingolipids were finally studied by the Langmuir monolayer technique, and the area of a single molecule of GIPC, or in interaction with phytosterols, was calculated. Using the calculation docking method, the energy of interaction between GIPCs and phytosterols was determined. A model was proposed in which GIPCs and phytosterols interact together to form liquid-ordered domains and in which the VLCFAs of GIPCs promote the interdigitation of the two membrane leaflets. The implications of domain formation and the asymmetrical distribution of lipids at the PM in plants are also discussed. Finally, we propose a model that reconsiders the intricate organization of the plant PM bilayer.     

Elemental analysis of uncultured magnetotactic bacteria exposed to heavy metals

Natural enrichments of magnetotactic bacteria were used to study the sites where heavy metals accumulate in uncultured bacteria. Most bacteria obtained by magnetic concentration from these enrichments contained, in addition to the magnetosomes, large phosphorus-rich granules in the cytoplasm. Metal (Zn, Mn, Sr, Cd, Al, Cr, and Pb) chlorides were added independently to the enrichments, and after 24 h, the elemental composition of the phosphorus-rich granules, magnetosomes, and "soft parts" (cytoplasm plus cell envelope) of whole bacteria was analyzed by energy-dispersive X-ray analysis on a transmission electron microscope. All bacteria contained Mn and Sr in the phosphorus-rich granules; some of them presented Mn peaks also in the soft parts. Zinc accumulation was variable and was found mainly in the phosphorus-rich granules, but also in the soft part of some bacteria. Some analyzed bacteria presented Zn peaks only in the soft parts, and some of them did not present Zn in any structure. Cadmium and Al were found only in the granules of some bacteria. Chromium was found in the soft parts of some bacteria. Lead was not detected in any bacteria. We concluded that the phosphorus-rich granules are major sites for metal accumulation by these bacteria. No conclusive results for magnetosomes were obtained because of the limitations of the analytical techniques particularly when used for whole cell analysis.     

Simultaneous storage of medical images in the spatial and frequency domain: A comparative study

Background  

Digital watermarking is a technique of hiding specific identification data for copyright authentication. This technique is adapted here for interleaving patient information with medical images, to reduce storage and transmission overheads.     

Randomly distributed crossovers may generate block-like patterns of linkage disequilibrium: an act of genetic drift

There is considerable interest in identifying and characterizing block-like patterns of linkage disequilibrium (LD; haplotype blocks) in the human genome as these may facilitate the identification of complex disease genes via genome-wide association studies. Although recombination hot-spots have been suggested as the primary mechanism to explain the block-like pattern of LD, other forces, such as genetic drift, may also be important. To this end, we have studied the effect of various recombination models on patterns of LD by using extensive simulations. As expected, haplotype blocks were observed under a model allowing recombination hot-spots. However, we also observed similar block-like patterns in the models where recombination crossovers are randomly and uniformly distributed, and we demonstrate that these blocks are generated by genetic drift. We caution that genetic drift may be an alternative mechanism (in addition to recombination hot-spots) that can lead to block-like patterns of LD. Our findings highlight the necessity of characterizing haplotype blocks in world-wide populations.     

Cell surface hydrophobicity and slime production of Staphylococcus epidermidis Brazilian isolates

The cell surface hydrophobicity of 60 isolates and three reference strains of Staphylococcus epidermidis was assayed by means of bacterial aggregation in liquid broth, phosphate-buffered saline, and in ammonium sulfate, as well as by affinity of the bacteria to n-hexadecane and polystyrene surfaces. In order to better characterize the isolates, the influence of bacterial growth time and enzyme treatment on cell hydrophobicity and the analysis of the slime production were also investigated. The strains presented the following profiles when assayed by the ammonium sulfate aggregation test (SAT): SAT < 1M, SAT 1M - <2M, SAT 2M - <4M, and SAT >or=4M. When SAT < 1M, the strains showed positive results for most of the cell surface hydrophobicity tests. None of the strains belonging to the groups with SAT >or= 1M showed spontaneous aggregation (SA), auto-aggregation (AA), or glass adherence, albeit 32 (62.7%) strains were polystyrene adherent and 42 (82.3%) presented weak adherence to n-hexadecane (>20%). The best correlation of the results was found among the AA and glass adherence tests (100%), followed by SA/ glass adherence (98%) and SA/ AA test (98%). The polystyrene adherence test and microbial adherence to n-hexadecane test (MATH) showed 78% correlation. Proteinase K treatment reduced bacterial adherence to polystyrene, but did not influence the SAT values. Three distinct groups of strains were distinguished by the polystyrene micromethod and glass tube adherence assay: 0.0-0.4 O.D. group, including non-glass adherent isolates; 0.5-0.7 O.D. group, including strains with variable profiles (adherent or non-adherent); and 0.8-1.3 O.D. group, composed of glass-adherent strains. Evaluation by a single method seemed not to reliably determine the surface hydrophobicity characteristics of S. epidermidis clinical isolates. Auto-aggregation properties of the strains that adhered to glass seemed related to slime expression, rather than cell surface hydrophobicity. Data also suggested involvement of protein components in adherence to polystyrene, but not in auto-aggregation properties assayed by SAT.     

Internal dynamics and ionization states of the macrophage migration inhibitory factor: comparison between wild-type and mutant forms

The macrophage migration inhibitory factor (MIF) is a cytokine that shares a common structural architecture and catalytic strategy with three isomerases: 4-oxalocrotonate tautomerase, 5-carboxymethyl-2-hydroxymuconate isomerase, and D-dopachrome tautomerase. A highly conserved N-terminal proline acts as a base-acid during the proton transfer reaction catalyzed by these enzymes. Such unusual catalytic strategy appears to be possible only due to the N-terminal proline pK(a) shifted to 5.0-6.0 units. Mutations of this residue result in a significant decrease of the catalytic activity of MIF. Two hypotheses have been proposed to explain the catalytic inefficiency of MIF: the lower basicity of primary amines with regard to secondary ones and the increased flexibility resulting from the replacement of a proline by residues like glycine. To investigate that, we have performed molecular dynamics simulations of MIF wild-type and its mutant P1G, as well as calculated the protonation properties of several mutant forms. It was found that the N-terminal glycine does not show larger fluctuations compared to proline, but the former residue is more exposed to the solvent throughout the simulations. The apparent pK(a) of these residues displays very little change (as expected from the structural rigidity of MIF) and is not significantly affected by the surrounding ionizable residues. Instead, the hydrophobic character of the active site seems to be the main factor in determining the pKa of the N-terminal residue and the catalytic efficiency of MIF.     

The otoconia of the guinea pig utricle: internal structure, surface exposure, and interactions with the filament matrix

A unique feature of the vertebrate gravity receptor organs, the saccule and utricle, is the mass of biomineral structures, the otoconia, overlying a gelatinous matrix also called "otoconial membrane" on the surface of the sensory epithelium. In mammals, otoconia are deposits of calcium carbonate in the form of composite calcite crystals. We used quick-freezing, deep etching to examine the otoconial mass of the guinea pig utricle. The deep-etching step exposed large expanses of intact and fractured otoconia, showing the fine structure and relationship between their internal crystal structure, their surface components, and the filament matrix in which they are embedded. Each otoconium has a compact central core meshwork of filaments and a composite outer shell of ordered crystallites and macromolecular aggregates. A distinct network of 20-nm beaded filaments covers the surface of the otoconia. The otoconia are interconnected and secured to the gelatinous matrix by surface adhesion and by confinement within a loose interotoconial filament matrix. The gelatinous matrix is a dense network made of yet another type of filament, 22 nm in diameter, which are cross-linked by shorter filaments, characteristically 11 nm in diameter. Our freeze-etching data provide a structural framework for considering the molecular nature of the components of the otoconial complex, their mechanical properties, and the degree of biological versus chemical control of otoconia biosynthesis.     

Pre-Columbian Floristic Legacies in Modern Homegardens of Central Amazonia

Historical ecologists have demonstrated legacy effects in apparently wild landscapes in Europe, North America, Mesoamerica, Amazonia, Africa and Oceania. People live and farm in archaeological sites today in many parts of the world, but nobody has looked for the legacies of past human occupations in the most dynamic areas in these sites: homegardens. Here we show that the useful flora of modern homegardens is partially a legacy of pre-Columbian occupations in Central Amazonia: the more complex the archaeological context, the more variable the floristic composition of useful native plants in homegardens cultivated there today. Species diversity was 10% higher in homegardens situated in multi-occupational archaeological contexts compared with homegardens situated in single-occupational ones. Species heterogeneity (β-diversity) among archaeological contexts was similar for the whole set of species, but markedly different when only native Amazonian species were included, suggesting the influence of pre-conquest indigenous occupations on current homegarden species composition. Our findings show that the legacy of pre-Columbian occupations is visible in the most dynamic of all agroecosystems, adding another dimension to the human footprint in the Amazonian landscape.     

Moderately Thermophilic Magnetotactic Bacteria from Hot Springs in Nevada

Populations of a moderately thermophilic magnetotactic bacterium were discovered in Great Boiling Springs, Nevada, ranging from 32 to 63°C. Cells were small, Gram-negative, vibrioid to helicoid in morphology, and biomineralized a chain of bullet-shaped magnetite magnetosomes. Phylogenetically, based on 16S rRNA gene sequencing, the organism belongs to the phylum Nitrospirae.Magnetotactic bacteria are a metabolically, morphologically, and phylogenetically heterogeneous group of prokaryotes that passively align and actively swim along magnetic field lines (3). This behavior, called magnetotaxis, is due to the presence of intracellular, membrane-bounded, single-magnetic-domain crystals of magnetite (Fe₃O₄) and/or greigite (Fe₃S₄) (3).Most known cultured magnetotactic bacteria are mesophilic and do not grow much above 30°C (e.g., Magnetospirillum species and Desulfovibrio magneticus strains MV-1 and MC-1 [D. A. Bazylinski, unpublished data]). Uncultured magnetotactic bacteria have been observed in numerous habitats that were mostly at 30°C and below. There is only one report describing thermophilic magnetotactic bacteria despite a number of efforts to look for them (e.g., in hydrothermal vents [D. A. Bazylinski, unpublished data]). Nash (12) reported the presence of thermophilic magnetotactic bacteria in microbial mats at about 45 to 55°C adjacent to the main flow in Little Hot Creek (but not in other springs in the same area at 40 to 80°C) and in microbial mats of other springs in central California at up to 58°C, all on the east side of the Sierra Nevada mountains. Cells biomineralized bullet-shaped crystals of magnetite and were phylogenetically affiliated with the phylum Nitrospirae (12). Few additional details were provided regarding the organisms and their habitat.In this study, water and surface sediment samples were taken from the Great Boiling Springs (GBS) geothermal field in Gerlach, NV. GBS is a series of hot springs that range from ambient temperature to ∼96°C (2, 5). The geology, chemistry, and microbial ecology of the springs have been described in some detail (2, 5). The pHs of the samples ranged from 6.4 to 7.5, while the salinities were about 4 to 5 ppt, as determined with a handheld Palm Abbe PA203 digital refractometer (MISCO Refractometer, Cleveland, OH). Samples were examined for the presence of magnetotactic bacteria using the hanging drop technique on-site and in the laboratory at room temperature with and without magnetic enrichment of the sample (15). Some samples taken back to the laboratory were kept at an elevated temperature (∼62°C), while others were kept at ambient temperature. There did not appear to be a significant difference in the number of magnetotactic cells in samples taken back to the laboratory and kept at these two temperatures. Only one morphotype of magnetotactic bacteria was found in samples from nine springs whose temperatures ranged from 32 to 63°C, and we estimate their numbers to be between 10³ to 10⁵ cells ml⁻¹ in surface sediments in sample bottles. We did not observe magnetotactic cells of this type in a large number of springs or pools that were at <32°C. Only one spring positive for the presence of these magnetotactic bacteria had sediment that was partially covered with a microbial mat, while sediment at most of the springs was dark gray in color. Cells were small (1.8 ± 0.4 by 0.4 ± 0.1 μm; n = 59), Gram negative, vibrioid to helicoid in morphology, and possessed a single polar flagellum (Fig. ​(Fig.1A).1A). Magnetotactic bacteria were not observed in springs that were at 67°C and above, suggesting the maximum survival and perhaps growth temperature for the organism is about 63°C. In the lab, cells remained viable and motile in samples kept at 25 to 62°C for several months. We refer to this organism as strain HSMV-1.Open in a separate windowFIG. 1.Transmission electron microscope (TEM) images of cells and magnetosomes of strain HSMV-1. (A) TEM image of unstained cell of HSMV-1 showing a single polar flagellum and a single chain of bullet-shaped magnetosomes. The electron-dense structures at the poles were found to be phosphorus-rich based on energy-dispersive X-ray analysis (data not shown) and therefore likely represent polyphosphate granules. (B) Higher-magnification TEM image of the magnetosome chain. (C) High-magnification TEM image of magnetosomes from which a selected area electron diffraction (SAED) pattern was obtained (inset of B). The SAED pattern corresponds to the [1 0−1] zone of magnetite, Fe₃O₄: reflection o, (0 0 0); reflection a, (1 −1 1) (0.48 nm); reflection b, (1 1 1) (0.48 nm); reflection c, (2 0 2) (0.30 nm); angle a-o-b, 70.5°. (D) Iron, sulfur, and oxygen elemental maps, derived from energy-filtering transmission electron microscopy (EFTEM), showing that the positions of the magnetosome crystals correlate with increased concentrations of Fe and O, but not S, consistent with the iron oxide magnetite (Fe₃O₄).Cells of HSMV-1 biomineralized a single chain of magnetosomes that traversed the cells along their long axis (Fig. 1A to C). Selected area electron diffraction (SAED) and energy-filtering transmission electron microscopy (EFTEM) elemental maps were determined on magnetosome crystals using a Tecnai model G2 F30 Super-Twin transmission electron microscope (FEI Company, Hillsboro OR). SAED patterns of HSMV-1 magnetosome crystals (Fig. ​(Fig.1B,1B, inset) indicated that they consisted of magnetite, while EFTEM elemental maps (Fe, O and S) (Fig. ​(Fig.1D)1D) clearly showed that the crystals consisted of an iron oxide and not an iron sulfide, again consistent with the mineral magnetite. Cells contained an average of 12 ± 6 magnetosome crystals per cell (n = 15 cells) that averaged 113 ± 34 by 40 ± 5 nm in size (n = 179). A plot of the length of the crystals as a function of the shape factor (width/length ratio) is provided in Figure S1 in the supplemental material and shows that the crystals fit in the theoretical single-magnetic-domain size range (4), along with all known mature magnetosome magnetite crystals from magnetotactic bacteria (3).Whole-cell PCR amplification of the 16S rRNA gene was performed by first magnetically purifying cells of HSMV-1 using the “capillary racetrack” described by Wolfe et al. (18). Purity of the collected cells was determined by microscopic examination, and contaminating cells were never observed. The 16S rRNA gene was amplified using bacteria-specific primers 27F 5′-AGAGTTTGATCMTGGCTCAG-3′ and 1492R 5′-TACGGHTACCTTGTTACGACTT-3′ (11). PCR products were cloned into pGEM-T Easy vector (Promega Corporation, Madison, WI) and sequenced (Functional Biosciences, Inc., Madison, WI). Six of eight clones sequenced had identical inserts.Alignment of 16S rRNA gene sequences was performed using the CLUSTAL W multiple alignment accessory application in the BioEdit sequence alignment editor (7). Phylogenetic trees were constructed using MEGA version 4 (17) by applying the neighbor-joining method (14). Bootstrap values were calculated with 1,000 replicates. The 16S rRNA gene sequence of strain HSMV-1 places the organism in the phylum Nitrospirae (Fig. ​(Fig.2),2), with its closest relative in culture being Thermodesulfovibrio hydrogeniphilus (87.2% identity) (8). Two other uncultured magnetotactic bacteria are phylogenetically affiliated with the phylum Nitrospirae, including the unnamed rod-shaped bacterium strain MHB-1 (86.5% identity) (6) and the very large Candidatus Magnetobacterium bavaricum (86.4% identity) (16). Interestingly, all the magnetotactic bacteria associated with the phylum Nitrospirae thus far (e.g., Candidatus Magnetobacterium bavaricum) contain bullet-shaped magnetite crystals in their magnetosomes.Open in a separate windowFIG. 2.Phylogenetic tree based on 16S rRNA gene sequences showing the phylogenetic position of strain HSMV-1 in the phylum Nitrospirae. Bootstrap values at nodes are percentages of 1,000 replicates. The magnetotactic bacteria Desulfovibrio magneticus and Candidatus Magnetoglobus multicellularis (outgroup; deltaproteobacteria) were used to root the tree. GenBank accession numbers are given in parentheses. Bar represents 2% sequence divergence.Fluorescent in situ hybridization (FISH) was used to authenticate the 16S rRNA gene sequence. A specific Alexa594-labeled probe for HSMV-1 was designed (HSMVp, 5′-CCTTCGCCACAGGCCTTCTA-3′, complementary to nucleotides 690 to 709 of the 16S rRNA molecule) based on the alignment of 10 of the most similar 16S rRNA gene sequences found in GenBank after BLAST analysis (1) and on cultivated members of the phylum Nitrospirae. FISH with the Alexa594-labeled probe was carried out after fixation of magnetically concentrated cells directly on the wells of gelatin-coated hydrophobic microscope slides with 4% paraformaldehyde. FISH was performed according to the work of Pernthaler et al. (13). The hybridization solution contained 10 ng/ml of the probe, 20% formamide, 0.9 M NaCl, 20 mM Tris-HCl (pH 7.4), 1 mM Na₂EDTA, and 0.01% sodium dodecyl sulfate (SDS). Cells of HSMV-1 hybridized to the HSMVp probe, while other cells in the sample did not (Fig. ​(Fig.3),3), indicating that the 16S rRNA gene sequence we obtained is from the magnetotactic bacterium under study. Strain HSMV-1 clearly represents a new genus (Fig. ​(Fig.2),2), and based on the phylogeny and what we currently know phenotypically about strain HSMV-1, we propose the name Candidatus Thermomagnetovibrio paiutensis (the GBS site was originally occupied by the Paiute Indian Tribe).Open in a separate windowFIG. 3.Fluorescent in situ hybridization (FISH) of cells of strain HSMV-1 using an HSMV-1-specific oligonucleotide rRNA probe (HSMVp). Cells used for FISH were magnetically concentrated by placing a magnet next to the side of the sample bottle for 30 min and then removed with a Pasteur pipette. This technique was used rather than the magnetic racetrack method in order to have many HSMV-1 cells as well as some other cells that could be used as a negative control. (A) Differential interference contrast (DIC) image of HSMV-1 cells (filled arrows) and other cells (negative control; empty arrows) from hot spring samples; (B) cells stained with 4′,6-diamidino-2-phenylindole (DAPI); (C) cells hybridized with the specific probe HSMVp.Nash (12) first reported thermophilic magnetotactic bacteria phylogenetically affiliated with the Nitrospirae phylum in hot springs, and it would be interesting and important to compare these organisms and their habitats. However, little can be compared at this time due to lack of information. Nash (12) reported that the one spring at Little Hot Creek was freshwater and that microbial mats were present at all springs where thermophilic magnetotactic bacteria were found. The water at our sampling sites was brackish, not freshwater, and microbial mats were not an important feature of our springs. Thus, it is difficult to determine without knowing the relationship between the organisms found by Nash (12) and strain HSMV-1 what environmental parameters are important to the growth and survival of these bacteria.It is also difficult to determine the temperature ranges for the survival and growth for strain HSMV-1 without having a pure culture. Data presented here suggest that the temperature range for both is quite wide, and this would be important for the continued presence of HSMV-1 at GBS, as temperatures in the hot springs are known to fluctuate greatly (2). Even if the maximum growth temperature of HSMV-1 is slightly lower than the maximum survival temperature (a conservative estimate) that we know of (63°C), it would still be considered a moderately thermophilic bacterium.The results presented here clearly show that some magnetotactic bacteria can be considered at least moderately thermophilic. They extend the upper temperature limit for environments where magnetotactic bacteria exist and likely grow (∼63°C) and where magnetosome magnetite is deposited, a finding that may prove significant in the study and interpretation of magnetofossils (9, 10).     

Quality of different aphids species as hosts for the parasitoid Aphidius ervi Haliday (Hymenoptera: Braconidae: Aphidiinae)

The suitability of Macrosiphum euphorbiae (Thomas), Aulacorthum solani (Kaltenbach) and Acyrthosiphon kondoi Shinji (Hemiptera: Aphididae) as hosts for the aphid parasitoid Aphidius ervi Haliday was evaluated by assessing host size, host preference, and host quality. Tests were carried out in an environmental chamber at 22±1oC, 70±10% RH and 12h photophase. Replicates (11) consisted of one 24h-old mated female of A. ervi without a previous oviposition experience. Female was released into a Petri dish (5 cm) with 20 2nd and 3rd instars of one of each aphid species tested on a leaf disc of the host plant onto a 1% water-agar layer. Parasitoid emergency was lower in A. kondoi (78.7%) compared to M. euphorbiae (92.2%) and A. solani (91.7%). Acyrthosiphon kondoi (0.36 mm) was the smallest host. The parasitoid showed preference (74.0% parasitism) for M. euphorbiae, the largest host (hind tibia length=0.73 mm), which in turn yielded larger A. ervi females (0.75 mm).