Large Fraction of Dead and Inactive Bacteria in Coastal Marine Sediments: Comparison of Protocols for Determination and Ecological Significance

It is now universally recognized that only a portion of aquatic bacteria is actively growing, but quantitative information on the fraction of living versus dormant or dead bacteria in marine sediments is completely lacking. We compared different protocols for the determination of the dead, dormant, and active bacterial fractions in two different marine sediments and at different depths into the sediment core. Bacterial counts ranged between (1.5 ± 0.2) × 10⁸ cells g⁻¹ and (53.1 ± 16.0) × 10⁸ cells g⁻¹ in sandy and muddy sediments, respectively. Bacteria displaying intact membrane (live bacterial cells) accounted for 26 to 30% of total bacterial counts, while dead cells represented the most abundant fraction (70 to 74%). Among living bacterial cells, nucleoid-containing cells represented only 4% of total bacterial counts, indicating that only a very limited fraction of bacterial assemblage was actively growing. Nucleoid-containing cells increased with increasing sediment organic content. The number of bacteria responsive to antibiotic treatment (direct viable count; range, 0.3 to 4.8% of the total bacterial number) was significantly lower than nucleoid-containing cell counts. An experiment of nutrient enrichment to stimulate a response of the dormant bacterial fraction determined a significant increase of nucleoid-containing cells. After nutrient enrichment, a large fraction of dormant bacteria (6 to 11% of the total bacterial number) was “reactivated.” Bacterial turnover rates estimated ranged from 0.01 to 0.1 day⁻¹ but were 50 to 80 times higher when only the fraction of active bacteria was considered (on average 3.2 day⁻¹). Our results suggest that the fraction of active bacteria in marine sediments is controlled by nutrient supply and availability and that their turnover rates are at least 1 order of magnitude higher than previously reported.     

Synoptic determination of living/dead and active/dormant bacterial fractions in marine sediments

The most widely used methods for the estimation of the living/dead fractions of bacterial cells involve specific stains that are able to reveal membrane integrity. Here, we have compared two different probes (propidium iodide and ethidium homodimer-2) that have different molecular weights and steric hindrance effects. We have also combined this method with the staining/destaining procedure that is currently used in the identification of potentially active cells. The procedure for marine sediments described here allows the synoptic (i.e. from the same filter) identification of: (i) the number of living bacteria; (ii) the number of active vs. dormant cells within this living fraction; (iii) the bacterial fraction with an intact nucleoid region without membrane integrity; and (iv) dead cells (devoid of the nucleoid region and without membrane integrity). Our results demonstrate that the concentration of propidium is crucial for the correct estimation of the dead bacterial fraction, ethidium homodimer-2 allows efficient and accurate estimates that are independent of the concentrations used and the sample storage. The active bacterial fraction represented c. 40% of the total bacterial abundance, the inactive/dormant fraction c. 30%, and the dead fraction was, on average, c. 30%. This method allows the processing of a large number of samples with high precision and at relatively low cost, and thus it provides additional synoptic insights into the metabolic state of bacteria in marine sediments.     

The deep subsurface biosphere is alive and well

For the first time, metabolically active bacterial cells have recently been quantified in deep marine sediments. In contrast to previous total cell counts that do not differentiate between active cells and inactive or dormant cells, these quantifications using oligonucleotide hybridization probes target active cells and their ribosomal (r)RNA. They demonstrate a sizable, active bacterial subsurface biosphere, and allow realistic estimates of cell-specific respiration rates and turnover times for living bacteria in this global extreme habitat. In situ activities and physiologies of these active subsurface microbiota emerge as high-priority research areas.     

Application of a rapid direct viable count method to deep-sea sediment bacteria

For the first time, a Live/Dead (L/D) Bacterial Viability Kit (BacLight ) protocol was adapted to marine sediments and applied to deep-sea sediment samples to assess the viability (based on membrane integrity) of benthic bacterial communities. Following a transect of nine stations in the Fram Strait (Arctic Ocean), we observed a decrease of both bacterial viability and abundance with increasing water (1250-5600 m) and sediment depth (0-5 cm). Percentage of viable (and thus potentially active) cells ranged between 20-60% within the first and 10-40% within the fifth centimetre of sediment throughout the transect, esterase activity estimations (FDA) similarly varied from highest (13.3+/-5.4 nmol cm(-3) h(-1)) to lowest values below detection limit down the sediment column. Allowing for different bottom depths and vertical sediment sections, bacterial viability was significantly correlated with FDA estimations (p<0.001), indicating that viability assessed by BacLight staining is a good indicator for bacterial activity in deep-sea sediments. Comparisons between total L/D and DAPI counts not only indicated a complete bacterial cell coverage, but a better ability of BacLight staining to detect cells under low activity conditions. Time course experiments confirmed the need of a rapid method for viability measurements of deep-sea sediment bacteria, since changes in pressure and temperature conditions caused a decrease in bacterial viability of up to 50% within the first 48 h after sample retrieval. The Bacterial Viability Kit proved to be easy to handle and to provide rapid and reliable information. It's application to deep-sea samples in absence of pressure-retaining gears is very promising, as short staining exposure time is assumed to lessen profound adverse effects on bacterial metabolism due to decompression.     

Method for enumeration of 5-cyano-2,3-ditoyl tetrazolium chloride (CTC)-active cells and cell-specific CTC activity of benthic bacteria in riverine, estuarine and coastal sediments

Bacteria are the most abundant and active organisms in marine sediments and are critical for nutrient cycling and as a food source to many benthic and pelagic organisms. Bacteria are found both as free-living cells and as particle-associated cells, which can make investigations of these communities difficult. We found that common procedures for extracting bacteria from sediments leave the bacteria clay particle-associated and the clay particles clump, which reduce the reproducibility of direct counts. We optimized a sonication/surfactant method that produces a homogeneous suspension of bacterial cells against a uniform background of clay particles, which results in reproducible samples for epifluorescence microscopy. We developed a method to estimate CTC-positive cells and cell-specific CTC content in intact cores of surficial sediment communities from riverine, estuarine and coastal sites. Benthic bacterial abundances averaged 4.9x10(8) cells/g dry wt sediments in Apalachicola River, Florida sediments, 4.9-13.8x10(9) cells/g dry wt sediments in a variety of Apalachicola Bay sediments and 3.6x10(8) cells/g dry weight in shallow, anoxic Gulf of Mexico sediments. Percent CTC-positive cells ranged from low values of 9-10% CTC-positive cells in Apalachicola River and Apalachicola Bay sediments to high values of 25% CTC-positive cells in anoxic Gulf of Mexico sediments. After correction for abiotic CTC reduction and chlorophyll interference, estimates of cell-specific CTC reduction ranged from 0.15 to 0.55 fmol CTC(red)/active cell in the Apalachicola Bay sediments to 1.6 to 3.8 fmol CTC(red)/active cell in anoxic Gulf of Mexico sediments.     

Large differences in the fraction of active bacteria in plankton,sediments, and biofilm

Generally, only a small fraction of free-living pelagic bacteria are metabolically active, while particle-associated bacteria usually exhibit a larger proportion of active bacteria. Most previous studies on the active fraction of bacteria focus on planktonic communities, and there are only a few studies on sediment and epiphytic biofilm bacteria. We compared the active fraction of the total number of bacteria in three different habitats of the littoral zone of Lake Erken, Sweden, including the sediments, the epiphytic biofilm on the submerged macrophyte Ranunculus circinatus, and the water column. Active bacteria were detected as those with an active electron transport system, identified by the capacity to reduce the tetrazolium salt CTC (5-cyano-2,3-ditolyltetrazolium chloride) into its fluorescent, water insoluble state. There were large differences between habitats. The active fraction of the total number of bacteria detected by fluorescence microscopy (annual mean +/- SD) in the sediments was 46 +/- 10%, on R. circinatus 37 +/- 18%, and in the water column 4 +/- 4%. The abundance of CTC-reducing cells was correlated with total bacterial abundance, and the fraction of CTC-reducing bacteria generally increased with total bacterial abundance, for all the habitats. Consequently, the difference in the fraction of CTC-reducing bacteria between the habitats could be attributed to different densities of bacteria, with a larger proportion of active bacteria at higher bacterial densities.     

Significance of size and nucleic acid content heterogeneity as measured by flow cytometry in natural planktonic bacteria.

Total bacterial abundances estimated with different epifluorescence microscopy methods (4',6-diamidino-2-phenylindole [DAPI], SYBR Green, and Live/Dead) and with flow cytometry (Syto13) showed good correspondence throughout two microcosm experiments with coastal Mediterranean water. In the Syto13-stained samples we could differentiate bacteria with apparent high DNA (HDNA) content and bacteria with apparent low DNA (LDNA) content. HDNA bacteria, "live" bacteria (determined as such with the Molecular Probes Live/Dead BacLight bacterial viability kit), and nucleoid-containing bacteria (NuCC) comprised similar fractions of the total bacterial community. Similarly, LDNA bacteria and "dead" bacteria (determined with the kit) comprised a similar fraction of the total bacterial community in one of the experiments. The rates of change of each type of bacteria during the microcosm experiments were also positively correlated between methods. In various experiments where predator pressure on bacteria had been reduced, we detected growth of the HDNA bacteria without concomitant growth of the LDNA bacteria, such that the percentage contribution of HDNA bacteria to total bacterial numbers (%HDNA) increased. This indicates that the HDNA bacteria are the dynamic members of the bacterial assemblage. Given how quickly and easily the numbers of HDNA and LDNA bacteria can be obtained, and given the similarity to the numbers of "live" cells and NuCC, the %HDNA is suggested as a reference value for the percentage of actively growing bacteria in marine planktonic environments.     

Advantages of distinguishing the active fraction in bacterioplankton assemblages: some examples

The difficulty of distinguishing between active and dormant or dead bacterial cells is an important problem for the aquatic microbiologist.Active cells can be detected under the microscope by the presence of an intact electron transport system able to reduce the colourless INT [2-(p-iodophenyl)-3-(p-nitrophenyl)-5-phenyl tetrazolium chloride] to an optically dense intracellular deposit.An improvement of this method has been applied to Lake Geneva and to a fish pond in the Ivory Coast. The portion of INT-reducing bacterial cells ranged from 1 to 71%, depending on place, depth, season and time of the day. In all cases bacterial activity, determined by uptake of ³H Thymidine or ¹⁴C glucose, and frequency of dividing cells were better correlated with the number of INT-reducing cells than with the total number of cells. This means that counts of cells able to reduce INT have a better metabolic significance than total cell counts. Some examples are developed which show the advantages of applying this method in cases where it is useful to distinguish active cells in a bacterial assemblage.     

Determination of Active Marine Bacterioplankton: a Comparison of Universal 16S rRNA Probes, Autoradiography, and Nucleoid Staining

We compared several currently discussed methods for the assessment of bacterial numbers and activity in marine waters, using samples from a variety of marine environments, from aged offshore seawater to rich harbor water. Samples were simultaneously tested for binding to a fluorescently labeled universal 16S rRNA probe; (sup3)H-labeled amino acid uptake via autoradiography; nucleoid-containing bacterial numbers by modified DAPI (4(prm1),6-diamidino-2-phenylindole) staining; staining with 5-cyano-2,3-ditolyl tetrazolium chloride (CTC), a compound supposed to indicate oxidative cell metabolism; and total bacterial counts (classical DAPI staining), taken as a reference. For the universal-probe counts, we used an image intensifying and processing system coupled to the epifluorescence microscope. All of the above-mentioned methods yielded lower cell counts than DAPI total counts. Universal-probe counts averaged about half of the corresponding DAPI count and were highly correlated to autoradiography counts (r(sup2) = 0.943; n = 7). Nucleoid-containing cell counts could be lower than DAPI counts by as much as 1 order of magnitude but sometimes matched autoradiography or probe counts. CTC counts were 2 orders of magnitude below DAPI counts. Universal 16S rRNA probe counts correlated well with autoradiography results, indicating a population with at least minimal metabolic activity. The greater variability of the nucleoid-containing cell counts calls for further investigation of the processes involved, and CTC counts were well below the range of the other methods tested.     

Enzymatic manganese(II) oxidation by metabolically dormant spores of diverse Bacillus species

Bacterial spores are renowned for their longevity, ubiquity, and resistance to environmental insults, but virtually nothing is known regarding whether these metabolically dormant structures impact their surrounding chemical environments. In the present study, a number of spore-forming bacteria that produce dormant spores which enzymatically oxidize soluble Mn(II) to insoluble Mn(IV) oxides were isolated from coastal marine sediments. The highly charged and reactive surfaces of biogenic metal oxides dramatically influence the oxidation and sorption of both trace metals and organics in the environment. Prior to this study, the only known Mn(II)-oxidizing sporeformer was the marine Bacillus sp. strain SG-1, an extensively studied bacterium in which Mn(II) oxidation is believed to be catalyzed by a multicopper oxidase, MnxG. Phylogenetic analysis based on 16S rRNA and mnxG sequences obtained from 15 different Mn(II)-oxidizing sporeformers (including SG-1) revealed extensive diversity within the genus Bacillus, with organisms falling into several distinct clusters and lineages. In addition, active Mn(II)-oxidizing proteins of various sizes, as observed in sodium dodecyl sulfate-polyacrylamide electrophoresis gels, were recovered from the outer layers of purified dormant spores of the isolates. These are the first active Mn(II)-oxidizing enzymes identified in spores or gram-positive bacteria. Although extremely resistant to denaturation, the activities of these enzymes were inhibited by azide and o-phenanthroline, consistent with the involvement of multicopper oxidases. Overall, these studies suggest that the commonly held view that bacterial spores are merely inactive structures in the environment should be revised.     

Factors Influencing Bacterial Production in a Shallow Estuarine System

The bacterioplankton of the marine and brackish water zones of the complex system Ria de Aveiro was characterized as profiles of bacterial abundance and biomass productivity. During the warm season, total bacteria ranged from 0.2 to 8.5 x 109 cells L-1 and active bacteria number from 0.1 to 3.1 x 109 cells L-1. Total and active bacterial numbers were, on average, three times higher in brackish than in marine water. Bacterial productivity on different dates and different tides in the marine zone varied from 0.05 to 4.5 mg C L-1 h-1. Here the average productivity (1.1 mg C L-1 h-1) was 3.5 times less than in brackish water (average 3.8 mg C L-1 h-1; range 0.7-14.2 mg C L-1 h-1). Specific productivity varied from 0.05 to 2.61 fg C cell-1 h-1, a range that was similar throughout the ecosystem. However, specific productivity per active cell was 19% higher in brackish water. Bacterial production variation was best explained by the number of active bacteria, which, in turn, was highly associated with total bacterial number, temperature, and particulate organic carbon. In the marine zone, bacterial production was also influenced by depth and salinity. In the brackish zone, the set of independent variables explained a smaller percentage of bacterial production variation than in marine zone, suggesting greater importance of other variables. In the marine zone, and mainly near low tide, productivity was significantly higher (average 3.3 times) at the surface (down to 0.5 m) than in the deeper layers of the water column. This stratification of bacterial productivity was linked to the increased specific productivity per active cell, as no modification in the proportion of active cells in the population could be detected. The vertical profile of bacterial production in the deeper zone of this estuarine ecosystem, in which no clear salinity or thermal stratification occurs throughout the tidal cycle, seemed to reflect a biochemical stratification generated by increased phytoplankton exudation and/or by photochemical transformation of semilabile or recalcitrant organic compounds. Shallower water masses tend to blur this surface effect. The relative importance of photochemical transformation in the pattern of estuarine bacterial production will therefore tend to vary with the bathymetry of the system.     

Arsenic resistance and removal by marine and non-marine bacteria

Arsenic resistance and removal was evaluated in nine bacterial strains of marine and non-marine origins. Of the strains tested, Marinomonas communis exhibited the second-highest arsenic resistance with median effective concentration (EC(50)) value of 510 mg As l(-1), and was capable of removing arsenic from culture medium amended with arsenate. Arsenic accumulation in cells amounted to 2290 microg As g(-1) (dry weight) when incubated on medium containing 5 mg As l(-1) of arsenate. More than half of the arsenic removed was related to metabolic activity: 45% of the arsenic was incorporated into the cytosol fraction and 10% was found in the lipid-bound fraction of the membrane, with the remaining arsenic considered to be adsorbed onto the cell surface. Potential arsenic resistance and removal were also examined in six marine and non-marine environmental water samples. Of the total bacterial colony counts, 28-100% of bacteria showed arsenic resistance. Some of the bacterial consortia, especially those from seawater enriched with arsenate, exhibited higher accumulated levels of arsenic than M. communis under the same condition. These results showed that arsenic resistant and/or accumulating bacteria are widespread in the aquatic environment, and that arsenic-accumulating bacteria such as M. communis are potential candidates for bioremediation of arsenic contaminated water.     

普通和稀释培养基研究太湖沉积物可培养细菌的多样性

采用普通牛肉汁培养基和 10倍稀释的普通牛肉汁培养基 (以下简称稀释培养基 )研究太湖沉积物中细菌多样性 ,发现在稀释培养基上生长的细菌数量普遍是在普通牛肉汁琼脂培养基上生长的细菌数量的 3～ 5倍。分离得到纯培养物的 16SrDNA部分序列 (5′端约 5 0 0bp)分析表明 ,不同培养基上生长的优势细菌类群存在差别 :普通培养基生长的细菌主要为γ_Proteobacteria(35. 1% ) ,其次为Actinobacteria(2 4 5 % )和Firmicutes(2 2 . 3% )等类群 ,其中大部分细菌与假单胞菌属 (Pseudomoas)、芽孢杆菌属 (Bacillus)和节杆菌属 (Archrobacter)细菌的系统关系密切 ;稀释培养基生长的细菌则主要为Actinobacteria(2 7. 1% )、Firmicutes(2 5 . 7% )、α_Proteobacteria(2 1. 4 % )和γ_Proteobacteria(15. 7% )等类群 ,与芽孢杆菌属 (Bacillus) (2 5. 7% )发育系统关系密切的细菌为优势属。研究结果表明同时采用两种培养基有助于从太湖沉积物中分离到更多种微生物。     

The application of viable count procedures for measuring viable cells in the various marine environments

Aims: To investigate whether the use of direct viable count (DVC), quantitative viable count (qDVC), colony‐forming units and the contribution of capsule‐bearing bacteria to the total number of bacteria and esterase‐active bacteria could be used to clearly differentiate viable cells in various trophic status of seawater. Methods and Results: Hundred and four marine isolates from various marine environments in Turkey (Western Black Sea, northern part of the Sea of Marmara, Northern Aegean Sea and eastern part of the Sea of Marmara) were screened. Seawater samples were taken from the surface (the upper 0–30 cm) and deeper layers (from 5 to 500 m) of the sea at different time periods between February 2002 and June 2007. For the assessment of cell elongation, minor modifications were made on DVC procedure in order to optimize the concentration of yeast extract and incubation time for enumeration of bacteria in response to nutrient addition. The best results were obtained when the yeast extract was used at a final concentration of 250 mg l^?1 (at 35°C 24 h incubation) for bacteria isolated from eutrophic areas and a final concentration of 50 mg l^?1 for those selected from oligotrophic areas. A positive correlation was found between the trophic level and the level of metabolically active bacteria. Among these methods, the bacterial number obtained by qDVC is higher than those gained by other methods. Conclusions: The results indicate that the qDVC procedure could easily differentiate between viable cells and dormant or dead cells. We suggest that this method may be applicable to detecting the level of metabolic potential of bacterial communities in marine environments. Significance and Impact of the Study: The study resulted in increased knowledge on the applicability of the qDVC method that arranges the substrate amount and incubation time as well as on the comparison of various viable bacteria count procedures related to trophic situation of seawater samples.     

Total Counts of Marine Bacteria Include a Large Fraction of Non-Nucleoid-Containing Bacteria (Ghosts)

Counts of heterotrophic bacteria in marine waters are usually in the order of 5 x 10(sup5) to 3 x 10(sup6) bacteria ml(sup-1). These numbers are derived from unspecific fluorescent staining techniques (J. E. Hobbie, R. J. Daley, and S. Jasper, Appl. Environ. Microbiol. 33:1225-1228, 1977; K. G. Porter and Y. S. Feig, Limnol. Oceanogr. 25:943-948, 1980) and are subsequently defined as total counts of bacteria. In samples from the Baltic Sea, the North Sea (Skagerrak), and the northeastern Mediterranean Sea, we found that only a minor fraction (2 to 32%) of total counts can be scored as bacteria with nucleoids. Lack of DNA no doubt means inactive cells; therefore, a much lower number of bacteria that grow at rates higher than those previously estimated must be responsible for the measured bacterial production in these seas. The remaining bacterium-sized and/or -shaped particles included in total counts may be cell residues of virus-lysed bacteria (ghosts) or remains of protozoan grazing.     

Barophilic Bacteria Associated with Digestive Tracts of Abyssal Holothurians

Abyssal holothurians and sediment samples were collected at depths of 4,430 to 4,850 m in the Demerara abyssal plain. Bacterial concentrations in progressive sections of the holothurian digestive tract, as well as in surrounding surface sediments, were determined by epifluorescence microscopy. Total bacterial counts in sediments recently ingested by the animals were 1.5- to 3-fold higher than in surrounding sediments at the deepest station. Lowest counts were observed consistently in the foregut, where the digestive processes of the holothurian are believed to occur. In most animals, counts increased 3- to 10-fold in the hindgut. Microbial activity at 3°C and in situ and atmospheric pressure were determined for gut and sediment samples by measuring the utilization of [¹⁴C]glutamic acid, the doubling time of the mixed-population of culturable bacteria, and the percentage of the total bacterial count responsive to yeast extract in the presence of nalidixic acid, using epifluorescence microscopy. A barophilic microbial population, showing elevated activity under deep-sea pressure, was detected by all three methods in sediments removed from the hindgut. Transmission electron micrographs revealed intact bacteria directly associated with the intestinal lining only in the hindgut. The bacteria are believed to be carried as an actively metabolizing, commensal gut flora that transforms organic matter present in abyssal sediments ingested by the holothurian. Using data obtained in this study, it was calculated that sediment containing organic matter altered by microbial activity cleared the holothurian gut every 16 h, suggesting that abyssal holothurians and their associated gut flora are important participants in nutrient cycles of the abyssal benthic ocean.     

Employing a triple metabarcoding approach to differentiate active,dormant and dead microeukaryotes in sediments

Microbial communities are commonly characterised through the metabarcoding of environmental DNA. This DNA originates from both viable (including dormant and active) and dead organisms, leading to recent efforts to distinguish between these states. In this study, we further these approaches by distinguishing not only between viable and dead cells but also between dormant and actively growing cells. This is achieved by sequencing both rRNA and rDNA, in conjunction with propidium monoazide cross-linked rDNA, to partition the active, dormant and relic fractions in environmental samples. We apply this method to characterise the diversity and assemblage structure of these fractions of microeukaryotes in intertidal sediments during a wet-dry-rewet incubation cycle. Our findings indicate that a significant proportion of microeukaryotic phylotypes detected in the total rDNA pools originate from dormant and relic microeukaryotes in the sediments, both in terms of richness (dormant, 13 ± 2%; relic, 47 ± 5%) and read abundance (dormant, 20 ± 7%; relic, 14 ± 5%). The richness and sequence proportion of dormant microeukaryotes notably increase during the transition from wet to dry conditions. Statistical analyses suggest that the dynamics of diversity and assemblage structure across different activity fractions are influenced by various environmental drivers. Our strategy offers a versatile approach that can be adapted to characterise other microbes in a wide range of environments.     

Enzymatic Manganese(II) Oxidation by Metabolically Dormant Spores of Diverse Bacillus Species

Bacterial spores are renowned for their longevity, ubiquity, and resistance to environmental insults, but virtually nothing is known regarding whether these metabolically dormant structures impact their surrounding chemical environments. In the present study, a number of spore-forming bacteria that produce dormant spores which enzymatically oxidize soluble Mn(II) to insoluble Mn(IV) oxides were isolated from coastal marine sediments. The highly charged and reactive surfaces of biogenic metal oxides dramatically influence the oxidation and sorption of both trace metals and organics in the environment. Prior to this study, the only known Mn(II)-oxidizing sporeformer was the marine Bacillus sp. strain SG-1, an extensively studied bacterium in which Mn(II) oxidation is believed to be catalyzed by a multicopper oxidase, MnxG. Phylogenetic analysis based on 16S rRNA and mnxG sequences obtained from 15 different Mn(II)-oxidizing sporeformers (including SG-1) revealed extensive diversity within the genus Bacillus, with organisms falling into several distinct clusters and lineages. In addition, active Mn(II)-oxidizing proteins of various sizes, as observed in sodium dodecyl sulfate-polyacrylamide electrophoresis gels, were recovered from the outer layers of purified dormant spores of the isolates. These are the first active Mn(II)-oxidizing enzymes identified in spores or gram-positive bacteria. Although extremely resistant to denaturation, the activities of these enzymes were inhibited by azide and o-phenanthroline, consistent with the involvement of multicopper oxidases. Overall, these studies suggest that the commonly held view that bacterial spores are merely inactive structures in the environment should be revised.     

海洋细菌抗菌和细胞毒活性的初步研究

从不同海域的生物、海水和海泥中分离海洋细菌,利用琼脂扩散法和MTT法对细菌培养液的乙酸乙酯提取物进行了抗菌和细胞毒活性筛选。比较了活性菌株与来源的相关性．结果表明,在分离的341株海洋细菌中。42株细菌的代谢产物具有抗菌活性,7株具有细胞毒活性,其中来源于海洋无脊椎动物和海藻的活性菌株比例(22％和11％)大于来源于海水和海泥的细菌(7％和5％)．细菌分类鉴定结果显示,具有活性的细菌大部分属于假单胞菌属、发光杆菌属、梭状芽孢杆菌属、交替单胞菌属和黄杆菌属．     

Entry of Vibrio harveyi and Vibrio fischeri into the viable but nonculturable state

AIMS: Physiological responses of marine luminous bacteria, Vibrio harveyi (ATCC 14216) and V. fischeri (UM1373) to nutrient-limited normal strength (35 ppt iso-osmolarity) and low (10 ppt hypo-osmolarity) salinity conditions were determined. METHODS AND RESULTS: Plate counts, direct viable counts, actively respiring cell counts, nucleoid-containing cell counts, and total counts were determined. Vibrio harveyi incubated at 22 degrees C in nutrient-limited artificial seawater (ASW) became nonculturable after approximately 62 and 45 d in microcosms of 35 ppt and 10 ppt ASW, respectively. In contrast, V. fischeri became nonculturable at approximately 55 and 31 d in similar microcosms. Recovery of both culturability and luminescence of cells in the viable but nonculturable state was achieved by addition of nutrient broth or nutrient broth supplemented with a carbon source, including luminescence-stimulating compounds. Temperature upshift from 22 degrees C to 30 degrees C or 37 degrees C did not result in recovery from nonculturability. CONCLUSIONS: The study confirms entry of V. harveyi and V. fischeri into the viable but nonculturable state under low-nutrient conditions and demonstrates nutrient-dependent resuscitation from this state. SIGNIFICANCE AND IMPACT OF THE STUDY: This study confirms loss of luminescence of V. harveyi and V. fischeri on entry into the viable but nonculturable state and suggests that enumeration of luminescent cells in water samples may be a rapid method to deduce the nutrient status of a water sample.