Evidences for Microbial Precipitation of Calcite in Speleothems from Krem Syndai in Jaintia Hills,Meghalaya, India

Speleothems from Krem Syndai, Meghalaya in Northeast India were studied for their microbial diversity using 16S rDNA-based phylogenetic approach and conventional microbiological techniques along with geochemistry, mineralogy and in vitro experiments to understand participation of microorganisms in CaCO₃ precipitation. Speleothems imaged by scanning electron microscopy showed round coccoid-like, sporangia-like and spinose calcified structures, numerous broken cocci shells with spotted interiors inside a calcite crystal, honeycomb long reticulate, smooth, flat, twisted, ribbon-like, tubular, beaded, microbe-mineralized filaments and extracellular polymeric substances (EPS). Fourier spectroscopy indicated the presence of various organic compounds. δ¹³C and δ¹⁸O isotopic ratios of speleothems ranged from ?4.65 to ?7.34‰ and ?3.06 to ?6.80‰, respectively. Total number of microbial cells using SYBR Gold was high. Fluorescence in situ hybridization (FISH) indicated approximately 3 × 10⁵ to 5 × 10⁵ cells g sed^–1 in the speleothems out of which the number of microbes belonging to Eubacteria ranged from 1.8 × 10⁵ to 3.6 × 10⁵ cells, g sed^–1. FISH showed ～45% active microbial cells of the total cell number in samples. DNA-based high-throughput amplicon sequencing revealed 19 bacterial phyla in the speleothem. Approximately 42% of the sequences were similar to Proteobacteria (Alphaproteobacteria: 22.4%, Betaproteobacteria: 8.9%, Gammaproteobacteria: 8.6%). Sequences similar to Nitrospiraceae (22.8%) had the highest proportion of sequences belonging to a single family. Bacterial strains isolated from the speleothems raised alkalinity and precipitated calcite in the laboratory cultures which was confirmed by X-ray diffraction (XRD) analyses. These isolates belonged to Bacillus spp., Actinomycetes spp., Streptomyces spp., Pseudomonas spp., Micrococcus spp., Staphylococcus spp., Xanthobacter spp. and Arthrobacter spp. Overall, the results showed unequivocal evidence of bacterial fingerprints during CaCO₃ precipitation in the cave.     

Biogenic Evidences of Moonmilk Deposition in the Mawmluh Cave,Meghalaya, India

Moonmilk, a microcrystalline secondary cave deposit, actively forms on the floor of Krem Mawmluh – a limestone cave in Meghalaya, Northeastern India. Due to the abundance of micrite and calcified microbial filaments, we hypothesize that these deposits form as a result of ongoing microbial interactions. Consistent with this idea, we report electron microscopic and microbiological evidences for the biological origin of moonmilk in Krem Mawmluh. Scanning electron microscopy indicated abundant calcified microbial filaments, needle calcite, fibre calcites (micro-fibre and nano-fibre calcite crystals), biofilm and microbial filaments in the moonmilk. The total viable culturable microbes showed high population densities for microbes in the moonmilk and moonmilk pool waters. In vitro culture experiments, confirmed the capability of many of the isolated strains to precipitate calcite and some of the identified isolates belonged to the Bacillus sp. and Actinomycetes. These results clearly support the biogenic nature of the deposits.     

Optimization of Mixed Cultivation of the Moderate Thermophilic Bioleaching Microorganisms for High Cell Density Using Statistical Methodology

The low functional microbial population density in the industrial bioleaching process has been a limiting factor for the high leaching efficiency, making the microbial cultivation and continuous inoculation an alternative for sustaining the microbial activity. In the present experiment, the defined mixed cultivation of Leptospirillum ferriphilum YSK, Sulfobacillus acidophilus TPY, Acidithiobacillus caldus S2, and Ferroplasma thermophilum L1 was evaluated and optimized by Statistical Methodology. Going through the Plackett–Burman experimental design, pH value, temperature, and c(MgSO₄·7H₂O) were considered as the most significant factors in the defined range. Then, the relationships were analyzed using the steepest ascent design, the central composite design, and finally the response surface methodology. It was suggested that the optimum parameters were pH 1.38, MgSO₄·7H₂O 0.552?g/L, temperature 44?°C, FeSO₄·7H₂O 40?g/L, sulfur 8?g/L, yeast 0.02% w/v, (NH₄)₂SO₄ 3g/L, K₂HPO₄ 0.5g/L, KCl 0.1g/L, Ca(NO₃)₂ 0.01?g/L, in which allowed total cell density of the microbial community to reach 7.63?×?10⁸ cells/mL in the cultivation period. The lab experiments were routinely undertaken with the expectation that the L. ferriphilum YSK, S. acidophilus TPY, A. caldus S2, F. thermophilum L1 could rapid grown from initial cell density of 0.25?×?10⁷ cells/mL to 2.82?×?10⁸ cells/mL, 1.68?×?10⁸ cells/mL, 2.76?×?10⁸ cells/mL, 2.51?×?10⁷ cells/mL, respectively in 58?h. It demonstrates a possibility to co-culture these microbes in a single reactor, providing an efficient way to regenerate of inoculation for biomining process.     

Unique Microbial Communities Inhabiting Underground Seawater in an Intertidal Area Utilized for Industrialized Aquaculture,as Compared with the Coastal Water

In recent decades, the decline of coastal water quality has promoted the birth of a new industrialized aquaculture mode in China, which involves the cultivation of organisms using underground seawater extracted from various depths below the intertidal zone. In view of the special physicochemical characteristics of underground seawater, the microbial community in this environment has attracted interest. In this study, the microbial community in the underground seawater of an intertidal area of the Qingdao coast of China was investigated. Compared with the upper coastal water, the underground seawater displayed lower numbers of microorganisms (2.7?±?0.3?×?10⁵ cells mL^?1 in underground seawater vs. 5.3?±?0.4?×?10⁵ cells mL^?1 in upper coastal seawater) but displayed much higher microbial diversity. At the phyla level, Proteobacteria, Bacteroidetes, Cyanobacteria, and Actinobacteria inhabited both environments, whereas bacteria in the phyla Planctomycetes, Deferribacteres, and Nitrospirae were recovered only from the underground seawater. Eighty-nine percent of the OTUs in the underground seawater were environmental specific. Furthermore, compared with coastal water, underground seawater displayed significant lower (p?<?0.05) concentration of NH₃-N, NO₂-N, PO₄-P, and DOC-C, and contained fewer potentially harmful pathogens (e.g., Verrucomicrobia/Opitutae) and more denitrifying bacteria (e.g., Shewanella denitrificans), thus making it more suitable for aquaculture.     

Active microbial ecosystem in Iron-Age tombs of the Etruscan civilization

Earth's microbial biosphere extends down through the crust and much of the subsurface, including those microbial ecosystems located within cave systems. Here, we elucidate the microbial ecosystems within anthropogenic 'caves'; the Iron-Age, subterranean tombs of central Italy. The interior walls of the rock (calcium-rich macco) were painted ~2500 years ago and are covered with CaCO₃ needles (known as moonmilk). The aims of the current study were to: identify biological/geochemical/biophysical determinants of and characterize bacterial communities involved in CaCO₃ precipitation; challenge the maxim that biogenic activity necessarily degrades surfaces; locate the bacterial cells that are the source of the CaCO₃ precipitate; and gain insight into the kinetics of moonmilk formation. We reveal that this environment hosts communities that consist primarily of bacteria that are mesophilic for temperature and xerotolerance (including Actinobacteria, Bacteroidetes and Proteobacteria); is populated by photosynthetic Cyanobacteria exhibiting heterotrophic nutrition (Calothrix and Chroococcidiopsis); and has CaCO₃ precipitating on the rock surfaces (confirmation that this process is biogenic) that acts to preserve rather than damage the painted surface. We also identified that some community members are psychrotolerant (Polaromonas), acidotolerant or acidophilic (members of the Acidobacteria), or resistant to ionizing radiation (Brevundimonas and Truepera); elucidate the ways in which microbiology impacts mineralogy and vice versa; and reveal that biogenic formation of moonmilk can occur rapidly, that is, over a period of 10 to 56 years. We discuss the paradox that these ecosystems, that are for the most part in the dark and lack primary production, are apparently highly active, biodiverse and biomass-rich.     

Microbial Community Diversity of Moonmilk Deposits at Ballynamintra Cave, Co. Waterford, Ireland

Caves are extreme and specialised habitats for terrestrial life that sometimes contain moonmilk, a fine-grained paste-like secondary mineral deposit that is found in subterranean systems worldwide. While previous studies have investigated the possible role of microorganisms in moonmilk precipitation, the microbial community ecology of moonmilk deposits is poorly understood. Bacterial and fungal community structure associated with four spatially isolated microcrystalline, acicular calcite moonmilk deposits at Ballynamintra Cave (S. Ireland) was investigated during this study. Statistical analyses revealed significant differences in microbial activity, number of bacterial species, bacterial richness and diversity, and fungal diversity (Shannon's diversity) among the moonmilk sites over an area of approximately 2.5 m². However, the number of fungal species and fungal community richness were unaffected by sampling location. SIMPER analysis revealed significant differences in bacterial and fungal community composition among the sampling sites. These data suggest that a rich assemblage of microorganisms exists associated with moonmilk, with some spatial diversity, which may reflect small-scale spatial differences in cave biogeochemistry.     

Sea ice microbial dynamics over an annual ice cycle in Prydz Bay, Antarctica

Microbial community dynamics within the fast sea ice of Prydz Bay (68°S?78°E) were investigated over an annual cycle at two sites (1 and 3?km offshore) between April and November 2008. There are few long-term sea ice studies, and few that cover the phase of winter darkness when autotrophic processes are curtailed. Mean chlorophyll a concentrations in the ice column ranged between 0.76 and 44.8?μg?L^?1 at the 1-km site (Site 1) and 3.11–144.6?μg?L^?1 at the 3-km site (Site 2). Highest chlorophyll a usually occurred at the base of the ice. Bacterial concentrations ranged between 0.30 and 2.08?×?10⁸?cells?L^?1, heterotrophic nanoflagellates (HNAN) between 0.21?×?10⁵ and 2.98?×?10⁵?cells?L^?1 and phototrophic nanoflagellates (PNAN) 0–1.06?×?10⁵?cells?L^?1. While HNAN occurred throughout the year, PNAN were largely absent in winter. Dinoflagellates were a conspicuous and occasionally an abundant element of the community (maximum 17,460?cells?L^?1), while ciliates were sparse. The bacterial community showed considerable morphological diversity with a dominance of filamentous forms. Bacterial production continued throughout the year ranging between 0 and 22.92?μg?C?L^?1?day^?1 throughout the ice column. Lowest rates occurred between late June and early August. The sea ice sustained an active and diverse microbial community through its annual extent. The data suggest that during winter darkness the microbial community is dominated by heterotrophic processes, sustained by a pool of dissolved organic carbon.     

Enhanced Calcite Dissolution in the Presence of the Aerobic Methanotroph Methylosinus trichosporium

Microbial aerobic methane oxidation (MOx) is intrinsically coupled to the production of carbon dioxide, favoring carbonate dissolution. Recently, microbial organic polymers were shown to be able to induce carbonate dissolution. To discriminate between different mechanisms causing calcite dissolution, experiments were conducted in the presence of solid calcite with (1) actively growing cells (2) starving cells, and (3) dead cells of the methanotrophic bacterium Methylosinus trichosporium under brackish conditions (salinity 10) near calcite saturation (saturation state (Ω) 1.76 to 2.22). Total alkalinity and the amount of dissolved calcium markedly increased in all experiments containing M. trichosporium cells. After initial system equilibration, similar calcite dissolution rates, ranging between 20.16 (dead cells) and 25.68 μmol L^?1 d^?1 (actively growing cells), were observed. Although concentrations of transparent exopolymer particles declined with time in the presence of actively growing and starving cells, they increased in experiments with dead cells. Scanning electron microscopy images of calcite crystals revealed visible surface corrosion after exposure to live and dead M. trichosporium cells. The results of this study indicate a strong potential for microbial MOx to affect calcite stability negatively, facilitating calcite dissolution. In addition to CO₂ production by methanotrophically active cells, we suggest that the release of acidic or Ca²⁺-chelating organic carbon compounds from dead cells could also enhance calcite dissolution.     

Selective determination of human immunoglobulin G by flow‐injection chemiluminescence

A novel flow‐injection chemiluminescence method was developed for the selective determination of human immunoglobulin G (IgG) in the presence of thiomersal by changing the flow rates of peristaltic pump. The study was based on the independence and additivity of the CL signals of human IgG and thiomersal in the galangin–potassium permanganate–polyphosphoric acid system. In meantime, two equations relating to the concentrations of mixing solutions of human IgG and thiomersal vs the CL intensity were established and solved, on the basis of which the content of thiomersal included in samples was simultaneously determined too. The enhanced CL intensity was in proportion to concerntrations in the range 8.0 × 10^?7 to 8.0 × 10^?5 g/mL for human IgG and 1.0 × 10^?7 to 2.0 × 10^?6 g/mL for thiomersal with the detection limits of 5.0 × 10^?7 g/mL for human IgG and 6.0 × 10^?8 g/mL for thiomersal, respectively. The relative standard deviation for 1.0 × 10^?5 g/mL human IgG was 0.8% and for 2.0 × 10^?7 g/mL thiomersal it was 2.0% (n = 10). The proposed method was applied to determine three synthetic samples with recoveries of 91.5–109.5%. In addition, the possible chemiluminescence mechanisms are discussed as well. Copyright © 2010 John Wiley & Sons, Ltd.     

Inactivation of Bacillus cereus by Na‐chlorophyllin‐based photosensitization on the surface of packaging

Aims: This study was focused on the possibility to inactivate food‐borne pathogen Bacillus cereus by Na‐chlorophyllin (Na‐Chl)‐based photosensitization in vitro and after attachment to the surface of packaging material. Methods and Results: Bacillus cereus in vitro or attached to the packaging was incubated with Na‐Chl (7·5 × 10^?8 to 7·5 × 10^?5 mol l^?1) for 2–60 min in phosphate buffer saline. Photosensitization was performed by illuminating cells under a light with a λ of 400 nm and an energy density of 20 mW cm^?2. The illumination time varied 0–5 min and subsequently the total energy dose was 0–6 J cm^?2. The results show that B. cereus vegetative cells in vitro or attached to the surface of packaging after incubation with 7·5 × 10^?7 mol l^?1 Na‐Chl and following illumination were inactivated by 7 log. The photoinactivation of B. cereus spores in vitro by 4 log required higher (7·5 × 10^?6 mol l^?1) Na‐Chl concentration. Decontamination of packaging material from attached spores by photosensitization reached 5 log at 7·5 × 10^?5 mol l^?1 Na‐Chl concentration. Comparative analysis of different packaging decontamination treatments indicates that washing with water can diminish pathogen population on the surface by <1 log, 100 ppm Na‐hypochlorite reduces the pathogens about 1·7 log and 200 ppm Na‐hypochlorite by 2·2 log. Meanwhile, Na‐Chl‐based photosensitization reduces bacteria on the surface by 4·2 orders of magnitude. Conclusions: Food‐borne pathogen B. cereus could be effectively inactivated (7 log) by Na‐Chl‐based photosensitization in vitro and on the surface of packaging material. Spores are more resistant than vegetative cells to photosensitization‐based inactivation. Comparison of different surface decontamination treatments indicates that Na‐Chl‐based photosensitization is much more effective antibacterial tool than washing with water or 200 ppm Na‐hypochlorite. Significance and Impact of the Study: Our data support the idea that Na‐Chl‐based photosensitization has great potential for future application as an environment‐friendly, nonthermal surface decontamination technique.     

GROWTH RESPONSES OF THE DIATOM,CYCLOTELLA CRYPTICA (BACILLARIOPHYCEAE), TO GIBBERELLIC ACID1

The plant hormone, gibberellic acid (GA), stimulated growth of a marine diatom, Cyclotella cryptica Reimann, Lewin and Guillard. Four concentrations of GA (5 × 20 × 25 × and 35 × 10^?6 g/mL) were added to axenic cultures of C. cryptica. Changes in cell densities, measured by cell counts and turbidimetric readings, confirmed that GA at 20 × 10^?6 g/mL produced maximum stimulation. There was an increase in the total number of cells produced and a shorter lag phase of growth at this concentration. Coulter counter measurements of cell size, as well as ocular micrometer measurements, indicated there was no significant variation in cell volumes of GA grown cells over that of the controls.     

Production of microbial protein from tree bark by Phanerochaete chrysosporium

Phanerochaete chrysosporium was grown in fermentors on NaOH-extracted maple, pine, and cedar barks at the optimum substrate concentration of 1% (w/v). The yields (mg protein/liter) on maple, pine, and cedar were 1500, 1200, and 880, respectively, which are probably due to the different lignin contents of the barks. Lignin is not utilized. The productivities at 30°C obtained for pine (4.07 × 10^?2 g protein/liter hr) and cedar (2.63 × 10^?2 g protein/liter hr) barks were greater than for maple (2.63 × 10^?2 g protein/liter hr). The substrate (bark) was the limiting component of the fermentation. Over the 26–38°C temperature range protein productivity increased by a factor of three (1.55 × 10^?2 vs. 4.61 × 10^?2 g protein/liter hr) for maple bark. Low agitation rates resulted in an overproduction of cellulase and reduced levels of microbial protein.     

Catalytic resonance scattering spectral determination of ultratrace horseradish peroxidase using rhodamine S

A highly sensitive and selective resonance scattering spectral assay was proposed for the determination of horseradish peroxidase (HRP), based on its catalytic effect on the H₂O₂ oxidation of KI to form I₃^?. The I₃^? combined respectively with rhodamine (Rh) dye such as rhodamine S (RhS), rhodamine 6G (Rh6G), rhodamine B (RhB) and butyl‐rhodamine B (b‐RhB), to form association particles (Rh‐I₃)_n. The four Rh systems all exhibit a stronger resonance scattering (RS) peak at 424 nm. For the RhS, Rh6G, RhB and b‐RhB systems, HRP concentration in the range of 3.2 × 10^?12 to 4.8 × 10^?9, 2 × 10^?11 to 3.2 × 10^?9, 1.6 × 10^?11 to 3.2 × 10^?9 and 1.6 × 10^?11 to 4 × 10^?9 g/mL was linear to its RS intensity at 424 nm, with a detection limit of 2.2 × 10^?12, 2.5 × 10^?12, 4.4 × 10^?12 and 2.6 × 10^?12 g/mL, respectively. This RhS system was most sensitive and stable, and was applied for the determination of HRP in the hepatitis B surface antibody labeling HRP and water samples, with satisfactory results. Copyright © 2009 John Wiley & Sons, Ltd.     

Effect of trace elements and vitamins on the growth of Methanosarcina barkeri

Growth of Methanosarcina barkeri on methanol as energy source was found to be dependent on cobalt and molybdenum. In the presence of 10^?6 M Co and 5 × 10^?7M Mo optimal growth occurred. Furthermore it could be demonstrated that nickel and selenium each in a concentration of 10^?7 M stimulated the growth of this methanogenic bacterium while the following elements tested in the range of 10^?7 M to 10^?3 had no influence: B, Cr, Cu, Mn, Pb. The requirement of Co and Ni for optimal growth are in accordance with the results that the cells contain the Co containing corrinoid Factor III (0.1 – 0.2 mg 5-hydroxylbenzimidazolylcyanocobamide per g wet cells) and Factor F₄₃₀, a nickel component. Studies on the vitamin dependency of M. barkeri showed that this strain needs only the vitamin riboflavin for the growth in a defined medium. Under these conditions a cell density of 2.6 g dry cells/l could be obtained in a fed batch culture.     

Application of microbial cells as multistep catalysts in potentiometric biosensing electrodes

The advantages of using intact microbial cells to mediate complex reaction sequences in the construction of biosensing electrodes are domonstrated. A potentiometric sensor was developed for nitrilotriacetic acid (NTA) in which a strain of Pseudomonas sp. was coupled to an ammonia gas-sensing electrode. the bacterial cells carry out a four-step reaction sequence to produce the measured species, ammonia, from NTA. The resulting microbial electrode responded to NTA in the concentration range of 1 × 10^?4 M to 7 × 10^?4M, with a slope of 35-40 mV/decade. The electrode was stable for up to one month.     

Microbial nitrate respiration of lactate at in situ conditions in ground water from a granitic aquifer situated 450 m underground

There is widespread interest in developing methods to investigate in situ microbial activity in subsurface environments. Novel experiments based on single borehole push–pull methods were conducted to measure in situ microbial activity at the Äspö Hard Rock Laboratory (HRL). Microbial nitrate reduction and lactate consumption were measured at in situ conditions at a depth of 450 m in the HRL tunnel. A circulation system was used to circulate ground water from the aquifer through pressure‐maintaining flow cells containing coupons for biofilm growth. The system allows microbial investigations at in situ pressure, temperature and chemistry. Four experiments were conducted in which a combination of a conservative tracer, nitrate and lactate was injected into the circulation system. Rate of nitrate utilization was 5 µm  h^?1 without lactate and 13 µm  h^?1 with lactate. Lactate consumption increased from 30  to 50 µm  h^?1 with the addition of an exogenous electron acceptor (nitrate). Attached and unattached cells were enumerated using epifluorescence microscopy to calculate cell‐specific rates of activity. The biofilm had an average cell density of 1 × 10⁶ cells cm^?2 and there was an average of 6 × 10⁵ unattached cells mL^?1 in circulation. Cell‐specific rates of lactate consumption were higher than previously reported using radiotracer methods in similar environments. The differences highlight the importance of conducting microbial investigations at in situ conditions. The results demonstrate that an indigenous community of microbes survives at a depth of 450 m in the Fennoscandian shield aquifer with the potential to oxidize simple organic molecules such as lactate.     

Capillary electrophoresis analysis of isoniazid using luminol-periodate potassium chemiluminescence system

A rapid and simple capillary electrophoresis method coupled with chemiluminescent (CL) detection was proposed for analysis of isoniazid (ISO) based on the enhancement effect of ISO to CL emission of luminol‐periodate potassium reaction. Under the optimal conditions, ISO can be assayed in the range of 7.0 × 10^?7 to 3.0 × 10^?5 g mL^?1 (R² = 0.9990) with a limit of detection of 3.0 × 10^?7 g mL^?1 (signal‐to‐noise ratio of 3). The whole analysis process can be completed within 2.5 min with a theoretical plate number of 6258. The relative standard deviations of the signal intensity and the migration time were 3.1 and 1.4% for a standard sample at 1.0 × 10^?5 g mL^?1 (n = 5), respectively. The presented novel strategy was successfully applied to the determination of ISO in commercial pharmaceutical preparations and spiked human serum samples. Copyright © 2010 John Wiley & Sons, Ltd.     

Microbial degradation of poly-β-hydroxybutyrate using landfill soils

The population of poly-β-hydroxybutyrate-degrading microorganisms and the biodegradation of PHB in local landfill soils were examined in vitro and in vivo. Forty-two PHB-degraders consisting of 12 bacteria, 25 actinomycetes and 5 moulds were isolated. The total PHB-degraders averaged 4.7 × 10⁷ and 20 × 10⁴ colony forming units (cfu)/g for San Mateo wet and dry soils, respectively, and 2.3 × 10⁷ and 8.5 × 10⁴ cfu/g for Carmona wet and dry samples, respectively. The PHB-degraders formed 0–59% of the total microbial population in San Mateo and 8–42% in Carmona. Complete (100%) degradation of PHB powder was observed for Chryseomonas-27 and Aspergillus-39 on day 5 in shake flask culture and for Streptomyces-4 on day 7. Burial test in landfill soils showed a 90–91% weight loss of PHB film strips within four weeks; the weight loss of polypropylene film strips was up to 0.12% only. Scanning electron micrographs of degraded films revealed the attachment of microbial cells and fungal mycelium and spores on the surfaces. Holes and cavities were also noted due to the microbial degradation processes.     

Induction of metamorphosis of pediveliger larvae of the mussel Mytilus galloprovincialis Lamarck, 1819 using neuroactive compounds,KCl, NH4Cl and organic solvents

Pediveliger larvae of Mytilus galloprovincialis were subjected to a series of bioassays to investigate the induction of metamorphosis using neuroactive compounds, K⁺, NH₄ ⁺ and organic solvents. Growth and survival of post-larvae obtained using ethanol and methanol were also observed. Epinephrine, phenylephrine, clonidine and metanephrine induced larval metamorphosis at 10^?6 to 10^?4 M in both 24-h and continuous exposure assays. In 24-h exposure assays, α-methyldopa at 5×10^?5 M and methoxyphenamine at 5×10^?5?10^?4 M induced 55?94% metamorphosis. Similarly, excess K⁺ at 3×10^?2 M induced 39% metamorphosis and NH₄ ⁺ at 1?5×10^?2 M induced 63–78% metamorphosis. The EC50s of seven organic solvents ranged from 0.04 to 0.82 M. Post-larvae that metamorphosed using ethanol and methanol survived as juveniles and grew at the same rate as those from microbial biofilm. Thus, the above compounds can be useful inducers of metamorphosis for antifouling studies using larvae and juveniles of M. galloprovincialis.     

Pathways of Chlorophenol Formation in Oxidative Biodegradation of BHC

Hexose 1-phosphate uridylyltransferase (EC 2.7.7.12) was present constitutively in Bifidobacterium bifidum. The enzyme was purified to a homogeneous state from B. bifidum grown on a glucose medium and characterized. The molecular weight of the enzyme is about 110,000.The pH optimum of the enzyme was 7.5. The enzyme was very labile on the acidic side below pH 4.5. Thymidine diphosphate glucose could serve as a substrate with about 60% efficiency of UDP-glucose. The Km values for UDP-gtucose, galactose 1-phosphate (Gal-l-P), UDP-galactose and glucose 1-phosphate (Glc-1-P) were estimated to be 2.3×10^?5M, 5.0 × 10^?4M, 3.1 × 10^?5 M and 1.4 × 10^?4M, respectively. From these results the physiological roles of the enzyme were considered in relation to galactose metabolism in B. bifidum.