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Single cell protein production potential of enriched microbial populations from rice paddy soils and roots: Insights into protein yield enhancement by Methylophilaceae

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Microbial protein is proposed as an alternative protein source with low environmental impact. Methane oxidizing bacteria are already produced at commercial scale from natural gas. However, their productivity is limited because of the creation of explosive atmospheres in the fermenters during production. This work demonstrates the applicability of bioreactors with a membrane-based gas supply via diffusion. Methanotrophic bacteria were successfully cultivated, with growth yields from 0.26 to 0.43 g-VSS g-CH4⁻¹, slightly below those observed in analogous fermenters relying on bubbling. However, ammonia yields ranged from 5.2 to 6.9 g-VSS g-NH3⁻¹, indicating higher nitrogen assimilation than in conventional fermenters. Indeed, protein content increased during the operational period reaching up to 51% of dry weight. The amino acid profile included the majority of the essential amino acids, demonstrating suitability as feed ingredient. Never during the operational period was an explosive atmosphere established in the reactor. Thus, bubble-free membrane bioreactors are a promising technology for microbial protein production relying on explosive gas mixtures.
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Conventional microbial protein production relies on the usage of pure chemicals and gases. Natural gas, which is a fossil resource, is the common input gas for bacterial protein production. Alternative sources for gas feedstock and nutrients can sufficiently decrease the operational cost and environmental impact of microbial protein production processes. In the present study, the effluents streams of municipal biowaste anaerobic digestion, were used to grow methane oxidising bacteria which can be used as protein source. Results demonstrated that a 40:60 CH4:O2 (v/v) gas feeding resulted in microbial biomass production of 0.95 g-DM/L by a Methylophilus dominated community. When raw biogas was used as input for methane corresponding to the same initial methane partial pressure as before, instead of pure methane, the growth was partially hindered (0.61 g-DM/L) due to the presence of H2S (IC50: 1376 ppm). Hence, desulfurization is suggested before using biogas for microbial protein production. At semi-continuous mode, results showed that the produced biomass had relatively high protein content (>40% of dry weight) and the essential amino acids lysine, valine, leucine and histidine were detected at high levels.
Article
Release of abiotic methane from marine seeps into the atmosphere is a major source of this potent greenhouse gas. Methanotrophic microorganisms in methane seeps use methane as carbon and energy source, thus significantly mitigating global methane emissions. Here we investigated microbial methane oxidation at the sediment‐water interface of a shallow marine methane seep. Metagenomics and metaproteomics, combined with 13C‐methane stable isotope probing, demonstrated that various members of the gammaproteobacterial family Methylococcaceae were the key players for methane oxidation, catalyzing the first reaction step to methanol. We observed a transfer of carbon to methanol‐oxidizing methylotrophs of the betaproteobacterial family Methylophilaceae, suggesting an interaction between methanotrophic and methylotrophic microorganisms that allowed for rapid methane oxidation. From our microcosms, we estimated methane oxidation rates of up to 871 nmol of methane per gram sediment and day. This implies that more than 50% of methane at the seep is removed by microbial oxidation at the sediment‐water interface, based on previously reported in situ methane fluxes. The organic carbon produced was further assimilated by different heterotrophic microbes, demonstrating that the methane‐oxidizing community supported a complex trophic network. Our results provide valuable eco‐physiological insights into this specialized microbial community performing an ecosystem function of global relevance. This article is protected by copyright. All rights reserved.
Chapter
Rice fields are a major source of atmospheric methane (CH4), a greenhouse gas. CH4 emissions from wetland rice fields represents globally 15–20% of the annual anthropogenic CH4 emissions, and about 4% of the global CH4 emissions. Methane emission from rice cultivation may increase from the 1990 level of 97 Tg/year to 145 Tg/year by 2025 due to the increase in acreage and intensification of paddy cultivation. Here we review the role of anaerobic methanogenic bacteria in methane emission. We discuss the factors that influence methane emissions from rice fields, such as water regime, cropping season, soil temperature, fertilizer application, soil physico-chemical properties, crop cultivation, agricultural practices, soil type, soil profile and crop management practices. These practices control soil bacterial communities. Other influencing factors include intercultural operations such as ploughing, puddling and frequent mixing of soil during the paddy field preparation. Methane emission from paddy field follows a seasonal pattern of variation due to influence of climatic factors like temperature, sunlight, and precipitation. Algae, microphytes, macrophytes and anoxygenic photosynthetic bacteria significantly reduce CH4 emissions when they grow actively under illuminated condition. Methane emission is limited by alternate flooding-drying; cultivars with few unproductive tillers, small root system, high oxidative ability, and high harvest index; excessive application of organic amendments; application of potassium, biochar, nitrate, sulfate and ferric iron; and urease and nitrification inhibitors.
Article
The rhizosphere is the most dynamic hotspot of microbial activity in the soil. Despite these dynamics, the spatial pattern of many rhizosphere properties may remain stable because they are continuously reproduced in the changing environment. Low substrate concentration can strongly reduce the rate response of an enzymatic reaction subjected to increased temperature and is recognized as a canceling effect on enzyme temperature sensitivity. Carbon input from rhizodeposits affects C availability in the rhizosphere, and thus the enzyme activities responsible for organic matter decomposition, and their temperature sensitivities, upset the dynamics and stability of biochemical processes in the rhizosphere. However, it is unclear whether a canceling effect occurs in the rhizosphere. We studied temperature effects on chitinase and phosphatase during rice (Oryza sativa L.) growth at 18 and 25 °C. The spatial distribution of enzyme activities was imaged using soil zymography and showed that the overall activities of these enzymes increased with temperature but decreased with rice growth. The temporal dynamics of hotspot areas were enzyme-specific. During growing days 14–30, hotspot areas decreased from 2-2.5% to 0.3–0.5% for chitinase, but increased from 2% to 6–7% for phosphatase. The distribution pattern of both enzymes shifted from being dispersed throughout the soil to being associated with the roots. For the first time, we showed the extent of rhizosphere enzyme activity in paddy soil and demonstrated that it is temporally stationary and independent of temperature. However, the temperature sensitivity of enzyme activities declined radically (Q10∼1.3–1.4) at the root surface compared to that of bulk soil (Q10 ∼1). We conclude that the spatio-temporal pattern of rhizosphere enzymatic hotspots is mainly affected by plant growth. High temperature sensitivity (Q10 > 1) at the root-soil interface for the tested enzymes revealed that warming will lead to faster nutrient mobilization in the rhizosphere than in root-free soil.
Article
Univariate ANOVA is reviewed from a user point-of-view with emphasis on understanding the model building and the assumptions underlying the method. Illustrative examples are taken from organic chemistry and analytical chemistry. The use of graphical techniques to visualize the ANOVA model as well as to analyse residuals is recommended. The main models of ANOVA are developed in some detail including one-factor ANOVA, crossed designs, nested designs, repeated measures ANOVA and variance components estimation. Hypothesis testing by F-tests-and follow up by pairwise comparison methods is shown. The distinction between random effects and fixed effects is explained. Methods to handle non-linearities by transformations or by using response surface methodology are mentioned. Throughout the paper the importance of experimental design is emphasized. References are given to ANOVA methods for more complicated models.
Article
A field experiment was conducted to illustrate the different degree and dynamics of microbial community structure and function in the rhizosphere across four growing stages (before plantation and three growth stages) using a combination of biochemical (enzyme assay and microbial biomass carbon) and molecular approaches of qPCR and PCR-DGGE (polymerase chain reaction-denaturing gradient gel electrophoresis). Rice plant cultivation promoted higher enzyme activities (invertase and urease), microbial biomass carbon (Cmic), bacterial (16S rRNA) and fungal (ITS rRNA) genes abundances in the rhizosphere compared to unplanted soil. Principal component analyses of PCR-DGGE profile also revealed that structures of bacterial and fungal communities of rice planted soil were well distinct from unplanted soil. Moreover, enzyme activities showed a significant positive correlation with the total microbial biomass in the rhizosphere throughout growth stages of rice plant. Relative fungal: bacterial ratios were significantly higher in rice planted soil compared to unplanted soil, suggesting rice plantation enhanced the fungal community in the rice rhizosphere environment. These results further suggest a significant linkage between the microbial community dynamics and function in the rhizosphere associated with rice plant over time.
Article
The emission of the greenhouse gas CH4 from ricepaddies is strongly influenced by management practicessuch as the input of ammonium-based fertilisers. Weassessed the impact of different levels (200 and 400kgN.ha–1) of urea and (NH4)2HPO4on the microbial processes involved in production andconsumption of CH4 in rice field soil. We usedcompartmented microcosms which received fertilisertwice weekly. Potential CH4 production rates weresubstantially higher in the rice rhizosphere than inunrooted soil, but were not affected by fertilisation.However, CH4 emission was reduced by the additionof fertiliser and was negatively correlated with porewater NH 4 plus concentration, probably as theconsequence of elevated CH4 oxidation due tofertilisation. CH4 oxidation as well as numbersof methanotrophs was distinctly stimulated by theaddition of fertiliser and by the presence of the riceplant. Without fertiliser addition,nitrogen-limitation of the methanotrophs will restrictthe consumption of CH4. This may have a majorimpact on the global CH4 budget, asnitrogen-limiting conditions will be the normalsituation in the rice rhizosphere. Elevated potentialnitrifying activities and numbers were only detectedin microcosms fertilised with urea. However, asubstantial part of the nitrification potential in therhizosphere of rice was attributed to the activity ofmethanotrophs, as was demonstrated using theinhibitors CH3F and C2H2.
Article
SUMMARY More than IOO Gram-negative, strictly aerobic, methane-utilizing bacteria were isolated. All used only methane and methanol of the substrates tested for growth. The organisms were classified into five groups on the basis of mor- phology, fine structure, and type of resting stage formed (exospores and different types of cysts) and into subgroups on other properties. Methods of enrichment, isolation and culture are described.
Article
The glutamate dehydrogenase gene of Escherichia coli has been cloned into broad host-range plasmids and can complement glutamate synthase mutants of Methylophilus methylotrophus. Assimilation of ammonia via glutamate dehydrogenase is more energy-efficient than via glutamate synthase, thus the recombinant organism converts more growth substrate, methanol, into cellular carbon.
Article
The methanotrophic bacterium Methylococcus capsulatus (Bath) grows on pure methane. However, in a single cell protein production process using natural gas as methane source, a bacterial consortium is necessary to support growth over longer periods in continuous cultures. In different bioreactors of Norferm Danmark A/S, three bacteria consistently invaded M. capsulatus cultures growing under semi-sterile conditions in continuous culture. These bacteria have now been identified as a not yet described member of the Aneurinibacillus group, a Brevibacillus agri strain, and an acetate-oxidiser of the genus Ralstonia. The physiological roles of these bacteria in the bioreactor culture growing on natural, non-pure methane gas are discussed. The heterotrophic bacteria do not have the genetic capability to produce either the haemolytic enterotoxin complex HBL or non-haemolytic enterotoxin.
The Earth’s energy budget, climate feedbacks, and climate sensitivity
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Single cell protein production: a review
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