Methanotrophic Bacterial Biomass As Potential Mineral Feed Ingredients for Animals
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Hydrogen Isotope Fractionation in Lipids of the Methane-Oxidizing Bacterium Methylococcus Capsulatus
Geochimica et Cosmochimica Acta, Vol. 66, No. 22, pp. 3955–3969, 2002 Copyright © 2002 Elsevier Science Ltd Pergamon Printed in the USA. All rights reserved 0016-7037/02 $22.00 ϩ .00 PII S0016-7037(02)00981-X Hydrogen isotope fractionation in lipids of the methane-oxidizing bacterium Methylococcus capsulatus 1, 2 3 1 ALEX L. SESSIONS, *LINDA L. JAHNKE, ARNDT SCHIMMELMANN, and JOHN M. HAYES 1Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA 2Exobiology Branch, NASA-Ames Research Center, Moffett Field, CA 94035, USA 3Biogeochemical Laboratories, Department of Geological Sciences, Indiana University, Bloomington, IN 47405, USA (Received December 10, 2001; accepted in revised form June 7, 2002) Abstract—Hydrogen isotopic compositions of individual lipids from Methylococcus capsulatus, an aerobic, methane-oxidizing bacterium, were analyzed by hydrogen isotope-ratio-monitoring gas chromatography–mass spectrometry (GC-MS). The purposes of the study were to measure isotopic fractionation factors between methane, water, and lipids and to examine the biochemical processes that determine the hydrogen isotopic composition of lipids. M. capsulatus was grown in six replicate cultures in which the ␦D values of methane and water were varied independently. Measurement of concomitant changes in ␦D values of lipids allowed estimation of the proportion of hydrogen derived from each source and the isotopic fractionation associated with the utilization of each source. All lipids examined, including fatty acids, sterols, and hopanols, derived 31.4 Ϯ 1.7% of their hydrogen from methane. This was apparently true whether the cultures were harvested during exponential or stationary phase. Examination of the relevant biochemical pathways indicates that no hydrogen is transferred directly (with C-H bonds intact) from methane to lipids. -
Gas Fermentation of C1 Feedstocks: Commercialization Status and Future Prospects
Review Gas fermentation of C1 feedstocks: commercialization status and future prospects Leonardo V. Teixeira, Liza F. Moutinho, and Aline S. Romão-Dumaresq, SENAI Innovation Institute for Biosynthetics, Technology Center for Chemical and Textile Industry, Rio de Janeiro, Brazil Received December 04, 2017; revised June 04, 2018; accepted June 05, 2018 View online at Wiley Online Library (wileyonlinelibrary.com); DOI: 10.1002/bbb.1912; Biofuels, Bioprod. Bioref. (2018) Abstract: The increasing emissions of carbon dioxide, methane and carbon oxide (collectively referred as C1 compounds) are likely to configure a major contribution to global warming and other envi- ronmental issues. The implementation of carbon capture and storage (CCS) is considered a crucial strategy to prevent global warming, but the overall costs of currently available CCS technologies are still prohibitive for its large-scale deployment. Using microorganisms capable of assimilating C1 com- pounds for producing value-added products could be an important driver for mitigating emissions and minimizing their deleterious consequences, while simultaneously deriving additional economic benefits from these compounds. This review summarizes the main microorganisms and metabolic routes being investigated, with special focus on both the products targeted and the current industrial initiatives. There are a number of companies investing in these routes and in some instances commercial deploy- ment was identified. Despite the variety of commercially-appealing products, genetic manipulation -
Reduced Net Methane Emissions Due to Microbial Methane Oxidation in a Warmer Arctic
LETTERS https://doi.org/10.1038/s41558-020-0734-z Reduced net methane emissions due to microbial methane oxidation in a warmer Arctic Youmi Oh 1, Qianlai Zhuang 1,2,3 ✉ , Licheng Liu1, Lisa R. Welp 1,2, Maggie C. Y. Lau4,9, Tullis C. Onstott4, David Medvigy 5, Lori Bruhwiler6, Edward J. Dlugokencky6, Gustaf Hugelius 7, Ludovica D’Imperio8 and Bo Elberling 8 Methane emissions from organic-rich soils in the Arctic have bacteria (methanotrophs) and the remainder is mostly emitted into been extensively studied due to their potential to increase the atmosphere (Fig. 1a). The methanotrophs in these wet organic the atmospheric methane burden as permafrost thaws1–3. soils may be low-affinity methanotrophs (LAMs) that require However, this methane source might have been overestimated >600 ppm of methane (by moles) for their growth and mainte- without considering high-affinity methanotrophs (HAMs; nance23. But in dry mineral soils, the dominant methanotrophs are methane-oxidizing bacteria) recently identified in Arctic min- high-affinity methanotrophs (HAMs), which can survive and grow 4–7 eral soils . Herein we find that integrating the dynamics of at a level of atmospheric methane abundance ([CH4]atm) of about HAMs and methanogens into a biogeochemistry model8–10 1.8 ppm (Fig. 1b)24. that includes permafrost soil organic carbon dynamics3 leads Quantification of the previously underestimated HAM-driven −1 to the upland methane sink doubling (~5.5 Tg CH4 yr ) north of methane sink is needed to improve our understanding of Arctic 50 °N in simulations from 2000–2016. The increase is equiva- methane budgets. -
Discovery, Taxonomic Distribution, and Phenotypic Characterization of a Gene Required for 3-Methylhopanoid Production
Discovery, taxonomic distribution, and phenotypic characterization of a gene required for 3-methylhopanoid production The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story matters. Citation Welander, P. V., and R. E. Summons. “Discovery, Taxonomic Distribution, and Phenotypic Characterization of a Gene Required for 3-methylhopanoid Production.” Proceedings of the National Academy of Sciences 109.32 (2012): 12905–12910. CrossRef. Web. As Published http://dx.doi.org/10.1073/pnas.1208255109 Publisher National Academy of Sciences (U.S.) Version Final published version Citable link http://hdl.handle.net/1721.1/77589 Terms of Use Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. Discovery, taxonomic distribution, and phenotypic characterization of a gene required for 3-methylhopanoid production Paula V. Welander1 and Roger E. Summons Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, 77 Massachusetts Avenue, E25-629, Cambridge, MA 02139 Edited by John M. Hayes, Woods Hole Oceanographic Institution, Berkeley, CA, and approved July 2, 2012 (received for review May 15, 2012) Hopanoids methylated at the C-3 position are a subset of bacterial majority of C-3 methylated hopanoid producers are aerobic triterpenoids that are readily preserved in modern and ancient se- methanotrophs. However, the production of 3-methylhopanoids diments and in petroleum. The production of 3-methylhopanoids has also been demonstrated in the acetic acid bacteria (12) indi- by extant aerobic methanotrophs and their common occurrence cating that the taxonomic distribution of 3-methylhopanoids is in modern and fossil methane seep communities, in conjunction not restricted to methanotrophs. -
The Ratio of Methanogens to Methanotrophs and Water-Level Dynamics Drive Methane Exchange Velocity in a Temperate Kettle-Hole Peat Bog
Biogeosciences Discuss., https://doi.org/10.5194/bg-2019-116 Manuscript under review for journal Biogeosciences Discussion started: 23 April 2019 c Author(s) 2019. CC BY 4.0 License. The ratio of methanogens to methanotrophs and water-level dynamics drive methane exchange velocity in a temperate kettle-hole peat bog Camilo Rey-Sanchez1,4, Gil Bohrer1, Julie Slater2, Yueh-Fen Li3, Roger Grau-Andrés2, Yushan Hao2, 5 Virginia I. Rich3, & G. Matt Davies2 1Department of Civil and Environmental Engineering and Geodetic Science, The Ohio State University, Columbus, Ohio, 43210, USA 2School of Environment and Natural Resources, The Ohio State University, Columbus, Ohio, 43210, USA 3Department of Microbiology, The Ohio State University, Columbus, Ohio, 43210, USA 10 4Current address, Department of Environmental Science, Management and Policy, University of California- Berkeley, California, 94720, USA Correspondence to: Camilo Rey-Sanchez ([email protected]) 15 Abstract. Peatlands are a large source of methane (CH4) to the atmosphere, yet the uncertainty around the estimates of CH4 flux from peatlands is large. To better understand the spatial heterogeneity in temperate peatland CH4 emissions and their response to physical and biological drivers, we studied CH4 dynamics throughout the growing seasons of 2017 and 2018 in Flatiron Lake Bog, a kettle-hole peat bog in Ohio. The site is composed of six different hydro-biological zones: an open water zone, four concentric vegetation zones surrounding the open water, and a restored zone connected to the main bog by a narrow 20 channel. At each of these locations, we monitored water level (WL), CH4 pore-water concentration at different peat depths, CH4 fluxes from the ground and from representative plant species using chambers, and microbial community composition with focus here on known methanogens and methanotrophs. -
Downloaded from the Fungene Database (
bioRxiv preprint doi: https://doi.org/10.1101/2020.09.21.307504; this version posted September 22, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. Enhancement of nitrous oxide emissions in soil microbial consortia via copper competition between proteobacterial methanotrophs and denitrifiers Jin Chang,a,b Daehyun Daniel Kim,a Jeremy D. Semrau,b Juyong Lee,a Hokwan Heo,a Wenyu Gu,b* Sukhwan Yoona# aDepartment of Civil and Environmental Engineering, Korea Advanced Institute of Science and Technology, Daejeon, 34141, Korea bDepartment of Civil and Environmental Engineering, University of Michigan, Ann Arbor, MI, 48109 Running Title: Methanotrophic influence on N2O emissions #Address correspondence to Sukhwan Yoon, [email protected]. *Present address: Department of Civil & Environmental Engineering, Stanford University, Palo Alto CA, 94305 bioRxiv preprint doi: https://doi.org/10.1101/2020.09.21.307504; this version posted September 22, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. Abstract Unique means of copper scavenging have been identified in proteobacterial methanotrophs, particularly the use of methanobactin, a novel ribosomally synthesized post-translationally modified polypeptide that binds copper with very high affinity. The possibility that copper sequestration strategies of methanotrophs may interfere with copper uptake of denitrifiers in situ and thereby enhance N2O emissions was examined using a suite of laboratory experiments performed with rice paddy microbial consortia. Addition of purified methanobactin from Methylosinus trichosporium OB3b to denitrifying rice paddy soil microbial consortia resulted in substantially increased N2O production, with more pronounced responses observed for soils with lower copper content. -
Methane Utilization in Methylomicrobium Alcaliphilum 20ZR: a Systems Approach Received: 8 September 2017 Ilya R
www.nature.com/scientificreports OPEN Methane utilization in Methylomicrobium alcaliphilum 20ZR: a systems approach Received: 8 September 2017 Ilya R. Akberdin1,2, Merlin Thompson1, Richard Hamilton1, Nalini Desai3, Danny Alexander3, Accepted: 22 January 2018 Calvin A. Henard4, Michael T. Guarnieri4 & Marina G. Kalyuzhnaya1 Published: xx xx xxxx Biological methane utilization, one of the main sinks of the greenhouse gas in nature, represents an attractive platform for production of fuels and value-added chemicals. Despite the progress made in our understanding of the individual parts of methane utilization, our knowledge of how the whole-cell metabolic network is organized and coordinated is limited. Attractive growth and methane-conversion rates, a complete and expert-annotated genome sequence, as well as large enzymatic, 13C-labeling, and transcriptomic datasets make Methylomicrobium alcaliphilum 20ZR an exceptional model system for investigating methane utilization networks. Here we present a comprehensive metabolic framework of methane and methanol utilization in M. alcaliphilum 20ZR. A set of novel metabolic reactions governing carbon distribution across central pathways in methanotrophic bacteria was predicted by in-silico simulations and confrmed by global non-targeted metabolomics and enzymatic evidences. Our data highlight the importance of substitution of ATP-linked steps with PPi-dependent reactions and support the presence of a carbon shunt from acetyl-CoA to the pentose-phosphate pathway and highly branched TCA cycle. The diverged TCA reactions promote balance between anabolic reactions and redox demands. The computational framework of C1-metabolism in methanotrophic bacteria can represent an efcient tool for metabolic engineering or ecosystem modeling. Climate change concerns linked to increasing concentrations of anthropogenic methane have spiked inter- est in biological methane utilization as a novel platform for improving ecological and human well-being1–4. -
(Antarctica) Glacial, Basal, and Accretion Ice
CHARACTERIZATION OF ORGANISMS IN VOSTOK (ANTARCTICA) GLACIAL, BASAL, AND ACCRETION ICE Colby J. Gura A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE December 2019 Committee: Scott O. Rogers, Advisor Helen Michaels Paul Morris © 2019 Colby Gura All Rights Reserved iii ABSTRACT Scott O. Rogers, Advisor Chapter 1: Lake Vostok is named for the nearby Vostok Station located at 78°28’S, 106°48’E and at an elevation of 3,488 m. The lake is covered by a glacier that is approximately 4 km thick and comprised of 4 different types of ice: meteoric, basal, type 1 accretion ice, and type 2 accretion ice. Six samples were derived from the glacial, basal, and accretion ice of the 5G ice core (depths of 2,149 m; 3,501 m; 3,520 m; 3,540 m; 3,569 m; and 3,585 m) and prepared through several processes. The RNA and DNA were extracted from ultracentrifugally concentrated meltwater samples. From the extracted RNA, cDNA was synthesized so the samples could be further manipulated. Both the cDNA and the DNA were amplified through polymerase chain reaction. Ion Torrent primers were attached to the DNA and cDNA and then prepared to be sequenced. Following sequencing the sequences were analyzed using BLAST. Python and Biopython were then used to collect more data and organize the data for manual curation and analysis. Chapter 2: As a result of the glacier and its geographic location, Lake Vostok is an extreme and unique environment that is often compared to Jupiter’s ice-covered moon, Europa. -
Global Molecular Analyses of Methane Metabolism in Methanotrophic Alphaproteobacterium, Methylosinus Trichosporium Ob3b
ORIGINAL RESEARCH ARTICLE published: 03 April 2013 doi: 10.3389/fmicb.2013.00070 Global molecular analyses of methane metabolism in methanotrophic Alphaproteobacterium, Methylosinus trichosporium OB3b. Part II. metabolomics and 13C-labeling study SongYang 1, Janet B. Matsen1, Michael Konopka1, Abigail Green-Saxena2, Justin Clubb1, Martin Sadilek 3, Victoria J. Orphan4, David Beck 1,5 and Marina G. Kalyuzhnaya6* 1 Department of Chemical Engineering, University of Washington, Seattle, WA, USA 2 Division of Biology, California Institute of Technology, Pasadena, CA, USA 3 Department of Chemistry, University of Washington, Seattle, WA, USA 4 Division of Geological and Planetary Sciences; California Institute of Technology, Pasadena, CA, USA 5 eScience Institute, University of Washington, Seattle, WA, USA 6 Department of Microbiology, University of Washington, Seattle, WA, USA Edited by: In this work we use metabolomics and 13C-labeling data to refine central metabolic Amy V. Callaghan, University of pathways for methane utilization in Methylosinus trichosporium OB3b, a model alphapro- Oklahoma, USA teobacterial methanotrophic bacterium. We demonstrate here that similar to non-methane Reviewed by: Alan A. DiSpirito, Ohio State utilizing methylotrophic alphaproteobacteria the core metabolism of the microbe is rep- University, USA resented by several tightly connected metabolic cycles, such as the serine pathway, the Amy V. Callaghan, University of ethylmalonyl-CoA (EMC) pathway, and the citric acid (TCA) cycle. Both in silico estimations Oklahoma, USA and stable isotope labeling experiments combined with single cell (NanoSIMS) and bulk *Correspondence: biomass analyses indicate that a significantly larger portion of the cell carbon (over 60%) is Marina G. Kalyuzhnaya, Department 13 of Microbiology, University of derived from CO2 in this methanotroph. -
Gas Fermentation at Calysta
Gas Fermentation at Calysta Intro for REMEDY workshop October 20, 2020 Gas Fermentation is the Next Step in Industrial Biotech • Lower cost feedstocks are needed for biological products to compete with petroleum derivatives • C1 feedstocks (CH4, CO, CO2) are accepted to be among the cheapest sources of carbon • C1 feedstocks are generally pollutants, with significant safety and solubility issues compared to traditional biofeedstocks • Calysta owns the world’s only commercially-validated gas fermentation technology allowing use of C1 feedstocks 22/10/2020 2 Calysta’s Methanotroph Platform Methylococcus capsulatus Bath • Gammaproteobacteria, type I methanotroph • Relatively fast growth rate (methane:oxygen mix) • Genome sequence available • Amenable to genetic manipulation • Only methanotroph proven at commercial scale • Variety of formats for strain testing: well plates, pressure bottles, 2L fermenters • Amended media and optimized feeding strategies produce high cell densities in small scale. 22/10/2020 3 3 Calysta’s Platform: Strain Engineering Calysta has developed a set of novel engineering tools for methanotrophs: • Reporter genes Different promoter gene-fusions with synthetic fluorescent and chromogenic proteins (non-Aequorea) expressed in M. capsulatus • Plasmids that replicate both in methanotrophs and in E. coli • Constitutive and inducible (low/med/high) promoters • Techniques for chromosomal knockin and knockouts 4 Calysta Performs Methanotrophic Fermentation at All Scales Fermentors High Throughput TPP NorFerm Commercial Plant -
Nitrification 31
NITROGEN IN SOILS/Nitrification 31 See also: Eutrophication; Greenhouse Gas Emis- Powlson DS (1993) Understanding the soil nitrogen cycle. sions; Isotopes in Soil and Plant Investigations; Soil Use and Management 9: 86–94. Nitrogen in Soils: Cycle; Nitrification; Plant Uptake; Powlson DS (1999) Fate of nitrogen from manufactured Symbiotic Fixation; Pollution: Groundwater fertilizers in agriculture. In: Wilson WS, Ball AS, and Hinton RH (eds) Managing Risks of Nitrates to Humans Further Reading and the Environment, pp. 42–57. Cambridge: Royal Society of Chemistry. Addiscott TM, Whitmore AP, and Powlson DS (1991) Powlson DS (1997) Integrating agricultural nutrient man- Farming, Fertilizers and the Nitrate Problem. Wallingford: agement with environmental objectives – current state CAB International. and future prospects. Proceedings No. 402. York: The Benjamin N (2000) Nitrates in the human diet – good or Fertiliser Society. bad? Annales de Zootechnologie 49: 207–216. Powlson DS, Hart PBS, Poulton PR, Johnston AE, and Catt JA et al. (1998) Strategies to decrease nitrate leaching Jenkinson DS (1986) Recovery of 15N-labelled fertilizer in the Brimstone Farm experiment, Oxfordshire, UK, applied in autumn to winter wheat at four sites in eastern 1988–1993: the effects of winter cover crops and England. Journal of Agricultural Science, Cambridge unfertilized grass leys. Plant and Soil 203: 57–69. 107: 611–620. Cheney K (1990) Effect of nitrogen fertilizer rate on soil Recous S, Fresnau C, Faurie G, and Mary B (1988) The fate nitrate nitrogen content after harvesting winter wheat. of labelled 15N urea and ammonium nitrate applied to a Journal of Agricultural Science, Cambridge 114: winter wheat crop. -
Specialized Metabolites from Methylotrophic Proteobacteria Aaron W
Specialized Metabolites from Methylotrophic Proteobacteria Aaron W. Puri* Department of Chemistry and the Henry Eyring Center for Cell and Genome Science, University of Utah, Salt Lake City, UT, USA. *Correspondence: [email protected] htps://doi.org/10.21775/cimb.033.211 Abstract these compounds and strategies for determining Biosynthesized small molecules known as special- their biological functions. ized metabolites ofen have valuable applications Te explosion in bacterial genome sequences in felds such as medicine and agriculture. Con- available in public databases as well as the availabil- sequently, there is always a demand for novel ity of bioinformatics tools for analysing them has specialized metabolites and an understanding of revealed that many bacterial species are potentially their bioactivity. Methylotrophs are an underex- untapped sources for new molecules (Cimerman- plored metabolic group of bacteria that have several cic et al., 2014). Tis includes organisms beyond growth features that make them enticing in terms those traditionally relied upon for natural product of specialized metabolite discovery, characteriza- discovery, and recent studies have shown that tion, and production from cheap feedstocks such examining the biosynthetic potential of new spe- as methanol and methane gas. Tis chapter will cies indeed reveals new classes of compounds examine the predicted biosynthetic potential of (Pidot et al., 2014; Pye et al., 2017). Tis strategy these organisms and review some of the specialized is complementary to synthetic biology approaches metabolites they produce that have been character- focused on activating BGCs that are not normally ized so far. expressed under laboratory conditions in strains traditionally used for natural product discovery, such as Streptomyces (Rutledge and Challis, 2015).