Greenhouse gases such as carbon dioxide, methane, nitrous oxide, moisture and ozone contribute to climate change and global warming by absorbing light energy in visible and infrared region (Lashof and Ahuja, 1990). Among green house gases methane is the second most important gas after CO2 which contributes to global warming (Van Nevel and Demeyer, 1996; IPCC, 2007). Methane makes up 16% of total global GHG emissions (Scheehle and Kruger, 2006) having 23 times more global warming potential than carbon dioxide (IPCC, 2007). Methane emissions from agriculture represent around 40% of those produced by human-related activities (Steinfeld et al., 2006) and is the single largest source (25%) in enteric fermentation in livestock, mainly ruminants (Olivier et al., 1999).
Methanogens belong to the domain Archaea under the phylum Euryarchaeota. Unlike Bacteria, methanogens lack peptidoglycan in the cell wall, replaced by pseudomurein in Methanobrevibacter and Methanobacterium, heteropolysaccharide in Methanosarcina, and protein in Methanomicrobium. Apart from cell wall, there are certain other characteristics that differentiate archaea from bacteria and eukarya. Antibiotic sensitivity is absent in archaea which is present in bacteria and eukarya. The cell membrane in archaea have branched carbon chains linked with an ether linkage to the respective alcohols whereas bacteria and eukarya have unbranched carbon chains linked with ester linkage to the respective alcohols.
SOURCES OF METHANE EMISSION
There are both natural and human sources of methane emissions. The main natural sources include wetlands, termites and the oceans. Natural sources create 36% of methane emissions. Important human sources come from landfills, livestock farming, as well as the production, transportation and use of fossil fuels. Human-related sources create the majority of methane emissions, accounting for 64% of the total.
Methane levels have more than doubled over the last 150 years because of human activities like fossil fuel use and intensive farming. Before the Industrial Revolution, the atmospheric concentration of methane was maintained in a safe range by natural sinks.
But for a long time now human activities have been creating methane emissions much more rapidly than the Earth can remove them, increasing global methane levels.
According to NRC (1994), methanogenesis is the production of methane by bacteria. Because they thrive without oxygen, methanogenic bacteria have an important role in the subsurface, where oxygen is often absent.It is the bacterial conversion of methanogenic substrates [acetate, formate, hydrogen, carbon dioxide] into methane.
Methanogenesis is a multistep process carried out by different groups of microorganisms. The various processes and microorganisms included are:-
Hydrolysis is used to break down larger polymers i.e. it involves the breakdown of large polysaccharides. Through hydrolysis large polymers, namely proteins, fats and carbohydrates, are broken down into smaller molecules such as amino acids, fatty acids, and simple sugars. While some of the products of hydrolysis, including hydrogen and acetate, may be used by methanogens later in the anaerobic digestion process, the majority of the molecules must be further broken down in the process of acidogenesis to be used to create methane. eg Fibrobacter succinogens, Ruminococcus albus etc
Acidogenesis is the next step of anaerobic digestion in which acidogenic microorganisms further break down the product of hydrolysis. These fermentative bacteria produce an acidic environment forming ammonia, H2, CO2, H2S, shorter volatile fatty acids, carbonic acids, alcohols, as well as trace amounts of other byproducts. e.g Lactobacillus spp
Acetogenesis is the creation of acetate from carbon and energy sources by acetogens. These microorganisms catabolize many of the products created in acidogenesis into acetic acid, CO2 and H2. Acetogens break down the biomass to a point to which methanogens can utilize much of the remaining material to create methane. e.g Clostridia spp
CO2 + 3 H2 → CH3 COOH
Methanogenesis constitutes the final stage in which methanogens create methane from the final products of acetogenesis as well as from some of the intermediate products from hydrolysis and acidogenesis. There are two general pathways involving the use of acetic acid and carbon dioxide, the two main products of the first three steps of anaerobic digestion, to create methane in methanogenesis:
CO2 + 4 H2 → CH4 + 2H2O
CH3COOH → CH4 + CO2
Based on the substrate utilized these methanogenic bacteria can be classified as:-
- Hydrogenotropic – utilizing hydrogen and formate as substrate. Example include Methanobrevibacter ruminantium.
- Acetoclastic – utilizing acetate as a substrate. Example include Methanosaeta
- Methylotropic – utilizing methyl groups as a substrate. Example include Methanosarcina barkeri.
The production of methane is through various pathways. The important ones include
- The predominant pathway is the hydrogenotrophic using CO2 as the carbon source and H2 as the main electron donor
- Methane is also produced from acetate via the acetoclastic pathway eg Methanosacrcina and Methanotrix (Methanosaeta).
- Formate is also an important electron donor used by many rumen hydrogenotrophic methanogens and may account for up to 18% of the methane produced in the rumen
- Methylamines and methanol produced in the rumen can also be used by methylotrophic methanogens of the order Methanosarcinales and Methanobacteriales.
All the pathways have in common the demethylation of methyl–coenzyme M to methane and the reduction of the heterodisulfide of coenzyme M and coenzyme B catalysed by methyl–coenzyme M and heterodisulfide reductases.
COENZYMES FOR METHANOGENESIS
Methanogenesis pathways utilize several coenzymes of which methanofuran (MF), tetrahydromethanopterin (H4MPT), tetrahydrosarcinapterin (H4SPT) and coenzyme M (or HS-CoM) carry the carbon moiety destined to generate methane, while coenzyme F420, coenzyme B (HS-CoB), methanophenazine and coenzyme F430 transfer electrons that are used in carbon reduction
In this pathway, carbon dioxide is captured by methanofuran(MF) to form an unstable compound called carboxy-MF which is reduced by formyl-MF dehydrogenase in an energy-dependent manner to formyl-MF with a low-potential ferredoxin serving as electron carrier. Formyl-MF dehydrogenase exists in two forms, one of which contains molybdenum and the other tungsten.
At the next step the formyl group is transferred to H4MPT by a transferase enzyme to form formyl-H4MPT. From this stage, H4MPT carries four forms of the fixed carbon representing three oxidation states. First formyl-H4MPT is dehydrated by methenyl-H4MPT cyclohydrolase to form methenyl-H4MPT which in turn is reduced to methylene-H4MPT by the action of one of the two enzymes, F420-dependent methylene-H4MPT dehydrogenase and a Fe-containing hydrogenase.Methylene-H4MPT is reduced with F420H2 and by the action of F420-dependent methylene-H4MPT reductase (Mer) providing the last H4MPT derivative on the pathway, methyl-H4MPT. The transfer of the methyl group from methyl-H4MPT to coenzyme M is catalyzed by a membrane-bound sodium ion (Na+)-pumping enzyme complex called methyl-H4MPT:coenzyme M methyl transferase. This complex not only yields methyl-coenzyme but also generates a Na+-gradient that is used for energy production.
The next step in the sequence yields methane. This last carbon-reduction reaction is catalyzed by CH3-CoM reductase with coenzyme B serving as an electron source, resulting in a heterodisulfide, CoM-S-S-CoB, as product in addition to methane. The heterodisulfide is reduced by a reductase to regenerate HS-CoM and HS-CoB. Hydrogen-oxidizing methanogens often carry two CH3-CoM reductase isozymes (McrI and McrII) one of which is effective under high hydrogen availability and the other under low hydrogen conditions.
About 70% of the biologically produced methane originates from acetate. The methyl group of acetate is reduced to methane and the carboxyl group is oxidized to CO2.
The process begins with the activation of acetate by the action of acetate kinase generating acetyl-CoA . At first there is generation of ADP that is converted back to ATP via electron transport phosphorylation at an ATPase. The next step is the breakage of the carbon-carbon bond of the acetate moiety in acetyl-CoA catalyzed by an acetyl-CoA decarbonylase/synthase-carbon monoxide dehydrogenase complex. The carbonyl group of acetyl-CoA is oxidized to CO2 by the CODH component and the two electrons generated by this process help to reduce ferredoxin .The methyl group of the acetyl group is transferred to H4MPT via a corrinoid cofactor of the CODH complex, producing CH3-H4MPT. The methyl group of CH3-H4MPT leads to methane via the actions of methyl-H4MPT:coenzyme M methyl transferase and methyl-CoM reductase.
Methanogenesis from methanol involves the formation of methyl-CoM as an intermediate. Methanol provides both carbon and reductant for methanogenesis and this process consumes four moles of methanol for every three moles methane generated. Of these, one mole of methanol is oxidized to CO2, generating six-electron equivalents of reductant, which are then used to convert three moles of methanol to three moles of methane.
The oxidation of methanol to CO2 involves a part of the CO2reduction pathway, but in the reverse direction. The methyl groups enter this oxidation process at the methyl-coenzyme M stage by the action of two methyl transferases, MT1 and MT2.MT1 is a two-subunit enzyme (MtaBC) and MT2 has one subunit (MtaA).
The first reaction involves transfer of the methyl group of methanol by MT1 to the corrinoid co-factor of its MtaC subunit; this is an automethylation process.Then MT2-M or MtaA transfers the methyl group from MtaC to HS-CoM, generating methyl-coenzyme M.). The methyl groups destined for oxidation are transferred from CH3-CoM to H4MPT by the membrane-bound methyl-H4MPT:coenzyme M methyl transferase.This endergonic reaction is assisted by a Na+-gradient and generates CH3-H4MPT which then leads to methane production similar to other pathways.
METHANOGENESIS FROM FORMATE
The carbon transfer and reduction steps in this process are similar to those described above for methanogensis from H2+CO2 . Both the CO2 and reducing power are derived from formate by the action of an F420-dependent formate dehydrogenase (FdhABC); FdhAB subunits form the enzyme that produces CO2 and reduced F420or F420H2 and FdhC is thought to import formate into the cell. CO2 is converted to methane using the CO2-reduction pathway i.e Hydrogenotropic pathway.
METHANOGENESIS IN RICE FIELDS AND WETLANDS
Wetlands and rice fields are characterized by water-logged soils and distinctive communities of plant and animal species that have evolved and adapted to the constant presence of water. Due to this high level of water saturation as well as warm weather, wetlands and rice fields are one of the most significant natural sources of atmospheric methane.
Anaerobic decomposition of organic material in flooded rice fields produces methane. Anaerobic conditions occur in rice field as a result of soil submergence. Water saturation of soil limits the transport of oxygen in soil resulting in higher activity of methanogens to produce methane. Under anaerobic and reduced conditions methanogens produce methane either by using CO2 and H2 or by using acetate. Under steady conditions methanogenesis by acetoclastic pathway predominates and accounts for 75-80% of total methane emitted.
Pathways of Methane Emission
Diffusion through the profile refers to the movement of methane up through soil and bodies of water to reach the atmosphere. The importance of diffusion as a pathway varies per wetland based on the type of soil and vegetation. For example, in peatlands, the amount of dead, organic matter results in relatively slow diffusion of methane through the soil. Additionally, because methane can travel more quickly through soil than water, diffusion plays a much bigger role in wetlands with drier soil.
Plant aerenchyma refers to the vessel-like transport tubes within the tissues of certain kinds of plants. Plants with arenchyma possess porous tissue that allows for direct travel of gases to and from the plant roots. Methane can travel directly up from the soil into the atmosphere using this transport system.
Ebullition refers to the sudden release of bubbles of methane into the air. These bubbles occur as a result of methane building up over time in the soil, forming pockets of methane gas. As these pockets of trapped methane grow in size, the level of the soil will slowly rise up as well. This phenomenon continues until so much pressure builds up that the bubble “pops,” transporting the methane up through the soil so quickly that it does not have time to be consumed by the methanotrophic organisms in the soil.
Factors affecting methane production
Temperature -it plays a very important role in methane production. At 40-500 C methanogenesis is done only by hydrogenotrophic methanogens.
Stage of plant –the stage of plant decides which form of methanogenic dominates at a particular stage. However, at flowering stage both acetoclastic and hydrogenotrophic methanogens are higher.
Soil depth -depth of the soil is important for survival of methanogens. Methanogens usually occur at a higher population in the top soil.
pH –The optimum pH for growth of these methanogens is 6.5-6.9, therefore it is important to maintain pH of soil at this range.
Addition of nitrates and sulphates -addition of nitrates and sulphates in the soil in form of fertilizers help reduce methane production, as these act as alternate sink to use hydrogen.
METHANOGENESIS IN TERMITES
The termite gut consists of fore gut (which includes the crop and muscular gizzard), the tubular mid gut (which as in other insects is a key site for secretion of digestive enzymes and for absorption of soluble nutrients) and relatively, a voluminous hindgut (which is also a major site for digestion and for absorption of nutrients). some bacteria colonize the foregut and midgut, bulk of intestinal microbiota is found in the hindgut, especially in the paunch.
Termites have good sources of wood-degrading enzymes such as xylanases, laccases; as their main dietary component is wood. Along with bacterial spp like Bacteroides Cellulomonas, Spiromusa termitida etc termites harbour flagellate protists that fill up the bulk of the hindgut paunch. The gut flagellate includes Trichonympha, Calonympha which degrade the lignocellulosic feed with formation of excess hydrogen as intermediate.
This large number of bacterial, archael and protozoal population inhabit the gut of termites. This partnership with a diverse community of bacterial, archaeal and eukaryotic gut symbionts break down the plant fibre and ferment the products to acetate and variable amounts of methane, with hydrogen as a central intermediate.
The fermentation of wood polysaccharides by the gut flagellates yields acetate and other short-chain fatty acids, which are resorbed by the host. Hydrogen is an important intermediate that drives the reduction of CO2, which yields additional acetate and some methane. Although H2 may strongly accumulate at the gut centre, most of it is consumed before it can escape from the gut.
Methanogenic archaea (methanogens) that inhabit the gut of termites generate enormous amount of methane that adds to the global atmospheric methane (CH4). The predominant species is Methanosarcina barkeri using acetate as major source of methane production. The total methane contribution due to termites is probably less than 15 Tg per year.
METHANOGENESIS IN LANDFILLS
A mixture of organic and inorganic wastes is disposed at a landfill with varying humidity and much heterogeneity. Approximately 75% of municipal waste is biodegradable organic material. Substances in waste have various decomposition rates. Food waste is most readily degraded. Garden waste forms a group with medium halflife (5 years). Paper, cardboard, wood and textile waste decomposes slowly (half-life of 15 years), while plastics and rubber are not degraded at all . A number of factors affect the quantity of gases formed at landfills and their composition, such as waste type and age, quantity and type of organic components, waste humidity and temperature.
MECHANISM OF METHANE FORMATION
The organic matter undergoes hydrolysis, acidogenesis, acetogenesis and ultimately methanogenic archaea act to produce methane.
These landfills receiving a wide variety of solid waste generally carries a fairly low pH level. The low pH level makes it difficult for most methanogens to survive. It was found that Methanosarcina barkeri can survive at this low pH levels. M. barkeri consumes the acids in its environment, producing methane and increasing the pH levels in its immediate area. This, in turn, makes that area more amenable for other methanogens.
As moisture leaches through the landfill, it disseminates those high pH level, making other parts of the landfill habitable for M. barkeri and other methane-producing microbes. M. barkeri then moves in and repeats the process, leaving neutral pH levels and healthy populations of other methanogens.
Since M. barkeri and its methanogen cousins produce large quantities of methane. This methane is often collected at landfill sites and used for power generation. Furthermore, methanogens break down solid waste as they go, compacting it so that it takes up less space.
Methane production due to landfills is around 25 Tg.
METHANOGENESIS IN OCEANS
A large amount of methane is generated in ocean sediments which travel a long way to get to the surface and escape to the atmosphere. While traveling through the oceans this generated methane gets eaten up by other microorganisms termed methanotrophs (methane eaters) prior to being released. But in spite of this, the methane production from oceans is very high.
This is because a high concentration of methane is also found in surface water which is oxygenated. It is reported that Methane from the aerobic oceans accounts for up to 4% of global methane production. A group of very simple and tiny bacteria help produce methane. Usually, these bacteria don't produce methane but they can produce the gas as a byproduct of their natural metabolism when they are starved for phosphorus. In phosphate-depleted waters, aerobic microbes could metabolise a compound called methylphosphonic acid (MPn) as a source of phosphate, releasing methane as a by-product.
These microorganisms in marine areas had the biosynthetic apparatus for MPn, suggesting that the molecule is widespread in ocean environments. One of these organisms is a marine microbe called Nitrosopumilus maritimus, part of a group whose members are among the most abundant microorganisms in marine surface waters.
Contribution of oceans to total methane production is 10 Tg.
METHANOGENESIS FROM FOSSIL FUELS
Methane is naturally present in fossil fuels due to long-term decomposition of organic matter. Methane from fossil-fuel production is primarily emitted through:
- the combustion of extracted fossil-fuels;
- the industry practices of venting, or intentionally releasing excess gas, and flaring, or intentionally burning excess gas; and
- fugitive emissions, which include unintentional leakage from the transportation, storage, and distribution of fossil fuels.
The combustion of fossil fuels mined, drilled, and otherwise extracted on federal lands and waters contributed approximately 62,000 metric tons (U.S.A) of methane to the atmosphere in 2012 alone, or more than 1.5 million metric tons of carbon dioxide equivalent.
While venting and flaring are only two of the many root causes of GHG emissions from public lands, the amount of methane these practices emit remains significant and, according to new estimates, has steadily increased over the past five years. The increases in venting and flaring levels are likely in part due to rising oil and natural gas production as well as the lack of adequate infrastructure to capture and process natural gas released during production.
METHANOGENESIS IN HERBIVORES
Emissions from enteric fermentation of pigs and horses are of minor importance but not negligible. Methane production is influenced in particular to diet composition and feeding practices The formation of CH4 in the digestive system (enteric fermentation) of pig and horse is mainly centered in the hind gut (colon).
Here, bacterial action degrades those organic species that passed the digestive tract undigested, mainly cellulose, hemicellulose and pectin which are summed up as bacterially fermentable substrates (BFS). Bacterial action converts these substrates to volatile fatty acids, CH4 and carbon dioxide. The fatty acids play an important role in the energy supply of pigs. In experiments with sows, about half the cellulose and about 90 % of the sugar (xylose), starch 4 and cellulose (pectin) as well as the protein casein that were applied to the animals intracaecally were degraded in the hind gut. The gross energy loss of feed in the form of methane is very less around 0.1%-1% GE of feed intake. The emission of methane from horse and pig is 0.14 Tg and 1.7 Tg respectively.
METHANOGENESIS IN RUMINANTS
Methane is produced in the rumen as a product of normal fermentation of feedstuffs. Although methane production can also occur in the lower gastrointestinal tract, as in nonruminants, 89% of methane emitted from ruminants is produced in the rumen and exhaled through the mouth and nose. Globally, ruminants produce 80 MMT of methane annually. India has largest livestock population & emit about 10.8 MMT of CH4 annually from enteric fermentation. Energy loss ranges from 4 to 12% of GE intake in cattle.
Methanogenic Strains in Rumen
In ruminants, the major strains found are Methanobrevibacter ruminantium, Methanosphaera, Methanomicrobium, Methanobacterium formicicum followed by Methanosarcina barkeri.
The methanogens in the bovine rumen utilize hydrogen and carbon dioxide to produce methane. Methanogens of the genus Methanosarcina grow slowly on hydrogen and carbon dioxide and therefore utilize methanol and methylamines to produce methane. Formate, which is formed in the production of acetate, can also be used as a substrate for methanogenesis. Volatile fatty acids (VFA) are not commonly used as substrates for methanogenesis as their conversion into carbon dioxide and hydrogen is a lengthy process, which is inhibited by rumen turnover. By removing hydrogen from the ruminal environment as a terminal step of carbohydrate fermentation, methanogens allow the microorganisms involved in fermentation to function optimally and support the complete oxidation of substrates. The fermentation of carbohydrates results in the production of hydrogen and if this end product is not removed, it can inhibit metabolism of rumen microorganisms.
Relation with other microbes
Methanogens are known to have symbiotic relationships involving interspecies hydrogen transfer with rumen microorganisms, especially with rumen protozoa where the methanogens can be associated intracellularly and extracellularly. Common protozoa in the bovine rumen found to have such a relationship are from the genera Entodinium, Polyplastron, Epidinium, and Ophryoscolex, while the methanogens most often associated with protozoa are from the orders Methanobacteriales and Methanomicrobiales. Anaerobic fungi, such as Neocallimastix frontalis, have also been found to have a relationship with methanogens involving interspecies hydrogen transfer whereby the fungi’s enzymatic activity has increased and metabolism has shifted towards acetate production.
Importance of methanogenesis in ruminants
It helps in the removal of excess hydrogen. A high hydrogen level will cause:-
- Decrease in overall degradation of carbohydrates.
- Decrease in rate of microbial growth
- Decrease in synthesis of microbial protein
Atmospheric methane is currently increasing at a rate of about 30 to 40 Tg (1012 g) per year. Stabilising global methane concentrations at current levels would require reductions in methane emissions or increased sinks for methane of approximately the same amount.
This reduction represents about 10% of current anthropogenic sources (of which ruminants contribute about 30%). This is much less than the percentage reduction necessary to stabilise the other major greenhouse gases. Additionally, because methane has a shorter atmospheric lifetime and greater radiative absorption capacity than carbon dioxide, methane reduction strategies offer an effective means of slowing global warming in the near term.
Abbanat D.R, Ferry J.G.1990 “Synthesis of acetyl coenzyme A by carbon monoxide dehydrogenase complex from acetate-grown Methanosarcina thermophila.” J Bacteriol. Vol. 172(12) .pp. 7145–7150(1990)
Bousquet P, et al. 2012”Source attribution of the changes in atmospheric methane for 2006-2008.” Atmos Chem Phys.Vol. 11. pp. 3689–3700(2012)
IPCC, “Intergovernmental panel on climate change,” in Climate Change 2001: A Scientific Basis, J. T. Houghton, Y. Ding, and D. J. Griggs, Eds., Cambridge University Press, Cambridge, UK,(2001)
Ellis.J.L, Kebreab.E, Odongo.N.E, Okine.E.K, and France.J, “Prediction of methane production from dairy and beef cattle,” Journal of Dairy Science, vol. 90, no. 7, pp. 3456–3467, (2007)
Forster.P, Ramaswamy.V, Artaxo.P, et al., “Changes in atmospheric constituents and in radiative forcing,” in Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, S. Solomon, D. Qin, M. Manning, et al., Eds., Cambridge University Press, Cambridge, UK, (2007)
Bousquet, P., Tyler S.C, Peylin.P, Van Der Werf G.R, Prigent.C, Hauglustaine D.A 2006. "Contribution of anthropogenic and natural sources to atmospheric methane variability." Nature 443, no. 7110 (2006)
D. A. Lashof and D. R. Ahuja, “Relative contributions of greenhouse gas emissions to global warming,”Nature, vol. 344, no. 6266, pp. 529–531(1990)
Ferry GJ 1992”Methane from Acetate” J Bacteriol.Vol. 174(17).pp. 5489–5495(1992)
Galand P. E, Fritze H, Conrad.H and Yrjälä .K 2005” Pathways for Methanogenesis and Diversity of Methanogenic Archaea” Appl Environ Microbiol.Vol. 71(4).pp. 2195–2198
Gomati Velu, Ramasamy K., Kumar K., Sivaramaiah Nallapeta 2011” Green house gas emissions from termite ecosystem” African Journal of Environmental Science and Technology Vol. 5(2), pp. 56-64(2011)
Janssen.H and Kirs.M 2008.” Structure of the Archaeal Community of the Rumen”Applied and Environmental Microbiology, Vol. 74.pp. 3619–3625(2008)
Johnson. E James 1996 ”A reevaluation of the open ocean source of methane to the atmosphere” J of Geophysical Research, Vol. 101. pp. 6953-6961
Metcalf W, Griffin B, Cicchillo R, Gao J, Janga S, et al. 2012” Synthesis of methylphosphonic acid by marine microbes: a source for methane in the aerobic ocean”Bio GeoScience Vol. 337, pp. 1104–1107 (2012)
Moss Angela R., Jouany Jean P, Newbold Jean P 2011 “Methane production by ruminants: its contribution to global warming” Ann. Zootech. Vol. 49,pp. 231–253(2000)
National Research Council .2010 Verifying Greenhouse Gas Emissions: Methods to Support International Climate Agreements
Pardis F, Hasfalina C, Umi K, Md Shah and Azni I 2013”. Characteristics of Methanogens and Methanotrophs in Rice Fields: A Review.“AsPac J. Mol. Biol. Biotechnol. Vol. 21 (1), pp. 3-17 (2013)
Thauer.R.K, Kaster.A.K, Seedorf.H, Buckel.W, Hedderich,R 2008”Methanogenic archaea: ecologically relevant differences in energy conservation”Nature Reviews Microbiology,Vol. 6. pp. 579–591(2008)
Satyanagalakshmi K,Sridhar. G and Sirohi. S 2015 “An overview of the role of rumen methanogens in methane production and its mitigation strategies” Afr.J.Biotechnol, Vol. 14(16), pp. 1427-1438(2015)
Staley.B.F, Reyes F.L, Barlaz M.A.” Effect of Spatial Differences in Microbial Activity, pH, and Substrate Levels on Methanogenesis Initiation in Refuse 2011”. Applied and Environmental Microbiology, Vol .77(7). pp. 241(2011)
Thauer R.K 1998 “ Biochemistry of methanogenesis: a tribute to Marjory Stephenson”. Microbiology UK Vol. 144.pp. 2377–2406.(1998)
Thauer R.K, Kaster A.K, Seedorf .H et al. 2008 “Methanogenic archaea: ecologically relevant differences in energy conservation. Nature Reviews. Microbiology Vol.6(8).pp. 579–591(2008)
Thauer, R.K. et.al.,”Methane Production 1989.” Ann. Rev. Microbiol, Vol. 43,pp. 43-67 (1989)
U. Dämmgen, J. Schulz, H. Kleine Klausing, N. J. Hutchings, H.-D. Haenel, C. Rösemann 2012 Agriculture and Forestry Research Vol. 62, pp. 83-96(2012)
Watanab. S, Higashitani.N,Tsurushima.N, and Tsunogai.S 1995,” Methane in the western North Pacific, J. Ocean.”J. Oceanography Vol. 51.pp. 39-60(1995)
Yusuf.O.Raifu,Zainura Z. Noor, Ahmad H. Abba 2012.”Green House Gas Emissions: Quantifying Methane Emission from Livestock”. American J. of Engineering and Applied Sciences Vol. 5 (1),pp. 1-8(2012)