Methane oxidation in termite hindguts: absence of evidence and evidence of absence

A steep oxygen gradient and the presence of methane render the hindgut internal periphery of termites a potential habitat for aerobic methane-oxidizing bacteria. However, methane emissions of various termites increased, if at all, only slightly when termites were exposed to an anoxic (nitrogen) atmosphere, and (14)CH(4) added to the air headspace over live termites was not converted to (14)CO(2). Evidence for the absence of methane oxidation in living termites was corroborated by the failure to detect pmoA, the marker gene for particulate methane monooxygenase, in hindgut DNA extracts of all termites investigated. This adds robustness to our concept of the degradation network in the termite hindgut and eliminates the gut itself as a potential sink of this important greenhouse gas.     

Effect of chemical treatments on methane emission by the hindgut microbiota in the termiteZootermopsis angusticollis

Selective removal of symbiotic hindgut microorganisms by chemical treatments reduced methane emission by the termiteZootermopsis angusticollis. Methane emission from untreated termites incubated in 25% H₂ increased 123%, from 10.3 nmol/termite/hour (U) to 22.9 U. Though linear with time, methane emission was not correlated with termite mass. Hyperbaric oxygen treatments reduced methane emission to unquantifiable levels and eliminated all but the protozoaTricercomitus andHexamastix. Exogenous H₂ restored 5% of methane emission to 1.3 U. 2-bromoethanesulfonic acid, fed on filter papers to termites, eliminated methane production. Epifluorescence microscopy showed that this treatment selectively removed methanogens from symbioses withTricercomitus, Hexamastix, andTrichomitopsis, but the protozoa did not appear to be affected. The insect molting hormone 20-hydroxyecdysone reduced methane production 86% to 1.6 U from an initial level of 11.4 U. Hydrogen incubation increased this rate to 77% of the initial rate, 8.8 U. Hormone treatment reduced the number ofTrichonympha in the hindgut and induced sexuality in these protozoa. A model suggests thatTrichonympha evolve most of the hydrogen and that methanogenic bacteria symbiotic withTrichomitopsis produce most of the methane in this hindgut ecosystem.     

Aerobic state of gut of Nasutitermes exitiosus and Coptotermes lacteus, high and low caste termites

The redox potential and pH of the gut of the termites Nasutitermes exitiosus and Coptotermes lacteus was investigated by feeding the insects with redox dyes and pH indicators. For N. exitiosus the E′₀ (pH 7.0) of the foregut was above +200 mV; the midgut was about +100 to +150 mV and the hindgut was in the region of ?20 to +30 mV. For C. lacteus the fore- and midgut were about +30 to +50 mV and the hindgut about ?20 to +20 mV. The colours of the ingested dyes indicated that the gut was aerobic in both termites. The pH of the whole gut ranged from 6.5 to 7.5 for N. exitiosus and 6.0 to 7.0 for C. lacteus.     

Role of bacteria in maintaining the redox potential in the hindgut of termites and preventing entry of foreign bacteria

The hindgut of the lower termites, Mastotermes darwiniensis and Coptotermes lacteus and the higher termite Nasutitermes exitiosus were made aerobic by exposure of the termites to pure oxygen, a procedure which killed their spirochaetes and their protozoa (lower termites only). The time taken for the hindgut to become anaerobic after the termites were restored to normal atmospheric conditions ranged from 2 to 4.5 hr. After oxygen treatment the number of gut bacteria increased some six- to ten-fold in all termite species, indicating that the bacteria are poised to use oxygen entering the gut. Removal of all the hindgut microbiota by feeding tetracycline caused the hindgut to become aerobic in M. darwiniensis and N. exitiosus. The transferring of M. darwiniensis to fresh wood, free of antibiotic, resulted in the return of the normal flora and the eventual establishment of anaerobic conditions in the hindgut. Thus the bacteria appear to be important in maintaining anaerobic conditions in the gut. Attempts to determine whether the protozoa (in the lower termites) played any part in maintaining the Eh of the hindgut were unsuccessful. Serratia marcescens failed to colonise the gut of normal C. lacteus and transiently colonized (for 5 days) the gut of normal N. exitiosus. Transient colonization by S. marcescens (from 6 to 10 days) occurred in N. exitiosus when its hindgut spirochaetes were killed and in C. lacteus when its spirochaetes and protozoa were killed, indicating a possible role for the spirochaetes and/or protozoa in influencing the bacteria allowed to reside in the hindgut. Exposure of normal termites to Serratia provoked an increase in the numbers of the normal gut bacteria.     

Localization and In Situ Activities of Homoacetogenic Bacteria in the Highly Compartmentalized Hindgut of Soil-Feeding Higher Termites (Cubitermes spp.)

Methanogenesis and homoacetogenesis occur simultaneously in the hindguts of almost all termites, but the reasons for the apparent predominance of methanogenesis over homoacetogenesis in the hindgut of the humivorous species is not known. We found that in gut homogenates of soil-feeding Cubitermes spp., methanogens outcompete homoacetogens for endogenous reductant. The rates of methanogenesis were always significantly higher than those of reductive acetogenesis, whereas the stimulation of acetogenesis by the addition of exogenous H₂ or formate was more pronounced than that of methanogenesis. In a companion paper, we reported that the anterior gut regions of Cubitermes spp. accumulated hydrogen to high partial pressures, whereas H₂ was always below the detection limit (<100 Pa) in the posterior hindgut, and that all hindgut compartments turned into efficient H₂ sinks when external H₂ was provided (D. Schmitt-Wagner and A. Brune, Appl. Environ. Microbiol. 65:4490–4496, 1999). Using a microinjection technique, we found that only the posterior gut sections P3/4a and P4b, which harbored methanogenic activities, formed labeled acetate from H¹⁴CO₃⁻. Enumeration of methanogenic and homoacetogenic populations in the different gut sections confirmed the coexistence of both metabolic groups in the same compartments. However, the in situ rates of acetogenesis were strongly hydrogen limited; in the P4b section, no activity was detected unless external H₂ was added. Endogenous rates of reductive acetogenesis in isolated guts were about 10-fold lower than the in vivo rates of methanogenesis, but were almost equal when exogenous H₂ was supplied. We conclude that the homoacetogenic populations in the posterior hindgut are supported by either substrates other than H₂ or by a cross-epithelial H₂ transfer from the anterior gut regions, which may create microniches favorable for H₂-dependent acetogenesis.     

Nitrogen mineralization, denitrification, and nitrate ammonification by soil-feeding termites: a 15N-based approach

Soil-feeding termites are abundant and play important roles in the biogeochemical processes in tropical soils. Previous studies indicated that they preferentially utilize the peptidic components of soil organic matter as a nutrient resource. Here, we determined the corresponding mineralization fluxes and elucidated other N transformation processes that occur during soil gut passage using ¹⁵N tracer techniques. Termite-based rates of N mineralization by Cubitermes umbratus and Cubitermes ugandensis in soil microcosms amended with ¹⁵NH₄ ⁺ were 6.6 and 9.2 nmol N day^?1 (g fresh wt)^?1, which means that the soil peptides fuel about 20 and 40% of the respiratory activity of these insects. Considering the areal biomass of soil-feeding termites in humid savannahs, soil-feeding termites should mineralize about 3% of the total N in their food soil per year. In addition to producing ammonia from ingested ¹⁵NO₃ ^? at approximately 10% of the mineralization rate, C. umbratus also formed N₂ at similar rates. The formation of labelled N₂ in microcosms amended with ¹⁵NH₄ ⁺ seems to be at least partially due to nitrification activity in the soil; evidence for the formation of nitrate in the posterior hindgut remains inconclusive. However, the so far unexplained increase of ¹⁵N abundance in the ammonia pools of the posterior hindgut compartments manifests additional hitherto unknown metabolic processes in this gut region. Collectively, our results not only reinforce the concept of nitrogenous soil components as an important dietary resource for soil-feeding termites, but also allow us to predict that N mineralization and nitrate ammonification activities in the termite gut should positively affect the dynamics of N in tropical soil.     

Hydrogen Profiles and Localization of Methanogenic Activities in the Highly Compartmentalized Hindgut of Soil-Feeding Higher Termites (Cubitermes spp.)

It has been shown that the coexistence of methanogenesis and reductive acetogenesis in the hindgut of the wood-feeding termite Reticulitermes flavipes is based largely on the radial distribution of the respective microbial populations and relatively high hydrogen partial pressures in the gut lumen. Using Clark-type microelectrodes, we showed that the situation in Cubitermes orthognathus and other soil-feeding members of the subfamily Termitinae is different and much more complex. All major compartments of agarose-embedded hindguts were anoxic at the gut center, and high H₂ partial pressures (1 to 10 kPa) in the alkaline anterior region rendered the mixed segment and the third proctodeal segment (P3) significant sources of H₂. Posterior to the P3 segment, however, H₂ concentrations were generally below the detection limit (<100 Pa). All hindgut compartments turned into efficient hydrogen sinks when external H₂ was supplied, but methane was formed mainly in the P3/4a and P4b compartments, and in the latter only when H₂ or formate was added. Addition of H₂ to the gas headspace stimulated CH₄ emission of living termites, indicating that endogenous H₂ production limits methanogenesis also in vivo. At the low H₂ partial pressures in the posterior hindgut, methanogens would most likely outcompete homoacetogens for this electron donor. This might explain the apparent predominance of methanogenesis over reductive acetogenesis in the hindgut of soil-feeding termites, although the presence of homoacetogens in the anterior, highly alkaline region cannot yet be excluded. In addition, the direct contact of anterior and posterior hindgut compartments in situ permits a cross-epithelial transfer of H₂ or formate, which would not only fuel methanogenesis in these compartments, but would also create favorable microniches for reductive acetogenesis. In situ rates and spatial distribution of H₂-dependent acetogenic activities are addressed in a companion paper (A. Tholen and A. Brune, Appl. Environ. Microbiol. 65:4497–4505, 1999).     

Association of methanogenic bacteria with flagellated protozoa from a termite hindgut

Epifluorescence microscopy was used to examine hindgut contents ofZootermopsis angusticollis (Hagen) termites for the presence of methanogenic bacteria, which can be identified on the basis of the fluorescence of the novel cofactors F₄₂₀ and F₃₅₀. Small, autofluorescent, rod-shaped bacteria of theMethanobrevibacter sp. morphotype were observed associated with three flagellates tentatively identified asTrichomitopsis termopsidis (Cleveland),Tricercomitus termopsidis Kirby andHexamastix termopsidis Kirby. Methanogens were not observed associated with any other protozoal morphotypes and were not numerous in the free-living state inZ. angusticollis hindgut fluid. Electron micrographs of thin sections of hindgut protozoa suggest methanogens are endosymbionts in the small trichomonad protozoa. Our observations are consistent with the finding of Odelson and Breznak that methane is a minor endproduct of the metabolism of termite gut microbiota.Deceased.     

Enzymes of acetate and glucose metabolism in termites

Extracts of tissues of the lower termites, Reticulitermes flavipes and Coptotermes lacteus, and the higher termite, Nasutitermes exitiosus, possess acetyl-CoA synthetase and all the enzymes of the tricarboxylic acid cycle and are thus able to oxidize acetate to CO₂. The specific activities of these enzymes in R. flavipes are sufficient to cope with the rate of acetogenesis by the gut microbiota. The presence of the malic enzyme and malate dehydrogenase, but not pyruvate carboxylase or phosphoenolpyruvate carboxykinase, indicates that they may be important as anaplerotic enzymes for the conversion of pyruvate to oxalacetate. An apparent absence of pyruvate dehydrogenase in all termites suggests that they do not convert pyruvate to acetyl-CoA, but rather convert acetate (transported from the hindgut) to this compound. All the enzymes of glycolysis were present in termite extracts. Thus any glucose absorbed from the midgut, and originating from hydrolysis of cellulose by salivary or midgut enzymes, can be metabolized by termites as an energy source.     

Nitrous Oxide (N2O) Emissions by Termites: Does the Feeding Guild Matter?

In the tropics, termites are major players in the mineralization of organic matter leading to the production of greenhouse gases including nitrous oxide (N₂O). Termites have a wide trophic diversity and their N-metabolism depends on the feeding guild. This study assessed the extent to which N₂O emission levels were determined by termite feeding guild and tested the hypothesis that termite species feeding on a diet rich in N emit higher levels of N₂O than those feeding on a diet low in N. An in-vitro incubation approach was used to determine the levels of N₂O production in 14 termite species belonging to different feeding guilds, collected from a wide range of biomes. Fungus-growing and soil-feeding termites emit N₂O. The N₂O production levels varied considerably, ranging from 13.14 to 117.62 ng N₂O-N d^-1 (g dry wt.)^-1 for soil-feeding species, with Cubitermes spp. having the highest production levels, and from 39.61 to 65.61 ng N₂O-N d^-1 (g dry wt.)^-1 for fungus-growing species. Wood-feeding termites were net N₂O consumers rather than N₂O producers with a consumption ranging from 16.09 to 45.22 ng N₂O-N d^-1 (g dry wt.)^-1. Incubating live termites together with their mound increased the levels of N₂O production by between 6 and 13 fold for soil-feeders, with the highest increase in Capritermes capricornis, and between 14 and 34 fold for fungus-growers, with the highest increase in Macrotermes muelleri. Ammonia-oxidizing (amoA-AOB and amoA-AOA) and denitrifying (nirK, nirS, nosZ) gene markers were detected in the guts of all termite species studied. No correlation was found between the abundance of these marker genes and the levels of N₂O production from different feeding guilds. Overall, these results support the hypothesis that N₂O production rates were higher in termites feeding on substrates with higher N content, such as soil and fungi, compared to those feeding on N-poor wood.     

Methane and hydrogen production in a termite-symbiont system

Methane and hydrogen emission rates and the ¹³C of CH₄ were observed for various termites in Australia, Thailand and Japan. Combined with the already reported emission rates of CH₄ in the literature, the phylogenetic trend was examined. Emission rates of the observed termites were categorized into five groups: group I with high CH₄ and low H₂ emission rates with a CH₄/H₂ ratio of typically 10/1; group II with high CH₄ and high H₂ emissions with a CH₄/H₂ ratio of 4/1–1/2; group III with low emission rates of CH₄ and H₂; group IV with high H₂ and insignificant CH₄ emissions; and group V with insignificant emissions for both CH₄ and H₂. In lower termites, there are both colonies infected and uninfected with methanogens even in the same species, and no specific trend in CH₄ and H₂ emissions was observed within a genus. Whether protozoa in the hindgut of termites are infected with methanogens or not and the differences in species compositions of protozoa are possibly responsible for the inter-colonial variations. The proportions of infected colonies were possibly small for the family Kalotermitidae (dry wood feeders), and relatively large for families of wet or damp wood feeders. The hydrogen emission rate possibly depends on the locality of methanogens: namely, whether they are intracellular symbionts of protozoa or whether they are attached to the hindgut wall. Emission rates of higher termites were classified into groups according to genera and the diet. Most species of soil or wood/soil interface feeders classified into group I, while the soil feeders Dicuspiditermes in Thailand and Amitermes in Australia were classified into groups with high H₂ emission rates. Typical wood-feeding termites and fungus-growing termites were classified into group III. The results indicate that higher termites tend to increase the CH₄ emission rate during dietary evolution from wood- to soil-feeding, and two types of the system with different efficiencies of interspecies transfer of H₂ have been formed. The ¹³C of CH₄ was discernible with a difference in the decomposition process in the termite–symbiont system among lower termites, fungus-growing termites and other higher termites.     

Substrates for Sulfate Reduction and Methane Production in Intertidal Sediments

The activity of and potential substrates for methane-producing bacteria and sulfate-reducing bacteria were examined in marsh, estuary, and beach intertidal sediments. Slow rates of methane production were detected in all sediments, although rates of sulfate reduction were 100- to 1,000-fold higher. After sulfate was depleted in sediments, the rates of methane production sharply increased. The addition of methylamine stimulated methanogenesis in the presence of sulfate, and [¹⁴C]methylamine was rapidly converted to ¹⁴CH₄ and ¹⁴CO₂ in freshly collected marsh sediment. Acetate, hydrogen, or methionine additions did not stimulate methanogenesis. [methyl-¹⁴C]methionine and [2-¹⁴C]acetate were converted to ¹⁴CO₂ and not to ¹⁴CH₄ in fresh sediment. No reduction of ¹⁴CO₂ to ¹⁴CH₄ occurred in fresh sediment. Molybdate, an inhibitor of sulfate reduction, inhibited [2-¹⁴C]acetate metabolism by 98.5%. Fluoracetate, an inhibitor of acetate metabolism, inhibited sulfate reduction by 61%. These results suggest that acetate is a major electron donor for sulfate reduction in marine sediments. In the presence of high concentrations of sulfate, methane may be derived from novel substrates such as methylamine.     

Metabolism of Acetate, Methanol, and Methylated Amines in Intertidal Sediments of Lowes Cove, Maine

The fates and the rates of metabolism of acetate, trimethylamine, methylamine, and methanol were examined to determine the significance of these compounds as in situ methane precursors in surface sediments of an intertidal zone in Maine. Concentrations of these potential methane precursors were generally <3 μM, with the exception of sediments containing fragments of the seaweed Ascophyllum nodosum, in which acetate was 96 μM. [2-¹⁴C]acetate turnover in all samples was rapid (turnover time <2 h), with ¹⁴CO₂ as the primary product. [¹⁴C]trimethylamine and methylamine turnover times were slower (>8 h) and were characterized by formation of both ¹⁴CH₄ and ¹⁴CO₂. Ratios of ¹⁴CH₄/¹⁴CO₂ from [¹⁴C]trimethylamine and methylamine in uninhibited sediments indicated that a significant fraction of these substrates were catabolized via a non-methanogenic process. Data from inhibition experiments involving sodium molybdate and 2-bromoethanesulfonic acid supported this interpretation. [¹⁴C]methanol was oxidized relatively slowly compared with the other substrates and was catabolized mainly to ¹⁴CO₂. Results from experiments with molybdate and 2-bromoethanesulfonic acid suggested that methanol was oxidized primarily through sulfate reduction. In Lowes Cove sediments, trimethylamine accounted for 35.1 to 61.1% of total methane production.     

Acetate Synthesis from H2 plus CO2 by Termite Gut Microbes

Gut microbiota from Reticulitermes flavipes termites catalyzed an H₂-dependent total synthesis of acetate from CO₂. Rates of H₂-CO₂ acetogenesis in vitro were 1.11 ± 0.37 μmol of acetate g (fresh weight)⁻¹ h⁻¹ (equivalent to 4.44 ± 1.47 nmol termite⁻¹ h⁻¹) and could account for approximately 1/3 of all the acetate produced during the hindgut fermentation. Formate was also produced from H₂ + CO₂, as were small amounts of propionate, butyrate, and lactate-succinate. However, H₂-CO₂ formicogenesis seemed largely unrelated to acetogenesis and was believed not to be a significant reaction in situ. Little or no CH₄ was formed from H₂ + CO₂ or from acetate. H₂-CO₂ acetogenesis was inhibited by O₂, KCN, CHCl₃, and iodopropane and could be abolished by prefeeding R. flavipes with antibacterial drugs. By contrast, prefeeding R. flavipes with starch resulted in almost complete defaunation but had little effect on H₂-CO₂ acetogenesis, suggesting that bacteria were the acetogenic agents in the gut. H₂-CO₂ acetogenesis was also observed with gut microbiota from Prorhinotermes simplex, Zootermopsis angusticollis, Nasutitermes costalis, and N. nigriceps; from the wood-eating cockroach Cryptocercus punctulatus; and from the American cockroach Periplaneta americana. Pure cultures of H₂-CO₂-acetogenic bacteria were isolated from N. nigriceps, and a preliminary account of their morphological and physiological properties is presented. Results indicate that in termites, CO₂ reduction to acetate, rather than to CH₄, represents the main electron sink reaction of the hindgut fermentation and can provide the insects with a significant fraction (ca. 1/3) of their principal oxidizable energy source, acetate.     

Uric Acid-Degrading Bacteria in Guts of Termites [Reticulitermes flavipes (Kollar)]

Uricolytic bacteria were present in guts of Reticulitermes flavipes in populations up to 6 × 10⁴ cells per gut. Of 82 strains isolated under strict anaerobic conditions, most were group N Streptococcus sp., Bacteroides termitidis, and Citrobacter sp. All isolates used uric acid (UA) as an energy source anaerobically, but not aerobically, and NH₃ was the major nitrogenous product of uricolysis. However, none of the isolates had an absolute requirement for UA. Utilization of heterocyclic compounds other than UA was limited. Fresh termite gut contents also degraded UA anaerobically, as measured by ¹⁴CO₂ evolution from [2-¹⁴C]UA. The magnitude of anaerobic uricolysis [0.67 pmol of UA catabolized/(gut × h)] was entirely consistent with the population density of uricolytic bacteria in situ. Uricolytic gut bacteria may convert UA in situ to products usable by termites for carbon, nitrogen, energy, or all three. This possibility is consistent with the fact that R. flavipes termites from UA, but they do not void the purine in excreta despite the lack of uricase in their tissues.     

Kinetic Parameters of the Conversion of Methane Precursors to Methane in a Hypereutrophic Lake Sediment

The kinetic parameters K_m, V_max, T_t (turnover time), and v (natural velocity) were determined for H₂ and acetate conversion to methane by Wintergreen Lake sediment, using short-term (a few hours) methods and incubation temperatures of 10 to 14°C. Estimates of the Michaelis-Menten constant, K_m, for both the consumption of hydrogen and the conversion of hydrogen to methane by sediment microflora averaged about 0.024 μmol g⁻¹ of dry sediment. The maximal velocity, V_max, averaged 4.8 μmol of H₂ g⁻¹ h⁻¹ for hydrogen consumption and 0.64 μmol of CH₄ g⁻¹ h⁻¹ for the conversion of hydrogen to methane during the winter. Estimated natural rates of hydrogen consumption and hydrogen conversion to methane could be calculated from the Michaelis-Menten equation and estimates of K_m, V_max, and the in situ dissolved-hydrogen concentration. These results indicate that methane may not be the only fate of hydrogen in the sediment. Among several potential hydrogen donors tested, only formate stimulated the rate of sediment methanogenesis. Formate conversion to methane was so rapid that an accurate estimate of kinetic parameters was not possible. Kinetic experiments using [2-¹⁴C]acetate and sediments collected in the summer indicated that acetate was being converted to methane at or near the maximal rate. A minimum natural rate of acetate conversion to methane was estimated to be about 110 nmol of CH₄ g⁻¹ h⁻¹, which was 66% of the V_max (163 nmol of CH₄ g⁻¹ h⁻¹). A 15-min preincubation of sediment with 5.0 × 10⁻³ atm of hydrogen had a pronounced effect on the kinetic parameters for the conversion of acetate to methane. The acetate pool size, expressed as the term K_m + S_n (S_n is in situ substrate concentration), decreased by 37% and T_t decreased by 43%. The V_max remained relatively constant. A preincubation with hydrogen also caused a 37% decrease in the amount of labeled carbon dioxide produced from the metabolism of [U-¹⁴C]valine by sediment heterotrophs.     

Influence of laboratory maintenance,relative humidity and coprophagy on [14C]lignin degradation by Nasutitermes exitiosus

[¹⁴C](lignin)-Acer rubrum L. was produced by infusing stems of A. rubrum with [¹⁴C](3′-side chain)-cinnamic acid. Groups (1g) of Nasutitermes exitiosus (Hill) were placed in sealed flasks which were aspirated over a 2-week period. These released up to 8.3% of the [¹⁴C](lignin)-A. rubrum as ¹⁴CO₂. Termites maintained under standard conditions as 50 g non-breeding groups for 4 months or more showed diminished ability to degrade lignin. Optimal lignin degradation and survival of N. exitiosus was at 90 and 96% relative humidity (r.h.). At 75, 80 and 85% r.h., fungal growth in bioassay flasks was seen, but lignin degradation did not increase. At 100% r.h. where bacterial growth in faeces may have been encouraged due to the development of free water, termite survival was poor and lignin degradation decreased. Starved termites contained much more radioactivity (21.8 and 30.8%) than fed termites (1.6% radioactivity), probably due to greater coprophagy on deprivation of food. However, lignin degradation was only marginally higher in starved termites, suggesting lignin becomes progressively more resistant to termite degradation after passage through the gut.     

Evidence for Aceticlastic Methanogenesis in the Presence of Sulfate in a Gas Condensate-Contaminated Aquifer

The anaerobic metabolism of acetate was studied in sediments and groundwater from a gas condensate-contaminated aquifer in an aquifer where geochemical evidence implicated sulfate reduction and methanogenesis as the predominant terminal electron-accepting processes. Most-probable-number tubes containing acetate and microcosms containing either [2-¹⁴C]acetate or [U-¹⁴C]acetate produced higher quantities of CH₄ compared to CO₂ in the presence or absence of sulfate.¹⁴CH₄ accounted for 70 to 100% of the total labeled gas in the [¹⁴C]acetate microcosms regardless of whether sulfate was present or not. Denaturing gradient gel electrophoresis of the acetate enrichments both with and without sulfate using Archaea-specific primers showed identical predominant bands that had 99% sequence similarity to members of Methanosaetaceae. Clone libraries containing archaeal 16S rRNA gene sequences amplified from sediment from the contaminated portion of the aquifer showed that 180 of the 190 clones sequenced belonged to the Methanosaetaceae. The production of methane and the high frequency of sequences from the Methanosaetaceae in acetate enrichments with and without sulfate indicate that aceticlastic methanogenesis was the predominant fate of acetate at this site even though sulfate-reducing bacteria would be expected to consume acetate in the presence of sulfate.     

Occurrence and metabolic role of the pyruvate dehydrogenase complex in the lower termite Coptotermes formosanus (Shiraki)

The activities of the pyruvate dehydrogenase complex in extracts of the gutted body, head, foregut/midgut and hindgut (hindgut epithelium and microorganisms) tissues of the lower termite Coptotermes formosanus (Shiraki) were determined by measuring the [¹⁴C]-acetyl-CoA produced from [2-¹⁴C]-pyruvate and the ¹⁴CO₂ produced from [1-¹⁴C]-pyruvate. The activities of pyruvate dehydrogenase, l-lactate dehydrogenase, acetyl-CoA synthetase, malate dehydrogenase (decarboxylating), and acetate kinase in the termite tissues and the hindgut also were determined. The sum (7.1 nmol/termite/h) of the pyruvate dehydrogenase complex activities in the termite tissues other than the hindgut was five times higher than the activity in the hindgut. Significant amounts of l-lactate dehydrogenase activity were found in all of the tissues. All of the tissues other than the hindgut had significant amounts of acetyl-CoA synthetase activity. Malate dehydrogenase (decarboxylating) activity was about ten times higher in the hindgut extract than in the gutted body and head extracts and the activity in the foregut/midgut extract was very low. These results indicate that acetyl-CoA for the TCA cycle is produced effectively in the tissues of the termite itself, both from pyruvate by the pyruvate dehydrogenase complex and from acetate by acetyl-CoA synthetase.     

Effect of Host Diet and Hindgut Microbial Composition on Cellulolytic Activity in the Hindgut of the American Cockroach, Periplaneta americana

Cellulase activity measured as filter paper digesting activity (FPase) and carboxymethyl cellulase (CMCase) was demonstrated in hindgut extracts of the cockroach Periplaneta americana. The highest activities measured amounted to 0.89 and 0.12 U · ml^-1 for CMCase and FPase, respectively. The cellulolytic capacity of the hindgut population increased dramatically when protozoa were present, and the activities were found to vary depending on the feeding regimen. Cellulose-rich diets induced high protozoal numbers, resulting in a high cellulase activity. A close correlation was found between the number of Nyctotherus ovalis organisms, the major protozoans in the hindgut, and both FPase and CMCase activity. Since the numbers of this protozoan also correlated with the methane production of the insect, it appears that N. ovalis is responsible for the major part of cellulolytic and methanogenic activity found in the hindgut of P. americana.