Response of rumen microbiota,and metabolic profiles of rumen fluid,liver and serum of goats to high-grain diets

Feeding ruminants a high-grain (HG) diet is a widely used strategy to improve milk yield and cost efficiency. However, it may cause certain metabolic disorders. At present, information about the effects of HG diets on the systemic metabolic profile of goats and the correlation of such diets with rumen bacteria is limited. In the present study, goats were randomly divided into two groups: one was fed the hay diet (hay; n = 5), while the other was fed HG diets (HG; n = 5). On day 50, samples of rumen contents, peripheral blood serum and liver tissues were collected to determine the metabolic profiles in the rumen fluid, liver and serum and the microbial composition in rumen. The results revealed that HG diets reduced (P < 0.05) the community richness and diversity of rumen microbiota, with an increase in the Chao 1 and Shannon index and a decrease in the Simpson index. HG diets also altered the composition of rumen microbiota, with 30 genera affected (P < 0.05). Data on the metabolome showed that the metabolites in the rumen fluid, liver and serum were affected (variable importance projection > 1, P <0.05) by dietary treatment, with 47, 10 and 27 metabolites identified as differentially metabolites. Pathway analysis showed that the common metabolites in the shared key pathway (aminoacyl-transfer RNA biosynthesis) in the rumen fluid, liver and serum were glycine, lysine and valine. These findings suggested that HG diets changed the composition of the rumen microbiota and metabolites in the rumen fluid, liver and serum, mainly involved in amino acid metabolism. Our findings provide new insights into the understanding of diet-related systemic metabolism and the effects of HG diets on the overall health of goats.     

Analysis of the sulfate-reducing bacterial and methanogenic archaeal populations in contrasting Antarctic sediments

The distribution and activity of communities of sulfate-reducing bacteria (SRB) and methanogenic archaea in two contrasting Antarctic sediments were investigated. Methanogenesis dominated in freshwater Lake Heywood, while sulfate reduction dominated in marine Shallow Bay. Slurry experiments indicated that 90% of the methanogenesis in Lake Heywood was acetoclastic. This finding was supported by the limited diversity of clones detected in a Lake Heywood archaeal clone library, in which most clones were closely related to the obligate acetate-utilizing Methanosaeta concilii. The Shallow Bay archaeal clone library contained clones related to the C(1)-utilizing Methanolobus and Methanococcoides and the H(2)-utilizing Methanogenium: Oligonucleotide probing of RNA extracted directly from sediment indicated that archaea represented 34% of the total prokaryotic signal in Lake Heywood and that Methanosaeta was a major component (13.2%) of this signal. Archaea represented only 0.2% of the total prokaryotic signal in RNA extracted from Shallow Bay sediments. In the Shallow Bay bacterial clone library, 10.3% of the clones were SRB-like, related to Desulfotalea/Desulforhopalus, Desulfofaba, Desulfosarcina, and Desulfobacter as well as to the sulfur and metal oxidizers comprising the Desulfuromonas cluster. Oligonucleotide probes for specific SRB clusters indicated that SRB represented 14.7% of the total prokaryotic signal, with Desulfotalea/Desulforhopalus being the dominant SRB group (10.7% of the total prokaryotic signal) in the Shallow Bay sediments; these results support previous results obtained for Arctic sediments. Methanosaeta and Desulfotalea/Desulforhopalus appear to be important in Lake Heywood and Shallow Bay, respectively, and may be globally important in permanently low-temperature sediments.     

Comparative study of bacterial groups within the human cecal and fecal microbiota

The composition of the human cecal microbiota is poorly known because of sampling difficulties. Samples of cecal fluid from eight subjects were collected via an intestinal tube. Feces were also collected. Total anaerobes, facultative anaerobes, bifidobacteria, and Bacteroides were enumerated by culture methods, and the predominant phylogenetic groups were quantified by molecular hybridization using a set of six rRNA-targeted probes. The numbers of strict anaerobes, bifidobacteria, Bacteroides, and members of the Clostridium coccoides group and Clostridium leptum subgroup were lower in the cecum. Facultative anaerobes represented 25% of total bacteria in the cecum versus 1% in the feces.     

The inclusion of ground hay, straw and paper in the diets fed to growing rabbits

In 3 experiments growing rabbits were divided into 2 groups. In each case half received a basal ration while the other half was given this ration supplemented with a ground fibrous material: 20% hay, 10% straw or 10% paper. All the diets were fed in pelleted form. In all the experiments the rabbits fed on the diets containing the added fibrous materials gained in weight slightly more rapidly and had slightly higher food conversion ratios than did those on the control diet, but the differences in the means were not significant. A study of the small intestine and caecum weights expressed as percentages of body weight and as the weights of 1-cm lengths showed that the added fibrous materials increased these weights except in 1 instance where the results were the same. Significant changes were recorded in the case of hay in both the percentage weight and the weight of 1-cm lengths of caecum and in the straw experiment in the weight of 1-cm lengths of small intestine. There were no significant changes in the results from the paper-fed rabbits.     

Vertical distribution of structure and function of the methanogenic archaeal community in Lake Dagow sediment

Detailed studies on the relation of structure and function of microbial communities in a sediment depth profile scarcely exist. We determined as functional aspect the vertical distribution of the acetotrophic and hydrogenotrophic CH4 production activity by measuring production rates and stable 13C/12C-isotopic signatures of CH4 in the profundal sediment of Lake Dagow. The structural aspect was determined by the composition of the methanogenic community by quantifying the abundance of different archaeal groups using 'real-time' polymerase chain reaction and analysis of terminal restriction fragment length polymorphism (T-RFLP). Methane production rates in the surface sediment (0-3 cm depth) were higher in August than in May, but strongly decreased with depth (down to 20 cm). The delta13C of the produced CH4 and CO2 indicated an increase in isotopic fractionation with sediment depth. The relative contribution of hydrogenotrophic to total methanogenesis, which was calculated from the isotopic signatures, increased with depth from about 22% to 38%. Total numbers of microorganisms were higher in August than in May, but strongly decreased with depth. The increase of microorganisms from May to August mainly resulted from Bacteria. The Archaea, on the other hand, exhibited a rather constant abundance, but also decreased with depth from about 1 x 10(8) copies of the archaeal 16S rRNA gene per gram of dry sediment at the surface to 4 x 10(7) copies per gram at 15-20 cm depth. T-RFLP analysis combined with phylogenetic analysis of cloned sequences of the archaeal 16S rRNA genes showed that the methanogenic community consisted mainly of Methanomicrobiales and Methanosaetaceae. The relative abundance of Methanosaetaceae decreased with depth, whereas that of Methanomicrobiales slightly increased. Hence, the vertical distribution of the functional characteristics (CH4 production from acetate versus H2/CO2) was reflected in the structure of the community consisting of acetotrophic (Methanosaetaceae) versus hydrogenotrophic (Methanomicrobiales) phenotypes.     

High-grain diets altered rumen fermentation and epithelial bacterial community and resulted in rumen epithelial injuries of goats

This study evaluated the effects of high-grain diets on the rumen fermentation, epithelial bacterial community, morphology of rumen epithelium, and local inflammation of goats during high-grain feeding. Twelve 8-month-old goats were randomly assigned to two different diets, a hay diet or a high-grain diet (65% grain, HG). At the end of 7 weeks of treatment, samples of rumen content and rumen epithelium were collected. Rumen pH was lower (P < 0.05), but the levels of volatile fatty acids and lipopolysaccharides were higher (P < 0.05) in the HG group than those in the hay group. The principal coordinate analysis indicated that HG diets altered the rumen epithelial bacterial community, with an increase in the proportion of genus Prevotella and a decrease in the relative abundance of the genera Shuttleworthia and Fibrobacteres. PICRUSt analysis suggested that the HG-fed group had a higher (P < 0.05) relative abundance of gene families related to energy metabolism; folding, sorting, and degradation; translation; metabolic diseases; and immune system. Furthermore, HG feeding resulted in the rumen epithelial injury and upregulated (P < 0.05) the gene expressions of IL-1β and IL-6, and the upregulations were closely related to the rumen pH, LPS level, and rumen epithelial bacteria abundance. In conclusion, our results indicated that the alterations in the rumen environment and epithelial bacterial community which were induced by HG feeding may result in the damage and local inflammation in the rumen epithelium, warranting further study of rumen microbial–host interactions in the HG feeding model.     

Changes in bacterial community structure in the colon of pigs fed different experimental diets and after infection with Brachyspira hyodysenteriae

Bacterial communities in the large intestines of pigs were compared using terminal restriction fragment length polymorphism (T-RFLP) analysis targeting the 16S ribosomal DNA. The pigs were fed different experimental diets based on either modified standard feed or cooked rice supplemented with dietary fibers. After feeding of the animals with the experimental diets for 2 weeks, differences in the bacterial community structure in the spiral colon were detected in the form of different profiles of terminal restriction fragments (T-RFs). Some of the T-RFs were universally distributed, i.e., they were found in all samples, while others varied in distribution and were related to specific diets. The reproducibility of the T-RFLP profiles between individual animals within the diet groups was high. In the control group, the profiles remained unchanged throughout the experiment and were similar between two independent but identical experiments. When the animals were experimentally infected with Brachyspira hyodysenteriae, causing swine dysentery, many of the T-RFs fluctuated, suggesting a destabilization of the microbial community.     

Profiles of bacterial community composition and metabolic potential through a plug-flow bioreactor fed with lake water

Bacterial community composition and metabolic potential changedthrough a bioreactor. Analyses of gradients in bioreactors maybe an alternative to conventional approaches attempting to unravelthe phenotype of bacterioplankton phylotypes.     

Activity, structure and dynamics of the methanogenic archaeal community in a flooded Italian rice field

Methane production was studied in an Italian rice field over two consecutive years (1998, 1999) by measuring the rates of total and acetate-dependent methanogenesis in soil and root samples. Population dynamics of methanogens were followed by terminal restriction fragment length polymorphism and real-time PCR targeting archaeal SSU rRNA genes. Rates of total and acetate-dependent methanogenesis in soil increased during the season, reached a maximum at about 70-80 days after flooding and then decreased again. In contrast, the size of the archaeal community remained relatively constant. Therefore, the seasonal changes in the methanogenic processes were probably not caused by changes in the size of the methanogenic community but in its activity. During the 1998/1999 winter period, a slight decrease in archaeal cell numbers was found. In both years, the dominant groups were methanogens affiliated with Rice cluster I, Methanosaetaceae, Methanosarcinaceae and Methanobacteriaceae. Correspondence analysis showed, however, that the archaeal community structure was different in 1998 and 1999. Methanogens with potential acetoclastic activity made up a larger fraction of the total archaeal community in 1999 (32-53%) than in 1998 (20-32%). Furthermore, the frequency of Methanosaetaceae relative to Methanosarcinaceae was significantly higher in 1999 than in 1998. This difference could be explained by the much lower soil acetate concentrations in 1999, to which Methanosaetaceae are physiologically better adapted than Methanosarcinaceae. Over the season, however, the composition of the archaeal community remained relatively constant and thus did not reflect the observed seasonal change in CH(4) production activity. The analysis of rice root samples in 1999 showed that the archaeal community structure on the roots was similar to that in soil but with acetoclastic methanogens being relatively less common. This observation is in agreement with domination of CH(4) production by H(2)/CO(2)-dependent methanogenesis on roots. Our study provided a link between size, structure and function of the methanogenic community in an Italian rice field.     

Dynamics of the methanogenic archaeal community during plant residue decomposition in an anoxic rice field soil

Incorporation of plant residues strongly enhances the methane production and emission from flooded rice fields. Temperature and residue type are important factors that regulate residue decomposition and CH(4) production. However, the response of the methanogenic archaeal community to these factors in rice field soil is not well understood. In the present experiment, the structure of the archaeal community was determined during the decomposition of rice root and straw residues in anoxic rice field soil incubated at three temperatures (15 degrees C, 30 degrees C, and 45 degrees C). More CH(4) was produced in the straw treatment than root treatment. Increasing the temperature from 15 degrees C to 45 degrees C enhanced CH(4) production. Terminal restriction fragment length polymorphism analyses in combination with cloning and sequencing of 16S rRNA genes showed that Methanosarcinaceae developed early in the incubations, whereas Methanosaetaceae became more abundant in the later stages. Methanosarcinaceae and Methanosaetaceae seemed to be better adapted at 15 degrees C and 30 degrees C, respectively, while the thermophilic Methanobacteriales and rice cluster I methanogens were significantly enhanced at 45 degrees C. Straw residues promoted the growth of Methanosarcinaceae, whereas the root residues favored Methanosaetaceae. In conclusion, our study revealed a highly dynamic structure of the methanogenic archaeal community during plant residue decomposition. The in situ concentration of acetate (and possibly of H(2)) seems to be the key factor that regulates the shift of methanogenic community.     

Effect of temperature on carbon and electron flow and on the archaeal community in methanogenic rice field soil

Temperature is an important factor controlling CH(4) production in anoxic rice soils. Soil slurries, prepared from Italian rice field soil, were incubated anaerobically in the dark at six temperatures of between 10 to 37 degrees C or in a temperature gradient block covering the same temperature range at intervals of 1 degrees C. Methane production reached quasi-steady state after 60 to 90 days. Steady-state CH(4) production rates increased with temperature, with an apparent activation energy of 61 kJ mol(-1). Steady-state partial pressures of the methanogenic precursor H(2) also increased with increasing temperature from <0.5 to 3.5 Pa, so that the Gibbs free energy change of H(2) plus CO(2)-dependent methanogenesis was kept at -20 to -25 kJ mol of CH(4)(-1) over the whole temperature range. Steady-state concentrations of the methanogenic precursor acetate, on the other hand, increased with decreasing temperature from <5 to 50 microM. Simultaneously, the relative contribution of H(2) as methanogenic precursor decreased, as determined by the conversion of radioactive bicarbonate to (14)CH(4), so that the carbon and electron flow to CH(4) was increasingly dominated by acetate, indicating that psychrotolerant homoacetogenesis was important. The relative composition of the archaeal community was determined by terminal restriction fragment length polymorphism (T-RFLP) analysis of the 16S rRNA genes (16S rDNA). T-RFLP analysis differentiated the archaeal Methanobacteriaceae, Methanomicrobiaceae, Methanosaetaceae, Methanosarcinaceae, and Rice clusters I, III, IV, V, and VI, which were all present in the rice field soil incubated at different temperatures. The 16S rRNA genes of Rice cluster I and Methanosaetaceae were the most frequent methanogenic groups. The relative abundance of Rice cluster I decreased with temperature. The substrates used by this microbial cluster, and thus its function in the microbial community, are unknown. The relative abundance of acetoclastic methanogens, on the other hand, was consistent with their physiology and the acetate concentrations observed at the different temperatures, i.e., the high-acetate-requiring Methanosarcinaceae decreased and the more modest Methanosaetaceae increased with increasing temperature. Our results demonstrate that temperature not only affected the activity but also changed the structure and the function (carbon and electron flow) of a complex methanogenic system.     

Effect of process temperature on bacterial and archaeal communities in two methanogenic bioreactors treating organic household waste

The bacterial and archaeal community structure was examined in two methanogenic anaerobic digestion processes degrading organic household waste at mesophilic (37 degrees C) and thermophilic (55 degrees C) temperatures. Analysis of bacterial clone libraries revealed a predominance of Bacteroidetes (34% of total clones) and Chloroflexi (27%) at the mesophilic temperature. In contrast, in the thermophilic clone library, the major group of clones were affiliated with Thermotogae (61%). Within the domain Archaea, the phyla Euryarchaeota and Crenarchaeota were both represented, the latter only at the mesophilic temperature. The dominating archaeons grouped with Methanospirillum and Methanosarcina species at the mesophilic and thermophilic temperature, respectively. Generally, there was a higher frequency of different sequences at the lower temperature, suggesting a higher diversity compared to the community present at the thermophilic temperature. Furthermore, it was not only the species richness that was affected by temperature, but also the phylogenetic distribution of the microbial populations.     

Effect of temperature on structure and function of the methanogenic archaeal community in an anoxic rice field soil.

Soil temperatures in Italian rice fields typically range between about 15 and 30 degrees C. A change in the incubation temperature of anoxic methanogenic soil slurry from 30 degrees C to 15 degrees C typically resulted in a decrease in the CH4 production rate, a decrease in the steady-state H2 partial pressure, and a transient accumulation of acetate. Previous experiments have shown that these changes were due to an alteration of the carbon and electron flow in the methanogenic degradation pathway of organic matter caused by the temperature shift (K. J. Chin and R. Conrad, FEMS Microbiol. Ecol. 18:85-102, 1995). To investigate how temperature affects the structure of the methanogenic archaeal community, total DNA was extracted from soil slurries incubated at 30 and 15 degrees C. The archaeal small-subunit (SSU) rRNA-encoding genes (rDNA) of these environmental DNA samples were amplified by PCR with an archaeal-specific primer system and used for the generation of clone libraries. Representative rDNA clones (n = 90) were characterized by terminal restriction fragment length polymorphism (T-RFLP) and sequence analysis. T-RFLP analysis produced for the clones terminally labeled fragments with a characteristic length of mostly 185, 284, or 392 bp. Sequence analysis allowed determination of the phylogenetic affiliation of the individual clones with their characteristic T-RFLP fragment lengths and showed that the archaeal community of the anoxic rice soil slurry was dominated by members of the families Methanosarcinaceae (185 bp) and Methanosaetaceae (284 bp), the kingdom Crenarchaeota (185 or 284 bp), and a novel, deeply branching lineage of the (probably methanogenic) kingdom Euryarchaeota (392 bp) that has recently been detected on rice roots (R. Grosskopf, S. Stubner, and W. Liesack, Appl. Environ. Microbiol. 64:4983-4989, 1998). The structure of the archaeal community changed when the temperature was shifted from 30 degrees C to 15 degrees C. Before the temperature shift, the clones (n = 30) retrieved from the community were dominated by Crenarchaeota (70%), "novel Euryarchaeota" (23%), and Methanosarcinacaeae (7%). Further incubation at 30 degrees C (n = 30 clones) resulted in a relative increase in members of the Methanosarcinaceae (77%), whereas further incubation at 15 degrees C (n = 30 clones) resulted in a much more diverse community consisting of 33% Methanosarcinaceae, 23% Crenarchaeota, 20% Methanosaetaceae, and 17% novel Euryarchaeota. The appearance of Methanosaetaceae at 15 degrees C was conspicuous. These results demonstrate that the structure of the archaeal community in anoxic rice field soil changed with time and incubation temperature.     

Effects of varying proportions of concentrates on ruminal-reducing power and bacterial community structure in dry dairy cows fed hay-based diets

The objectives of this study were to evaluate the influence of diet composition on ruminal parameters, more particularly redox potential (Eh). Four Holstein dry dairy cows, fitted with ruminal cannulas, were allocated in a 4 × 4 Latin square design. They were given four experimental hay-based diets D0, D25, D42 and D56 consisting of 0%, 25%, 42% and 56% of ground wheat and barley concentrate mixture, respectively. They were fed at a daily feeding rate of 8.0 kg DM per cow during a 24-day experimental period (a 21-day diet adaptation, three consecutive days of measurement and sampling). The physicochemical parameters, such as pH and Eh, were measured and Clark's exponent (rH) was calculated from 1 h before feeding to 8 h after feeding at 1-h interval. Samples of ruminal fluid were taken at 0, 1, 2, 4, 6 and 8 h after feeding for the determination of volatile fatty acid (VFA) and ammonia N (NH3-N) concentrations. Ruminal bacterial populations were also studied by means of capillary electrophoresis single-strand conformation polymorphism (CE-SSCP) technique to focus on the structure of the ruminal microbiota and the diversity index was calculated. Mean ruminal Eh and rH were not modified by the concentrate-to-forage ratio and averaged - 210 mV and 6.30, respectively, across diets. The pH decreased slightly by 0.10 pH unit between treatments D0 and D56 with an average of 6.58. Nevertheless, the time during which physicochemical parameters remained at nadir value after feeding varied with diets: 2 and 7 h for D0 and 6 and 5 h for D56, respectively for pH and Eh. Moreover, fermentative parameters were altered by treatments: total VFA and NH3-N were greater in D56 (72.2 mM and 17.5 mg/100 ml) compared with D0 (65.2 mM and 14.2 mg/100 ml). However, neither the structure of bacterial populations of the rumen nor the diversity index (Shannon) was altered by treatments.