Distribution and activity of the anaerobic methanotrophic community in a nitrogen-fertilized Italian paddy soil.

In order to mitigate methane emissions from paddy fields, it is important to understand the sources and sinks. Most paddy fields are heavily fertilized with nitrite and nitrate, which can be used as electron acceptors by anaerobic methanotrophs. Here we show that slurry incubations of Italian paddy field soil with nitrate and 13C-labelled methane have the potential for nitrate-dependent anaerobic oxidation of methane (79.9 nmol g-1dw d-1). Community analysis based on 16S rRNA amplicon sequencing and qPCR of the water-logged soil and the rhizosphere showed that anaerobic oxidation of methane-associated archaea (AAA), including Methanoperedens nitroreducens, comprised 9% (bulk soil) and 1% (rhizosphere) of all archaeal reads. The NC10 phylum bacteria made up less than 1% of all bacterial sequences. The phylogenetic analysis was complemented by qPCR showing that AAA ranged from 0.28 × 106 to 3.9 × 106 16S rRNA gene copies g-1dw in bulk soil and 0.27 × 106 to 2.8 × 106 in the rhizosphere. The abundance of NC10 phylum bacteria was an order of magnitude lower. Revisiting published diversity studies, we found that AAA have been detected, but not linked to methane oxidation, in several paddy fields. Our data suggest an important role of AAA in methane cycling in paddy fields.

Cross-epithelial hydrogen transfer from the midgut compartment drives methanogenesis in the hindgut of cockroaches.

In the intestinal tracts of animals, methanogenesis from CO(2) and other C(1) compounds strictly depends on the supply of electron donors by fermenting bacteria, but sources and sinks of reducing equivalents may be spatially separated. Microsensor measurements in the intestinal tract of the omnivorous cockroach Blaberus sp. showed that molecular hydrogen strongly accumulated in the midgut (H(2) partial pressures of 3 to 26 kPa), whereas it was not detectable (<0.1 kPa) in the posterior hindgut. Moreover, living cockroaches emitted large quantities of CH(4) [105 +/- 49 nmol (g of cockroach)(-1) h(-1)] but only traces of H(2). In vitro incubation of isolated gut compartments, however, revealed that the midguts produced considerable amounts of H(2), whereas hindguts emitted only CH(4) [106 +/- 58 and 71 +/- 50 nmol (g of cockroach)(-1) h(-1), respectively]. When ligated midgut and hindgut segments were incubated in the same vials, methane emission increased by 28% over that of isolated hindguts, whereas only traces of H(2) accumulated in the headspace. Radial hydrogen profiles obtained under air enriched with H(2) (20 kPa) identified the hindgut as an efficient sink for externally supplied H(2). A cross-epithelial transfer of hydrogen from the midgut to the hindgut compartment was clearly evidenced by the steep H(2) concentration gradients which developed when ligated fragments of midgut and hindgut were placed on top of each other-a configuration that simulates the situation in vivo. These findings emphasize that it is essential to analyze the compartmentalization of the gut and the spatial organization of its microbiota in order to understand the functional interactions among different microbial populations during digestion.

Hydrogenosomes: convergent adaptations of mitochondria to anaerobic environments.

Hydrogenosomes are membrane-bound organelles that compartmentalise the final steps of energy metabolism in a number of anaerobic eukaryotes. They produce hydrogen and ATP. Here we will review the data, which are relevant for the questions: how did the hydrogenosomes originate, and what was their ancestor? Notably, there is strong evidence that hydrogenosomes evolved several times as adaptations to anaerobic environments. Most likely, hydrogenosomes and mitochondria share a common ancestor, but an unequivocal proof for this hypothesis is difficult because hydrogenosomes lack an organelle genome - with one remarkable exception (Nyctotherus ovalis). In particular, the diversity of extant hydrogenosomes hampers a straightforward analysis of their origins. Nevertheless, it is conceivable to postulate that the common ancestor of mitochondria and hydrogenosomes was a facultative anaerobic organelle that participated in the early radiation of unicellular eukaryotes. Consequently, it is reasonable to assume that both, hydrogenosomes and mitochondria are evolutionary adaptations to anaerobic or aerobic environments, respectively.

Multiple acquisition of methanogenic archaeal symbionts by anaerobic ciliates.

Anaerobic heterotrichous ciliates (Armophoridae and Clevelandellidae) possess hydrogenosomes that generate molecular hydrogen and ATP. This intracellular source of hydrogen provides the basis for a stable endosymbiotic association with methanogenic archaea. We analyzed the SSU rRNA genes of 18 heterotrichous anaerobic ciliates and their methanogenic endosymbionts in order to unravel the evolution of this mutualistic association. Here, we show that the anaerobic heterotrichous ciliates constitute at least three evolutionary lines. One group consists predominantly of gut-dwelling ciliates, and two to three, potentially four, additional clades comprise ciliates that thrive in freshwater sediments. Their methanogenic endosymbionts belong to only two different taxa that are closely related to free-living methanogenic archaea from the particular ecological niches. The close phylogenetic relationships between the endosymbionts and free-living methanogenic archaea argue for multiple acquisitions from environmental sources, notwithstanding the strictly vertical transmission of the endosymbionts. Since phylogenetic analysis of the small-subunit (SSU) rRNA genes of the hydrogenosomes of these ciliates indicates a descent from the mitochondria of aerobic ciliates, it is likely that anaerobic heterotrichous ciliates hosted endosymbiotic methanogens prior to their radiation. Therefore, our data strongly suggest multiple acquisitions and replacements of endosymbiotic methanogenic archaea during their host's adaptation to the various ecological niches.

Voltage-dependent reversal of anodic galvanotaxis in Nyctotherus ovalis.

Aerobic and anaerobic ciliates swim towards the cathode when they are exposed to a constant DC field. Nyctotherus ovalis from the intestinal tract of cockroaches exhibits a different galvanotactic response: at low strength of the DC field the ciliates orient towards the anode whereas DC fields above 2-4 V/cm cause cathodic swimming. This reversal of the galvanotactic response is not due to backward swimming. Rather the ciliates turn around and orient to the cathode with their anterior pole. Exposure to various cations, chelators, and Ca(2+)-channel inhibitors suggests that Ca(2+)-channels similar to the "long lasting" Ca(2+)-channels of vertebrates are involved in the voltage-dependent anodic galvanotaxis. Evidence is presented that host-dependent epigenetic factors can influence the voltage-threshold for the switch from anodic to cathodic swimming.

Evolution of anaerobic ciliates from the gastrointestinal tract: phylogenetic analysis of the ribosomal repeat from Nyctotherus ovalis and its relatives.

The 18S and 5.8S rDNA genes and the internal transcribed spacers ITS-1 and ITS-2 of ciliates living in the hindgut of frogs, millipedes, and cockroaches were analyzed in order to study the evolution of intestinal protists. All ciliates studied here belong to the genus Nycrotherus. Phylogenetic analysis revealed that these ciliates from a monophyletic group that includes the distantly related anaerobic free-living heterotrichous ciliates Metopus palaeformis and Metopus contortus. The intestinal ciliates from the different vertebrate and invertebrate hosts are clearly divergent at the level of their rDNA repeats. This argues for the antiquity of the associations and a predominantly vertical transmission. This mode of transmission seems to be controlled primarily by the behavior of the host. The different degrees of divergence between ciliates living in different strains of one and the same cockroach species most likely reflect the different geographical origins of the hosts. In addition, host switches must have occurred during the evolution of cockroaches, since identical ciliates were found only in distantly related hosts. These phenomena prevent the reconstruction of potential cospeciation events.

Intestinal methanogenesis in primates--a genetic and evolutionary approach.

The presence of significant numbers of intestinal methanogens among vertebrates does neither depend on elaborated morphological structures nor on predominantly plant-based diets. Phylogenetic rather than dietary restrictions limit the occurrence of methanogenic bacteria also in the hindguts of primates. The Old-World monkeys are methanogenic--with the only exceptions of Cheirogaleid lemurs and bush-babies. In contrast, among New World monkeys the lack of intestinal methanogens is observed frequently in capuchins and marmosets. Since the absence of methanogens does not parallel distinct morphological, physiological, or ethological characteristics, it is likely that methanogenesis depends on a hereditary predisposition. In humans, methane-producers account for approximately 50% of the European populations. In this study, 56 individuals belonging to 5 families were studied for the occurrence of methane in the breath. The results of this screen are compatible with the assumption that the trait "methane emission" segregates as an autosomal, dominant character. Our findings suggest a high specificity of the symbiosis between primates and methanogenic bacteria. Therefore, the persistence of significant numbers of methanogens in the hindgut might be facilitated by a specific receptor for methanogenic bacteria.