Endosymbiotic Methanogenic Bacteria In Anaerobic Ciliates: Significance For the Growth Efficiency of the Host

ABSTRACT Endosymbiotic methanogenic bacteria of three species of anaerobic ciliates (Plagiopyla frontata, Metopus conforms , and M. palaeformis) were inactivated with the specific methanogen inhibitor 2-bromoethanesulfonic acid. the absence of endosymbiont methanogens reduced growth rate and growth yield by about 30% in P. frontata and M. contortus , while no significant change in fitness was observed in M. palaeformis. In Plagiopyla the growth rate constant is not affected by an artificially increased pH₂ neither in normal nor in methanogen-free ciliates. the energetic advantage conferred by endosymbiont methanogens in Plagiopyla and in Metopus contortus probably is due to excretion of organic material from the bacteria at the expense of bacterial reproduction. It is unlikely that the maintenance of a low pH₂ within the cells due to H₂-consumption by the bacteria is important to the ciliates.     

Chemosensory Behaviour of Strombidium purpureum, an Anaerobic Oligotrich with Endosymbiotic Purple Non-Sulphur Bacteria

ABSTRACT. Strombidium purpureum Kahl, is an anaerobic oligotrichous ciliate with endosymbiotic phototrophic bacteria. Like other anaerobic ciliates, S. purpureum reacts to O₂-pressure. In the light, the ciliates avoid even traces of O₂ (< 1% atmospheric saturation). In the dark, however, the ciliates accumulate in water with a pO₂ of 1–4% atmospheric saturation. Experiments show that ciliates which have accumulated in the dark under microaerophilic conditions react when the light is turned on, and their ability to escape is enhanced by steep O₂-gradients. The ciliates orient themselves in O₂-gradients by a series of phobic responses. They tumble whenever they swim towards a higher O₂-tension and thus they eventually all swim in the direction of lower pO₂. The ecological implications of such behaviour are discussed.     

The Contribution of Ciliated Protozoa to Plankton and Benthos Biomass in a European Ricefield

The densities and biomass of ciliates inhabiting the water-sediment interface and the water column of an experimental ricefield were investigated throughout four annual cycles. Ciliate abundance and biomass were higher at the water-sediment interface than in the water column. In both sites, large ciliates (> 10⁵μm³) contributed the higher biomass values, but the highest densities were found in the intermediate size class (10⁴-10⁵μm³). The prorodontid Coleps hirtus dominated the ciliate assemblage and usually comprised > 50% of total ciliate density. Blooms of C. hirtus , occurred in June in the water column and in July at the sediment surface. During the four cycles of rice cultivation, the average daily values for production of the entire ciliate community was 69.6 mgC/m²/d, and the net production efficiency (K₂) was 72.0%. The estimated production values in the present study are high if compared to production measured for ciliates in other freshwater ecosystems.     

Hydrogenosome-Methanogen Assemblages in the Echinoid Endocommensal Plagiopylid Ciliates,Lechriopyla mystax Lynch, 1930 and Plagiopyla minuta Powers, 19331

ABSTRACT. Lechriopyla mystax Lynch, 1930 and Plagiopyla minula Powers, 1933 contain hydrogenosome-methanogen assemblages similar to those reported for other plagiopylid ciliates. These assemblages are stacks of elongate ovoid hydrogenosomes alternating with methanogens; these stacks are surrounded by cisternae of the rough endoplasmic reticulum that are often accompanied by Golgi complexes. The individual methanogens in the larger ciliate, L. mystax, are about four times the volume of those in the smaller ciliate, P. minuta, but both ciliates appear to contain Gram-negative methanococcoid bacteria, possibly Methanoplanus sp. The endoplasmic reticulum-Golgi complex probably plays a significant role in exploitation of the methanogens by the host ciliate.     

Epibiotic Bacteria on Several Ciliates from Marine Sediments

ABSTRACT Bacterial epibionts were observed on the surface of the marine sediment ciliate Geleia fossata. Rod-shaped bacteria, from 2-10 X10³ per ciliate, were universally positioned in ciliated grooves, in apparent spatial association with dikinetids. SEM and TEM examination of the ciliates confirmed that a tight affiliation exists between the epibiotic bacteria and ciliate cortex infrastructures. These observations, as well as the distinct bacterial distribution pattern over ciliate surface, suggest that there is a close epibiont/host physiological integration. Epibiotic bacteria were also observed on the surfaces of other sediment ciliates from the genera Loxophyllum, Tracheloraphis, Geleia, Paraspathidium , and Cyclidium. These findings indicate that the bacterial/protozoa associations are widespread in the marine benthic environment. The potential benefits for both epibionts and their hosts are discussed.     

Hydrogen turnover by psychrotrophic homoacetogenic and mesophilic methanogenic bacteria in anoxic paddy soil and lake sediment

Abstract The effect of temperature on CH₄ production, turnover of dissolved H₂, and enrichment of H₂-utilizing anaerobic bacteria was studied in anoxic paddy soil and sediment of Lake Constance. When anoxic paddy soil was incubated under an atmosphere of H₂/CO₂, rates of CH₄ production increased 25°C, but decreased at temperatures lower than 20°C. Chloroform completely inhibited methano-genesis in anoxic paddy soil and lake sediment, but did not or only partially inhibit the turnover of dissolved H₂, especially at low incubation temperatures. Cultures with H₂ as energy source resulted in the enrichment of chemolithotrophic homoacetogenic bacteria whenever incubation temperatures were lower than 20°C. Hydrogenotrophic methanogens could only be enriched at 30°C from anoxic paddy soil. A homoacetogen     

Spectacular abundance of ciliates in anoxic pond water: contribution of symbiont photosynthesis to host respiratory oxygen requirements

Abstract: Very large numbers (3466 ml⁻¹) of ciliated protozoa were found living beneath the oxic-anoxic boundary in a stratified freshwater pond. Most ciliates (96%) contained symbiotic algae ( Chlorella spp.). Peak abundance was in anoxic water with almost 1 mol free CO₂ m⁻³ and a midday irradiance of 6 μmol photon m⁻² s⁻¹. Photosynthetic rate measurements of metalimnetic water indicated a light compensation point of 1.7 μmol photon m⁻² s⁻¹ which represents 0.6% of sub-surface light. We calculate that photosynthetic evolution of O₂ by symbionts is sufficient to meet the demand of the host ciliates for 13 to 14 hours each day. Each 'photosynthetic ciliate' may therefore become an aerobic island surrounded by anoxic water.     

Soil type links microbial colonization of rice roots to methane emission

Most of the methane (CH₄) emission from rice fields is derived from plant photosynthates, which are converted to CH₄. Rice cluster I (RC-1) archaea colonizing the rhizosphere were found to be the methanogens responsible for this process. Hence, RC-1 methanogens seem to play a crucial role in emission of the greenhouse gas CH₄. We determined the community composition and activity of methanogens colonizing the roots of eight different rice cultivars after growth on both Italian rice soil and river bank soil, which contained different communities of methanogenic archaea. The community composition was analyzed by terminal restriction fragment length polymorphism and cloning/sequencing of the archaeal 16S rRNA gene and the mcrA gene coding for a subunit of the methyl coenzyme M reductase. When grown on rice field soil, the methanogenic community of the different rice cultivars was always dominated by RC-1 methanogens. In contrast, roots were colonized by Methanomicrobiales when grown on river bank soil, in which RC-1 methanogens were initially not detectable. Roots colonized with Methanomicrobiales compared with RC-1 exhibited lower CH₄ production and CH₄ emission rates. The results show that the type of methanogens colonizing rice roots has a potentially important impact on the global CH₄ cycle.     

Distribution of cytochromes in methanogenic bacteria

Abstract Various methanogenic bacteria belonging to the orders Methanobacteriales, Methanococcales , and Methanomicrobiales were examined for the presence of cytochromes. Those methanogens which are capable of growing only on H ₂+ CO ₂ or formate were found to lack cytochromes. However, membrane-bound cytochromes were detected in species able to utilize methanol, methylamines or acetate.     

The microplankton organisms at the oxic-anoxic interface in the pelagial of the Black Sea

Abstract The semi-permanent anoxia in the deep-waters of the Black Sea supported the formation of a unique microplankton community at the oxicanoxic interface. One group of ciliates ( Pleuronema marinum, Askenasia sp., species of the families Tracheliidae, Holophryidae and Amphileptidae) inhabited the water layer just above the upper boundary of H₂S, and was spatially associated with and fed on large colorless sulphur bacteria ( Thiovulum spp.). Other ciliates (species of order Scuticociliatida) populated the upper layer of the H₂S zone. A significant part of them possessed ectosymbiotic bacteria. Since the metazoans were not found in the O₂ and H₂S boundary layer, the protist community is considered to be the main factor in utilization of chemotrophic bacterial production.