Community Composition Of Archaea Research Articles

Limited effects of depth (0–80 cm) on communities of archaea, bacteria and fungi in paddy soil profiles

AbstractMost current microbial studies in paddy soils have focused on the top (0–20 cm) layer where rice roots are concentrated. To better understand the vertical distribution of microorganisms in paddy soils, we investigated the abundances, diversities and community compositions of archaea, bacteria and fungi in six geographically and climatically distinct paddy soil profiles from 0–80‐cm depth. Although microbial abundances and operational taxonomic unit (OTU) diversities largely decreased with soil depth, only the community composition of archaea (not bacteria or fungi) was associated with soil depth, echoing that only one archaeal OTU, but no bacterial or fungal OTUs, differed significantly in relative abundance between depth intervals. Mean annual temperature, precipitation and soil iron and manganese concentrations were significantly correlated with the ordinations of microbial communities for all three domains. Besides these common environmental factors, bacterial and archaeal community structures were also influenced by soil chloride and sulphate concentrations, whereas the concentrations of organic matter and total nitrogen were important explanatory factors for the variation in fungal community composition. Further analyses on putative bacterial functions showed significant differences between sampling sites rather than depth intervals, and suggested that bacterial OTUs that significantly varied in relative abundance across sampling sites might be functionally related to organic matter decomposition, sulphur oxidation and reduction, as well as nitrate reduction. Altogether, in the studied paddy soil profiles, the community composition and putative functions of bacteria were largely the same between different vertical layers, each with a thickness of 20 cm. This study suggests that the community compositions of archaea, bacteria and fungi are mainly driven by different soil chemical properties rather than soil depth, which could be linked to the ecological traits of the three microbial domains.Highlights Communities of archaea, bacteria and fungi were investigated in six paddy soil profiles. Soil depth was only correlated with archaeal community structure Environmental factors influenced community composition differently for different domains. Bacterial OTUs contributing to variation in community composition among sites were functionally linked to C, N and S cycling.

Diversity of Archaea and Its Correlation with Environmental Factors in the Ebinur Lake Wetland.

The diversity and community composition of archaea in soil samples from three wetlands (SP1, SP2, and SP3) of Ebinur Lake were studied by constructing 16S rDNA cloning library. The correlation between the diversity of archaea and soil environmental factors was analyzed by CANOCO software. The aim of this study was to reveal the differences of community structures of archaea in different sample sites, to provide a theoretical basis for further study on degradation and restoration of Ebinur Lake wetland. The results showed that Euryarchaeota accounted for 57.1% was the most dominant phylum observed, followed by Thaumarchaeota and Crenarchaeota for the three wetland soil analyzed. Compared with SP3 site, the proportions of Euryarchaeota were decreased by 16.70% and 31.78%, while Thaumarchaeota increased by 7.26% and 17.64% in the SP1 and SP2, respectively. Crenarchaeota was found only in SP3. Shannon-wiener diversity indices in SP1, SP2, and SP3 sites were 3.44, 3.87, and 3.94, respectively, indicating that the diversity of archaea in three plots was: SP3 > SP2 > SP1. Redundancy analysis (RDA) showed that electrical conductivity (EC), soil moisture (SM), hydrogen potential (pH), and soil organic matter content (SOM) may affect archaeal communities. Compared to EC and pH, SM and SOM may have a greater impact on the community composition of archaea.

Biogeographic Distribution Patterns of the Archaeal Communities Across the Black Soil Zone of Northeast China.

Although archaea are ubiquitous in various environments, the knowledge gaps still exist regarding the biogeographical distribution of archaeal communities at regional scales in agricultural soils compared with bacteria and fungi. To provide a broader biogeographical context of archaeal diversity, this study quantified the abundance and community composition of archaea across the black soil zone in northeast China using real-time PCR and high-throughput sequencing (HTS) methods. Archaeal abundances across all soil samples ranged from 4.04 × 107 to 26.18 × 107 16S rRNA gene copies per gram of dry soil. Several soil factors were positively correlated with the abundances including soil pH, concentrations of total C, N, and P, and available K in soil, and soil water content. Approximately 94.2, 5.7, and 0.3% of archaeal sequences, and 31, 151, and 3 OTUs aligned within the phyla Thaumarchaeota, Euryarchaeota, and Crenarchaeota, respectively. Within the phylum of Thaumarchaeota, group 1.1b was a dominating genus accounting for an average of 87% archaeal sequences and phylogenetically classified as Nitrososphaera, a genus of ammonia oxidizing archaea. The response of dominating OTUs to environmental factors differed greatly, suggesting the physiological characteristics of different archaeal members is diversified in the black soils. Although the number of OTUs was not related with any particular soil parameters, the number of OTUs within Thaumarchaeota and Euryarchaeota was marginally related with soil pH. Archaeal community compositions differed between samples, and a Canonical correspondence analysis (CCA) analysis indicated that soil pH and the latitude of sampling locations were two dominating factors in shifting community structures. A variance partitioning analysis (VPA) analysis showed that the selected soil parameters (32%) were the largest drivers of community variation, in particular soil pH (21%), followed by geographic distances (19%). These findings suggest that archaeal communities have distinct biogeographic distribution pattern in the black soil zone and soil pH was the key edaphic factor in structuring the community compositions.

Diversity and distribution of archaea community along a stratigraphic permafrost profile from Qinghai-Tibetan Plateau, China.

Accompanying the thawing permafrost expected to result from the climate change, microbial decomposition of the massive amounts of frozen organic carbon stored in permafrost is a potential emission source of greenhouse gases, possibly leading to positive feedbacks to the greenhouse effect. In this study, the community composition of archaea in stratigraphic soils from an alpine permafrost of Qinghai-Tibetan Plateau was investigated. Phylogenic analysis of 16S rRNA sequences revealed that the community was predominantly constituted by Crenarchaeota and Euryarchaeota. The active layer contained a proportion of Crenarchaeota at 51.2%, with the proportion of Euryarchaeota at 48.8%, whereas the permafrost contained 41.2% Crenarchaeota and 58.8% Euryarchaeota, based on 16S rRNA gene sequence analysis. OTU1 and OTU11, affiliated to Group 1.3b/MCG-A within Crenarchaeota and the unclassified group within Euryarchaeota, respectively, were widely distributed in all sediment layers. However, OTU5 affiliated to Group 1.3b/MCG-A was primarily distributed in the active layers. Sequence analysis of the DGGE bands from the 16S rRNAs of methanogenic archaea showed that the majority of methanogens belonged to Methanosarcinales and Methanomicrobiales affiliated to Euryarchaeota and the uncultured ZC-I cluster affiliated to Methanosarcinales distributed in all the depths along the permafrost profile, which indicated a dominant group of methanogens occurring in the cold ecosystems.

Response of the methanogenic microbial communities in Amazonian oxbow lake sediments to desiccation stress

Methanogenic microbial communities in soil and sediment function only when the environment is inundated and anoxic. In contrast to submerged soils, desiccation of lake sediments happens only rarely. However, some predictions suggest that extreme events of drying will become more common in the Amazon region, and this will promote an increase in sediments drying and exposure. We asked whether and how such methanogenic communities can withstand desiccation stress. Therefore, we determined the rates and pathways of CH(4) production (analysis of CH(4) and δ(13) C of CH(4), CO(2) and acetate), the copy numbers of bacterial and archaeal 16S rRNA genes and mcrA genes (quantitative PCR), and the community composition of Archaea and Bacteria (T-RFLP and pyrosequencing) in oxbow lake sediments of rivers in the Brazilian Amazon region. The rivers were of white water, black water and clear water type. The measurements were done with sediment in fresh state and after drying and rewetting. After desiccation and rewetting the composition of both, the archaeal and bacterial community changed. Since lake sediments from white water rivers exhibited only negligible methanogenic activity, probably because of relatively high iron and low organic matter content, they were not further analysed. The other sediments produced CH(4), with hydrogenotrophic methanogenesis usually accounting for > 50% of total activity. After desiccation and rewetting, archaeal and bacterial gene copy numbers decreased. The bacterial community showed a remarkable increase of Clostridiales from about 10% to > 30% of all Bacteria, partially caused by proliferation of specific taxa as the numbers of OTU shared with fresh sediment decreased from about 9% to 3%. Among the Archaea, desiccation specifically enhanced the relative abundance of either Methanocellales (black water) and/or Methanosarcinaceae (clear water). Despite the changes in gene copy numbers and composition of the microbial community, rates of CH(4) production even increased after desiccation-rewetting, demonstrating that the function of the methanogenic microbial community had not been impaired. This result indicates that the increase in extreme events of drying may increase methane production in flooded sediments.

PH dominates variation in tropical soil archaeal diversity and community structure

Little is known of the factors influencing soil archaeal community diversity and composition in the tropics. We sampled soils across a range of forest and nonforest environments in the equatorial tropics of Malaysia, covering a wide range of pH values. DNA was PCR-amplified for the V1-V3 region of the 16S rRNA gene, and 454-pyrosequenced. Soil pH was the best predictor of diversity and community composition of Archaea, being a stronger predictor than land use. Archaeal OTU richness was highest in the most acidic soils. Overall archaeal abundance in tropical soils (determined by qPCR) also decreased at higher pH. This contrasts with the opposite trend previously found in temperate soils. Thaumarcheota group 1.1b was more abundant in alkaline soils, whereas group 1.1c was only detected in acidic soils. These results parallel those found in previous studies in cooler climates, emphasizing niche conservatism among broad archaeal groups. Among the most abundant operational taxonomic units (OTUs), there was clear evidence of niche partitioning by pH. No individual OTU occurred across the entire range of pH values. Overall, the results of this study show that pH plays a major role in structuring tropical soil archaeal communities.

High abundance of Crenarchaeota in a temperate acidic forest soil

The objective of the study was to elucidate the depth distribution and community composition of Archaea in a temperate acidic forest soil. Numbers of Archaea and Bacteria were measured in the upper 18 cm of the soil, and soil cores were sampled on two separate occasions using quantitative PCR targeting 16S rRNA genes. Maximum numbers of Archaea were 0.6-3.8 x 10(8) 16S rRNA genes per gram of dry soil. Numbers of Bacteria were generally higher, but Archaea always accounted for a high percentage of the total gene numbers (12-38%). The archaeal community structure was analysed by the construction of clone libraries and by terminal restriction length polymorphism (T-RFLP) using the same Archaea-specific primers. With the reverse primer labelled, T-RFLP analysis led to the detection of four T-RFs. Three had lengths of 83, 185 and 218 bp and corresponded to uncultured Crenarchaeota. One (447 bp) was assigned to Thermoplasmales. Labelling of the forward primer allowed further separation of the T-RF into Crenarchaeota Group I.1c and Group I.1b, and indicated that Crenarchaeota of the Group I.1c were the predominant 16S rRNA genotype (<or=85%) in the soil. The abundance of Archaea and concentration of ammonia and nitrate decreased with soil depth. Hence it is unclear if the detected Crenarchaeota Group I.1c participated in ammonia oxidation or had another phenotype.