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Symbiotic microbiomes of Sphagnum have been confirmed to play a fundamental role in carbon and nitrogen cycles, however, little is known about microbiomes associated with other bryophytes in subtropical peatland ecosystems. To explore the differences in community structure, metabolic potential and interaction relationship of bacterial microbiomes associated with different bryophytes species, the gametophytes of three bryophyte species (Sphagnum palustre, Aulacomnium androgynum, and Polytrichum commune) and their underlying peat sediments were collected from the subtropical Dajiuhu Peatland and subjected to Illumina high-throughout sequencing of 16S rRNA gene. Results showed that bacterial diversity was lowest in S. palustre, the dominant moss species, among the three moss species investigated in Dajiuhu Peatland. Bacterial communities from bryophytes clearly separated with those from sediments as indicated by both phylogenetic and taxonomical approaches. Linear discriminant analysis effect size (LEfSe) identified 30 and 36 indicator taxa in mosses and peat sediments. Bacteroidetes, Verrucomicrobia and Thermoleophilia significantly enriched in S. palustre, A. androgynum and P. commune, Chloroflexi, Proteobacteria and Acidobacteria subgroup 6 was indicator taxa for corresponding underlying sediments, respectively. Despite of these differences in compositions, bacterial functional structures were similar among all bryophytes, such as abundant aerobic heterotrophs, rare nitrifiers and denitrifiers. This phenomenon was also observed among the underlying sediments. Network analysis indicated that Proteobacteria and Acidobacteria located in the center of network and exerted strong interactions to other taxa. The sub-network of bacterial communities in sediments was more connected and microbial groups were more competitive than those in bryophytes subnetwork. Our results offer new insight into the community structure, ecological function and interaction pattern of bacterial microbiomes in the Dajiuhu Peatland across different habitats. [ABSTRACT FROM AUTHOR]

Frequency‐dependent anelastic attenuation is a fact that must be considered when inverting seismic data. The shallow attenuation characteristics of large sedimentary basins with frequent earthquakes in mainland China are still unclear, which hinders the study of strong ground motion. Borehole seismometers distributed in these areas provide information on shallow structures. In this study, the direct and surface‐reflected phases in local earthquake borehole seismograms were extracted to calculate the average S wave anelastic attenuation of shallow sediments in mainland China. Relying on the seismograms recorded by 103 borehole stations, the attenuation values and lithologies of the shallow sediments above the borehole seismometers were estimated by applying a multi‐time window analysis method. We suggested that the QS−1 values generally decrease from 0.04–0.50 at 1 Hz to 0.01–0.05 at 10 Hz. We obtained the empirical relationships among attenuation, velocity, and depth and found that the dominant mechanisms for attenuation above and below a depth of 400 m could be different due to sediment compositions and scales. Certain borehole depths and corresponding Vs values were corrected by analyzing the time difference variation and the QS−1 distinction. Plain Language Summary: The energy of seismic waves propagating through a medium will dissipate due to internal friction and non‐uniform scattering along the propagation path. Attenuation is an important feature of Earth's media. Strong attenuation has a significant influence on predictions of strong ground motion, especially for sedimentary basins. Moreover, compared to velocity, attenuation is more sensitive to changes in rock properties caused by stress. Therefore, it is important to understand the attenuation of shallow sediments in mainland China, which has high seismicity. More than 100 borehole stations have been established through the development of a seismic network in China. Relying on the seismograms recorded by these underground stations, the attenuation and velocity values and lithologies of the shallow sediments above the borehole seismometers were estimated by applying a robust and reliable analysis method. We also obtained the empirical relationships among attenuation, velocity, and depth. These results can be most useful in the prediction of strong ground motion. The method adopted in this study will also be useful for the evaluation of anelastic attenuation in other sedimentary basins. Key Points: The average QS−1 and VS values of shallow sediments across mainland China are obtainedThe empirical relationships among attenuation, velocity, and depth are obtainedCertain seismometer installation depths and corresponding VS values are corrected [ABSTRACT FROM AUTHOR]

To investigate the vertical variation of microbial functional groups particular nitrogen fixers and ammonia oxidizers, sediment samples from a 155 cm deep peat profile were collected from the acidic Dajiuhu Peatland and subsequently subjected to clone library construction and quantification. Results showed that nifH gene abundance varied between 105–108 copies per gram dry sediment and reduced gradually with depth. The abundances of ammonia oxidizing archaea (AOA) and ammonia oxidizing bacteria (AOB) abundance were generally comparable in each sample. More AOA was observed with a depth ≤55 cm, whereas AOB was more abundant with a depth >55 cm. Phylogenetically nifH could be divided into 94 OTUs which mainly affiliated with α-Proteobacteria. AOA were affiliated with Nitrosotalea from Group 1.1a associated (nearly 90%) and Nitrososphaera from Group I.1b. All AOB belonged to Nitrosospira. Notably, DJH11 with the depth of 50–55 cm was observed to have the highest abundance and the highest diversity of nitrogen fixers and ammonia oxidizers among all the samples. Pearson's correlation analysis showed a positive relationship between water content and pH with the nifH gene abundance. Our results offer the first insight about the microbial community composition and diversity involved in nitrogen cycles in the Dajiuhu Peatland. [ABSTRACT FROM AUTHOR]