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Hua, Z.-S.

Publications and source records attributed to Hua, Z.-S..

5 recordsLinked to original sources

The recovery of 12,789 genomes revealed the diversity, function, and microbial interactions of the geothermal spring microbiome

Geothermal springs, characterized by extreme physicochemical conditions, represent ecologically and evolutionarily significant habitats that foster unique microbial communities and drive adaptive evolutionary processes. Despite their importance, the complex microbial interactions and underlying mechanisms governing community assembly in these environments remain poorly understood. In this study, we conducted systematic sampling across 49 geothermal springs in Tengchong, Yunnan, over a six-year period (2016-2021), and performed metagenomic sequencing on 152 samples. We successfully reconstructed 12,789 non-redundant microbial genomes, revealing an exceptionally high level of phylogenetic and functional diversity within the spring microbiomes. Our analyses demonstrate that pH and temperature are the primary deterministic drivers shaping both microbial species composition and functional potential, thereby segregating the communities into three distinct groups: acidic, hyperthermal, and thermal. Furthermore, ecological network analysis revealed that extreme environmental conditions significantly alter network topology, resulting in less complex but more efficient microbial interaction networks. Collectively, this study provides a comprehensive resource and mechanistic insights into the microbial diversity, community structure, and species interactions in geothermal spring ecosystems.

microbiology↗

The anaerobic WOR-3 Bacteria: Hydrogenotrophic metabolism and unique carbon fixation via Archaeal form III RuBisCO

The uncultured WOR-3 phylum is widely distributed in anaerobic environments, including hot springs, marine ecosystems, and hydrothermal vents, yet its ecological roles and metabolic capabilities remain poorly understood. In this study, we analyzed 180 medium- to high-quality metagenome-assembled genomes (MAGs), including 59 newly reconstructed from environmental samples and 121 retrieved from the Genome Taxonomy Database (GTDB). Phylogenetic analyses resolved the WOR-3 lineage into four subgroups (subgroup 1-4). Metabolic reconstruction revealed significant divergence of the carbon, sulfur, nitrogen and hydrogen metabolism pathways among the different subgroups. Subgroup 1 was characterized by fermentative metabolism involving formate and ethanol, and uniquely exhibited potential for carbon fixation via Calvin cycle, as indicated by the presence of ribulose-1,5-bisphosphate carboxylase/oxygenase (RuBisCO) gene. Notably, WOR-3 RuBisCO is phylogenetically affiliated with archaeal form III, although the carbon fixation pathway follows the canonical bacterial Calvin cycle--a feature of potential evolutionary significance. Subgroup 3 exhibits metabolic versatility, including genes for dissimilatory sulfate reduction, sulfur oxidation, partial denitrification, and fatty acid degradation. In addition, all subgroups harbored key components of hydrogen metabolism, including widespread NiFe hydrogenases and Rnf complexes, supporting H2-dependent electron transfer and energy conservation under anaerobic conditions. Featuring near-universal presence of complexes I and II and frequent occurrence of terminal oxidases (cydAB and coxABC)--suggests a facultative anaerobic lifestyle. Collectively, this study expands the genomic framework for the WOR-3 phylum and provides novel insights into the metabolic versatility and ecological functions of this previously uncharacterized lineage in biogeochemical cycles of carbon, nitrogen, and sulfur. IMPORTANCEThe WOR-3 phylum represents a widespread but poorly understood bacterial lineage inhabiting diverse anaerobic/microaerobic environments. By integrating 180 metagenome-assembled genomes, including 59 newly reconstructed, this study provides the most comprehensive genomic framework to date for WOR-3. Phylogenomic and metabolic analyses revealed four distinct subgroups with divergent capacities for carbon, sulfur, and nitrogen metabolism. Notably, subgroup 1 encodes a complete Calvin-Benson-Bassham (CBB) cycle featuring an archaeal-type form III RuBisCO, suggesting an unusual evolutionary trajectory for carbon fixation in this lineage. Subgroup 3 exhibits versatile metabolic potential, including dissimilatory sulfur metabolism, partial denitrification, and fatty acid degradation, highlighting its possible roles in multiple biogeochemical processes. The widespread presence of hydrogenases and respiratory complexes across all subgroups supports energy conservation under anaerobic or microaerobic conditions. These findings not only expand the taxonomic and functional landscape of the WOR-3 phylum but also offer key insights into its ecological roles in global element cycling.

microbiology↗

Phylogenomic analyses reveal that Panguiarchaeum is a clade of genome-reduced Asgard archaea

The Asgard archaea are a diverse archaeal phylum important for our understanding of cellular evolution because they include the lineage that gave rise to eukaryotes. Recent phylogenomic work has focused on characterising the diversity of Asgard archaea in an effort to identify the closest extant relatives of eukaryotes. However, resolving archaeal phylogeny is challenging, and the positions of two recently-described lineages - Njordarchaeales and Panguiarchaeales - are uncertain, in ways that directly bear on hypotheses of early evolution. In initial phylogenetic analyses, these lineages branched either with Asgards or with the distantly-related Korarchaeota, and it has been suggested that their genomes may be affected by metagenomic contamination. Resolving this debate is important because these clades include genome-reduced lineages that may help inform our understanding of the evolution of symbiosis within Asgard archaea. Here, we performed phylogenetic analyses revealing that the Njordarchaeales and Pangiuarchaeales constitute the new class Njordarchaeia within Asgard archaea. We found no evidence of metagenomic contamination affecting phylogenetic analyses. Njordarchaeia exhibit hallmarks of adaptations to (hyper-)thermophilic lifestyles, including biased sequence compositions that can induce phylogenetic artifacts unless adequately modelled. Panguiarchaeum is metabolically distinct from its relatives, with reduced metabolic potential and various auxotrophies. Phylogenetic reconciliation recovers a complex common ancestor of Asgard archaea that encoded the Wood-Ljungdahl pathway. The subsequent loss of this pathway during the reductive evolution of Panguiarchaeum may have been associated with the switch to a symbiotic lifestyle based on H2-syntrophy. Thus, Panguiarchaeum may contain the first obligate symbionts within Asgard archaea.

evolutionary biology↗

Inference and reconstruction of the heimdallarchaeial ancestry of eukaryotes

In the ongoing debates about eukaryogenesis, the series of evolutionary events leading to the emergence of the eukaryotic cell from prokaryotic ancestors, members of the Asgard archaea play a key role as the closest archaeal relatives of eukaryotes. However, the nature and phylogenetic identity of the last common ancestor of Asgard archaea and eukaryotes remain unresolved. Here, we analyze distinct phylogenetic marker datasets of an expanded genomic sampling of Asgard archaea and evaluate competing evolutionary scenarios using state-of-the-art phylogenomic approaches. We find that eukaryotes are placed, with high confidence, as a well-nested clade within Asgard archaea, as a sister lineage to Hodarchaeales, a newly proposed order within Heimdallarchaeia. Using sophisticated gene tree/species tree reconciliation approaches, we show that, in analogy to the evolution of eukaryotic genomes, genome evolution in Asgard archaea involved significantly more gene duplication and fewer gene loss events compared to other archaea. Finally, we infer that the last common ancestor of Asgard archaea likely was a thermophilic chemolithotroph, and that the lineage from which eukaryotes evolved adapted to mesophilic conditions and acquired the genetic potential to support a heterotrophic lifestyle. Our work provides key insights into the prokaryote-to-eukaryote transition and the platform for the emergence of cellular complexity in eukaryotic cells.

evolutionary biology↗

Metagenomic discovery of Candidatus Parvarchaeales related lineages sheds light on the adaptation and diversification from neutral-thermal to acidic-mesothermal environments

Candidatus Parvarchaeales, representing a DPANN archaeal group with limited metabolic potentials and reliance on hosts for their growth, were initially found in acid mine drainage (AMD). Due to the lack of representatives, however, their ecological roles and adaptation to extreme habitats such as AMD, as well as how they diverge across the lineage remain largely unexplored. By applying genome-resolved metagenomics, 28 Parvarchaeales-associated metagenome-assembled genomes (MAGs) representing two orders and five genera were recovered. Among them, we identified three new genera and proposed the names Candidatus Jingweiarchaeum, Candidatus Haiyanarchaeum, and Candidatus Rehaiarchaeum with the former two belonging to a new order Candidatus Jingweiarchaeales. Further analyses of metabolic potentials revealed substantial niche differentiation between Jingweiarchaeales and Parvarchaeales. Jingweiarchaeales may rely on fermentation, salvage pathways, partial glycolysis, and pentose phosphate pathway (PPP) for energy reservation, while the metabolic potentials of Parvarchaeales might be more versatile. Comparative genomic analyses suggested that Jingweiarchaeales are more favorable to habitats with higher temperatures and Parvarchaeales are better adapted to acidic environments. We further revealed that the thermal adaptation of these lineages especially for Haiyanarchaeum might rely on innate genomic features such as the usage of specific amino acids, genome streamlining, and hyperthermal featured genes such as rgy. Notably, the acidic adaptation of Parvarchaeales was possibly driven by horizontal gene transfer (HGT). Reconstruction of ancestral states demonstrated that both may originate from thermal and neutral environments and later spread to mesothermal and acidic environments. These evolutionary processes may also be accompanied by adaptation toward oxygen-rich environments via HGT. ImportanceCandidatus Parvarchaeales may represent a lineage uniquely distributed in extreme environments such as AMD and hot springs. However, little is known about the strategies and processes of how they adapted to these extreme environments. By the discovery of potential new order-level lineages - Jingweiarchaeales and in-depth comparative genomic analysis, we unveiled the functional differentiation of these lineages. Further, we show that the adaptation to high-temperature and acidic environments of these lineages was driven by different strategies, with the prior relying more on innate genomic characteristics and the latter more on the acquisition of genes associated with acid tolerance. Finally, by reconstruction of ancestral states of OGT and pI, we showed the potential evolutionary process of Parvarchaeales-related lineages with regard to the shift from a high-temperature environment of their common ancestors to low-temperature (potentially acidic) environments.

microbiology↗