Abstract
Recent metagenomic advancements have offered unprecedented insights into soil viral ecology. However, it remains a challenge to select the suitable metagenomic method for investigating soil viruses under different environmental conditions. Here, we assessed the performance of viral size-fraction metagenomes (viromes) and total metagenomes in capturing viral diversity from hypersulfidic soils with neutral pH and sulfuric soils with pH <3.3. Viromes effectively enhanced the sequencing coverage of viral genomes in both soil types. Viomes of hypersulfidic soils outperformed total metagenomes by recovering a significantly higher number of viral operational taxonomic units (vOTUs). However, total metagenomes of sulfuric soils recovered ~4.5 times more vOTUs than viromes on average. Altogether, our findings suggest that the choice between viromes and total metagenomes for studying soil viruses should be carefully considered based on the specific environmental conditions.
Keywords: soil viruses, total metagenomes, viromes, viral diversity, acid sulfate soils
Main text
Viruses are highly abundant on Earth and contribute significantly to biogeochemical cycles. Total metagenomes, extracting all microbial DNA, have been used to study the soil virosphere [1, 2]. However, the vast diversity of soil microbiota and “relic” DNA poses obstacles to the reconstruction of viral genomes using total metagenomes [3, 4]. To address these limitations, researchers have turned to soil viral size-fraction metagenomes (viromes) for reducing cellular contamination and enhancing viral particle concentration [5]. Several studies demonstrated that viromes outperformed total metagenomes in uncovering rare virosphere in agriculture and peatland soils [6, 7]. However, viromes also have drawbacks, including low DNA yields, extraction of only free viral particles, and labour-intensive procedures [5]. The broader applicability of viromes remains relatively unexplored due to significant variations in soil biophysiochemical properties across different types [8]. Therefore, it becomes imperative to evaluate the effectiveness of viromes versus total metagenomes across diverse soil types for accurately understanding soil viral dynamics.
Here, we collected 36 samples from Adelaide, South Australia, including two types of acid sulfate soils (18 hypersulfidic soil samples with neutral pH from a current mangrove swamp on the Garden Island and 18 sulfuric soil samples with pH <3.3 from adjacent disturbed areas). Since 1935, the disturbed area has experienced reclamation for agriculture and industry, leading to the oxidation of sulfidic materials and generation of substantial acid and sulfuric soils [9, 10]. We constructed both virome and total metagenome libraries to retrieve the viral diversity, following established protocols [7, 11] (see Supplementary materials).
The virome and total metagenome sequencing yielded approximately 850 and 870 Gb of raw data, respectively. For viromes, 29 682 contigs (> 10 kb) were assembled from hypersulfidic soils and 650 from sulfuric soils (Fig. 1A). About 93.7% and 76.8% of contigs were identified as viral contigs in hypersulfidic and sulfuric soils, respectively (Fig. 1B). In contrast, for total metagenomes, 232 261 contigs were assembled (Fig. 1A), while the proportion of viral contigs was considerably lower, at 2.9% for hypersulfidic soils and 2.8% for sulfuric soils (Fig. 1B). Consistent with previous findings [6, 7], viromes showed a notable 20 to 30-fold increase in the recovery percentage of viral contigs compared to total metagenomes. All viral contigs were clustered into 16 359 viral operational taxonomic units (vOTUs) (Fig. 1C). On average, 30.7% and 45.0% of virome reads from hypersulfidic and sulfuric soils, respectively, were mapped to vOTUs, higher than that of total metagenomes (~1%–2%) (Figure 1D). These results highlight the effectiveness of viromes in enriching viral particles compared to total metagenomes.
Figure 1.
Comparisons of the performance of viromes and total metagenomes in recovering viral diversity from hypersulfidic and sulfuric soils. (A) The number of all contigs assembled and viral contigs identified from viromes and total metagenomes of hypersulfidic and sulfuric soils. (B) The average percentage of contigs belonging to viral genomes, determined by per virome and total metagenome from both soil types. (C) Venn diagram showing the shared and unique vOTUs among the two soil types with the two metagenomic methods. (D) The percentage of reads mapped to vOTUs, assessed by each virome and total metagenome from hypersulfidic and sulfuric soils. (E) The number of vOTUs recovered per virome and total metagenome based on the reads mapping to all vOTUs. (F) The size of viral clusters from viromes or total metagenomes in hypersulfidic and sulfuric soils. (G) Percentage of putative lysogenic viruses in total metagenomes of the two soil types. Different letters above the boxes show the significant difference determined by the Kruskal–Wallis nonparametric test.
Viromes of hypersulfidic soils revealed the highest number of vOTUs (14094), followed by total metagenomes of hypersulfidic soils (4151) and sulfuric soils (1360), and viromes of sulfuric soils (430) (Fig. 1C). The accumulation curves for vOTUs reached saturation (Fig. S1), suggesting that our sampling effort was adequate to capture the richness of vOTUs. In hypersulfidic soils, each virome yielded 5.1 times more vOTUs compared to total metagenomes. Conversely, in sulfuric soils, the viral richness per total metagenome exceeded viromes by 4.5 times (Fig. 1E). This aligns with observations from human gut viral metadata, where total metagenomes identified more viral contigs than viromes [12]. Furthermore, vOTUs were grouped into viral clusters (VCs) using vConTACT2 (Figs 1F and S2) [13]. The number of VCs clustered from the viromes of hypersulfidic was higher than that from total metagenomes, while sulfuric soils showed an opposite trend (Fig. 1F). These results suggest that viromes outperform total metagenomes in capturing higher viral diversity from hypersulfidic soils, whereas sulfuric soils, considered as extreme environments, showed an opposite pattern.
The better performance of total metagenomes over viromes in sulfuric soils may be mainly attributed to the prolonged extreme acidity of the environment, which may directly impact the persistence of most free viral particles [14, 15]. Additionally, previous studies showed that heavy metals can significantly elevate lysogenic virus abundance [16], and in some extreme environments, one or more viruses were present in nearly every cell [17]. In sulfuric soils, harsh conditions may induce the shift from lytic to lysogenic viral strategies for survival adaption. This is partially supported by the significantly higher proportion of lysogenic vOTUs in the total metagenome of sulfuric soils compared to hypersulfidic soils (Fig. 1G). Those factors collectively render viromes less effective in capturing prevalent viral signals within this environment (Table S1). Moreover, technical factors can also influence the performance of different metagenomes in capturing the diversity of soil viruses. For instance, the steps involved in virome DNA extraction and library preparation may lead to the reduction of viral diversity in sulfuric soils. Additionally, the lower biological complexity in extreme environments, such as sulfuric soils, may contribute to an enhanced efficiency of vOTU recovery from total metagenomes [5, 18].
Viromes have been widely recognized as a powerful tool for studying soil viral ecology. Our results support viromes as a promising approach for studying viruses in natural soil systems. However, in extreme environments such as sulfuric soils, total metagenomes can be the initial consideration due to their efficiency and lower labour requirements in capturing a comprehensive viral profile. Moreover, future studies should encompass a broad array of soil types to refine the application of metagenomic methods in characterizing the soil virosphere.
Supplementary Material
Acknowledgements
Great thanks to Dr. Rob Fitzpatrick in soil collection and soil classification, and Dr. Qinglin Chen and Mr Ziyang He in soil collection.
Contributor Information
Li Bi, School of Agriculture, Food and Ecosystem Sciences, Faculty of Science, The University of Melbourne, Parkville, Victoria 3010, Australia.
Ji-Zheng He, School of Agriculture, Food and Ecosystem Sciences, Faculty of Science, The University of Melbourne, Parkville, Victoria 3010, Australia.
Hang-Wei Hu, School of Agriculture, Food and Ecosystem Sciences, Faculty of Science, The University of Melbourne, Parkville, Victoria 3010, Australia.
Author contributions
LB, HWH, and JZH developed the original concept. LB and HWH performed experiments, analyzed data, and wrote the manuscript. All authors have contributed to revising the manuscript.
Conflicts of interest
The authors declare no competing interests.
Funding
This work was supported by Australian Research Council Discovery Project (DP210100332) and Future Fellowship (FT230100158).
Data availability
Raw sequencing data from this study were submitted to the NCBI under the project PRJNA1016489. All viral genomes can be accessed at FigShare (https://doi.org/10.6084/m9.figshare.25016585.v1).
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Associated Data
This section collects any data citations, data availability statements, or supplementary materials included in this article.
Supplementary Materials
Data Availability Statement
Raw sequencing data from this study were submitted to the NCBI under the project PRJNA1016489. All viral genomes can be accessed at FigShare (https://doi.org/10.6084/m9.figshare.25016585.v1).