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Wenchao Zhang

Publications and source records attributed to Wenchao Zhang.

2 recordsLinked to original sources

nf-core/pacsomatic: a scalable somatic analytic pipeline using PacBio HiFi data.

MOTIVATION: Pacific Biosciences (PacBio) HiFi long-read sequencing enables robust characterization of complex genomic regions, repetitive elements, and structural variants (SVs) that are often inaccessible to short-read technologies. To fully leverage HiFi reads to advance cancer genomics and epigenetics, researchers require an end-to-end, scalable and optimized bioinformatics workflow. The nf-core framework meets this need by providing rigorously tested, community-curated pipelines that ensure reproducibility, transparency, and broad compatibility across computational environments. RESULTS: We present nf-core/pacsomatic, an automated Nextflow DSL2 pipeline designed for comprehensive paired tumor-normal somatic analysis using PacBio HiFi data. The workflow includes steps for read alignments against reference genome, somatic SNV/indel, SV, and CNV calling, CpG methylation profiling and differential methylation region (DMR) detection. Additional downstream modules support functional annotation, mutational signature analysis, tumor purity and ploidy estimation, and homologous recombination deficiency (HRD) assessment. Utilizing nf-core's modular design and containerized execution, nf-core/pacsomatic provides a stable framework for the reproducible discovery of biological insights. AVAILABILITY: nf-core/pacsomatic is available under the MIT License at nf-core (https://nf-co.re/pacsomatic) and github (https://github.com/nf-core/pacsomatic).

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[Soil C, N and P contents and their relationships with soil physical properties in wetlands of Dongting Lake floodplain].

Eight representative soil profiles were installed on three types of wetland (two profiles on Carex spp. -dominated floodplain, four on Phragmites-dominated floodplain, and two on paddy soil) in Dongting Lake floodplain of China in 2004, and their C, N and P contents, microbial biomass C, N and P, <0.001 mm clay particles, and bulk density were measured. The results indicated the spatial distribution of soil C and N and soil microbial biomass C, N, and P were very similar in the profiles (0-100 cm) of three types of wetland, being decreased gradually with depth, except for soil TP which was constant in the profiles. The percentages of soil microbial biomass C, N and P to soil organic C, total nitrogen and total phosphorus decreased gradually with depth. In top layer (0-10 cm), the contents of soil organic C and microbial biomass C and the percentage of soil microbial biomass C to organic C were 19.63-50.20 g x kg(-1), 424.63 - 1 597.36 mg kg(-1), and 3.17% - 4.82%, respectively, the contents of soil total N and microbial biomass N and the percentage of soil microbial biomass N to total N were 1.85-4.45 g x kg(-1), 57.90 - 259.47 mg x kg(-1), and 3.13% - 6.42%, respectively, and the content of soil microbial biomass P and the percentage of soil microbial biomass P to soil total P was 24.16 - 200.99 mg x kg(-1) and 1.09% - 11.20%, respectively. The bulk density of soil top layer (0 -10 cm) was 0.65 - 1.04 g x cm(-3), and the content of < 0.001 mm clay particles was 26.24% - 39.48%. The contents of soil organic C and N and microbial biomass N and P in 0 - 10 cm layer were the highest in Carex spp.-dominated floodplain, followed by paddy soil, and Phragmites-dominated floodplain. Also in 0 - 10 cm layer, the soil microbial biomass C in Carex spp. dominated floodplain and paddy soil was higher than that in Phragmites-dominated floodplain, while the soil bulk density in Phragmites-dominated floodplain was higher than that in paddy soil, and much higher than that in Carex spp. -dominated floodplain. The amount of soil < 0.001 mm clay particles in Carex spp. -dominated floodplain and Phragmites-dominated floodplain was higher than that in paddy soil. In these three types of wetland, soil organic C and N and microbial biomass C, N and P had a significant logarithm correlation (P < 0.01) with <0.001 mm clay particles, and a significant index correlation (P <0.01) with bulk density.

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