ArticleFrontiers in microbiology2019
Distribution and Succession Feature of Antibiotic Resistance Genes Along a Soil Development Chronosequence in Urumqi No.1 Glacier of China.
Article in Frontiers in microbiology, 2019. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 7 papers.
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7 citing papers in PubMed, 24 citations in OpenAlex.
- Antimicrobial resistance as a signature of soil restoration across a 143-year chronosequence.ISME communications · 2026Article
- Antibiotic resistome in the glacier forelands of polar regions.Applied and environmental microbiology · 2025Article
- Prevalence and dynamics of antimicrobial resistance in pioneer and developing Arctic soils.BMC microbiology · 2025Article
- Protist predation promotes antimicrobial resistance spread through antagonistic microbiome interactions.The ISME journal · 2024Article
- The global distribution and environmental drivers of the soil antibiotic resistome.Microbiome · 2022Article
- Arctic PsychrotolerantAntibiotics (Basel, Switzerland) · 2022Article
- Impacts of organic materials amendment on the soil antibiotic resistome in subtropical paddy fields.Frontiers in microbiology · 2022Article
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Authors and funding
7 authors at 6 institutions in 2 countries.
Funding
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Abstract
Primary succession of plant and microbial communities in the glacier retreating foreland has been extensively studied, but shifts of antibiotic resistance genes (ARGs) with the glacier retreating due to global warming remain elusive. Unraveling the diversity and succession features of ARGs in pristine soil during glacier retreating could contribute to a mechanistic understanding of the evolution and development of soil resistome. In this study, we quantified the abundance and diversity of ARGs along a 50-year soil development chronosequence by using a high-throughput quantitative PCR (HT-qPCR) technique. A total of 24 ARGs and two mobile genetic elements (MGEs) were detected from all the glacier samples, and the numbers of detected ARGs showed a unimodal pattern with an increasing trend at the early stage (0∼8 years) but no significant change at later stages (17∼50 years). The
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