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Journal Article
- Genetic Characteristics and Phylogeographic Dynamics of Echovirus
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Yan Wang , Pir Tariq Shah , Yue Liu , Amina Nawal Bahoussi , Li Xing
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J. Microbiol. 2023;61(9):865-877. Published online September 15, 2023
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DOI: https://doi.org/10.1007/s12275-023-00078-w
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Abstract
- Echoviruses belong to the genus Enterovirus in the Picornaviridae family, forming a large group of Enterovirus B (EVB)
within the Enteroviruses. Previously, Echoviruses were classified based on the coding sequence of VP1. In this study,
we performed a reliable phylogenetic classification of 277 sequences isolated from 1992 to 2019 based on the full-length
genomes of Echovirus. In this report, phylogenetic, phylogeographic, recombination, and amino acid variability landscape
analyses were performed to reveal the evolutional characteristics of Echovirus worldwide. Echoviruses were clustered into
nine major clades, e.g., G1–G9. Phylogeographic analysis showed that branches G2–G9 were linked to common strains,
while the branch G1 was only linked to G5. In contrast, strains E12, E14, and E16 clustered separately from their G3 and
G7 clades respectively, and became a separate branch. In addition, we identified a total of 93 recombination events, where
most of the events occurred within the VP1-VP4 coding regions. Analysis of amino acid variation showed high variability in
the a positions of VP2, VP1, and VP3. This study updates the phylogenetic and phylogeographic information of Echovirus
and indicates that extensive recombination and significant amino acid variation in the capsid proteins drove the emergence
of new strains.
Observational Study
- Early gut microbiota in very low and extremely low birth weight preterm infants with feeding intolerance: a prospective case-control study
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Ling Liu , Dang Ao , Xiangsheng Cai , Peiyi Huang , Nali Cai , Shaozhu Lin , Benqing Wu
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J. Microbiol. 2022;60(10):1021-1031. Published online August 19, 2022
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DOI: https://doi.org/10.1007/s12275-022-2180-2
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Citations
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Abstract
- The potential role of the gut microbiota in the pathogenesis
of feeding intolerance (FI) remains unclear. Understanding
the role of the gut microbiota could provide a new avenue for
microbiota-targeted therapeutics. This study aimed to explore
the associations between aberrant gut microbiota and FI in
very low or extremely low birth weight (VLBW/ELBW) preterm
infants. In this observational case-control study, VLBW/
ELBW infants were divided into two groups: FI group and
feeding tolerance (FT) group. 16S rRNA gene sequencing was
performed to analyze the gut microbial diversity and composition
of the infants. The differences in the gut microbiota of
the two groups were compared. In total, 165 stool samples
were obtained from 44 infants, among which, 31 developed
FI and 13 served as controls. Alpha diversity was the highest
in the meconium samples of the two groups. LEfSe analysis
revealed that the abundances of Peptostreptococcaceae, Clostridiales
and Clostridia in the FT group were significantly higher
than in the FI group. At the phylum level, the FI group was dominated
by Proteobacteria, and the FT group was dominated
by Firmicutes. The meconium samples of the FI group had
higher proportions of γ-proteobacteria and Escherichia-Shigella
and a lower proportion of Bacteroides compared with the FT
group. Kyoto Encyclopedia of Genes and Genomes (KEGG)
analysis demonstrated that aberrant gut bacteria in the FI group
were strongly associated with dysregulation of C5-Brancheddibasic-
acid-metabolism, protein kinases, and sporulation.
These findings reveal candidate microbial markers to prevent
FI. Increased relative abundances of γ-proteobacteria
and Escherichia-Shigella and decreased abundance of Bacteroides
in meconium were associated with an increased risk
of FI, while Peptostreptococcaceae, Clostridiales and Clostridia
reduced the risk of FI in VLBW/ELBW infants.
Journal Articles
- Assessing the microcystins concentration through optimized protein phosphatase inhibition assay in environmental samples
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Kyoung-Hee Oh , Kung-Min Beak , Yuna Shin , Young-Cheol Cho
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J. Microbiol. 2022;60(6):602-609. Published online April 30, 2022
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DOI: https://doi.org/10.1007/s12275-022-2020-4
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Abstract
- Protein phosphatase (PPase) inhibition assay (PPIA) is widely
used to analyze the concentration of microcystins (MCs) because
it is comparatively less expensive and faster than other
assays. This study aimed to optimize the PPIA by determining
a suitable reaction terminator and an optimal methanol
concentration in the sample. The most suitable reaction time
was 90 min, with the corresponding methanol concentration
in the sample being 15% or less. When p-nitrophenyl phosphate
(pNPP) was used as a substrate, copper chloride solution
was suitably used as a reaction terminator, and when 4-
methylumbelliferyl phosphate (MUP) was used, a glycine buffer
not only increased the measurement sensitivity of the reaction
product but also terminated the enzymatic reaction.
When PPase 1 and MUP were used as an enzyme and a substrate,
respectively, the limit of quantitation for MC-leucine/
arginine (LR) was 0.02 μg/L, whereas it was 0.1 μg/L when
pNPP was used as a substrate. The proposed method facilitated
the measurement of MC-LR concentration without
additional pretreatments, such as concentration or purification;
therefore, this method was suitable and feasible for the
continuous monitoring of MCs in drinking water.
- The relationship between bacterial diversity and organic carbon mineralization in soft rock and sand compound soil
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Zhen Guo , Juan Li , Lei Ge , Chenxi Yang , Jichang Han
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J. Microbiol. 2020;58(9):750-760. Published online July 24, 2020
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DOI: https://doi.org/10.1007/s12275-020-0130-4
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Abstract
- The soil organic carbon (SOC) mineralization rate in sandy
soil plays an important role in improving soil quality, and a
research is needed to determine management practices that
optimize the mineralization rate. When sandy soil is improved
by adding soft rock, the specific promotion process of bacterium
to SOC mineralization remain unclear. To investigate
these mechanisms, we selected four treatments with soft
rock to sand volume ratios of 0:1 (CK), 1:5 (C1), 1:2 (C2)
and 1:1 (C3) to study. The mineralization rate of organic carbon
was measured using the lye absorption method. Highthroughput
sequencing and scanning electron microscopy
were used to determine the bacterial community structure
and soil microstructure, respectively. The results showed that
the organic carbon content of the sandy soil increased significantly
(182.22–276.43%) after using the soft rock treatments.
The SOC mineralization rate could be divided into two
stages: a rapid decline during days 1–8 and a slow decline
during days 8–60. With increased incubation time, the intensity
of the cumulative release of organic carbon gradually
weakened. Compared with the CK treatment, the SOC mineralization
accumulation (Ct) and the potential mineralizable
organic carbon content (C0) in the C1, C2, and C3 treatments
increased significantly, by 106.98–225.94% and 112.22–
254.08%, respectively. The cumulative mineralization rate (Cr)
was 18.11% and 21.38% smaller with treatments C2 and C3,
respectively. The SOC mineralization rate constant (k) decreased
significantly after the addition of soft rock, while the
half-turnover period (Th) changed inversely with k. Compared
with the CK treatment, the number of gene copies of
the soil bacteria increased by 15.38–272.53% after adding soft
rock, with the most significant increase in treatment C3. The
bacterial diversity index also increased significantly under
treatment C3. The three dominant bacteria were Proteobacteria,
Actinobacteria, and Chloroflexi. The correlation between
Cr and one of the non-dominant bacteria, Firmicutes,
was large, and the bacteria had a significant positive correlation
with k. At the same time, the abundance of Firmicutes
under treatments C2 and C3 was small. As the proportion
of soft rock increased, the soil particles changed from point
contact to surface contact, and the adhesion on the surface
of the particles gradually increased. Results from this study
show that the retention time of SOC can be increased and
the carbon sequestration effect is better when the ratio of
soft rock to sand is set to 1:2.
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