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1.
Microbial Diversity in the Indian Ocean Sediments: An Insight into the Distribution and Associated Factors.
Ambati, M, Kumar, MS
Current microbiology. 2022;(4):115
Abstract
Indian Ocean is the third largest oceanic division of the world and shelter to a huge microbial diversity. These microbes play an important role in the metabolism of carbon, sulfur, nitrogen, and phosphorus in the ocean water. They are also major contributors of carbon fixing and sequestration, as much as terrestrial plants to achieve CO2 emissions reduction. The prokaryotic community in the East Indian Ocean primarily comprises of heterotrophic bacteria like Alphaproteobacteria and Gammaproteobacteria, followed by Firmicutes and Actinobacteria. The Arabian Sea and the Bay of Bengal are typically characterized by presence of vast areas of oxygen minimum zones (OMZs) and have been witnessing a shift in the microbial diversity due to the changing conditions in the ocean water. Several canonical correspondence analyses reveal temperature, salinity, and phosphate levels as crucial environmental factors in propelling the distribution of diazotrophs. The viral consortia are dominated by the Caudovirales, an order of tailed bacteriophages. Due to the rapid change in the environmental factors such as topography, temperature, and sunlight contributing toward climate change, their role in sustaining the chemical composition of the ocean can be drastically affected especially with the evidence of several bacterial and fungal communities responding to latitudinal and temperature change. Therefore, we aim to critically review the status of microbial diversity in Indian Ocean to predict their response toward climate change as they are the sentinels of change in marine life and to understand the dynamics of microbial communities in the various locations of Indian Ocean.
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2.
Aequorivita iocasae sp. nov., a halophilic bacterium isolated from sediment collected at a cold seep field in the South China Sea.
Zhang, H, Wang, H, Cao, L, Chen, H, Zhong, Z, Wang, M, Lian, C, Liu, R, Zhou, L, Li, C
International journal of systematic and evolutionary microbiology. 2022;(2)
Abstract
A moderately halophilic bacterium, designated strain KX20305T, was isolated from sediment collected from a cold seep field in the South China Sea. Cells of strain KX20305T were Gram-stain-negative, rod-shaped, non-motile, facultatively anaerobic, oxidase- and catalase-positive, and grew optimally at 25-30 °C, pH 6.0-8.0 and with 3-6 % (w/v) NaCl. Phylogenetic analysis based on 16S rRNA gene sequences showed that strain KX20305T grouped with members of the genus Aequorivita, including Aequorivita aquimaris D-24T (98.3 % sequence similarity), Aequorivita vladivostokensis KMM 3516T (98.1 %) and Aequorivita echinoideorum CC-CZW007T (97.5 %). Genome sequencing of strain KX20305T revealed a genome size of 3.35 Mb and a DNA G+C content of 38.71 mol%. Genomic average nucleotide identity (orthoANI) values of strain KX20305T with A. aquimaris D-24T, A. vladivostokensis KMM 3516T and A. echinoideorum JCM 30378T were 83.8, 81.7 and 75.4 %, respectively, while in silico DNA-DNA hybridization (GGDC) values for strain KX20305T with these strains were 27.2, 25.0 and 19.6 %, respectively. The major fatty acids of strain KX20305T were iso-C15 : 0, iso-C17 : 0 3-OH and 10-methyl C16 : 0/iso-C17 : 1 ω9c. The predominant respiratory quinone was menaquinone-6 (MK-6). The polar lipids mainly comprised phosphatidylethanolamine, two unidentified aminolipids and two unidentified lipids. Based on comparative analysis of phylogenetic, phylogenomic, phenotypic and chemotaxonomic characteristics, strain KX20305T represents a novel species of the genus Aequorivita, for which the name Aequorivita iocasae sp. nov. is proposed. The type strain is KX20305T (=KCTC 82699T=MCCC 1K06238T=JCM 34635T).
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3.
Psychrosphaera ytuae sp. nov., isolated from the deep-sea cold seep sediment of South China Sea.
Xu, XD, Zhang, J, Sun, QL, Sun, YY, Tang, YZ
International journal of systematic and evolutionary microbiology. 2021;(8)
Abstract
In this study, we report a Gram-stain-negative, rod-shaped, non-pigmented, motile and aerobic bacterium named strain MTZ26T, which was isolated from deep-sea sediment sampled at a cold seep in the South China Sea. Growth of strain MTZ26T occurred at 4-40 °C (optimum, 25-30 °C), pH 6.0-10.0 (optimum, 7.0-8.0) and with 1.0-11.0 % (w/v) NaCl (optimum, 6.0-8.0 %). Phylogenetic analysis based on 16S rRNA gene sequences indicated that strain MTZ26T belonged to the genus Psychrosphaera and was closely related to Psychrosphaera aestuarii PSC101T (97.5 % sequence similarity) and Psychrosphaera haliotis KDW4T (97.5 %). Genomic analysis indicated that strain MTZ26T contains a circular chromosome of 3 331 814 bp with G+C content of 42.2 mol%. The predominant respiratory quinone of MTZ26T was ubiquinone-8. The polar lipids of MTZ26T contained phosphatidylglycerol, phosphatidylethanolamine, one unidentified aminophospholipid and one unidentified phospholipid. The major fatty acids of strain MTZ26T contained C15:0, C16:0, C17:0, C17 : 1 ω8c, C10 : 0 3-OH, C11 : 0 3-OH, C15 : 1 ω8c and summed feature 8 (C18 : 1 ω7c or/and C18 : 1 ω6c). Results of phylogenetic, physiological, biochemical and morphological analyses suggested that strain MTZ26T represents a novel species of the genus Psychrosphaera, and the name Psychrosphaera ytuae sp. nov. is proposed with the type strain MTZ26T (=MCCC 1K05568T=JCM 34321T).
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4.
Shewanella nanhaiensis sp. nov., a marine bacterium isolated from sediment of South China Sea, and emended descriptions of Shewanella woodyi, Shewanella hanedai and Shewanella canadensis.
Cao, WR, Li, X, Sun, YY, Jiang, MY, Xu, XD, Li, YJ
International journal of systematic and evolutionary microbiology. 2021;(12)
Abstract
A Gram-stain-negative, motile, facultative anaerobic and rod-shaped bacterium, designated strain NR704-98T, was isolated from marine sediment of the northern South China Sea. Cells were positive for oxidase and catalase activity. Growth was observed at 4-30 °C (optimum 20-25 °C), at pH 6-9 (pH 7) and with 0.5-7 % NaCl (2 %). The 16S rRNA gene-based phylogenetic analysis revealed that the nearest phylogenetic neighbours of strain NR704-98T were Shewanella woodyi MS32T (97.9 %), Shewanella hanedai 281T (97.1 %), Shewanella sediminis HAW-EB3T (96.8 %) and Shewanella canadensis HAW-EB2T (96.7 %). Based on the results of phylogenomic analysis, the average nucleotide identity and the digital DNA-DNA hybridization values between strain NR704-98T and the previously mentioned type strains of species of the genus Shewanella were in the range of 74.9-93.1 % and 20.6-51.4 %, respectively. The respiratory quinones were Q-7 and Q-8. The predominant fatty acids (>10 %) of strain NR704-98T were C16 : 0, summed feature 3 (C16 : 1 ω7c and/or C16 : 1 ω6c) and iso-C15 : 0. Phosphatidylethanolamine, phosphatidylglycerol, two unidentified aminophospholipids and five unidentified lipids were detected in strain NR704-98T. Based on the phylogenetic and phenotypic characteristics, strain NR704-98T is considered to represent a novel species of the genus Shewanella, for which the name Shewanella nanhaiensis sp. nov. is proposed. The type strain is NR704-98T (=KCTC 82799T=MCCC 1K06091T).
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5.
Phytoplankton settling quality has a subtle but significant effect on sediment microeukaryotic and bacterial communities.
Albert, S, Hedberg, P, Motwani, NH, Sjöling, S, Winder, M, Nascimento, FJA
Scientific reports. 2021;(1):24033
Abstract
In coastal aphotic sediments, organic matter (OM) input from phytoplankton is the primary food resource for benthic organisms. Current observations from temperate ecosystems like the Baltic Sea report a decline in spring bloom diatoms, while summer cyanobacteria blooms are becoming more frequent and intense. These climate-driven changes in phytoplankton communities may in turn have important consequences for benthic biodiversity and ecosystem functions, but such questions are not yet sufficiently explored experimentally. Here, in a 4-week experiment, we investigated the response of microeukaryotic and bacterial communities to different types of OM inputs comprising five ratios of two common phytoplankton species in the Baltic Sea, the diatom Skeletonema marinoi and filamentous cyanobacterium Nodularia spumigena. Metabarcoding analyses on 16S and 18S ribosomal RNA (rRNA) at the experiment termination revealed subtle but significant changes in diversity and community composition of microeukaryotes in response to settling OM quality. Sediment bacteria were less affected, although we observed a clear effect on denitrification gene expression (nirS and nosZ), which was positively correlated with increasing proportions of cyanobacteria. Altogether, these results suggest that future changes in OM input to the seafloor may have important effects on both the composition and function of microbenthic communities.
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6.
New Microbial Biodiversity in Marine Sediments.
Baker, BJ, Appler, KE, Gong, X
Annual review of marine science. 2021;:161-175
Abstract
Microbes in marine sediments represent a large portion of the biosphere, and resolving their ecology is crucial for understanding global ocean processes. Single-gene diversity surveys have revealed several uncultured lineages that are widespread in ocean sediments and whose ecological roles are unknown, and advancements in the computational analysis of increasingly large genomic data sets have made it possible to reconstruct individual genomes from complex microbial communities. Using these metagenomic approaches to characterize sediments is transforming our view of microbial communities on the ocean floor and the biodiversity of the planet. In recent years, marine sediments have been a prominent source of new lineages in the tree of life. The incorporation of these lineages into existing phylogenies has revealed that many belong to distinct phyla, including archaeal phyla that are advancing our understanding of the origins of cellular complexity and eukaryotes. Detailed comparisons of the metabolic potentials of these new lineages have made it clear that uncultured bacteria and archaea are capable of mediating key previously undescribed steps in carbon and nutrient cycling.
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7.
Description of Novosphingopyxis iocasae sp. nov., isolated from deep sea sediment from the Mariana Trench, and emended description of the genus Novosphingopyxis.
Zhou, HZ, Zhang, J, Sun, QL
International journal of systematic and evolutionary microbiology. 2021;(7)
Abstract
In this study, we reported a Gram-stain-negative, orange-coloured, rod-shaped, motile and faculatively anaerobic bacterium named strain PB63T, which was isolated from the deep-sea sediment from the Mariana Trench. Growth of PB63T occurred at 10-35 °C (optimum, 28 °C), pH 5.0-8.0 (optimum, 5.0-6.0) and with 0-7 % (w/v) NaCl (optimum, 2-3 %). The results of phylogenetic analysis based on 16S rRNA gene sequences indicated that PB63T represented a member of the genus Novosphingopyxis and was closely related to Novosphingopyxis baekryungensis DSM 16222T (97.9 % sequence similarity). PB63T showed tolerance to a variety of heavy metals, including Co2+, Zn2+, Mn2+ and Cu2+. The complete genome of PB63T was obtained, and many genes involved in heavy metal resistance were found. The genomic DNA G+C content of PB63T was 62.8 mol%. The predominant respiratory quinone of PB63T was ubiquinone-10 (Q-10). The polar lipids of PB63T contained diphosphatidylglycerol, phosphatidylglycerol, phosphatidylethanolamine, sphingoglycolipid, glycolipid, phosphatidylcholines and three unidentified lipids. The major fatty acids of PB63T included summed feature 8 (C18 : 1ω7c or/and C18 : 1ω6c), C14 : 0 2-OH, 11-methyl C18 : 1ω7c, C16 : 0, summed feature 3 (C16 : 1ω7c and/or C16 : 1ω6c) and C17 : 1ω6c. The results of phylogenetic, physiological, biochemical and morphological analyses indicated that strain PB63T represents a novel species of the genus Novosphingopyxis, and the name Novosphingopyxis iocasae sp. nov. is proposed with the type species PB63T (=CCTCC AB 2019195T=JCM 34178T).
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8.
The Complexity of Spills: The Fate of the Deepwater Horizon Oil.
Passow, U, Overton, EB
Annual review of marine science. 2021;:109-136
Abstract
The Deepwater Horizon oil spill was the largest, longest-lasting, and deepest oil accident to date in US waters. As oil and natural gas jetted from release points at 1,500-m depth in the northern Gulf of Mexico, entrainment of the surrounding ocean water into a buoyant plume, rich in soluble hydrocarbons and dispersed microdroplets of oil, created a deep (1,000-m) intrusion layer. Larger droplets of liquid oil rose to the surface, forming a slick of mostly insoluble, hydrocarbon-type compounds. A variety of physical, chemical, and biological mechanisms helped to transform, remove, and redisperse the oil and gas that was released. Biodegradation removed up to 60% of the oil in the intrusion layer but was less efficient in the surface slick, due to nutrient limitation. Photochemical processes altered up to 50% (by mass) of the floating oil. The surface oil expression changed daily due to wind and currents, whereas the intrusion layer flowed southwestward. A portion of the weathered surface oil stranded along shorelines. Oil from both surface and intrusion layers were deposited onto the seafloor via sinking marine oil snow. The biodegradation rates of stranded or sedimented oil were low, with resuspension and redistribution transiently increasing biodegradation. The subsequent research efforts increased our understanding of the fate of spilled oil immensely, with novel insights focusing on the importance of photooxidation, the microbial communities driving biodegradation, and the formation of marine oil snow that transports oil to the seafloor.
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9.
Seonamhaeicola maritimus sp. nov., isolated from coastal sediment.
Cao, WR, Lu, DC, Sun, XK, Sun, YY, Saren, G, Yu, XK, Du, ZJ
International journal of systematic and evolutionary microbiology. 2020;(2):902-908
Abstract
A Gram-stain-negative, facultatively anaerobic, non-motile, rod-shaped and orange-pigmented bacterium, designated 1505T, was isolated from marine sediment that was obtained off the coast of Weihai, PR China. Strain 1505T was found to grow at 10-35 °C (optimum, 28 °C), at pH 6.0-9.0 (optimum, 7.5) and in the presence of 1-4 % (w/v) NaCl (optimum, 2 %). Cells were positive for oxidase and catalase activity. The 16S rRNA gene based phylogenetic analysis revealed that the nearest phylogenetic neighbours of strain 1505T were Seonamhaeicola algicola Gy8T (97.1 %), Seonamhaeicola marinus B011T (96.3 %) and Seonamhaeicola aphaedonensis KCTC 32578T (95.6 %). Based on phylogenomic analysis, the average nucleotide identity values between strain 1505T and S. algicola Gy8T, S. marinus B011T and S. aphaedonensis KCTC 32578T were 75.9, 76.0 and 77.7 %, respectively; the digital DNA-DNA hybridization values based on the draft genomes between strain 1505T and S. algicola Gy8T, S. marinus B011T and S. aphaedonensis KCTC 32578T were 20.0, 20.7 and 21.4 %, respectively. Menaquinone-6 (MK-6) was detected as the major respiratory quinone. The dominant cellular fatty acids were iso-C15 : 1 G and C18 : 1ω9c. The DNA G+C content of strain 1505T was 33.3 mol%. The polar lipids included phosphatidylethanolamine, six aminolipids and four unidentified lipids. Based on its phylogenetic and phenotypic characteristics, strain 1505T is considered to represent a novel species of the genus Seonamhaeicola, for which the name Seonamhaeicola maritimus sp. nov. is proposed. The type strain is 1505T (=KCTC 72528T=MCCC 1H00389T).
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10.
Micromonospora fluminis sp. nov., isolated from mountain river sediment.
Camacho Pozo, MI, Wieme, AD, Rodríguez Pérez, S, Llauradó Maury, G, Peeters, C, Snauwaert, C, Lescaylle Veranes, Y, Peña Zamora, L, Schumann, P, Vandamme, PA
International journal of systematic and evolutionary microbiology. 2020;(12):6428-6436
Abstract
During a bioprospection of bacteria with antimicrobial activity, the actinomycete strain A38T was isolated from a sediment sample of the Carpintero river located in the Gran Piedra Mountains, Santiago de Cuba province (Cuba). This strain was identified as a member of the genus Micromonospora by means of a polyphasic taxonomy study. Strain A38T was an aerobic Gram-positive filamentous bacterium that produced single spores in a well-developed vegetative mycelium. An aerial mycelium was absent. The cell wall contained meso-diaminopimelic acid and the whole-cell sugars were glucose, mannose, ribose and xylose. The major cellular fatty acids were isoC15:0, 10 methyl C17:0, anteiso-C17:0 and iso-C17:0. The predominant menaquinones were MK-10(H4) and MK-10(H6). Phylogenetic analysis of 16S rRNA gene sequences revealed that this strain was closely related to Micromonospora tulbaghiae DSM 45142T (99.5 %), Micromonospora citrea DSM 43903T (99.4 %), Micromonospora marina DSM 45555T (99.4 %), Micromonospora maritima DSM 45782T (99.3 %), Micromonospora sediminicola DSM 45794T (99.3 %), Micromonospora aurantiaca DSM 43813T (99.2 %) and Micromonospora chaiyaphumensis DSM 45246T (99.2 %). The results of OrthoANIu analysis showed the highest similarity to Micromonospora chalcea DSM 43026T (96.4 %). However, the 16S rRNA and gyrB gene sequence-based phylogeny and phenotypic characteristics provided support to distinguish strain A38T as a novel species. On the basis of the results presented here, we propose to classify strain A38T (=LMG 30467T=CECT 30034T) as the type strain of the novel species Micromonospora fluminis sp. nov.