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  • Elsevier  (3)
  • 2020-2024  (3)
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  • 1
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    phoH-carrying virus communities responded to multiple factors and their correlation network with prokaryotes in sediments along Bohai Sea, Yellow Sea, and East China Sea in China (2022)
    Elsevier
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    Publication Date: 2024-02-07
    Description: Viruses carrying phoH genes are an important functional group that may boost phosphate metabolism of their prokaryote hosts and affect phosphorus cycle in the ocean. However, at present, very little is known about the phoH-carrying viruses' community structure and diversity in marine sediments, as well as their correlation network with prokaryotes and environment. Here, via a large spatial scale investigation along the Bohai Sea, Yellow Sea, and East China Sea, for the first time, diverse unknown benthic phoH-carrying viruses were uncovered, which were mainly affiliated to three clusters. Interestingly, these viruses presented a very distinct community structure compared to those in seawaters. Correlation network analysis implied that these viruses might mainly infect the prokaryotes of Gamm-/Delta-proteobacteria, Thaumarchaeota, and Cyanobacteria in sediments. Distinct virus-prokaryote correlation network modules were shown in different sea areas. These modules' highly nested feature implied their coevolution with prokaryotes during long-term arms race. Their distribution in sediments was influenced by multiple factors including geographic separation and the key environmental variables of total organic carbon and total phosphorus, and responded to terrestrial inputs and coastal aquaculture activities. The results of this study provide novel insights into the benthic virus communities potentially participating in phosphorus cycling in the ocean.
    Type: Article , PeerReviewed
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  • 2
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    Bacterial reworking of particulate organic matter in a dynamic marginal sea: Implications for carbon sequestration (2023)
    Elsevier
    Details
    Publication Date: 2024-02-07
    Description: Concentrations of particulate organic carbon (POC) and total hydrolyzable amino sugars (THAS) were measured along a transect of the dynamic South Yellow Sea (SYS) to investigate the bioreactivity and bacterial reworking of particulate organic matter (POM). Results showed that POM bioavailability was linked with primary production, as revealed by the significant correlation between chlorophyll-a concentrations and the diagenetic indicator glucosamine/galactosamine (GlcN/GalN). Production of bioavailable POM could rapidly stimulate microbial activity, generating hot spots of heterotrophic alteration. Lower GlcN/GalN ratios (〈3) observed in the entire SYS indicate that POM underwent extensive microbial alteration. In particular, extremely low GlcN/GalN ratios (∼0.7) were found in the Yellow Sea Cold Water Mass, reflecting high bacterial alteration of POM. Estimates based on the bacterial biomarker muramic acid showed that on average ∼13% of POM in the SYS was of bacterial origin. Elevated bacterial contributions were found in both nearshore and offshore areas. Strong mixing in the nearshore and the presence of cyclonic eddies in offshore waters may increase the residence time of POM in the water column and thus promote bacterial transformation of POM. Overall, our findings indicate that bacterial reworking of POM varies with productivity and that the extensive bacterial transformation of the remaining POM observed in the water column probably enhances long-term carbon sequestration.
    Type: Article , PeerReviewed
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  • 3
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    Variations in isoprenoid tetraether lipids through the water column of the Western Pacific Ocean: Implications for sedimentary TEX86 records (2024)
    Elsevier
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    Publication Date: 2024-03-25
    Description: The TetraEther indeX of 86 carbon atoms (TEX86) is widely used as a proxy to reconstruct past sea surface temperatures. Most current applications of TEX86 are primarily based on analyzing the composition of isoprenoid glycerol dialkyl glycerol tetraethers (isoGDGTs) that comprise TEX86 in sediments, with the assumption that the sedimentary isoGDGTs are mainly derived from the surface mixed layer. Here we report on the variations in the isoGDGT distribution, archaeal abundance and community through the water column of the Western Pacific Ocean, directly testing the export depth of isoGDGTs and constraining the temperature records of TEX86. Our data show that maximum isoGDGT concentrations occurred in subsurface waters (150–200 m) with maximum archaeal abundances. The ratio between isoGDGTs bearing 2 vs. 3 cyclopentane moieties, i.e. [2/3] ratio, increased with depth, which is likely related to the shift of the archaeal community from Ca. Nitrosopelagicus-dominance to norank_f__Nitrosopumilaceae-dominance. Models based on the [2/3] ratios in the water column predicted an average export depth of isoGDGTs to sediments of around 150–200 m, consistent with the robust relationship between the compiled sedimentary TEX86 and the annual mean subsurface temperature. Taken together, our findings support that TEX86 records subsurface rather than surface temperatures in the open ocean.
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