scholarly journals Zooplankton carcasses stimulate microbial turnover of allochthonous particulate organic matter

2021 ◽  
Author(s):  
Darshan Neubauer ◽  
Olesya Kolmakova ◽  
Jason Woodhouse ◽  
Robert Taube ◽  
Kai Mangelsdorf ◽  
...  
Keyword(s):  
Organic Matter ◽  
Microbial Community ◽  
Biochemical Properties ◽  
Taxonomic Composition ◽  
Interactive Effects ◽  
Complex Microbial Community ◽  
Eukaryotic Microorganisms ◽  
Microbial Turnover ◽  
Metabolic Activities ◽  
Global Carbon

AbstractCarbon turnover in aquatic environments is dependent on biochemical properties of organic matter (OM) and its degradability by the surrounding microbial community. Non-additive interactive effects represent a mechanism where the degradation of biochemically persistent OM is stimulated by the provision of bioavailable OM to the degrading microbial community. Whilst this is well established in terrestrial systems, whether it occurs in aquatic ecosystems remains subject to debate. We hypothesised that OM from zooplankton carcasses can stimulate the degradation of biochemically persistent leaf material, and that this effect is influenced by the daphnia:leaf OM ratio and the complexity of the degrading microbial community. Fresh Daphnia magna carcasses and 13C-labelled maize leaves (Zea mays) were incubated at different ratios (1:1, 1:3 and 1:5) alongside either a complex microbial community (<50 µm) or solely bacteria (<0.8 µm). 13C stable-isotope measurements of CO2 analyses were combined with phospholipid fatty acids (PLFA) analysis and DNA sequencing to link metabolic activities, biomass and taxonomic composition of the microbial community. Our experiments indicated a significantly higher respiration of leaf-derived C when daphnia-derived OM was most abundant (i.e. daphnia:leaf OM ratio of 1:1). This process was stronger in a complex microbial community, including eukaryotic microorganisms, than a solely bacterial community. We concluded that non-additive interactive effects were a function of increased C–N chemodiversity and microbial complexity, with the highest net respiration to be expected when chemodiversity is high and the degrading community complex. This study indicates that identifying the interactions and processes of OM degradation is one important key for a deeper understanding of aquatic and thus global carbon cycle.

scholarly journals Illuminating microbial metabolic activities in the dark deep ocean with metaproteomics

2018 ◽  
Author(s):  
Zhang-Xian Xie ◽  
Shu-Feng Zhang ◽  
Hao Zhang ◽  
Ling-Fen Kong ◽  
Lin Lin ◽  
...  
Keyword(s):  
Organic Matter ◽  
Microbial Community ◽  
Dissolved Organic Matter ◽  
Metabolic Activity ◽  
Deep Ocean ◽  
Viral Proteins ◽  
Life Forms ◽  
Cytoplasmic Proteins ◽  
Proteomic Study ◽  
Metabolic Activities

AbstractThe deep ocean is the largest habitat on earth and holds diverse microbial life forms. Significant advances have been made in microbial diversity and their genomic potential in the deep ocean, however, little is known about microbial metabolic activity that is crucial to regulate the bathypelagic carbon sequestration. Here, we characterized proteomes covering large particulate (>0.7 μm), small particulate (0.2-0.7 μm) and dissolved (10 kDa-0.2 μm) fractions collected at a depth of 3000 m in the South China Sea. The Rhodospirillales, SAR324, SAR11, Nitrosinae/Tectomicrobia were the major contributors in the particulate fraction whereas Alteromonadales and viruses dominated the dissolved counterpart. Frequent detection of transcription or translation proteins in the particulate fractions indicated active metabolism of SAR324, Archaea, SAR11, and possible viable surface microbes, e.g. Prochlorococcus. Transporters for diverse substrates were the most abundant functional groups, and numerous spectra of formate dehydrogenases and glycine betaine transporters unveiled the importance of methylated compounds for the survival of deep-sea microbes. Notably, abundant non-viral proteins, especially transporters and cytoplasmic proteins, were detected in the dissolved fraction, indicating their potential roles in nutrient scavenging and the stress response. Our size-based proteomic study implied the holistic microbial activity mostly acting on the labile dissolved organic matter as well as the potential activities of surface microbes and dissolved non-viral proteins in the deep ocean.ImportanceThe deep ocean produces one third of the biological CO2 in the ocean. However, little is known about metabolic activity of the bathypelagic microbial community which is crucial for understanding the biogeochemical cycling of organic matter, especially the formation of bulk refractory dissolved organic matter (DOM), one of the largest reservoirs of reduced carbon on Earth. This study provided the protein evidence firstly including both particulate and dissolved fractions to comprehensively decipher the active microbes and metabolic processes involved in the DOM recycling in the deep ocean. Our data supported the hypothesis of the carbon and energy supply from the labile DOM after the solution of sinking particles to the bathypelagic microbial community.

scholarly journals Unified concepts for understanding and modelling turnover of dissolved organic matter from freshwaters to the ocean: the UniDOM model

2019 ◽  
Vol 146 (2) ◽  
pp. 105-123 ◽  
Author(s):  
T. R. Anderson ◽  
E. C. Rowe ◽  
L. Polimene ◽  
E. Tipping ◽  
C. D. Evans ◽  
...  
Keyword(s):  
Organic Matter ◽  
Dissolved Organic Matter ◽  
Inverse Function ◽  
State Variables ◽  
Ongoing Research ◽  
Global Carbon Budget ◽  
Microbial Turnover ◽  
Age Model ◽  
Microbial Consumption ◽  
Global Carbon

AbstractThe transport of dissolved organic matter (DOM) across the land-ocean-aquatic-continuum (LOAC), from freshwater to the ocean, is an important yet poorly understood component of the global carbon budget. Exploring and quantifying this flux is a significant challenge given the complexities of DOM cycling across these contrasting environments. We developed a new model, UniDOM, that unifies concepts, state variables and parameterisations of DOM turnover across the LOAC. Terrigenous DOM is divided into two pools, T1 (strongly-UV-absorbing) and T2 (non- or weakly-UV-absorbing), that exhibit contrasting responses to microbial consumption, photooxidation and flocculation. Data are presented to show that these pools are amenable to routine measurement based on specific UV absorbance (SUVA). In addition, an autochtonous DOM pool is defined to account for aquatic DOM production. A novel aspect of UniDOM is that rates of photooxidation and microbial turnover are parameterised as an inverse function of DOM age. Model results, which indicate that ~ 5% of the DOM originating in streams may penetrate into the open ocean, are sensitive to this parameterisation, as well as rates assigned to turnover of freshly-produced DOM. The predicted contribution of flocculation to DOM turnover is remarkably low, although a mechanistic representation of this process in UniDOM was considered unachievable because of the complexities involved. Our work highlights the need for ongoing research into the mechanistic understanding and rates of photooxidation, microbial consumption and flocculation of DOM across the different environments of the LOAC, along with the development of models based on unified concepts and parameterisations.

The distribution of active β-glucosidase-producing microbial communities in composting

2017 ◽  
Vol 63 (12) ◽  
pp. 998-1008 ◽  
Author(s):  
Xiangyun Zang ◽  
Meiting Liu ◽  
Han Wang ◽  
Yihong Fan ◽  
Haichang Zhang ◽  
...  
Keyword(s):  
Microbial Community ◽  
Microbial Communities ◽  
Cellulose Degradation ◽  
Cellulose Hydrolysis ◽  
Bacterial Phyla ◽  
Metabolic Activities ◽  
Bacteria And Fungi ◽  
A Minor ◽  
Dominant Bacteria ◽  
Global Carbon

The composting ecosystem is a suitable source for the discovery of novel microorganisms and secondary metabolites. Cellulose degradation is an important part of the global carbon cycle, and β-glucosidases complete the final step of cellulose hydrolysis by converting cellobiose to glucose. This work analyzes the succession of β-glucosidase-producing microbial communities that persist throughout cattle manure – rice straw composting, and evaluates their metabolic activities and community advantage during the various phases of composting. Fungal and bacterial β-glucosidase genes belonging to glycoside hydrolase families 1 and 3 (GH1 and GH3) amplified from DNA were classified and gene abundance levels were analyzed. The major reservoirs of β-glucosidase genes were the fungal phylum Ascomycota and the bacterial phyla Firmicutes, Actinobacteria, Proteobacteria, and Deinococcus–Thermus. This indicates that a diverse microbial community utilizes cellobiose. The succession of dominant bacteria was also detected during composting. Firmicutes was the dominant bacteria in the thermophilic phase of composting; there was a shift to Actinomycetes in the maturing stage. Proteobacteria accounted for the highest proportions during the heating and thermophilic phases of composting. By contrast, the fungal phylum Ascomycota was a minor microbial community constituent in thermophilic phase of composting. Combined with the analysis of the temperature, cellulose degradation rate and the carboxymethyl cellulase and β-glucosidase activities showed that the bacterial GH1 family β-glucosidase genes make greater contribution in cellulose degradation at the later thermophilic stage of composting. In summary, even GH1 bacteria families β-glucosidase genes showing low abundance in DNA may be functionally important in the later thermophilic phase of composting. The results indicate that a complex community of bacteria and fungi expresses β-glucosidases in compost. Several β-glucosidase-producing bacteria and fungi identified in this study may represent potential indicators of composting in cellulose degradation.

scholarly journals DOM degradation by light and microbes along the Yukon River-coastal ocean continuum

2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Brice K. Grunert ◽  
Maria Tzortziou ◽  
Patrick Neale ◽  
Alana Menendez ◽  
Peter Hernes
Keyword(s):  
Organic Matter ◽  
Dissolved Organic Matter ◽  
Salinity Gradient ◽  
Coastal Ocean ◽  
Interactive Effects ◽  
The Arctic ◽  
Yukon River ◽  
Spring Freshet ◽  
Dom Composition

AbstractThe Arctic is experiencing rapid warming, resulting in fundamental shifts in hydrologic connectivity and carbon cycling. Dissolved organic matter (DOM) is a significant component of the Arctic and global carbon cycle, and significant perturbations to DOM cycling are expected with Arctic warming. The impact of photochemical and microbial degradation, and their interactive effects, on DOM composition and remineralization have been documented in Arctic soils and rivers. However, the role of microbes, sunlight and their interactions on Arctic DOM alteration and remineralization in the coastal ocean has not been considered, particularly during the spring freshet when DOM loads are high, photoexposure can be quite limited and residence time within river networks is low. Here, we collected DOM samples along a salinity gradient in the Yukon River delta, plume and coastal ocean during peak river discharge immediately after spring freshet and explored the role of UV exposure, microbial transformations and interactive effects on DOM quantity and composition. Our results show: (1) photochemical alteration of DOM significantly shifts processing pathways of terrestrial DOM, including increasing relative humification of DOM by microbes by > 10%; (2) microbes produce humic-like material that is not optically distinguishable from terrestrial humics; and (3) size-fractionation of the microbial community indicates a size-dependent role for DOM remineralization and humification of DOM observed through modeled PARAFAC components of fluorescent DOM, either through direct or community effects. Field observations indicate apparent conservative mixing along the salinity gradient; however, changing photochemical and microbial alteration of DOM with increasing salinity indicate changing DOM composition likely due to microbial activity. Finally, our findings show potential for rapid transformation of DOM in the coastal ocean from photochemical and microbial alteration, with microbes responsible for the majority of dissolved organic matter remineralization.

scholarly journals Microbial Community Structure Affects Marine Dissolved Organic Matter Composition

2016 ◽  
Vol 3 ◽  
Author(s):  
Elizabeth B. Kujawinski ◽  
Krista Longnecker ◽  
Katie L. Barott ◽  
Ralf J. M. Weber ◽  
Melissa C. Kido Soule
Keyword(s):  
Organic Matter ◽  
Community Structure ◽  
Microbial Community ◽  
Dissolved Organic Matter ◽  
Microbial Community Structure ◽  
Organic Matter Composition

scholarly journals Exploring the taxonomical and functional profile of As Burgas hot spring focusing on thermostable β-galactosidases

2021 ◽  
Vol 11 (1) ◽  
Author(s):  
María-Eugenia DeCastro ◽  
Michael P. Doane ◽  
Elizabeth Ann Dinsdale ◽  
Esther Rodríguez-Belmonte ◽  
María-Isabel González-Siso
Keyword(s):  
Microbial Community ◽  
Hot Spring ◽  
Functional Characterization ◽  
Tca Cycle ◽  
Maximal Activity ◽  
Sulfur Cycle ◽  
E Coli ◽  
Complex Microbial Community ◽  
Relationship Of ◽  
The Relationship

AbstractIn the present study we investigate the microbial community inhabiting As Burgas geothermal spring, located in Ourense (Galicia, Spain). The approximately 23 Gbp of Illumina sequences generated for each replicate revealed a complex microbial community dominated by Bacteria in which Proteobacteria and Aquificae were the two prevalent phyla. An association between the two most prevalent genera, Thermus and Hydrogenobacter, was suggested by the relationship of their metabolism. The high relative abundance of sequences involved in the Calvin–Benson cycle and the reductive TCA cycle unveils the dominance of an autotrophic population. Important pathways from the nitrogen and sulfur cycle are potentially taking place in As Burgas hot spring. In the assembled reads, two complete ORFs matching GH2 beta-galactosidases were found. To assess their functional characterization, the two ORFs were cloned and overexpressed in E. coli. The pTsbg enzyme had activity towards o-Nitrophenyl-β-d-galactopyranoside (ONPG) and p-Nitrophenyl-β-d-fucopyranoside, with high thermal stability and showing maximal activity at 85 °C and pH 6, nevertheless the enzyme failed to hydrolyze lactose. The other enzyme, Tsbg, was unable to hydrolyze even ONPG or lactose. This finding highlights the challenge of finding novel active enzymes based only on their sequence.

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