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Yin X, Zhou G, Wang H, Han D, Maeke M, Richter-Heitmann T, Wunder LC, Aromokeye DA, Zhu QZ, Nimzyk R, Elvert M, Friedrich MW. Unexpected carbon utilization activity of sulfate-reducing microorganisms in temperate and permanently cold marine sediments. THE ISME JOURNAL 2024; 18:wrad014. [PMID: 38365251 PMCID: PMC10811731 DOI: 10.1093/ismejo/wrad014] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/10/2023] [Revised: 11/21/2023] [Accepted: 11/29/2023] [Indexed: 02/18/2024]
Abstract
Significant amounts of organic carbon in marine sediments are degraded, coupled with sulfate reduction. However, the actual carbon and energy sources used in situ have not been assigned to each group of diverse sulfate-reducing microorganisms (SRM) owing to the microbial and environmental complexity in sediments. Here, we probed microbial activity in temperate and permanently cold marine sediments by using potential SRM substrates, organic fermentation products at very low concentrations (15-30 μM), with RNA-based stable isotope probing. Unexpectedly, SRM were involved only to a minor degree in organic fermentation product mineralization, whereas metal-reducing microbes were dominant. Contrastingly, distinct SRM strongly assimilated 13C-DIC (dissolved inorganic carbon) with H2 as the electron donor. Our study suggests that canonical SRM prefer autotrophic lifestyle, with hydrogen as the electron donor, while metal-reducing microorganisms are involved in heterotrophic organic matter turnover, and thus regulate carbon fluxes in an unexpected way in marine sediments.
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Affiliation(s)
- Xiuran Yin
- State Key Laboratory of Marine Resource Utilization in South China Sea, Hainan University, 58 Renmin Avenue, Haikou 570228, China
- Faculty of Biology/Chemistry, University of Bremen, Leobener Strasse 3, Bremen D-28359, Germany
- MARUM, Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, Bremen D-28359, Germany
- Max Planck Institute for Marine Microbiology, Celsiusstrasse 1, Bremen D-28359, Germany
| | - Guowei Zhou
- State Key Laboratory of Marine Resource Utilization in South China Sea, Hainan University, 58 Renmin Avenue, Haikou 570228, China
- School of Resources and Environmental Engineering, Anhui University, 111 Jiulong Road, Hefei, Anhui 230601, China
| | - Haihua Wang
- State Key Laboratory of Marine Resource Utilization in South China Sea, Hainan University, 58 Renmin Avenue, Haikou 570228, China
- Faculty of Biology/Chemistry, University of Bremen, Leobener Strasse 3, Bremen D-28359, Germany
- College of Urban and Environmental Sciences, Peking University, No. 5 Yiheyuan Road, Beijing 100871, China
| | - Dukki Han
- Department of Marine Bioscience, Gangneung-Wonju National University, 7 Jukheon-gil, Gangneung-si 25457, Republic of Korea
| | - Mara Maeke
- Faculty of Biology/Chemistry, University of Bremen, Leobener Strasse 3, Bremen D-28359, Germany
- Max Planck Institute for Marine Microbiology, Celsiusstrasse 1, Bremen D-28359, Germany
| | - Tim Richter-Heitmann
- Faculty of Biology/Chemistry, University of Bremen, Leobener Strasse 3, Bremen D-28359, Germany
| | - Lea C Wunder
- Faculty of Biology/Chemistry, University of Bremen, Leobener Strasse 3, Bremen D-28359, Germany
- Max Planck Institute for Marine Microbiology, Celsiusstrasse 1, Bremen D-28359, Germany
| | - David A Aromokeye
- Faculty of Biology/Chemistry, University of Bremen, Leobener Strasse 3, Bremen D-28359, Germany
| | - Qing-Zeng Zhu
- MARUM, Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, Bremen D-28359, Germany
| | - Rolf Nimzyk
- Faculty of Biology/Chemistry, University of Bremen, Leobener Strasse 3, Bremen D-28359, Germany
| | - Marcus Elvert
- MARUM, Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, Bremen D-28359, Germany
- Faculty of Geosciences, University of Bremen, Klagenfurter Strasse 2-4, Bremen D-28359, Germany
| | - Michael W Friedrich
- Faculty of Biology/Chemistry, University of Bremen, Leobener Strasse 3, Bremen D-28359, Germany
- MARUM, Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse 8, Bremen D-28359, Germany
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2
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Ramasamy KP, Brugel S, Eriksson K, Andersson A. Pseudomonas ability to utilize different carbon substrates and adaptation influenced by protozoan grazing. ENVIRONMENTAL RESEARCH 2023:116419. [PMID: 37321339 DOI: 10.1016/j.envres.2023.116419] [Citation(s) in RCA: 3] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/27/2023] [Revised: 06/09/2023] [Accepted: 06/12/2023] [Indexed: 06/17/2023]
Abstract
Bacteria are major utilizers of dissolved organic matter in aquatic systems. In coastal areas bacteria are supplied with a mixture of food sources, spanning from refractive terrestrial dissolved organic matter to labile marine autochthonous organic matter. Modelling scenarios indicate that in northern coastal areas, the inflow of terrestrial organic matter will increase, and autochthonous production will decrease, thus bacteria will experience a change in the food source composition. How bacteria will cope with such changes is not known. Here, we tested the ability of an isolated bacterium from the northern Baltic Sea coast, Pseudomonas sp., to adapt to varying substrates. We performed a 7-months chemostat experiment, where three different substrates were provided: glucose, representing labile autochthonous organic carbon, sodium benzoate representing refractive organic matter, and acetate - a labile but low energy food source. Growth rate has been pointed out as a key factor for fast adaptation, and since protozoan grazers speed-up the growth rate we added a ciliate to half of the incubations. The results show that the isolated Pseudomonas is adapted to utilize both labile and ring-structured refractive substrates. The growth rate was the highest on the benzoate substrate, and the production increased over time indicating that adaptation did occur. Further, our findings indicate that predation can cause Pseudomonas to change their phenotype to resist and promote survival in various carbon substrates. Genome sequencing reveals different mutations in the genome of adapted populations compared to the native populations, suggesting the adaptation of Pseudomonas sp. To changing environment.
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Affiliation(s)
- Kesava Priyan Ramasamy
- Department of Ecology and Environmental Science, Umeå University, Sweden; Umeå Marine Sciences Centre, Umeå University, Hörnefors, Sweden.
| | - Sonia Brugel
- Department of Ecology and Environmental Science, Umeå University, Sweden; Umeå Marine Sciences Centre, Umeå University, Hörnefors, Sweden
| | - Karolina Eriksson
- Department of Ecology and Environmental Science, Umeå University, Sweden; Umeå Marine Sciences Centre, Umeå University, Hörnefors, Sweden
| | - Agneta Andersson
- Department of Ecology and Environmental Science, Umeå University, Sweden; Umeå Marine Sciences Centre, Umeå University, Hörnefors, Sweden
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3
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Watanabe T, Kubo K, Kamei Y, Kojima H, Fukui M. Dissimilatory microbial sulfur and methane metabolism in the water column of a shallow meromictic lake. Syst Appl Microbiol 2022; 45:126320. [DOI: 10.1016/j.syapm.2022.126320] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 12/09/2021] [Revised: 03/10/2022] [Accepted: 03/21/2022] [Indexed: 01/04/2023]
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4
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Johnson MD, Scott JJ, Leray M, Lucey N, Bravo LMR, Wied WL, Altieri AH. Rapid ecosystem-scale consequences of acute deoxygenation on a Caribbean coral reef. Nat Commun 2021; 12:4522. [PMID: 34312399 PMCID: PMC8313580 DOI: 10.1038/s41467-021-24777-3] [Citation(s) in RCA: 21] [Impact Index Per Article: 7.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/02/2021] [Accepted: 06/30/2021] [Indexed: 02/07/2023] Open
Abstract
Loss of oxygen in the global ocean is accelerating due to climate change and eutrophication, but how acute deoxygenation events affect tropical marine ecosystems remains poorly understood. Here we integrate analyses of coral reef benthic communities with microbial community sequencing to show how a deoxygenation event rapidly altered benthic community composition and microbial assemblages in a shallow tropical reef ecosystem. Conditions associated with the event precipitated coral bleaching and mass mortality, causing a 50% loss of live coral and a shift in the benthic community that persisted a year later. Conversely, the unique taxonomic and functional profile of hypoxia-associated microbes rapidly reverted to a normoxic assemblage one month after the event. The decoupling of ecological trajectories among these major functional groups following an acute event emphasizes the need to incorporate deoxygenation as an emerging stressor into coral reef research and management plans to combat escalating threats to reef persistence.
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Affiliation(s)
- Maggie D Johnson
- Smithsonian Tropical Research Institute, Balboa, Ancon, Republic of Panama.
- Tennenbaum Marine Observatories Network, MarineGEO, Smithsonian Institution, Edgewater, MD, USA.
- Biology Department, Woods Hole Oceanographic Institution, Woods Hole, MA, USA.
| | - Jarrod J Scott
- Smithsonian Tropical Research Institute, Balboa, Ancon, Republic of Panama
| | - Matthieu Leray
- Smithsonian Tropical Research Institute, Balboa, Ancon, Republic of Panama
| | - Noelle Lucey
- Smithsonian Tropical Research Institute, Balboa, Ancon, Republic of Panama
| | - Lucia M Rodriguez Bravo
- Smithsonian Tropical Research Institute, Balboa, Ancon, Republic of Panama
- Facultad de Ciencias Marinas, Universidad Autónoma de Baja California, Ensenada, Mexico
| | - William L Wied
- Smithsonian Tropical Research Institute, Balboa, Ancon, Republic of Panama
- Department of Biological Sciences, Center for Coastal Oceans Research, Florida International University, Miami, FL, USA
| | - Andrew H Altieri
- Smithsonian Tropical Research Institute, Balboa, Ancon, Republic of Panama
- Department of Environmental Engineering Sciences, University of Florida, Gainesville, FL, USA
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5
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Suominen S, van Vliet DM, Sánchez-Andrea I, van der Meer MTJ, Sinninghe Damsté JS, Villanueva L. Organic Matter Type Defines the Composition of Active Microbial Communities Originating From Anoxic Baltic Sea Sediments. Front Microbiol 2021; 12:628301. [PMID: 34025597 PMCID: PMC8131844 DOI: 10.3389/fmicb.2021.628301] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/11/2020] [Accepted: 04/06/2021] [Indexed: 11/13/2022] Open
Abstract
Carbon cycling in anoxic marine sediments is dependent on uncultured microbial communities. Niches of heterotrophic microorganisms are defined by organic matter (OM) type and the different phases in OM degradation. We investigated how OM type defines microbial communities originating from organic-rich, anoxic sediments from the Baltic Sea. We compared changes in the sediment microbial community, after incubation with different stable isotope labeled OM types [i.e., particulate algal organic matter (PAOM), protein, and acetate], by using DNA stable isotope probing (DNA-SIP). Incorporation of 13C and/or 15N label was predominantly detected in members of the phyla Planctomycetes and Chloroflexi, which also formed the majority (>50%) of the original sediment community. While these phylum-level lineages incorporated label from all OM types, phylogenetic analyses revealed a niche separation at the order level. Members of the MSBL9 (Planctomycetes), the Anaerolineales (Chloroflexi), and the class Bathyarchaeota, were identified as initial degraders of carbohydrate-rich OM, while other uncultured orders, like the CCM11a and Phycisphaerales (Planctomycetes), Dehalococcoidia, and JG30-KF-CM66 (Chloroflexi), incorporated label also from protein and acetate. Our study highlights the importance of initial fermentation of complex carbon pools in shaping anoxic sediment microbial communities and reveals niche specialization at the order level for the most important initial degraders in anoxic sediments.
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Affiliation(s)
- Saara Suominen
- Department of Marine Microbiology and Biogeochemistry, NIOZ Royal Netherlands Institute for Sea Research, Den Burg, Netherlands
| | - Daan M. van Vliet
- Wageningen Food and Biobased Research (WFBR), Bornse Weilanden 9, Wageningen, Netherlands
- Laboratory of Microbiology, Wageningen University, Wageningen, Netherlands
| | | | - Marcel T. J. van der Meer
- Department of Marine Microbiology and Biogeochemistry, NIOZ Royal Netherlands Institute for Sea Research, Den Burg, Netherlands
| | - Jaap S. Sinninghe Damsté
- Department of Marine Microbiology and Biogeochemistry, NIOZ Royal Netherlands Institute for Sea Research, Den Burg, Netherlands
- Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Utrecht, Netherlands
| | - Laura Villanueva
- Department of Marine Microbiology and Biogeochemistry, NIOZ Royal Netherlands Institute for Sea Research, Den Burg, Netherlands
- Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Utrecht, Netherlands
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6
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Arcobacter peruensis sp. nov., a Chemolithoheterotroph Isolated from Sulfide- and Organic-Rich Coastal Waters off Peru. Appl Environ Microbiol 2019; 85:AEM.01344-19. [PMID: 31585991 DOI: 10.1128/aem.01344-19] [Citation(s) in RCA: 28] [Impact Index Per Article: 5.6] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/14/2019] [Accepted: 09/05/2019] [Indexed: 02/06/2023] Open
Abstract
Members of the epsilonproteobacterial genus Arcobacter have been identified to be potentially important sulfide oxidizers in marine coastal, seep, and stratified basin environments. In the highly productive upwelling waters off the coast of Peru, Arcobacter cells comprised 3 to 25% of the total microbial community at a near-shore station where sulfide concentrations exceeded 20 μM in bottom waters. From the chemocline where the Arcobacter population exceeded 106 cells ml-1 and where high rates of denitrification (up to 6.5 ± 0.4 μM N day-1) and dark carbon fixation (2.8 ± 0.2 μM C day-1) were measured, we isolated a previously uncultivated Arcobacter species, Arcobacter peruensis sp. nov. (BCCM LMG-31510). Genomic analysis showed that A. peruensis possesses genes encoding sulfide oxidation and denitrification pathways but lacks the ability to fix CO2 via autotrophic carbon fixation pathways. Genes encoding transporters for organic carbon compounds, however, were present in the A. peruensis genome. Physiological experiments demonstrated that A. peruensis grew best on a mix of sulfide, nitrate, and acetate. Isotope labeling experiments further verified that A. peruensis completely reduced nitrate to N2 and assimilated acetate but did not fix CO2, thus coupling heterotrophic growth to sulfide oxidation and denitrification. Single-cell nanoscale secondary ion mass spectrometry analysis of samples taken from shipboard isotope labeling experiments also confirmed that the Arcobacter population in situ did not substantially fix CO2 The efficient growth yield associated with the chemolithoheterotrophic metabolism of A. peruensis may allow this Arcobacter species to rapidly bloom in eutrophic and sulfide-rich waters off the coast of Peru.IMPORTANCE Our multidisciplinary approach provides new insights into the ecophysiology of a newly isolated environmental Arcobacter species, as well as the physiological flexibility within the Arcobacter genus and sulfide-oxidizing, denitrifying microbial communities within oceanic oxygen minimum zones (OMZs). The chemolithoheterotrophic species Arcobacter peruensis may play a substantial role in the diverse consortium of bacteria that is capable of coupling denitrification and fixed nitrogen loss to sulfide oxidation in eutrophic, sulfidic coastal waters. With increasing anthropogenic pressures on coastal regions, e.g., eutrophication and deoxygenation (D. Breitburg, L. A. Levin, A. Oschlies, M. Grégoire, et al., Science 359:eaam7240, 2018, https://doi.org/10.1126/science.aam7240), niches where sulfide-oxidizing, denitrifying heterotrophs such as A. peruensis thrive are likely to expand.
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7
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Broman E, Sachpazidou V, Pinhassi J, Dopson M. Oxygenation of Hypoxic Coastal Baltic Sea Sediments Impacts on Chemistry, Microbial Community Composition, and Metabolism. Front Microbiol 2017; 8:2453. [PMID: 29312168 PMCID: PMC5733055 DOI: 10.3389/fmicb.2017.02453] [Citation(s) in RCA: 20] [Impact Index Per Article: 2.9] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/19/2017] [Accepted: 11/27/2017] [Indexed: 01/24/2023] Open
Abstract
The Baltic Sea has undergone severe eutrophication during the last century, resulting in increased algal blooms and the development of hypoxic bottom waters. In this study, we sampled oxygen deficient sediment cores from a Baltic Sea coastal bay and exposed the bottom water including the sediment surface to oxygen shifts via artificial addition of air during laboratory incubation. Surface sediment (top 1 cm) from the replicate cores were sliced in the field as well as throughout the laboratory incubations and chemical parameters were analyzed along with high throughput sequencing of community DNA and RNA. After oxygenation, dissolved iron decreased in the water overlying the sediment while inorganic sulfur compounds (thiosulfate and tetrathionate) increased when the water was kept anoxic. Oxygenation of the sediment also maintained RNA transcripts attributed to sulfide and sulfur oxidation as well as nitrogen fixation in the sediment surface. Based on 16S rRNA gene and metatranscriptomic analyses it was found that oxygenation of the sediment surface caused a bloom of the Epsilonproteobacteria genus Arcobacter. In addition, the formation of a thick white film was observed that was likely filamentous zero-valent sulfur produced by the Arcobacter spp. Based on these results, sulfur cycling and nitrogen fixation that were evident in the field samples were ongoing during re-oxygenation of the sediment. These processes potentially added organic nitrogen to the system and facilitated the re-establishment of micro- and macroorganism communities in the benthic zone.
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Affiliation(s)
- Elias Broman
- Biology and Environmental Sciences, Centre for Ecology and Evolution in Microbial Model Systems, Linnaeus University, Kalmar, Sweden
| | - Varvara Sachpazidou
- Biology and Environmental Sciences, Centre for Ecology and Evolution in Microbial Model Systems, Linnaeus University, Kalmar, Sweden
| | - Jarone Pinhassi
- Biology and Environmental Sciences, Centre for Ecology and Evolution in Microbial Model Systems, Linnaeus University, Kalmar, Sweden
| | - Mark Dopson
- Biology and Environmental Sciences, Centre for Ecology and Evolution in Microbial Model Systems, Linnaeus University, Kalmar, Sweden
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8
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Liu S, Wawrik B, Liu Z. Different Bacterial Communities Involved in Peptide Decomposition between Normoxic and Hypoxic Coastal Waters. Front Microbiol 2017; 8:353. [PMID: 28326069 PMCID: PMC5339267 DOI: 10.3389/fmicb.2017.00353] [Citation(s) in RCA: 13] [Impact Index Per Article: 1.9] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/16/2016] [Accepted: 02/20/2017] [Indexed: 11/13/2022] Open
Abstract
Proteins and peptides are key components of the labile dissolved organic matter pool in marine environments. Knowing which types of bacteria metabolize peptides can inform the factors that govern peptide decomposition and further carbon and nitrogen remineralization in marine environments. A 13C-labeled tetrapeptide, alanine-valine-phenylalanine-alanine (AVFA), was added to both surface (normoxic) and bottom (hypoxic) seawater from a coastal station in the northern Gulf of Mexico for a 2-day incubation experiment, and bacteria that incorporated the peptide were identified using DNA stable isotope probing (SIP). The decomposition rate of AVFA in the bottom hypoxic seawater (0.018–0.035 μM h-1) was twice as fast as that in the surface normoxic seawater (0.011–0.017 μM h-1). SIP experiments indicated that incorporation of 13C was highest among the Flavobacteria, Sphingobacteria, Alphaproteobacteria, Acidimicrobiia, Verrucomicrobiae, Cyanobacteria, and Actinobacteria in surface waters. In contrast, highest 13C-enrichment was mainly observed in several Alphaproteobacteria (Thalassococcus, Rhodobacteraceae, Ruegeria) and Gammaproteobacteria genera (Colwellia, Balneatrix, Thalassomonas) in the bottom water. These data suggest that a more diverse group of both oligotrophic and copiotrophic bacteria may be involved in metabolizing labile organic matter such as peptides in normoxic coastal waters, and several copiotrophic genera belonging to Alphaproteobacteria and Gammaproteobacteria and known to be widely distributed may contribute to faster peptide decomposition in the hypoxic waters.
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Affiliation(s)
- Shuting Liu
- Marine Science Institute, The University of Texas at Austin, Port Aransas TX, USA
| | - Boris Wawrik
- Department of Microbiology and Plant Biology, The University of Oklahoma, Norman OK, USA
| | - Zhanfei Liu
- Marine Science Institute, The University of Texas at Austin, Port Aransas TX, USA
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9
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Thureborn P, Franzetti A, Lundin D, Sjöling S. Reconstructing ecosystem functions of the active microbial community of the Baltic Sea oxygen depleted sediments. PeerJ 2016; 4:e1593. [PMID: 26823996 PMCID: PMC4730985 DOI: 10.7717/peerj.1593] [Citation(s) in RCA: 20] [Impact Index Per Article: 2.5] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/23/2015] [Accepted: 12/22/2015] [Indexed: 11/24/2022] Open
Abstract
Baltic Sea deep water and sediments hold one of the largest anthropogenically induced hypoxic areas in the world. High nutrient input and low water exchange result in eutrophication and oxygen depletion below the halocline. As a consequence at Landsort Deep, the deepest point of the Baltic Sea, anoxia in the sediments has been a persistent condition over the past decades. Given that microbial communities are drivers of essential ecosystem functions we investigated the microbial community metabolisms and functions of oxygen depleted Landsort Deep sediments by metatranscriptomics. Results show substantial expression of genes involved in protein metabolism demonstrating that the Landsort Deep sediment microbial community is active. Identified expressed gene suites of metabolic pathways with importance for carbon transformation including fermentation, dissimilatory sulphate reduction and methanogenesis were identified. The presence of transcripts for these metabolic processes suggests a potential for heterotrophic-autotrophic community synergism and indicates active mineralisation of the organic matter deposited at the sediment as a consequence of the eutrophication process. Furthermore, cyanobacteria, probably deposited from the water column, are transcriptionally active in the anoxic sediment at this depth. Results also reveal high abundance of transcripts encoding integron integrases. These results provide insight into the activity of the microbial community of the anoxic sediment at the deepest point of the Baltic Sea and its possible role in ecosystem functioning.
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Affiliation(s)
- Petter Thureborn
- School of Natural Sciences, Technology and Environmental Studies, Södertörn University , Huddinge , Sweden
| | - Andrea Franzetti
- School of Natural Sciences, Technology and Environmental Studies, Södertörn University, Huddinge, Sweden; Department of Earth and Environmental Sciences, University of Milano-Bicocca, Milano, Italy
| | - Daniel Lundin
- BILS, Bioinformatics Infrastructure for Life Sciences, Science for Life Laboratories, Solna, Sweden; Centre for Ecology and Evolution in Microbial model Systems-EEMiS, Linnaeus University, Kalmar, Sweden
| | - Sara Sjöling
- School of Natural Sciences, Technology and Environmental Studies, Södertörn University , Huddinge , Sweden
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10
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Winkel M, Pjevac P, Kleiner M, Littmann S, Meyerdierks A, Amann R, Mußmann M. Identification and activity of acetate-assimilating bacteria in diffuse fluids venting from two deep-sea hydrothermal systems. FEMS Microbiol Ecol 2014; 90:731-46. [DOI: 10.1111/1574-6941.12429] [Citation(s) in RCA: 18] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/28/2014] [Revised: 09/10/2014] [Accepted: 09/16/2014] [Indexed: 12/01/2022] Open
Affiliation(s)
- Matthias Winkel
- Department of Molecular Ecology; Max Planck Institute for Marine Microbiology; Bremen Germany
| | - Petra Pjevac
- Department of Molecular Ecology; Max Planck Institute for Marine Microbiology; Bremen Germany
| | - Manuel Kleiner
- Department of Symbiosis; Max Planck Institute for Marine Microbiology; Bremen Germany
| | - Sten Littmann
- Department of Biogeochemistry; Max Planck Institute for Marine Microbiology; Bremen Germany
| | - Anke Meyerdierks
- Department of Molecular Ecology; Max Planck Institute for Marine Microbiology; Bremen Germany
| | - Rudolf Amann
- Department of Molecular Ecology; Max Planck Institute for Marine Microbiology; Bremen Germany
| | - Marc Mußmann
- Department of Molecular Ecology; Max Planck Institute for Marine Microbiology; Bremen Germany
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11
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Glaubitz S, Abraham WR, Jost G, Labrenz M, Jürgens K. Pyruvate utilization by a chemolithoautotrophic epsilonproteobacterial key player of pelagic Baltic Sea redoxclines. FEMS Microbiol Ecol 2013; 87:770-9. [PMID: 24279499 DOI: 10.1111/1574-6941.12263] [Citation(s) in RCA: 7] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/23/2013] [Revised: 11/14/2013] [Accepted: 11/20/2013] [Indexed: 11/27/2022] Open
Abstract
Pelagic redoxclines of the central Baltic Sea are dominated by the epsilonproteobacterial group Sulfurimonas GD17, considered to be the major driver of chemolithoautotrophic denitrification in this habitat. Autecological investigations of a recently isolated representative of this environmental group, Sulfurimonas gotlandica str. GD1(T), demonstrated that the bacterium grows best under sulfur-oxidizing, denitrifying conditions. However, in the presence of bicarbonate, this strain is able to use pyruvate as both an additional carbon source and an alternative electron donor. These observations suggested that the environmental group GD17 actively metabolizes organic substrates in situ. To examine this possibility, we used RNA-based stable isotope probing (RNA-SIP) on a natural redoxcline community provided with ¹³C-labeled pyruvate. While in this experiment, we were able to identify putative heterotrophic microorganisms, the uptake of ¹³C-pyruvate in GD17 nucleic acids could not be established. To resolve these contradictory findings, combined incorporation experiments with ¹⁴C- and ¹³C-labeled pyruvate were carried out in cells of strain GD1(T) cultivated under chemolithoautotrophic conditions, which favor pyruvate uptake rather than oxidation. An analysis of the labeled biomolecules revealed that pyruvate was mostly incorporated in cellular components such as amino acids, whose synthesis requires only minimal transformation. Carbon transfer into nucleic acids was not observed, explaining the inability of RNA-SIP to detect pyruvate incorporation by strain GD1(T) and the environmental group GD17. Together, these findings suggest that by integrating organic compounds such as pyruvate into cellular components S. gotlandica GD1(T) is able to replenish chemolithoautotrophic growth and thus ensure its survival in nutrient-limited habitats such as marine pelagic redoxclines.
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Affiliation(s)
- Sabine Glaubitz
- Section Biological Oceanography, Leibniz-Institute for Baltic Sea Research Warnemuende (IOW), Rostock, Germany
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