Parameters Governing the Community Structure and Element Turnover in Kermadec Volcanic Ash and Hydrothermal Fluids as Monitored by Inorganic Electron Donor Consumption, Autotrophic CO2 Fixation and 16S Tags of the Transcriptome in Incubation Experiments
The microbial community composition and its functionality was assessed for hydrothermal fluids and volcanic ash sediments from Haungaroa and hydrothermal fluids from the Brothers volcano in the Kermadec island arc (New Zealand). The Haungaroa volcanic ash sediments were dominated by epsilonproteobac...
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Published in | Frontiers in microbiology Vol. 10; p. 2296 |
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Main Authors | , , , , , , , , , , , |
Format | Journal Article |
Language | English |
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09.10.2019
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Abstract | The microbial community composition and its functionality was assessed for hydrothermal fluids and volcanic ash sediments from Haungaroa and hydrothermal fluids from the Brothers volcano in the Kermadec island arc (New Zealand). The Haungaroa volcanic ash sediments were dominated by epsilonproteobacterial
Sulfurovum
sp. Ratios of electron donor consumption to CO
2
fixation from respective sediment incubations indicated that sulfide oxidation appeared to fuel autotrophic CO
2
fixation, coinciding with thermodynamic estimates predicting sulfide oxidation as the major energy source in the environment. Transcript analyses with the sulfide-supplemented sediment slurries demonstrated that
Sulfurovum
prevailed in the experiments as well. Hence, our sediment incubations appeared to simulate environmental conditions well suggesting that sulfide oxidation catalyzed by
Sulfurovum
members drive biomass synthesis in the volcanic ash sediments. For the Haungaroa fluids no inorganic electron donor and responsible microorganisms could be identified that clearly stimulated autotrophic CO
2
fixation. In the Brothers hydrothermal fluids
Sulfurimonas
(49%) and
Hydrogenovibrio/Thiomicrospira
(15%) species prevailed. Respective fluid incubations exhibited highest autotrophic CO
2
fixation if supplemented with iron(II) or hydrogen. Likewise catabolic energy calculations predicted primarily iron(II) but also hydrogen oxidation as major energy sources in the natural fluids. According to transcript analyses with material from the incubation experiments
Thiomicrospira/Hydrogenovibrio
species dominated, outcompeting
Sulfurimonas
. Given that experimental conditions likely only simulated environmental conditions that cause
Thiomicrospira/Hydrogenovibrio
but not
Sulfurimonas
to thrive, it remains unclear which environmental parameters determine
Sulfurimonas’
dominance in the Brothers natural hydrothermal fluids. |
---|---|
AbstractList | The microbial community composition and its functionality was assessed for hydrothermal fluids and volcanic ash sediments from Haungaroa and hydrothermal fluids from the Brothers volcano in the Kermadec island arc (New Zealand). The Haungaroa volcanic ash sediments were dominated by epsilonproteobacterial
Sulfurovum
sp. Ratios of electron donor consumption to CO
2
fixation from respective sediment incubations indicated that sulfide oxidation appeared to fuel autotrophic CO
2
fixation, coinciding with thermodynamic estimates predicting sulfide oxidation as the major energy source in the environment. Transcript analyses with the sulfide-supplemented sediment slurries demonstrated that
Sulfurovum
prevailed in the experiments as well. Hence, our sediment incubations appeared to simulate environmental conditions well suggesting that sulfide oxidation catalyzed by
Sulfurovum
members drive biomass synthesis in the volcanic ash sediments. For the Haungaroa fluids no inorganic electron donor and responsible microorganisms could be identified that clearly stimulated autotrophic CO
2
fixation. In the Brothers hydrothermal fluids
Sulfurimonas
(49%) and
Hydrogenovibrio/Thiomicrospira
(15%) species prevailed. Respective fluid incubations exhibited highest autotrophic CO
2
fixation if supplemented with iron(II) or hydrogen. Likewise catabolic energy calculations predicted primarily iron(II) but also hydrogen oxidation as major energy sources in the natural fluids. According to transcript analyses with material from the incubation experiments
Thiomicrospira/Hydrogenovibrio
species dominated, outcompeting
Sulfurimonas
. Given that experimental conditions likely only simulated environmental conditions that cause
Thiomicrospira/Hydrogenovibrio
but not
Sulfurimonas
to thrive, it remains unclear which environmental parameters determine
Sulfurimonas’
dominance in the Brothers natural hydrothermal fluids. The microbial community composition and its functionality was assessed for hydrothermal fluids and volcanic ash sediments from Haungaroa and hydrothermal fluids from the Brothers volcano in the Kermadec island arc (New Zealand). The Haungaroa volcanic ash sediments were dominated by epsilonproteobacterial Sulfurovum sp. Ratios of electron donor consumption to CO2 fixation from respective sediment incubations indicated that sulfide oxidation appeared to fuel autotrophic CO2 fixation, coinciding with thermodynamic estimates predicting sulfide oxidation as the major energy source in the environment. Transcript analyses with the sulfide-supplemented sediment slurries demonstrated that Sulfurovum prevailed in the experiments as well. Hence, our sediment incubations appeared to simulate environmental conditions well suggesting that sulfide oxidation catalyzed by Sulfurovum members drive biomass synthesis in the volcanic ash sediments. For the Haungaroa fluids no inorganic electron donor and responsible microorganisms could be identified that clearly stimulated autotrophic CO2 fixation. In the Brothers hydrothermal fluids Sulfurimonas (49%) and Hydrogenovibrio/Thiomicrospira (15%) species prevailed. Respective fluid incubations exhibited highest autotrophic CO2 fixation if supplemented with iron(II) or hydrogen. Likewise catabolic energy calculations predicted primarily iron(II) but also hydrogen oxidation as major energy sources in the natural fluids. According to transcript analyses with material from the incubation experiments Thiomicrospira/Hydrogenovibrio species dominated, outcompeting Sulfurimonas. Given that experimental conditions likely only simulated environmental conditions that cause Thiomicrospira/Hydrogenovibrio but not Sulfurimonas to thrive, it remains unclear which environmental parameters determine Sulfurimonas’ dominance in the Brothers natural hydrothermal fluids. |
Author | Kleint, Charlotte Sander, Sylvia G. Bach, Wolfgang Perner, Mirjam Gonnella, Giorgio Diehl, Alexander Indenbirken, Daniela Sass, Katharina Böhnke, Stefanie Zitoun, Rebecca Koschinsky, Andrea Kurtz, Stefan |
AuthorAffiliation | 5 Department of Chemistry, University of Otago , Dunedin , New Zealand 2 Center for Bioinformatics (ZBH), Universität Hamburg , Hamburg , Germany 6 Heinrich Pette Institute, Leibniz Institute for Experimental Virology , Hamburg , Germany 4 Department of Physics and Earth Sciences, Jacobs University Bremen , Bremen , Germany 1 Molecular Biology of Microbial Consortia, Institute of Plant Science and Microbiology, Universität Hamburg , Hamburg , Germany 3 Department of Geosciences, MARUM – Centre for Marine Environmental Sciences, University of Bremen , Bremen , Germany |
AuthorAffiliation_xml | – name: 6 Heinrich Pette Institute, Leibniz Institute for Experimental Virology , Hamburg , Germany – name: 5 Department of Chemistry, University of Otago , Dunedin , New Zealand – name: 1 Molecular Biology of Microbial Consortia, Institute of Plant Science and Microbiology, Universität Hamburg , Hamburg , Germany – name: 4 Department of Physics and Earth Sciences, Jacobs University Bremen , Bremen , Germany – name: 3 Department of Geosciences, MARUM – Centre for Marine Environmental Sciences, University of Bremen , Bremen , Germany – name: 2 Center for Bioinformatics (ZBH), Universität Hamburg , Hamburg , Germany |
Author_xml | – sequence: 1 givenname: Stefanie surname: Böhnke fullname: Böhnke, Stefanie – sequence: 2 givenname: Katharina surname: Sass fullname: Sass, Katharina – sequence: 3 givenname: Giorgio surname: Gonnella fullname: Gonnella, Giorgio – sequence: 4 givenname: Alexander surname: Diehl fullname: Diehl, Alexander – sequence: 5 givenname: Charlotte surname: Kleint fullname: Kleint, Charlotte – sequence: 6 givenname: Wolfgang surname: Bach fullname: Bach, Wolfgang – sequence: 7 givenname: Rebecca surname: Zitoun fullname: Zitoun, Rebecca – sequence: 8 givenname: Andrea surname: Koschinsky fullname: Koschinsky, Andrea – sequence: 9 givenname: Daniela surname: Indenbirken fullname: Indenbirken, Daniela – sequence: 10 givenname: Sylvia G. surname: Sander fullname: Sander, Sylvia G. – sequence: 11 givenname: Stefan surname: Kurtz fullname: Kurtz, Stefan – sequence: 12 givenname: Mirjam surname: Perner fullname: Perner, Mirjam |
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Copyright | Copyright © 2019 Böhnke, Sass, Gonnella, Diehl, Kleint, Bach, Zitoun, Koschinsky, Indenbirken, Sander, Kurtz and Perner. 2019 Böhnke, Sass, Gonnella, Diehl, Kleint, Bach, Zitoun, Koschinsky, Indenbirken, Sander, Kurtz and Perner |
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Notes | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 Edited by: Mark Alexander Lever, ETH Zürich, Switzerland Present address: Stefanie Böhnke and Mirjam Perner, Geomicrobiology, GEOMAR, Helmholtz Centre for Ocean Research Kiel, Kiel, Germany Sylvia G. Sander, Marine Environment Studies Laboratory, International Atomic Energy Agency, Monaco, Monaco This article was submitted to Extreme Microbiology, a section of the journal Frontiers in Microbiology Reviewed by: Kathleen Scott, University of South Florida, Tampa, United States; Ida Helene Steen, University of Bergen, Norway |
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SubjectTerms | autotrophic CO2 fixation microbial hydrogen oxidation microbial hydrothermal vent communities microbial iron oxidation microbial sulfide oxidation Microbiology MiSeq |
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Title | Parameters Governing the Community Structure and Element Turnover in Kermadec Volcanic Ash and Hydrothermal Fluids as Monitored by Inorganic Electron Donor Consumption, Autotrophic CO2 Fixation and 16S Tags of the Transcriptome in Incubation Experiments |
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