A microbial consortium couples anaerobic methane oxidation to denitrification

By A. Raghoebarsing, A. Pol, K. Pas-Schoonen, A. Smolders, K. Ettwig, W. Rijpstra, Stefan Schouten, J. Damsté, H. J. M. Camp, M. Jetten and 1 more. Nature, 2006

1,326 citations recorded by the source corpus.

Subfields: Ecology, Environmental Chemistry, Molecular Biology

View Paper: https://www.semanticscholar.org/paper/3d84e4fa842e8a647a3de8c497da59974214aa91

How researchers see this paper

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In Ecology

1. K. Knittel
2. Antje Boetius
3. B. Orcutt
4. Michael Russell
5. R. Thauer
6. T. Treude
7. A. Reitz
8. S. Kleindienst

In Environmental Chemistry

1. Antje Boetius
2. K. Knittel
3. William F. Martin
4. J. Stolz
5. R. Thauer
6. R. Oremland
7. B. Orcutt
8. F. Wolfe-Simon

In Molecular Biology

1. William F. Martin
2. Michael Russell
3. C. Griebler
4. T. Lueders
5. Antje Boetius
6. B. Orcutt
7. K. Knittel
8. T. Treude

Citations in the corpus

• Methane emissions from wetlands: biogeochemical, microbial, and modeling perspectives from local to global scales (2013, background): “, 2011), denitrification of nitrate (Smith et al., 1991; Raghoebarsing et al., 2006), and possibly organic TEAs (Smemo & Yavitt, 2011), has led to additional work on the importance of AOM in freshwater ecosystems.”
• Arsenic in the Evolution of Earth and Extraterrestrial Ecosystems (2009, background): “…oxidant for anaerobic methane oxidation has been sulfate in marine systems (Reeburgh 2007), this general phenomenon also couples with nitrate (Raghoebarsing et al. 2006), potentially with Fe (III) and Mn (IV) (Beal et al. 2009), and arsenate is at least a theoretically possibility (Thauer…”
• Beyond carbon and nitrogen: how the microbial energy economy couples elemental cycles in diverse ecosystems (2011, background): “However, recent studies have revealed anaerobic CH4 oxidation coupled to NO2 – reduction (Raghoebarsing et al. 2006) and Mn and Fe reduction (Beal et al.”
• Methanogenic archaea: ecologically relevant differences in energy conservation (2008, background): “AOM usually occurs when methane is the only available electron donor and the concentration of suitable electron acceptors is high, which is the case in marine sediments that are located directly above methane hydrates (high sulphate concentrations) or organic-rich freshwater sediments that contain h”
• Reviews and syntheses: to the bottom of carbon processing at the seafloor (2017, background): “…released (ammonium, manganese(II), iron(II), hydrogen sulfide and methane) are reoxidized (Jørgensen, 1977, 2006; Berner and Westrich, 1985; Aller and Rude, 1988; Soetaert et al., 1996; Boetius et al., 2000; Strous and Jetten, 2004; Raghoebarsing et al., 2006; Middelburg and Levin, 2009).”
• Mathematical modelling of anaerobic digestion processes: applications and future needs (2015, background): “However, oxidised nitrogen has also been found to act as electron acceptors for the anoxic oxidation of methane (denitrifying anaerobic methane oxidation, DAMO process) (Raghoebarsing et al. 2006).”
• Electron transfer in syntrophic communities of anaerobic bacteria and archaea (2009, methodology): “AOM coupled to denitrification has also been describe”
• Nitrite-driven anaerobic methane oxidation by oxygenic bacteria (2010, background): “napABCDE nirSJF D/GH/L norZ (1) norZ (2) norZ (3)”