Novel microbial communities of the Haakon Mosby mud volcano and their role as a methane sink
By H. Niemann, T. Lösekann, D. de Beer, M. Elvert, T. Nadalig, K. Knittel, R. Amann, E. Sauter, M. Schlüter, M. Klages and 2 more. Nature, 2006
626 citations recorded by the source corpus.
Subfields: Ecology, Environmental Chemistry, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/33300cd4f6f0c6f3b24e39388e3f86171b7b3593
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Citations in the corpus
- Impact of natural oil and higher hydrocarbons on microbial diversity, distribution, and activity in Gulf of Mexico cold-seep sediments (2010, result): “…al., 2004; Orcutt et al., 2005) and supported by this study, AOM and SR activities in GOM seep sediments are comparable to those observed in other cold-seep environments (for example, Boetius et al., 2000; Hinrichs and Boetius, 2002; Niemann et al., 2006; Sahling et al., 2002; Treude et al., 2003).”
- Seabed methane emissions and the habitat of frenulate tubeworms on the Captain Arutyunov mud volcano (Gulf of Cadiz) (2009, background): “Furthermore, high rates of aerobic methanotrophy constituting the major pathway of methane oxidation has been documented for the central plain of the methane-emitting Håkon Mosby mud volcano (Niemann et al. 2006).”
- Feast and famine — microbial life in the deep-sea bed (2007, background): “These chemosynthetic ecosystems are usually found on continental margins at depths of 200–3,500 m and are characterized by the venting of hydrocarbons at fluid-flow velocities of a few tens of centimetres to a few metres per yea”
- Electron transfer in syntrophic communities of anaerobic bacteria and archaea (2009, background): “In sulphate-dependent AOM, different clades of methane-converting archaea termed ANME-1, ANME-2 and ANME-3 were identified on the basis of 16S ribosomal RNA difference”
- Single-cell identification in microbial communities by improved fluorescence in situ hybridization techniques (2008, background): “Similarly, the microbial communities that inhabit different sediment zones around a deep-sea mud volcano and meditate anaerobic methane oxidation and sulphate reduction could be determined and quantified along defined physicochemical gradients (see, for example, Ref”