Multiple archaeal groups mediate methane oxidation in anoxic cold seep sediments

By V. Orphan, C. House, K. Hinrichs, K. McKeegan, E. Delong. Proceedings of the National Academy of Sciences of the United States of America, 2002

670 citations recorded by the source corpus.

Subfields: Ecology, Environmental Chemistry, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/cf4ec1ad728cc9bc77a6de6a70a4c25e0409b444

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Ecology

1. Antje Boetius
2. L. Levin
3. K. Knittel
4. A. Teske
5. M. Elvert
6. K. Hinrichs
7. H. Niemann
8. E. Suess

In Environmental Chemistry

1. Antje Boetius
2. L. Levin
3. E. Suess
4. M. Elvert
5. K. Knittel
6. A. Teske
7. H. Niemann
8. A. Pearson

In Global and Planetary Change

1. Antje Boetius
2. L. Levin
3. E. Suess
4. K. Knittel
5. M. Elvert
6. A. Teske
7. H. Niemann

Citations in the corpus

• Hydrate Ridge: A natural laboratory for the study of microbial life fueled by methane from near-surface gas hydrates. (2004, methodology): “An important method in the study of AOM is the combination of the 16S rDNA based methods with an analysis of lipid compounds of archaea and sulfatereducing bacteria and their stable isotope signatures, allowing for an integration of phylogenetic and functional analysis (Hinrichs et al., 1999; Boetiu”
• ECOLOGY OF COLD SEEP SEDIMENTS: INTERACTIONS OF FAUNA WITH FLOW, CHEMISTRY AND MICROBES (2005, background): “They typically live in syntrophic consortia with sulphate-reducing bacteria in the Desulfosarcina/Desulfococcus and Desulfobulbu groups (Orphan et al. 2002, Knittel et al. 2003), although the exact nature of the interactions is poorly understood (reviewed in Valentine 2002, Widdel et al. 2004).”
• Diagnostic lipid biomarker and stable carbon isotope signatures of microbial communities mediating the anaerobic oxidation of methane with sulphate (2008, background): “Intriguingly, the magnitude of stable carbon isotope fractionation is different for the various ANME groups (Orphan et al., 2002; Blumenberg et al., 2004; Elvert et al., 2005).”
• Building the Biomarker Tree of Life (2005, background): “Currently they are classifi ed broadly among three new categories of Euryarchaeota, ANME-1, ANME-2, and ANME-3 (Boetius et al. 2000; Orphan et al. 2001, 2002; Knittel et al. 2005).”
• Diversity and Distribution of Methanotrophic Archaea at Cold Seeps (2005, background): “The second archaeal group mediating AOM is ANME-1 (34, 41), which is distantly related to the Methanosarcinales and Methanomicrobiales.”
• Intact polar lipids of anaerobic methanotrophic archaea and associated bacteria (2008, background): “, 2002) but also frequently as monospecific aggregates or as single cells without a clear bacterial partner (Orphan et al., 2002).”
• Microbial Communities of Deep Marine Subsurface Sediments: Molecular and Cultivation Surveys (2006, background): “…et al. 2001); and sulfatedependent, methanotrophic consortia analogous to those found at methane seeps and vents (Hinrichs et al. 1999; Boetius et al. 2000; Orphan et al. 2001, 2002; Michaelis et al. 2002; Teske et al. 2002, 2003) were expected to dominate the sulfatemethane transition zones.”