Microbial Diversity of Hydrothermal Sediments in the Guaymas Basin: Evidence for Anaerobic Methanotrophic Communities

By A. Teske, K. Hinrichs, V. Edgcomb, Alvin de Vera Gomez, David T. Kysela, S. Sylva, Mitchell L Sogin, H. Jannasch. Applied and Environmental Microbiology, 2002

710 citations recorded by the source corpus.

Subfields: Ecology, Environmental Chemistry, Mechanics of Materials

View Paper: https://www.semanticscholar.org/paper/0756967c0f8a9ce6ed9c86be944a2ea29285019e

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. A. Teske
3. B. Jørgensen
4. K. Knittel
5. N. Ogawa
6. N. Ohkouchi
7. M. Elvert
8. Y. Chikaraishi

In Environmental Chemistry

1. Antje Boetius
2. B. Jørgensen
3. A. Teske
4. M. Elvert
5. K. Knittel
6. H. Niemann
7. William F. Martin
8. B. Orcutt

In Mechanics of Materials

1. Antje Boetius
2. M. Elvert
3. B. Jørgensen
4. H. Niemann
5. J. Baross
6. J. Brocks
7. A. Pearson
8. E. Suess

Citations in the corpus

• Microbial Communities of Deep Marine Subsurface Sediments: Molecular and Cultivation Surveys (2006, background): “They were subsequently detected in additional hydrothermal vent sites (Reysenbach et al. 2000; Teske et al. 2002) before appearing as a dominant clone group in cold subsurface sediments (Reed et al.”
• Feast and famine — microbial life in the deep-sea bed (2007, background): “Hydrocarbon turnover, resulting in high sulphide fluxes at cold seeps, is usually dominated by sulphate-reducing bacteria of the deltaproteobacteri”
• Diagnostic lipid biomarker and stable carbon isotope signatures of microbial communities mediating the anaerobic oxidation of methane with sulphate (2008, background): “No free biphytanediols were detected at the Guaymas Basin at an ANME-2c dominated site (Teske et al., 2002).”
• Diversity and Distribution of Methanotrophic Archaea at Cold Seeps (2005, background): “The archaeal community of hydrothermally active sediments of Guaymas Basin (58) consists of 13 phylogenetic lineages.”
• Hydrothermal vents and the origin of life (2008, background): “These methanogens can use several organic compounds, some of which have been implicated in anaerobic methane oxidation (AMO) in both hydrothermal sediment”
• The uncultured microbial majority. (2003, background): “The following recently identified lineages are shown in Figure 2: SC3 and SC4, identified from arid soil (27); NC10, identified from aquatic microbial formations in flooded caves (46); BRC1, identified from bulk soil and rice roots of flooded rice microcosms (24); ABY1, identified from lake bacterio”
• Building the Biomarker Tree of Life (2005, background): “2003); hot-temperature CH4 seeps (Teske et al. 2002; Schouten et al. 2003b); in the Black Sea (Thiel et al.”
• Sedimentary membrane lipids recycled by deep-sea benthic archaea (2010, background): “Teske, A. & Sorensen, K. B. Uncultured archaea in deep marine subsurface sediments: Have we caught them all? ISME J. 2, 3–18 (2008).”
• Anaerobic Metabolism: Linkages to Trace Gases and Aerobic Processes (2003, background): “They have been recovered from hydrothermal vents (Takai and Horikoshi, 1999; Teske et al., 2002), methane hydrates (Lanoil et al.”
• Impact of natural oil and higher hydrocarbons on microbial diversity, distribution, and activity in Gulf of Mexico cold-seep sediments (2010, background): “Members of these and other sulfate-reducing bacteria (SRB) are specific to cold seeps (SEEP-SRB groups 1–4) and are also commonly found as free-living cells, sometimes in instances when non-methane hydrocarbons are present (Dhillon et al., 2003; Knittel et al., 2003; Mills et al., 2004; Orphan et al”