His primary scientific interests are in Methane, Environmental chemistry, Ecology, Anaerobic oxidation of methane and Anoxic waters. His Methane study integrates concerns from other disciplines, such as Submarine pipeline, Salinity, Estuary, Hydrology and Archaea. His work deals with themes such as Organic matter, Sulfur and Bathymodiolus, which intersect with Environmental chemistry.
In general Ecology, his work in Mussel is often linked to Energy source linking many areas of study. His Anaerobic oxidation of methane research focuses on Carbonate and how it connects with Bottom water, Mud volcano, Geomorphology, Pore water pressure and Biomass. His Anoxic waters research is multidisciplinary, incorporating perspectives in Sulfate-reducing bacteria and Hopanoids.
His primary areas of investigation include Oceanography, Environmental chemistry, Geochemistry, Methane and Hydrothermal circulation. His work on Water column and Cruise is typically connected to Black sea and Environmental science as part of general Oceanography study, connecting several disciplines of science. His Environmental chemistry study combines topics from a wide range of disciplines, such as Ecology, Organic matter and Carbon, Isotopes of carbon.
The Geochemistry study combines topics in areas such as Petroleum seep, Sulfide and Seafloor spreading. In the subject of general Methane, his work in Anaerobic oxidation of methane is often linked to Microbial mat, thereby combining diverse domains of study. The study incorporates disciplines such as Seawater, Deep sea and Ultramafic rock in addition to Hydrothermal circulation.
Richard Seifert mainly investigates Oceanography, Geochemistry, Environmental science, Cruise and Environmental chemistry. His work on Water column as part of general Oceanography research is frequently linked to Black sea, bridging the gap between disciplines. Richard Seifert has researched Geochemistry in several fields, including Petroleum seep, Sulfide, Organic matter and Hydrothermal vent.
While the research belongs to areas of Petroleum seep, Richard Seifert spends his time largely on the problem of Carbonate, intersecting his research to questions surrounding Anaerobic oxidation of methane. His work in Pore water pressure addresses issues such as Sediment, which are connected to fields such as Hydrogen sulphide, Mineralogy, Total organic carbon, Sedimentology and Anoxic waters. His Mud volcano study frequently links to other fields, such as Methane.
His scientific interests lie mostly in Geochemistry, Oceanography, Hydrothermal vent, Methane and Flux. Geochemistry is closely attributed to Organic matter in his work. His Hydrothermal vent research is multidisciplinary, incorporating elements of Ecology, Sulfide and Hydrogen.
His Sulfide research includes elements of Environmental chemistry, Deep sea, Basalt and Ultramafic rock. In his research, Anaerobic oxidation of methane and Archaea is intimately related to Stable-isotope probing, which falls under the overarching field of Methane. His work often combines Anaerobic oxidation of methane and Microbial mat studies.
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Microbial reefs in the Black Sea fueled by anaerobic oxidation of methane
Walter Michaelis;Richard Seifert;Katja Nauhaus;Tina Treude.
Membrane lipid patterns typify distinct anaerobic methanotrophic consortia
Martin Blumenberg;Richard Seifert;Joachim Reitner;Thomas Pape.
Proceedings of the National Academy of Sciences of the United States of America (2004)
Probable modern analogue of Kuroko-type massive sulphide deposits in the Okinawa Trough back-arc basin
P. Halbach;Ko Ichi Nakamura;M. Wahsner;J. Lange.
Geochemistry of hydrothermal fluids from the ultramafic-hosted Logatchev hydrothermal field, 15°N on the Mid-Atlantic Ridge: Temporal and spatial investigation
Katja Schmidt;Andrea Koschinsky;Dieter Garbe-Schönberg;Leandro M. de Carvalho.
Chemical Geology (2007)
Highly isotopically depleted isoprenoids: molecular markers for ancient methane venting
Volker Thiel;Jörn Peckmann;Richard Seifert;Patrick Wehrung.
Geochimica et Cosmochimica Acta (1999)
Hydrogen is an energy source for hydrothermal vent symbioses.
Jillian M. Petersen;Frank U. Zielinski;Thomas Pape;Richard Seifert.
Methane distribution in European tidal estuaries
J. J. Middelburg;J. Nieuwenhuize;Niels Iversen;N. Hogh.
Biosynthesis of hopanoids by sulfate-reducing bacteria (genus Desulfovibrio).
Martin Blumenberg;Martin Krüger;Katja Nauhaus;Helen M. Talbot.
Environmental Microbiology (2006)
Mud volcanoes and gas hydrates in the Black Sea: new data from Dvurechenskii and Odessa mud volcanoes
G. Bohrmann;M. Ivanov;J.-P. Foucher;V. Spiess.
Geo-marine Letters (2003)
Metabolites of xenobiotica and mineral oil constituents linked to macromolecular organic matter in polluted environments
Hans H. Richnow;Richard Seifert;Jens Hefter;Matthias Kästner.
Organic Geochemistry (1994)
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