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Gas formation. Formation temperatures of thermogenic and biogenic methane.
Stolper, D A; Lawson, M; Davis, C L; Ferreira, A A; Santos Neto, E V; Ellis, G S; Lewan, M D; Martini, A M; Tang, Y; Schoell, M; Sessions, A L; Eiler, J M.
Afiliación
  • Stolper DA; Division of Geological and Planetary Sciences, California Institute of Technology, 1200 East California Boulevard, Pasadena, CA 91125, USA. dstolper@caltech.edu.
  • Lawson M; ExxonMobil Upstream Research Company, Houston, TX, USA.
  • Davis CL; ExxonMobil Upstream Research Company, Houston, TX, USA.
  • Ferreira AA; Division of Geochemistry, Petrobras Research and Development Center (CENPES), Rio de Janeiro, RJ, Brazil.
  • Santos Neto EV; Division of Geochemistry, Petrobras Research and Development Center (CENPES), Rio de Janeiro, RJ, Brazil.
  • Ellis GS; U.S. Geological Survey, Denver Federal Center, Denver, CO, USA.
  • Lewan MD; U.S. Geological Survey, Denver Federal Center, Denver, CO, USA.
  • Martini AM; Department of Geology, Amherst College, Amherst, MA, USA.
  • Tang Y; Power, Environmental, and Energy Research Institute, Covina, CA, USA.
  • Schoell M; GasConsult International Inc, Berkeley, CA, USA.
  • Sessions AL; Division of Geological and Planetary Sciences, California Institute of Technology, 1200 East California Boulevard, Pasadena, CA 91125, USA.
  • Eiler JM; Division of Geological and Planetary Sciences, California Institute of Technology, 1200 East California Boulevard, Pasadena, CA 91125, USA.
Science ; 344(6191): 1500-3, 2014 Jun 27.
Article en En | MEDLINE | ID: mdl-24970083
ABSTRACT
Methane is an important greenhouse gas and energy resource generated dominantly by methanogens at low temperatures and through the breakdown of organic molecules at high temperatures. However, methane-formation temperatures in nature are often poorly constrained. We measured formation temperatures of thermogenic and biogenic methane using a "clumped isotope" technique. Thermogenic gases yield formation temperatures between 157° and 221°C, within the nominal gas window, and biogenic gases yield formation temperatures consistent with their comparatively lower-temperature formational environments (<50°C). In systems where gases have migrated and other proxies for gas-generation temperature yield ambiguous results, methane clumped-isotope temperatures distinguish among and allow for independent tests of possible gas-formation models.
Asunto(s)

Texto completo: 1 Bases de datos: MEDLINE Asunto principal: Euryarchaeota / Yacimiento de Petróleo y Gas / Metano Idioma: En Revista: Science Año: 2014 Tipo del documento: Article País de afiliación: Estados Unidos

Texto completo: 1 Bases de datos: MEDLINE Asunto principal: Euryarchaeota / Yacimiento de Petróleo y Gas / Metano Idioma: En Revista: Science Año: 2014 Tipo del documento: Article País de afiliación: Estados Unidos