| Literature DB >> 24970083 |
D A Stolper1, M Lawson2, C L Davis2, A A Ferreira3, E V Santos Neto3, G S Ellis4, M D Lewan4, A M Martini5, Y Tang6, M Schoell7, A L Sessions8, J M Eiler8.
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.Entities:
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Year: 2014 PMID: 24970083 DOI: 10.1126/science.1254509
Source DB: PubMed Journal: Science ISSN: 0036-8075 Impact factor: 47.728