<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Wang, David T</style></author><author><style face="normal" font="default" size="100%">Gruen, Danielle S</style></author><author><style face="normal" font="default" size="100%">Lollar, Barbara Sherwood</style></author><author><style face="normal" font="default" size="100%">Hinrichs, Kai-Uwe</style></author><author><style face="normal" font="default" size="100%">Stewart, Lucy C</style></author><author><style face="normal" font="default" size="100%">Holden, James F</style></author><author><style face="normal" font="default" size="100%">Hristov, Alexander N</style></author><author><style face="normal" font="default" size="100%">Pohlman, John W</style></author><author><style face="normal" font="default" size="100%">Morrill, Penny L</style></author><author><style face="normal" font="default" size="100%">Könneke, Martin</style></author><author><style face="normal" font="default" size="100%">Delwiche, Kyle B</style></author><author><style face="normal" font="default" size="100%">Reeves, Eoghan P</style></author><author><style face="normal" font="default" size="100%">Sutcliffe, Chelsea N</style></author><author><style face="normal" font="default" size="100%">Ritter, Daniel J</style></author><author><style face="normal" font="default" size="100%">Seewald, Jeffrey S</style></author><author><style face="normal" font="default" size="100%">McIntosh, Jennifer C</style></author><author><style face="normal" font="default" size="100%">Hemond, Harold F</style></author><author><style face="normal" font="default" size="100%">Kubo, Michael D</style></author><author><style face="normal" font="default" size="100%">Cardace, Dawn</style></author><author><style face="normal" font="default" size="100%">Hoehler, Tori M</style></author><author><style face="normal" font="default" size="100%">Ono, Shuhei</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Methane cycling. Nonequilibrium clumped isotope signals in microbial methane.</style></title><secondary-title><style face="normal" font="default" size="100%">Science</style></secondary-title><alt-title><style face="normal" font="default" size="100%">Science</style></alt-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Animals</style></keyword><keyword><style  face="normal" font="default" size="100%">Carbon Cycle</style></keyword><keyword><style  face="normal" font="default" size="100%">Carbon Isotopes</style></keyword><keyword><style  face="normal" font="default" size="100%">Cattle</style></keyword><keyword><style  face="normal" font="default" size="100%">Groundwater</style></keyword><keyword><style  face="normal" font="default" size="100%">Hydrogen</style></keyword><keyword><style  face="normal" font="default" size="100%">Methane</style></keyword><keyword><style  face="normal" font="default" size="100%">Methanomicrobiales</style></keyword><keyword><style  face="normal" font="default" size="100%">Temperature</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2015</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2015 Apr 24</style></date></pub-dates></dates><volume><style face="normal" font="default" size="100%">348</style></volume><pages><style face="normal" font="default" size="100%">428-31</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;Methane is a key component in the global carbon cycle, with a wide range of anthropogenic and natural sources. Although isotopic compositions of methane have traditionally aided source identification, the abundance of its multiply substituted &quot;clumped&quot; isotopologues (for example, (13)CH3D) has recently emerged as a proxy for determining methane-formation temperatures. However, the effect of biological processes on methane's clumped isotopologue signature is poorly constrained. We show that methanogenesis proceeding at relatively high rates in cattle, surface environments, and laboratory cultures exerts kinetic control on (13)CH3D abundances and results in anomalously elevated formation-temperature estimates. We demonstrate quantitatively that H2 availability accounts for this effect. Clumped methane thermometry can therefore provide constraints on the generation of methane in diverse settings, including continental serpentinization sites and ancient, deep groundwaters.&lt;/p&gt;</style></abstract><issue><style face="normal" font="default" size="100%">6233</style></issue><custom1><style face="normal" font="default" size="100%">http://www.ncbi.nlm.nih.gov/pubmed/25745067?dopt=Abstract</style></custom1></record></records></xml>