Non-oxidative CH 4 coupling is promoted by silica with incorporatedi ron sites, but the role of these sites and their speciation under reactionc onditions are poorly understood.H ere, silica-supported iron(II) single sites, prepared via surface organometallic chemistry and stable at 1020 8Ci nv acuum,a re shown to rapidlyi nitiate CH 4 coupling at 1000 8C, leading to 15-22 %h ydrocarbons selectivity at 3-4 %c onversion. During this process, iron reducesa nd forms carburized iron(0)n anoparticles. This reactivity contrasts with what is observed for (iron-free) partially dehydroxylateds ilica, that readily converts methane, albeit with low hydrocarbon selectivity and after an induction period.T his study supports that iron sites facilitate faster initiation of radical reactions and tame the surface reactivity.Non-oxidative coupling of CH 4 (NOCM) is ao ne-step methane conversionp rocess to higherh ydrocarbons( Scheme 1), which circumvents the conventionalt wo-steps ynthesis based on steam reforming and Fischer-Tropsch process. [1] NOCM is highly endothermic, requiring hight emperatures, which also thermodynamically favour the competing reaction methane decarbonization that yields H 2 and coke. [2] While oxidative coupling of CH 4 avoidst he latter process, oxidative conditions lead to the production of CO 2 ,r esultingi nl ow hydrocarbon yields. [3] Recent reports suggestedt hat highly dispersed metal sites improvet he selectivity of NOCM to hydrocarbons,o pening new opportunities. [4] Metal-exchanged zeolites, such as those based on molybdenum and iron can convert CH 4 into hydrocarbonsu nder nonoxidative conditions, whereint he interplay between Brønsted sites, the pore system, and the metals ite is crucial. [5] However, the thermali nstabilityo fz eolites limits the temperature range withinw hich they may be applied, preventing high conversions from being reached, spurring the interestt oi dentify more thermally stable oxides.F or example, am aterial prepared by melting of iron orthosilicate and quartzw as reported to produce hydrocarbons withs electivity over 99 %a t1 000 8C. [4b] This outstanding activity is ascribed to the formationof isolated Fe-sites, promoting the activation of CH 4 and yielding methyl radicals. Recent studies have reported similar outcomes, albeitw ith lower yields andt he production of ab roader spectrum of hydrocarbons, includingC 2 H 6 and C 3 ÀC 5 hydrocarbons,a long with the formation of iron carbiden anoparticles. [4c-e] These observations contrast with those relatedt o otheri ron(0) and iron oxide systemss upported on silica or alumina,a sw ell as bare supports, all of which predominately induce CH 4 decarbonization. [6] The low selectivity toward hydrocarbonsc an originate from longerc ontact times,l ow metal dispersion, and ah igh ratio of surfacea rea of the materialt o the void space in the reactor bed, all of which would favour the formationof coke. [4c, 6] These results imply that iron facilitates CH 4 activation;h owever,i ts structure and mechanistic role remain ...