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\subsection{Phylogeneitic affiliation of $^{13}$C-cellulose and $^{13}$C-xylose -responsive microorganisms}  % Fakesubsubsection:\textit{Verrucomicrobia} are ubiquitous in soil  \textit{Verrucomicrobia} are ubiquitous in cosmopolitan  soil worldwide  \citep{Bergmann_2011}. \textit{Verrucomicrobia} microbes \citep{Bergmann_2011}  and  can comprise up to 23\% of 16S rRNA gene sequences in high-throughput DNA sequencing surveys of  SSU rRNA genes in soil \citep{Bergmann_2011} and represent as high as  9.8\% of soil 16S rRNA \citep{Buckley_2001}. Many \textit{Verrucomicrobia}  cultivars have been established were first isolated  in the last decade \cite{Wertz_2011} but only one of the 15 most abundant verrucomicrobial phylotypes in a global  soil sample collection shared greater than 93\% sequence identity with an  cultured  isolate \citep{Bergmann_2011}. Genomic analyses and physiological profiling of \textit{Verrucomicrobia} isolates revealed \texit{Verrucomicrobia}  are capable of  methanotrophy and diazotrophy \citep{Wertz_2011}within \textit{Verrucomicrobia} (CITE  and reviewed by \citet{Wertz_2011}). \citet{Wertz_2011}.  \textit{Verrucomicrobia} cultivars degrade cellulose in culture and select  \textit{Verrucomicrobia} genomes possess the genes necessary to degrade cellulose \citep{Otsuka_2012, Wertz_2011}.  Although, we have learned many functional roles of  \textit{Verrucomicrobia} in the environment, the The  function and or global significance of soil \textit{Verrucomicrobia} in global C-cycling is  unknown. unknown, however.  For example, only one of the putative verrucomicrobial cellulose degraders identified in this experiment is closely related to a named  cultivar (OTU.XX, Table~\ref{tab:cell}) and only XX\% of all  verrucomicrobial OTUs found in this study share at least 97\% sequence 

distributed soil samples \citep{Bergmann_2011}. \textit{Verrucomicrobia}  lineages particularly \textit{Spartobacteria}, given their ubiquity and  abundance in soil as well as their demonstrated incorporation of $^{13}$C from  $^{13}$C-cellulose, may be decomposing contributos to  cellulose in soil worldwide. decomposition on a   global scale.  % Fakesubsubsection:Soil \textit{Chloroflexi} have been found to assimilate  Soil \textit{Chloroflexi} have been found to assimilate cellulose before in  DNA-SIP studies with $^{13}$C-cellulose \citep{Schellenberger_2010}. Previously  identified \textit{Chloroflexi} $^{13}$C-cellulose-responders weresimilarly  underrepresented in culture collections as the \citep{Schellenberger_2010}.  The  \textit{Chloroflexi} identified as cellulose degraders in this study \citep{Schellenberger_2010}. are also only distantly related to  isolates (TABLE XX).  Chloroflexi are among the six most abundant soil phyla commonly recovered from  soil microbial diversity surveys CITE. Chloroflexi are typically not as as  abundant as \textit{Verrucomicrobia}, XX, and XX but have similar abundance as 

the SSU rRNA gene sequences from this study share at most XX\% sequence  identity with the type strain for the \textit{Herpetosiphon} genus (\textit{H.  geysericola} CHECK SPELLING). \textit{H. geysericola} is a predatory bacterium  shown to prey upon XX in culture. In our study study,  "Herpetosiphon" $^{13}$C-cellulose responders did not show a delayed response to  $^{13}$C-cellulose as compared to other responders but nonetheless could have  become labeled by feeding on primary $^{13}$C-cellulose degraders. The prey  specificity of predatory bacteria is not well established especially \textit{in  situ}. $^{13}$C-labelingby as  would be positively correlated with prey specificity. If the predator specifically preyed upon one population then it  could take on the same labeling \% as that population. Preying on multiple  types would produce a mixed and potentially diluted labeling signature if some  of the prey populations were unlabeled. not isotopically labeled.  % Fakesubsubsection:\textit{Acidobacteria} did not incorporate $^{13}$C  We also observed $^{13}$C-incorporation from cellulose from \textit{Proteobacteria}, \textit{Planctomycetes} and \textit{Bacteroidetes}.  

earliest assimilated C will be converted into biomass. Leftover labile C and  new biomass C is assimilated by slower growing \textit{Actinobacteria},  \textit{Proteobacteria} and \textit{Bacteroidetes} types that are tuned to  lower C substrate concentrations, are  predatory bacteria (e.g. \textit{Agromyces}) \textit{Agromyces}),  and/or are  specialized for consuming viral lysate. Polymeric C is likely assimilated by fungal cellulose degraders before bacterial degraders but the  differences in fungal and bacterial soil C assimilation are outside the scope  of this study. Polymeric C enters the bacterial community after several weeks.  Canonical cellulose degrading bacteria such as \textit{Cellvibrio} are major  cellulose degraders but uncharacterized lineages in the \textit{Chloroflexi}  and \textit{Verrucomicrobia}, specifically the \textit{Spartobacteria} \textit{Spartobacteria},  are significant contributors to soil  cellulose decomposition. C originally from polymeric substrates may also enter the bacterial community via predatory  actions of lineages that specifically prey upon cellulose degraders that are  perhaps members of the \textit{Herpetosiphon} genus although it is not known at  this time the scale, relative contibution,  if it exists, any,  of the this  predatory action. The assimilation of C from polymeric substrates precipitates a smaller trophic cascade because  polymeric C degraders exhibit lower growth efficiency than their labile C  degrading counterparts. counterparts and thus less assimilated C is converted into biomass that  can move higher tropic levels.  \subsection{DNA-SIP methods considerations}  % Fakesubsubsection:We found that control gradients yield amplifiable  We found that control gradients yield amplifiable DNA well into the heavy