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. 2016 Aug 9;6:31312. doi: 10.1038/srep31312

Table 2. Identity of the 5 most abundant OTUs (based on 16S rRNA sequences) for each valley following the lowest taxonomic level of the SILVA modified database52.

Number of reads OTU Valley SILVA taxonomy % identity Accession number Genbank taxonomy Isolation source
68710 1 KWK (22%) Methanoregula 100 GU224062 uncultured archaeon lake water
BGR (14%)
SAS (11%)
44091 2 SAS (12%) Methanosaeta 100 LN626810 uncultured archaeon Marine bioreactor
KWK (8%)
BGR (6%)
24882 1324 KWK (8%) Methanoregula 99 JN397914 uncultured archaeon spring pit
SAS (3%)
22248 7 KWK (10%) MEG 97 GU127467 uncultured archaeon reservoir anoxic water
BGR (9%)
20494 111 BGR (14%) MEG 98 AY294414 uncultured archaeon hydrocarbon-contaminated aquifer
19308 362 SAS (4%) Methanoregula 98 KJ955705 uncultured Methanoregula hydrocarbon-contaminated sediment
17934 9 BGR (8%) Euryarchaeota 90 AB019748 uncultured archaeon deep-sea hydrothermal vent
10585 1255 SAS (3%) Methanoregula 98 JF304133 uncultured archaeon outfall sediment
9430 11 KWK (6%) Thermoplasmatales 93 EU910624 uncultured euryarchaeote sediment

OTU refers to the taxon identity numbers in Fig. 3. The groups Euryarchaeota, Miscellaneous Euryarchaeotic Group (MEG) and Thermoplasmatales could not be further assigned. Percent (%) is the proportion of each OTU expressed as a percentage of the total 16S rRNA reads for the archaeal communities in each valley.