Additional file 6: Table S4. of Potential for hydrogen-oxidizing chemolithoautotrophic and diazotrophic populations to initiate biofilm formation in oligotrophic, deep terrestrial subsurface waters

Extracted ATP and estimated cell numbers from the planktonic cells in the water phase as well as from the biofilms formed on garnet grains and glass beads. Values from this study presented as averages of three replicates ± SD. (PDF 78 kb

Additional file 10: Figure S5. of Potential for hydrogen-oxidizing chemolithoautotrophic and diazotrophic populations to initiate biofilm formation in oligotrophic, deep terrestrial subsurface waters

Dendrogram of alignment from all near-complete reconstructed genomes (clustered bins showing >50% of the aligned base is the same). (PDF 578 kb

Additional file 5: Table S3. of Potential for hydrogen-oxidizing chemolithoautotrophic and diazotrophic populations to initiate biofilm formation in oligotrophic, deep terrestrial subsurface waters

Sequencing information for each approved phylogenetic bin from the metagenomes. (PDF 95 kb

The effect of M-value threshold on sensitivity and specificity for detection of different degrees of probe-target mismatch: (A) ≥ 1 mismatch (B) ≥ 2 mismatches (C) ≥ 3 mismatches and (D) ≥ 4 mismatches

M-values ranging from -3.0 to -0.25 are plotted with an interval of -0.25. An M-value of <p><b>Copyright information:</b></p><p>Taken from "Performance of a 70-mer oligonucleotide microarray for genotyping of "</p><p>http://www.biomedcentral.com/1471-2180/8/73</p><p>BMC Microbiology 2008;8():73-73.</p><p>Published online 8 May 2008</p><p>PMCID:PMC2396164.</p><p></p