Characterization of active members in C and N cycles in the subsurface environment of the Witwatersrand Basin

Fracture fluid from various depths and locations in Beatrix gold mine (Gold Fields Ltd.), located in the Welkom region on the 2.9 Ga Witwatersrand Basin of South Africa has been previously studied. Research has shown differential geochemistry data and distinctive community structure which varies from the dominance of different Proteobacterial classes in waters with paleometeoric 18O and 2H signatures including methanotrophs to one dominated by Firmicutes including Candidatus Desulforudis audaxviator-like taxa, which are associated with more saline waters with high concentrations of dissolved H2, hydrocarbons from water-rock reaction and 18O and 2H signatures above the Global Meteoric Water Line. Archaea seem to be a minority and all are euryarchaeota including methanogenic genera. The question is:Which of them are actively driving the subsurface C and N cycles? At shaft 3 on level 26, 1.3 kmbls, fracture water from 42 m behind the tunnel wall located in the Main quartzite formation was collected and analyzed. The temperature, pH, Eh, dissolved O2 and salinity of this hydrocarbon-containing fracture water ranged from 35 to 38°C, 8.2 to 8.8, -30 to -100 mV, 0.3 to 30 μM and 4.2 to 4.3 ppt, respectively. Gas comprised 60% CH4 and 20% N2. The same fracture formerly yielded Halicephalobus mephisto, the first reported subsurface nematode. Microorganisms were captured on filters in two field seasons. Defined by 16S rDNA, 2011 January sample contains β-Proteobacteria (50%), Firmicutes (39%) and α- and γ-Proteobacteria (7%). Of the Firmicutes, 90% were represented by Ca. D. audaxviator. All archaea detected are closestly related to sequences also reported from South African gold mines, with Crenarchaeota accounting for 77% of the clones. Prospective methane-oxidation and production were assessed by amplifying genes encoding for particulate methane monooxygenase alpha subunit (pmoA) and methyl-coenzyme M reductase alpha subunit (mcrA). PmoA genes of Type II methanotrophs were found three times more than Type I methanotrophs. A pmoA gene sequence represents 42% of the library matches only and is identical to a putative protein sequence annotated on Ca. D. audaxviator genome, but further analysis is required to validate its candidature of methanotrophy. The cluster of mcrA gene sequences is related to a novel group of anaerobic methanotrophs (ANME) defined by environmental sequences. 2011 July samples from the same borehole revealed an absence of Firmicutes. Two β-Proteobacterial sequences dominated the bacterial 16S rDNA clone library, accounting for 54% and 25%. The first 16S rRNA clone library for the region confirmed a complete lack of Firmicutes with active Proteobacteria (71% α-, 17% β- and 6% γ-Proteobacteria). Only 3% of the active community is confidently inferred as methylotrophs while 22% belongs to N2 fixer Rhizobium sp. which has been demonstrated to stimulate methanotrophic growth and 28% is related to Polymorphum gilvum, which is known for n-alkane degradation. Active members responsible for CH4 metabolism will be supported by presenting the results of archaeal 16S rRNA, pmoA, mcrA and nitrogenase gene diversities. The lack of Firmicutes in July samples could be attributed to collection methods: different filter membrane, faster flowrate but shorter sampling duration, and less total volume of water filtered.