2014
DOI: 10.3389/fmicb.2014.00610
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Chemolithotrophy in the continental deep subsurface: Sanford Underground Research Facility (SURF), USA

Abstract: The deep subsurface is an enormous repository of microbial life. However, the metabolic capabilities of these microorganisms and the degree to which they are dependent on surface processes are largely unknown. Due to the logistical difficulty of sampling and inherent heterogeneity, the microbial populations of the terrestrial subsurface are poorly characterized. In an effort to better understand the biogeochemistry of deep terrestrial habitats, we evaluate the energetic yield of chemolithotrophic metabolisms a… Show more

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Cited by 106 publications
(187 citation statements)
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References 44 publications
(58 reference statements)
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“…Geochemical measurements were made either on site, or upon return to the laboratory (Osburn et al, 2014). In this study, we examined deep fracture fluids from legacy boreholes drilled ∼1.5 kilometers below surface (kmbs), accessing a deeply circulating terrestrial aquifer.…”
Section: Methodsmentioning
confidence: 99%
“…Geochemical measurements were made either on site, or upon return to the laboratory (Osburn et al, 2014). In this study, we examined deep fracture fluids from legacy boreholes drilled ∼1.5 kilometers below surface (kmbs), accessing a deeply circulating terrestrial aquifer.…”
Section: Methodsmentioning
confidence: 99%
“…The metabolic capability of the predominant sulfur-driven autotrophic denitrifiers drives the links between the N, S, and C cycles. Previous studies have reported the high energetic potential of S-N reactions in other deep continental sites (50), and expression of mRNA coding for nitrate reductase in marine subseafloor sediment cores where NO 3 − was not detectable (51), indicating that the role of nitrate reduction and/or denitrification in the deep subsurface has been overlooked. Active subsurface metabolic landscapes that intertwine H 2 -driven processes, S-N coupling, and dissimilatory NO 3 -dependent reactions may be more prevalent in both continental and marine subsurface systems than previously thought.…”
Section: Concluding Remarkmentioning
confidence: 99%
“…Biodiversity (BHSU) Microbiology Surface, 300L, [45,46,47] 2000L, 4100L, 4550L, 4850L Biofuels (SDSMT) Biofuels 4550L, 4850L, [48,49,50,51], 5000L [52,53,54,55] Lignocellulose (SDSU) Biofuels 1700L, 4850L [56,57] Syngas (SDSMT) Biofuels 4850L [58,59,60] Life UndergroundWater in drill holes, Surface, 800L, [61] NASA Astrobiology Institute geomicrobiology 4850L Engineering Xilinx, Inc. Chip error testing 4850L The LUX collaboration published results in October 2013 from their first underground data run [23] and started a longer run (nominally 300 live days) in October 2014. LUX is expecting to complete their experimental program in 2016.…”
Section: Biologymentioning
confidence: 99%