86Kr excess and other noble gases identify a billion-year-old radiogenically-enriched groundwater system.

Deep within the Precambrian basement rocks of the Earth, groundwaters can sustain subsurface microbial communities, and are targets of investigation both for geologic storage of carbon and/or nuclear waste, and for new reservoirs of rapidly depleting resources of helium. Noble gas-derived residence times have revealed deep hydrological settings where groundwaters are preserved on millions to billion-year timescales. Here we report groundwaters enriched in the highest concentrations of radiogenic products yet discovered in fluids, with an associated 86Kr excess in the free fluid, and residence times >1 billion years. This brine, from a South African gold mine 3 km below surface, demonstrates that ancient groundwaters preserved in the deep continental crust on billion-year geologic timescales may be more widespread than previously understood. The findings have implications beyond Earth, where on rocky planets such as Mars, subsurface water may persist on long timescales despite surface conditions that no longer provide a habitable zone.

Rapid microbial methanogenesis during CO2 storage in hydrocarbon reservoirs.

Carbon capture and storage (CCS) is a key technology to mitigate the environmental impact of carbon dioxide (CO2) emissions. An understanding of the potential trapping and storage mechanisms is required to provide confidence in safe and secure CO2 geological sequestration1,2. Depleted hydrocarbon reservoirs have substantial CO2 storage potential1,3, and numerous hydrocarbon reservoirs have undergone CO2 injection as a means of enhanced oil recovery (CO2-EOR), providing an opportunity to evaluate the (bio)geochemical behaviour of injected carbon. Here we present noble gas, stable isotope, clumped isotope and gene-sequencing analyses from a CO2-EOR project in the Olla Field (Louisiana, USA). We show that microbial methanogenesis converted as much as 13-19% of the injected CO2 to methane (CH4) and up to an additional 74% of CO2 was dissolved in the groundwater. We calculate an in situ microbial methanogenesis rate from within a natural system of 73-109 millimoles of CH4 per cubic metre (standard temperature and pressure) per year for the Olla Field. Similar geochemical trends in both injected and natural CO2 fields suggest that microbial methanogenesis may be an important subsurface sink of CO2 globally. For CO2 sequestration sites within the environmental window for microbial methanogenesis, conversion to CH4 should be considered in site selection.

Earth-like Habitable Environments in the Subsurface of Mars.

In Earth's deep continental subsurface, where groundwaters are often isolated for >106 to 109 years, energy released by radionuclides within rock produces oxidants and reductants that drive metabolisms of non-photosynthetic microorganisms. Similar processes could support past and present life in the martian subsurface. Sulfate-reducing microorganisms are common in Earth's deep subsurface, often using hydrogen derived directly from radiolysis of pore water and sulfate derived from oxidation of rock-matrix-hosted sulfides by radiolytically derived oxidants. Radiolysis thus produces redox energy to support a deep biosphere in groundwaters isolated from surface substrate input for millions to billions of years on Earth. Here, we demonstrate that radiolysis by itself could produce sufficient redox energy to sustain a habitable environment in the subsurface of present-day Mars, one in which Earth-like microorganisms could survive wherever groundwater exists. We show that the source localities for many martian meteorites are capable of producing sufficient redox nutrients to sustain up to millions of sulfate-reducing microbial cells per kilogram rock via radiolysis alone, comparable to cell densities observed in many regions of Earth's deep subsurface. Additionally, we calculate variability in supportable sulfate-reducing cell densities between the martian meteorite source regions. Our results demonstrate that martian subsurface groundwaters, where present, would largely be habitable for sulfate-reducing bacteria from a redox energy perspective via radiolysis alone. We present evidence for crustal regions that could support especially high cell densities, including zones with high sulfide concentrations, which could be targeted by future subsurface exploration missions.

Hydrothermal 15N15N abundances constrain the origins of mantle nitrogen.

Nitrogen is the main constituent of the Earth's atmosphere, but its provenance in the Earth's mantle remains uncertain. The relative contribution of primordial nitrogen inherited during the Earth's accretion versus that subducted from the Earth's surface is unclear1-6. Here we show that the mantle may have retained remnants of such primordial nitrogen. We use the rare 15N15N isotopologue of N2 as a new tracer of air contamination in volcanic gas effusions. By constraining air contamination in gases from Iceland, Eifel (Germany) and Yellowstone (USA), we derive estimates of mantle δ15N (the fractional difference in 15N/14N from air), N2/36Ar and N2/3He. Our results show that negative δ15N values observed in gases, previously regarded as indicating a mantle origin for nitrogen7-10, in fact represent dominantly air-derived N2 that experienced 15N/14N fractionation in hydrothermal systems. Using two-component mixing models to correct for this effect, the 15N15N data allow extrapolations that characterize mantle endmember δ15N, N2/36Ar and N2/3He values. We show that the Eifel region has slightly increased δ15N and N2/36Ar values relative to estimates for the convective mantle provided by mid-ocean-ridge basalts11, consistent with subducted nitrogen being added to the mantle source. In contrast, we find that whereas the Yellowstone plume has δ15N values substantially greater than that of the convective mantle, resembling surface components12-15, its N2/36Ar and N2/3He ratios are indistinguishable from those of the convective mantle. This observation raises the possibility that the plume hosts a primordial component. We provide a test of the subduction hypothesis with a two-box model, describing the evolution of mantle and surface nitrogen through geological time. We show that the effect of subduction on the deep nitrogen cycle may be less important than has been suggested by previous investigations. We propose instead that high mid-ocean-ridge basalt and plume δ15N values may both be dominantly primordial features.

Bilirubin does not modulate ionotropic glutamate receptors or glutamate transporters.

Bilirubin, a product of haemoglobin metabolism, has been suggested to damage neurons by increasing activation of N-methyl-D-aspartate (NMDA) receptors when it reaches high levels in the blood [15,19], as occurs in neonatal jaundice [7]. Bilirubin is also generated in the brain following synthesis of the messenger carbon monoxide (CO) by haem oxygenase, and haem oxygenase is upregulated in Alzheimer's disease [23]. We examined the effect of bilirubin on currents generated by NMDA and alpha-amino-3-hydroxy-5-methyl-4-isoxazole propionate (AMPA) receptors in hippocampal pyramidal cells, and on glutamate transporter currents in retinal glial cells. Bilirubin did not modulate either receptor-gated currents or transporter currents. These data show the negative, but important result that bilirubin does not induce neuronal death by acting directly on NMDA or AMPA receptors, nor indirectly by blocking glutamate uptake and raising the extracellular concentration of glutamate.

Modulation of extracellular glutamate concentration in rat brain slices by cystine-glutamate exchange.

1. The role of cystine-glutamate exchange in controlling the extracellular glutamate concentration in the central nervous system was examined by whole-cell clamping neurons in rat brain slices, and using their glutamate receptors as sensors of extracellular glutamate concentration. 2. Applying cystine to cerebellar slices generated a membrane current in Purkinje cells which was abolished by glutamate receptor blockers. Similar cystine-evoked currents were seen in pyramidal cells of frontal cortex slices. 3. Control experiments on non-N-methyl-D-aspartate (non-NMDA) receptors in enzymatically isolated Purkinje cells showed that cystine did not produce a current in slice Purkinje cells by directly activating glutamate receptors, nor by potentiating the action of background levels of glutamate on receptors. Experiments on isolated salamander Muller cells showed that cystine did not block Na+-dependent GLAST glutamate transporters (homologous to the transporters in the Bergmann glia ensheathing the Purkinje cells), nor did it block the current produced by EAAT4 and EAAC1 glutamate transporters in Purkinje cells. Thus the cystine-evoked current in Purkinje cells is not due to a rise in extracellular glutamate concentration caused by block of Na+-dependent uptake. 4. The dependence of cystine-evoked current on cystine concentration in slice Purkinje cells could be fitted by a Michaelis-Menten relation with a Km of 250 microM. The Km predicted from this for cystine activating glutamate efflux is less than 140 microM, because of the non-linear dependence on glutamate concentration of the Purkinje cell current. The current evoked by 1 mM cystine was little affected by removal of extracellular chloride or addition of 1 mM furosemide (frusemide), but was potentiated by 1 mM 4,4'-diisothiocyanatostilbene-2, 2'-disulfonic acid (DIDS). 5. These data suggest that external cystine generates a current in slice Purkinje cells by activating cystine-glutamate exchange in cells of the slice, releasing glutamate which activates non-NMDA receptors in the Purkinje cell membrane.

Stoichiometry of the glial glutamate transporter GLT-1 expressed inducibly in a Chinese hamster ovary cell line selected for low endogenous Na+-dependent glutamate uptake.

Glutamate transport across the plasma membrane of neurons and glia is powered by the transmembrane electrochemical gradients for sodium, potassium, and pH, but there is controversy over the number of Na+ cotransported with glutamate. The stoichiometry of glutamate transporters is important because it determines a lower limit to the extracellular glutamate concentration, [glu]o, in both normal and pathological conditions. We used whole-cell clamping to study the stoichiometry of the glial transporter GLT-1, the most abundant glutamate transporter in the brain, expressed under control of the Tet-On system in a Chinese hamster ovary (CHO) cell line selected for low endogenous glutamate transport. After the induction of GLT-1 expression with doxycycline, glutamate evoked a Na+-dependent inward current with the voltage dependence and pharmacology of GLT-1 and acidified the cell cytoplasm. Raising [K+]o around cells clamped with electrodes containing sodium and glutamate evoked an outward reversed uptake current. These responses were reduced by the specific GLT-1 blocker dihydrokainate (DHK). DHK evoked an outward current with NO3-, but not with Cl-, as the main intracellular anion, suggesting that the anion conductance of the transporter is active even without external glutamate but generates little current in the absence of highly permeable anions like NO3-. Measuring the reversal potential of the transporter current in various ionic conditions suggested that the transport of one glutamate anion is coupled to the cotransport of three Na+ and one H+ and to the countertransport of one K+. This suggests that in ischemia, when [K+]o rises to 60 mM, the reversal of glutamate transporters will raise [glu]o to >50 microM.