Natural hydrocarbons are largely formed by the thermal decomposition of organic matter (thermogenesis) or by microbial processes (bacteriogenesis). But the discovery of methane at an East Pacific Rise hydrothermal vent and in other crustal fluids supports the occurrence of an abiogenic source of hydrocarbons. These abiogenic hydrocarbons are generally formed by the reduction of carbon dioxide, a process which is thought to occur during magma cooling and-more commonly-in hydrothermal systems during water-rock interactions, for example involving Fischer-Tropsch reactions and the serpentinization of ultramafic rocks. Suggestions that abiogenic hydrocarbons make a significant contribution to economic hydrocarbon reservoirs have been difficult to resolve, in part owing to uncertainty in the carbon isotopic signatures for abiogenic versus thermogenic hydrocarbons. Here, using carbon and hydrogen isotope analyses of abiogenic methane and higher hydrocarbons in crystalline rocks of the Canadian shield, we show a clear distinction between abiogenic and thermogenic hydrocarbons. The progressive isotopic trends for the series of C1-C4 alkanes indicate that hydrocarbon formation occurs by way of polymerization of methane precursors. Given that these trends are not observed in the isotopic signatures of economic gas reservoirs, we can now rule out the presence of a globally significant abiogenic source of hydrocarbons.

[1] H 2 is probably the most important substrate for terrestrial subsurface lithoautotrophic microbial communities. Abiotic H 2 generation is an essential component of subsurface ecosystems truly independent of surface photosynthesis. Here we report that H 2 concentrations in fracture water collected from deep siliclastic and volcanic rock units in the Witwatersrand Basin, South Africa, ranged up to two molar, a value far greater than observed in shallow aquifers or marine sediments. The high H 2 concentrations are consistent with that predicted by radiolytic dissociation of H 2 O during radioactive decay of U, Th, and K in the host rock and the observed He concentrations. None of the other known H 2 -generating mechanisms can account for such high H 2 abundance either because of the positive free energy imposed by the high H 2 concentration or pH or because of the absence of required mineral phases. The radiolytic H 2 is consumed by methanogens and abiotic hydrocarbon synthesis. Our calculations indicate that radiolytic H 2 production is a ubiquitous and virtually limitless source of energy for deep crustal chemolithoautotrophic ecosystems.

No abstract

No abstract

No abstract

Equilibrium headspace analysis of toluene for δ2H isotopic composition by continuous flow compound specific isotope mass spectrometry was determined to have an accuracy and reproducibility of ±5‰. Using this analytical approach, the hydrogen isotope fractionation produced by anaerobic biodegradation of toluene was evaluated in laboratory experiments using a mixed methanogenic consortium. A large, reproducible 2H-enrichment in the residual toluene of greater than 60‰ was observed at greater than 95% degradation, reflecting the preferential biodegradation of molecules containing the light (1H) isotope. Recent studies evaluating the magnitude of carbon isotope fractionation produced during biodegradation of aromatic hydrocarbons have documented heavy isotope (13C) enrichment in the residual contaminant approximately an order of magnitude smaller than those reported here for 2H. The very large isotopic enrichment in 2H suggests that under anaerobic conditions compound specific hydrogen isotope analysis may provide a more reliable means of validating intrinsic bioremediation of aromatic hydrocarbons than stable carbon isotope analysis. Combined application of stable carbon and hydrogen isotope analysis in an anaerobic groundwater has the potential to provide two important diagnostic tools. Relatively insensitive to biodegradation by mixed consortia, stable carbon isotope values may provide information about different sources of contaminant, while hydrogen isotope values provide an assessment of the degree of attenuation due to biodegradation.

Summary. An antihuman globulin (AHG) gel centrifugation technique (AHG gel test) employing microtubes (DiaMed®) has been compared for sensitivity in detection of unexpected antibodies with a saline indirect antiglobulin test (SIAT) which uses a cell‐to‐serum ratio between 1:120 and 1:200 and provides positive reactions at a concentration of a standard anti‐D of 2 ng/mL (0·01 IU/ml) or less. For most antibodies examined the AHG gel test was slightly less sensitive than the SIAT but both methods were capable of detecting anti‐D at concentrations of 2 ng/ml or less. The importance of defining in detail the conventional tube test method used in such evaluations is emphasized since previous reports of sensitivity of the DiaMed AHG gel test indicate considerable variation in technique and comparative sensitivity.

The effects of laudanosine, a metabolite of atracurium, on the behaviour of conscious mice, rats and dogs, and on cardiovascular function in conscious and anaesthetized dogs have been evaluated: EEG studies were performed in anaesthetized dogs. In mice and rats, i.v. bolus doses of laudanosine 10-20 mg kg-1, caused convulsions and hind limb extensions; these effects were prevented by pretreatment with diazepam. After the continuous infusion of laudanosine to conscious dogs, plasma concentrations in the order of 1.2 micrograms ml-1 did not cause behavioural disturbances. In anaesthetized dogs, laudanosine plasma concentrations of more than 6 micrograms ml-1 caused hypotension and bradycardia, laudanosine concentrations greater than 10 micrograms ml-1 induced epileptic EEG spiking and plasma concentrations greater than 17 micrograms ml-1 produced prolonged seizures. There is a wide difference between laudanosine plasma concentrations in patients given atracurium by bolus injection or by short-term infusion for surgical use and those required to induce epileptic activity in dogs. However, during the prolonged infusion of atracurium to patients this difference will be decreased. It is unlikely that the use of atracurium, in patients, would result in plasma concentrations of laudanosine capable of producing neurological or cardiovascular disturbances.