@article {1737, title = {Methane cycling. Nonequilibrium clumped isotope signals in microbial methane.}, journal = {Science}, volume = {348}, year = {2015}, month = {2015 Apr 24}, pages = {428-31}, abstract = {

Methane is a key component in the global carbon cycle, with a wide range of anthropogenic and natural sources. Although isotopic compositions of methane have traditionally aided source identification, the abundance of its multiply substituted "clumped" isotopologues (for example, (13)CH3D) has recently emerged as a proxy for determining methane-formation temperatures. However, the effect of biological processes on methane{\textquoteright}s clumped isotopologue signature is poorly constrained. We show that methanogenesis proceeding at relatively high rates in cattle, surface environments, and laboratory cultures exerts kinetic control on (13)CH3D abundances and results in anomalously elevated formation-temperature estimates. We demonstrate quantitatively that H2 availability accounts for this effect. Clumped methane thermometry can therefore provide constraints on the generation of methane in diverse settings, including continental serpentinization sites and ancient, deep groundwaters.

}, keywords = {Animals, Carbon Cycle, Carbon Isotopes, Cattle, Groundwater, Hydrogen, Methane, Methanomicrobiales, Temperature}, issn = {1095-9203}, doi = {10.1126/science.aaa4326}, author = {Wang, David T and Gruen, Danielle S and Lollar, Barbara Sherwood and Hinrichs, Kai-Uwe and Stewart, Lucy C and Holden, James F and Hristov, Alexander N and Pohlman, John W and Morrill, Penny L and K{\"o}nneke, Martin and Delwiche, Kyle B and Reeves, Eoghan P and Sutcliffe, Chelsea N and Ritter, Daniel J and Seewald, Jeffrey S and McIntosh, Jennifer C and Hemond, Harold F and Kubo, Michael D and Cardace, Dawn and Hoehler, Tori M and Ono, Shuhei} } @article {1206, title = {Hydrogen-limited growth of hyperthermophilic methanogens at deep-sea hydrothermal vents.}, journal = {Proc Natl Acad Sci U S A}, volume = {109}, year = {2012}, month = {2012 Aug 21}, pages = {13674-9}, abstract = {

Microbial productivity at hydrothermal vents is among the highest found anywhere in the deep ocean, but constraints on microbial growth and metabolism at vents are lacking. We used a combination of cultivation, molecular, and geochemical tools to verify pure culture H(2) threshold measurements for hyperthermophilic methanogenesis in low-temperature hydrothermal fluids from Axial Volcano and Endeavour Segment in the northeastern Pacific Ocean. Two Methanocaldococcus strains from Axial and Methanocaldococcus jannaschii showed similar Monod growth kinetics when grown in a bioreactor at varying H(2) concentrations. Their H(2) half-saturation value was 66 μM, and growth ceased below 17-23 μM H(2), 10-fold lower than previously predicted. By comparison, measured H(2) and CH(4) concentrations in fluids suggest that there was generally sufficient H(2) for Methanocaldococcus growth at Axial but not at Endeavour. Fluids from one vent at Axial (Marker 113) had anomalously high CH(4) concentrations and contained various thermal classes of methanogens based on cultivation and mcrA/mrtA analyses. At Endeavour, methanogens were largely undetectable in fluid samples based on cultivation and molecular screens, although abundances of hyperthermophilic heterotrophs were relatively high. Where present, Methanocaldococcus genes were the predominant mcrA/mrtA sequences recovered and comprised \~{}0.2-6\% of the total archaeal community. Field and coculture data suggest that H(2) limitation may be partly ameliorated by H(2) syntrophy with hyperthermophilic heterotrophs. These data support our estimated H(2) threshold for hyperthermophilic methanogenesis at vents and highlight the need for coupled laboratory and field measurements to constrain microbial distribution and biogeochemical impacts in the deep sea.

}, keywords = {Archaea, Biodiversity, Coculture Techniques, DNA, Ribosomal, Ecosystem, Gases, Geography, Hydrogen, Hydrothermal Vents, Kinetics, Methane, Molecular Sequence Data, Temperature, Time Factors, Water Microbiology}, issn = {1091-6490}, doi = {10.1073/pnas.1206632109}, author = {Ver Eecke, Helene C and Butterfield, David A and Huber, Julie A and Lilley, Marvin D and Olson, Eric J and Roe, Kevin K and Evans, Leigh J and Merkel, Alexandr Y and Cantin, Holly V and Holden, James F} } @article {1212, title = {Characterization of malate dehydrogenase from the hyperthermophilic archaeon Pyrobaculum islandicum.}, journal = {Extremophiles}, volume = {11}, year = {2007}, month = {2007 Sep}, pages = {741-6}, abstract = {

Native and recombinant malate dehydrogenase (MDH) was characterized from the hyperthermophilic, facultatively autotrophic archaeon Pyrobaculum islandicum. The enzyme is a homotetramer with a subunit mass of 33 kDa. The activity kinetics of the native and recombinant proteins are the same. The apparent K ( m ) values of the recombinant protein for oxaloacetate (OAA) and NADH (at 80 degrees C and pH 8.0) were 15 and 86 microM, respectively, with specific activity as high as 470 U mg(-1). Activity decreased more than 90\% when NADPH was used. The catalytic efficiency of OAA reduction by P. islandicum MDH using NADH was significantly higher than that reported for any other archaeal MDH. Unlike other archaeal MDHs, specific activity of the P. islandicum MDH back-reaction also decreased more than 90\% when malate and NAD(+) were used as substrates and was not detected with NADP(+). A phylogenetic tree of 31 archaeal MDHs shows that they fall into 5 distinct groups separated largely along taxonomic lines suggesting minimal lateral mdh transfer between Archaea.

}, keywords = {Citric Acid Cycle, Hydrogen-Ion Concentration, Kinetics, Malate Dehydrogenase, Malates, Molecular Weight, NAD, NADP, Oxaloacetic Acid, Phylogeny, Protein Conformation, Protein Subunits, Pyrobaculum, Recombinant Proteins, Sequence Analysis, Protein, Substrate Specificity, Temperature}, issn = {1431-0651}, doi = {10.1007/s00792-007-0081-2}, author = {Yennaco, Lynda J and Hu, Yajing and Holden, James F} } @article {1216, title = {Microbe-metal interactions in marine hydrothermal environments.}, journal = {Curr Opin Chem Biol}, volume = {7}, year = {2003}, month = {2003 Apr}, pages = {160-5}, abstract = {

Marine hydrothermal microorganisms respond rapidly to changes in the concentrations and availability of metals within their environment. Hyperthermophilic archaea appear to possess novel mechanisms for metal detoxification, dissimilatory metal reduction and metal assimilation that may be absent in their mesophilic and bacterial counterparts. For example, tungsten was found in high concentrations in a hydrothermal sulfide deposit where hyperthermophiles were also most abundant, consistent with the unique requirement of these organisms for this element. Furthermore, newly isolated genera of iron-reducing hyperthermophiles expand the scope of carbon cycling in hydrothermal environments. The advent of genome sequences and new molecular techniques will facilitate our further understanding of microbe-mineral interactions in these environments.

}, keywords = {Archaea, Bacteria, Environment, Marine Biology, Metals, Seawater, Temperature}, issn = {1367-5931}, author = {Holden, James F and Adams, Michael W W} }