Hydrogen-Limited Growth of Hyperthermophilic Methanogens at Deep-Sea Hydrothermal Vents

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Hydrogen-Limited Growth of Hyperthermophilic Methanogens at Deep-Sea Hydrothermal Vents Hydrogen-limited growth of hyperthermophilic methanogens at deep-sea hydrothermal vents Helene C. Ver Eeckea, David A. Butterfieldb, Julie A. Huberc, Marvin D. Lilleyd, Eric J. Olsond, Kevin K. Roeb, Leigh J. Evanse, Alexandr Y. Merkelf, Holly V. Cantinc, and James F. Holdena,1 aDepartment of Microbiology, University of Massachusetts, Amherst, MA 01003; bJoint Institute for the Study of the Atmosphere and Ocean and dSchool of Oceanography, University of Washington, Seattle, WA 98195; cJosephine Bay Paul Center, Marine Biological Laboratory, Woods Hole, MA 02543; eCooperative Institute for Marine Resources Studies, Oregon State University, Newport, OR 97365; and fWinogradsky Institute of Microbiology, Russian Academy of Sciences, Moscow 117312, Russia Edited by David M. Karl, University of Hawaii, Honolulu, HI, and approved June 29, 2012 (received for review April 21, 2012) Microbial productivity at hydrothermal vents is among the highest Deep-sea hydrothermal vents are among the most productive found anywhere in the deep ocean, but constraints on microbial regions within igneous ocean crust and provide a starting point growth and metabolism at vents are lacking. We used a combina- for modeling subseafloor microbial processes associated with tion of cultivation, molecular, and geochemical tools to verify pure hydrothermal circulation in basalt. Thermophilic and hyperther- culture H2 threshold measurements for hyperthermophilic metha- mophilic methanogens belonging to the order Methanococcales nogenesis in low-temperature hydrothermal fluids from Axial Vol- are commonly found autotrophs in vent environments (14–21). fi cano and Endeavour Segment in the northeastern Paci c Ocean. These organisms anaerobically convert H2 and CO2 into biomass, Two Methanocaldococcus strains from Axial and Methanocaldo- CH4 and H2O. Limited data suggest that the abundances of coccus jannaschii showed similar Monod growth kinetics when methanogens and the extent of methanogenic fluid chemistry al- grown in a bioreactor at varying H2 concentrations. Their H2 teration are elevated in ultramafic vent sites, where serpentini- μ – half-saturation value was 66 M, and growth ceased below 17 zation leads to high H concentrations (16, 19–21), and at volcanic μ 2 23 MH2, 10-fold lower than previously predicted. By comparison, eruption sites, where posteruption H is also more abundant (14, fl 2 measured H2 and CH4 concentrations in uids suggest that there – fl fi Methanocaldococcus 22 25). In contrast, methanogen abundances and uid alterations was generally suf cient H2 for growth at are often low to undetectable in other midocean ridge and vol- Axial but not at Endeavour. Fluids from one vent at Axial (Marker canic arc hydrothermal systems, where H concentrations are also 113) had anomalously high CH concentrations and contained 2 4 relatively low (20, 26–29). This pattern of H -limited methano- various thermal classes of methanogens based on cultivation 2 genesis generally fits those predicted in bioenergetic models (11, and mcrA/mrtA analyses. At Endeavour, methanogens were largely undetectable in fluid samples based on cultivation and 13), but the temperature-dependent maintenance energy data molecular screens, although abundances of hyperthermophilic het- used for these models lack data for methanogenesis and all other erotrophs were relatively high. Where present, Methanocaldococ- anaerobic metabolisms above 65 °C (30). Without empirically cus genes were the predominant mcrA/mrtA sequences recovered determined growth kinetic constraints, H2 availability cannot be fi and comprised ∼0.2–6% of the total archaeal community. Field shown de nitively to be a key factor driving methanogen abun- and coculture data suggest that H2 limitation may be partly ame- dance and distribution at thermophilic growth temperatures in liorated by H2 syntrophy with hyperthermophilic heterotrophs. vent systems. The purposes of this study were to define the Monod growth These data support our estimated H2 threshold for hyperthermo- philic methanogenesis at vents and highlight the need for coupled kinetics on H2 and minimum H2 concentrations required for laboratory and field measurements to constrain microbial distribu- the growth of Methanocaldococcus jannaschii and two Meth- tion and biogeochemical impacts in the deep sea. anocaldococcus species isolated from deep-sea hydrothermal vents at Axial Volcano, strains JH146 and JH123. Sequencing t is estimated that perhaps a third [56–90 petagrams (Pg)] of and quantitative PCR (qPCR) analysis were used to determine fi Ithe Earth’s total bacterial and archaeal carbon (106–333 Pg) the diversity and abundance of methanogen-speci c methyl exists within marine subsurface sediments (1–3). These global coenzyme M reductase (mcrA) genes in low-temperature vent estimates do not include microbial carbon in igneous ocean fluids from Axial Volcano and nearby Endeavour Segment. The crust, wherein an additional 200 Pg of carbon has been proposed abundances of thermophilic and hyperthermophilic metha- to exist primarily within its porous extrusive layer (layer 2A), nogens and hyperthermophilic heterotrophs were determined where hydrothermal fluids circulate through basalt as old as 65 using culture-dependent techniques from the same fluids. Fi- Ma (4). Therefore, microbes in marine sediments and ocean nally, these data were correlated with fluid geochemistry from crust have the potential to have a significant impact on bio- the two sites, as well as with methanogen abundance and geo- geochemical fluxes and carbon cycles in the deep ocean. Meth- chemical data from vent sites worldwide, to link our predictions anogenesis and sulfate reduction are often the predominant of high-temperature methanogenesis with in situ measurements. anaerobic microbial processes in many deep subsurface marine sediments, especially near continental margins (5, 6), and methanogens and sulfate reducers are also frequently found in Author contributions: H.C.V., D.A.B., J.A.H., and J.F.H. designed research; H.C.V., D.A.B., J.A.H., deep subsurface terrestrial basalts (7–9). However, models of E.J.O., K.K.R., L.J.E., A.Y.M., H.V.C., and J.F.H. performed research; H.C.V., D.A.B., J.A.H., the rates and constraints of various aerobic and anaerobic M.D.L., and J.F.H. analyzed data; and H.C.V., D.A.B., J.A.H., and J.F.H. wrote the paper. biogeochemical processes in deep subsurface environments, The authors declare no conflict of interest. especially within hard rock, are nascent because of these envi- This article is a PNAS Direct Submission. ronments being difficult to access. This has generated interest Freely available online through the PNAS open access option. in quantitatively modeling habitability and biogeochemical Data deposition: The sequences reported in this paper have been deposited in the Gen- processes within the deep subsurface using bioenergetic pre- Bank database (accession nos. HQ635140–HQ635763). dictions of microbial metabolism, based on the supply of geo- 1To whom correspondence should be addressed. E-mail: [email protected]. chemical energy and the metabolic energy demand of the This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10. organisms (10–13). 1073/pnas.1206632109/-/DCSupplemental. 13674–13679 | PNAS | August 21, 2012 | vol. 109 | no. 34 www.pnas.org/cgi/doi/10.1073/pnas.1206632109 Downloaded by guest on September 24, 2021 Results and Discussion decreasing H2 concentrations (Fig. 1 and Fig. S1). The minimum Growth Kinetics and H Limitation of Methanocaldococcus spp. Three H2 concentration for the growth of M. jannaschii was between 17 2 μ μ hyperthermophilic Methanocaldococcus species were grown in M and 23 M (Fig. 1A), whereas the minimum concentration B a gas flow-controlled bioreactor at either 82 °C or 70 °C to de- for strains JH146 (Fig. 1 ) and JH123 (Fig. S1) was between 10 μM and 17 μM. Statistically, there was no difference in the termine the effect of H2 concentration on growth. Two of the fi H2-dependent Monod growth kinetic parameters, namely, the organisms (JH146 and JH123) had been puri ed from low- growth rate half-saturation constant (K ) and maximum growth fl s temperature hydrothermal uids collected at Axial Volcano in rate (μmax), for the three organisms (Fig. 1C). The Ks for the 2008. The third organism was the commercially available M. pooled data for all three strains was 66 μM. The effect of hy- jannaschii DSM 2661 strain. All three organisms had longer drostatic pressure on our minimum H2 and Ks estimates was not doubling times and lower maximum cell concentrations with tested. Pressure has a very minor effect on values of standard molal Gibbs energy (ΔGr°) for reactions occurring in the aqueous phase (11, 31). Growth rates and hydrogenase activities of M. jannaschii increased modestly with pressure (32–34). However, A it is not known whether pressure significantly affects the organ- ) 10 ism’saffinity for aqueous H2, and this is area for future research. 7 In comparison, the H2 Ks values for the mesophilic metha- 8 nogens Methanospirillum hungatei and Methanobacterium bryantii, , × 10 each grown at 37 °C, were 6.6 μM and 18 μM, respectively (35, -1 36), and the minimum H2 threshold for M. bryantii was 2.4 μM 6 (36). Therefore, the generally higher demand for H2 by Meth- ls (ml anocaldococcus spp. may be a reflection of higher growth energy 4 requirements for hydrogenotrophic methanogens at hyper- thermophilic temperatures, as previously predicted (11). The minimum H2 threshold for methanogenesis at 82 °C in this study 2 was more than 10-fold lower than had been predicted (11), but this reflects the need to refine the parameters used to predict maintenance energies for hyperthermophiles in bioenergetics Number of CellNumber 0 0 2 4 6 8 10 12 14 models through experimentation. For example, increasing the SCIENCES activation energy (E ) in the Hoehler model (11) from 69.4 to ENVIRONMENTAL − a Time (h) 80 kJ mol 1 decreases cellular maintenance energies at 82 °C B more than 36-fold, which would predict a lower minimum H 10 2 ) threshold for the organisms.
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