海洋单细胞四爿藻基因组DNA的微量提取

四爿藻具有坚硬的囊壳和特殊的细胞壁组成,细胞不易破碎,且含有丰富的糖蛋白,易对DNA造成污染,使其基因组DNA提取较为困难、纯度不高。研究对比传统的CTAB法与高盐低pH法提取四爿藻DNA,高盐低pH法快速经济,得到的基因组DNA纯度较高,是一种行之有效的四爿藻基因组DNA提取方法。该法通过改变抽提介质,提高细胞破碎效率,减少抽提次数,有效去除污染,提取的基因组DNA不仅可以成功进行nrDNA转录间隔区(ITS)扩增,而且扩增产物适合于进行测序分析,这为其它淡水和海洋单细胞及多细胞藻类基因组DNA的提取也提供了借鉴。     

Alkalization of the Medium by Unicellular Green Algae during Uptake Dissolved Inorganic Carbon

When Chlorella vulgaris 11h, Chlorella vulgaris C-l, Chlamydomonasreinhardtii, Chlamydomonas moewusii, Scenedesmus obliquus, orDunaliella tertiolecta were illuminated in with 0.5 mM NaHCO₃,the pH of the medium increased in a few minutes from 6 to about9 or 10. The alkalization, which was accompanied by O₂ evolution,was dependent on light, external dissolved inorganic carbon(DIC) as HCO^-₃, and algae grown or adapted to a low, air-levelCO₂ in order to develop a DIC concentrating mechanism. Therewas little pH increase by algae without a DIC concentratingprocess from growth on 3% CO₂ in air. Photosynthetic O₂ evolutionwithout alkalization occurred using either internal DIC or externalCO₂ at acidic pH. The PH increase stopped between pH 9 to 10,but the alkalization would restart upon re-acidification betweenpH 6 and 8. Alkalization was suppressed by the carbonic anhydraseinhibitors, acetazolamide, ethoxyzolamide or carbon oxysulfide.The pH increase appeared to be the consequence of the externalconversion of HCO^–₃ into CO₂ plus OH^– during photosynthesisby cells with a high affinity for CO₂ uptake. Cells grown onhigh CO₂ to suppress the DIC pump, when given low levels ofHCO^–₃ in the light, acidified the medium from pH 10 to7. Air adapted Scenedesmus cells with a HCO^–₃ pump, aswell as a CO₂ pump, alkalized the medium very rapidly in thelight to a pH of over 10, as well as slower in the dark or inthe light with DCMU or without external DIC and O₂ evolution.Alkalization of the medium during photosynthetic DIC uptakeby algae has been considered to be part of the global carboncycle for converting H₂CO₃ to HCO^–₃ and for the formationof carbonate salts by calcareous algae from the alkaline conversionof bicarbonate to carbonate. These processes seem to be a consequenceof the algal CO₂ concentrating process. ¹Present address: Department of Biology, Faculty of Science,Niigata University, Niigata, 950-21 Japan.     

Characterization of the Key Step for Light-driven Hydrogen Evolution in Green Algae

Under anaerobic conditions, several species of green algae perform a light-dependent hydrogen production catalyzed by a special group of [FeFe] hydrogenases termed HydA. Although highly interesting for biotechnological applications, the direct connection between photosynthetic electron transport and hydrogenase activity is still a matter of speculation. By establishing an in vitro reconstitution system, we demonstrate that the photosynthetic ferredoxin (PetF) is essential for efficient electron transfer between photosystem I and HydA1. To investigate the electrostatic interaction process and electron transfer between PetF and HydA1, we performed site-directed mutagenesis. Kinetic analyses with several site-directed mutagenesis variants of HydA1 and PetF enabled us to localize the respective contact sites. These experiments in combination with in silico docking analyses indicate that electrostatic interactions between the conserved HydA1 residue Lys³⁹⁶ and the C terminus of PetF as well as between the PetF residue Glu¹²² and the N-terminal amino group of HydA1 play a major role in complex formation and electron transfer. Mapping of relevant HydA1 and PetF residues constitutes an important basis for manipulating the physiological photosynthetic electron flow in favor of light-driven H₂ production.     

On the Properties of the Starch Granules from Unicellular Green Algae

Starch granules from Chlorella, Chlamydomonas and Scenedesmus, grown heterotro-phically in a medium containing organic carbon sources, were isolated by means of the toluol treatment of the sonicate of alga. The toluol treatment separated the starch granules in the water layer from the cells and cell debris coagulated in the upper toluol layer.

The starch granules of Chlorella vulgaris and Chlamydomonas sp. were composed of amylose (12 to 3%) and amylopectin. The amylose content of the starch granules of Scenedesmus basilensis was 22 %. All the X-ray diffraction patterns of algal starch obtained in this investigation were of the A-type, identical to that of corn starch.     

Carbon Concentration Mechanism(s) in Unicellular Green Algae and Cyanobacteria

Unicellular green algae and cyanobacteria have mechanism(s) to actively concentrate dissolved inorganic carbon (DIC) into the cells, only if they are grown with air levels of CO₂. The DIC concentration mechanisms are environmental adaptations to actively transport and accumulate inorganic carbon into the chloroplasts of green algae or into the carboxysomes of cyanobacteria. The current working model of cyanobacterial carbon concentration mechanism consists of at least two basic components: an active C_i transport system and a Rubisco-rich polyhedral carboxysome. In case of unicellular green algae, the working model for DIC concentration mechanism includes several isoforms of carbonic anhydrase (CA), and ATPase driven active bicarbonate transporters at the plasmalemma and at the inner chloroplast envelopes. In the past twenty years, significant progress has been made in isolating and characterizing the isoforms of carbonic anhydrase. However, active transporters are yet to be characterized. This mini-review summarizes the current status of research on DIC-pumps including its significance and possible application to increase the productivity of plants of economic importance.     

Effect of Manganese on Hydrogen and Oxygen Evolution of Blue Green Algae Spirulina platensi

This paper reports that the hydrogen evolution in dark and the oxygen evolution by light from intact cells of Spirulina platensis treated with 0.8 mol/l this (pH 8.0) were inactivated, but they were restored after removing tris. The restoration of activity is related to manganese and increased with its amount raised in the liquid medium. If the manganese in medium is too high, the inhibition of hydrogen and oxygen evolution will take place. DCMU, methylamine, hydroxyl, amine hydrochloride which are the inhibitors of PS Ⅱ inhibit not only evolution of oxygen, but also of hydrogen.     

Phylogeny and Molecular Evolution of the Green Algae

The green lineage (Viridiplantae) comprises the green algae and their descendants the land plants, and is one of the major groups of oxygenic photosynthetic eukaryotes. Current hypotheses posit the early divergence of two discrete clades from an ancestral green flagellate. One clade, the Chlorophyta, comprises the early diverging prasinophytes, which gave rise to the core chlorophytes. The other clade, the Streptophyta, includes the charophyte green algae from which the land plants evolved. Multi-marker and genome scale phylogenetic studies have greatly improved our understanding of broad-scale relationships of the green lineage, yet many questions persist, including the branching orders of the prasinophyte lineages, the relationships among core chlorophyte clades (Chlorodendrophyceae, Ulvophyceae, Trebouxiophyceae and Chlorophyceae), and the relationships among the streptophytes. Current phylogenetic hypotheses provide an evolutionary framework for molecular evolutionary studies and comparative genomics. This review summarizes our current understanding of organelle genome evolution in the green algae, genomic insights into the ecology of oceanic picoplanktonic prasinophytes, molecular mechanisms underlying the evolution of complexity in volvocine green algae, and the evolution of genetic codes and the translational apparatus in green seaweeds. Finally, we discuss molecular evolution in the streptophyte lineage, emphasizing the genetic facilitation of land plant origins.     

Induction of Inorganic Carbon Accumulation in the Unicellular Green Algae Scenedesmus obliquus and Chlamydomonas reinhardtii

The induction of a dissolved inorganic carbon (DIC) accumulating mechanism in the two algal species Scenedesmus obliquus (WT) and Chlamydomonas reinhardtii (137 c+) was physiologically characterized by monitoring DIC uptake kinetics at a low and constant DIC concentration (120-140 micromolar), after transfer from high-DIC culturing conditions. A potentiometric titration method was used to measure and calculate algal DIC uptake. Full acclimation to low-DIC conditions was obtained within a period of 90 min, after which time the DIC uptake had been increased 7 to 10 times. Experiments were also conducted in the presence of inhibitors against DIC accumulation. The inhibitor of extracellular carbonic anhydrase (CA), acetazolamide (50 micromolar), inhibited the adaptation partly, while the inhibitor of both extra- and intracellular CA, ethoxyzolamide (50 micromolar) totally inhibited the acclimation. Cycloheximide (10 micrograms per milliliter), which inhibits protein synthesis on cytoplasmic ribosomes, and vanadate (180 micromolar), which inhibits the plasmamembrane bound ATPase, also inhibited the acclimation totally. These results taken together suggest that the algae are dependent on intracellular CA, plasmamembrane bound ATPase, and de novo protein synthesis for DIC accumulation. Also, these components are more important than extracellular CA for the overall function of the DIC-accumulating mechanism.     

Quantum Requirements of Photosynthetic Oxygen Evolution and 77 K Fluorescence Emission Spectra in Unicellular Green Algae Grown Under Low- and High-CO2-Conditions

Quantum requirements of photosynthetic oxygen evolution at 682 nm and fluorescence spectra at liquid nitrogen temperature (77 K), were investigated in Dunaliella tertiolecta, Chlamydomonas reinhardtii C-9, Chlorella vulgaris 11g, Chlorella vulgaris C3, and Chlorella pyrenoidosa 8b grown under low- and high-CO₂ conditions. Dunaliella, Chlamydomonas and C. vulgaris 11g show higher quantum requirements and a higher ratio of F_710–740/F_680–695 fluorescence when grown under low-CO₂ conditions, indicating a change in excitation energy distribution towards PS I. In C. pyrenoidosa the quantum requirement for low-CO₂ grown cells is higher than in high-CO₂ grown cells, but there was practically no change in the fluorescence ratio. In C. vulgaris C3, the quantum requirements of low- and high-CO₂ grown cells are the same, but the fluorescence ratio is higher in high-CO₂ grown cells than in low-CO₂ grown cells. These results indicate that most of the low-CO₂ grown cells require more PS I light than high-CO₂ grown cells. It is possible that this energy is used for cyclic electron flow. In C. vulgaris C 3, a mechanism may exist for excitation energy distribution which leads to the same quantum requirements under low- and high-CO₂ conditions.     

Electrophysiology of Turgor Regulation in Marine Siphonous Green Algae

We review electrophysiological measures of turgor regulation in some siphonous green algae, primarily the giant-celled marine algae, Valonia and Ventricaria, with particular comparison to the well studied charophyte algae Chara and Lamprothamnium. The siphonous green algae have a less negative plasma membrane potential, and are unlikely to have a proton-based chemiosmotic transport system, dominated by active electrogenic K⁺ uptake. We also make note of the unusual cellular structure of the siphonous green algae. Hypertonic stress, due to increased external osmotic pressure, is accompanied by positive-going potential difference (PD), increase in conductance, and slow turgor regulation. The relationship between these is not yet resolved, but may involve changes in K⁺ conductance (G _K) or active K⁺ transport at both membranes. Hypotonic turgor regulation, in response to decreased external osmotic pressure, is ∼3 times faster than hypertonic turgor regulation. It is accompanied by a negative-going PD, although conductance also increases. The conductance increase and the magnitude of the PD change are strongly correlated with the magnitude of hypotonic stress.     

Carbon Oxysulfide Inhibition of the CO(2)-Concentrating Process of Unicellular Green Algae

Carbonyl sulfide (COS), a substrate for carbonic anhydrase, inhibited alkalization of the medium, O₂ evolution, dissolved inorganic carbon accumulation, and photosynthetic CO₂ fixation at pH 7 or higher by five species of unicellular green algae that had been air-adapted for forming a CO₂-concentrating process. This COS inhibition can be attributed to inhibition of external HCO₃⁻ conversion to CO₂ and OH⁻ by the carbonic anhydrase component of an active CO₂ pump. At a low pH of 5 to 6, COS stimulated O₂ evolution during photosynthesis by algae with low CO₂ in the media without alkalization of the media. This is attributed to some COS hydrolysis by carbonic anhydrase to CO₂. Although COS had less effect on HCO₃⁻ accumulation at pH 9 by a HCO₃⁻ pump in Scenedesmus, COS reduced O₂ evolution probably by inhibiting internal carbonic anhydrases. Because COS is hydrolyzed to CO₂ and H₂S, its inhibition of the CO₂ pump activity and photosynthesis is not accurate, when measured by O₂ evolution, by NaH¹⁴CO₃ accumulation, or by ¹⁴CO₂ fixation.     

Dark Anaerobic Inactivation of Photosynthetic Oxygen Evolution by Chlamydomonas reinhardtii

When intact cells of Chlamydomonas reinhardtii were anaerobicallyincubated in the dark, rapid inactivation of oxygen evolutionwith benzoquinone as the Hill oxidant occurred. Measurementsof electron transport using thylakoids isolated after anaerobictreatment showed that the inactivation occurred at, or before,the secondary electron acceptor of PS II, whereas PS I activitywas largely unaffected. In addition, after anaerobic treatmentfluorescence transients measured with no addition or with dibromomethylisopropylbenzoquinonepresent were virtually the same as those obtained with DCMUpresent. When 10 mM NaHCO₃ was added to inactivated cells, partof the oxygen evolution capacity was restored rapidly. However,almost complete recovery (within 20 to 25 min) required theaddition of oxygen as well. This recovery was not light-dependentand was faster in the presence of 1 mM KCN. We suggest thatthe in activation of benzoquinone-dependent oxygen evolutionwas due to both bicarbonate depletion and reduction of the plastoquinonepool. ¹Present address: Institute of Molecular Biophysics, FloridaState University, Tallahassee, Florida 32306, U.S.A. (Received January 17, 1984; Accepted February 25, 1984)     

Isolation of Prasinoviruses of the Green Unicellular Algae Ostreococcus spp. on a Worldwide Geographical Scale

Ostreococcus spp. are extremely small unicellular eukaryotic green algae found worldwide in marine environments, and they are susceptible to attacks by a diverse group of large DNA viruses. Several biologically distinct species of Ostreococcus are known and differ in the ecological niches that they occupy: while O. tauri (representing clade C strains) is found in marine lagoons and coastal seas, strains belonging to clade A, exemplified by O. lucimarinus, are present in different oceans. We used laboratory cultures of clonal isolates of these two species to assay for the presence of viruses in seawater samples from diverse locations. In keeping with the distributions of their host strains, we found a decline in the abundance of O. tauri viruses from a lagoon in southwest France relative to the Mediterranean Sea, whereas in the ocean, no O. tauri viruses were detected. In contrast, viruses infecting O. lucimarinus were detected from distantly separated oceans. DNA sequencing, phylogenetic analyses using a conserved viral marker gene, and a Mantel test revealed no relationship between geographic and phylogenetic distances in viruses infecting O. lucimarinus.Viruses are the most abundant and genetically diverse biological entities in marine environments (48). The three ways most often used to assess eukaryotic algal virus diversity are (i) using a functional host-virus system to quantify viruses specific to one host strain (i.e., culture-based studies) (4), (ii) using PCR amplification and sequencing a conserved gene (10, 12-14, 28), and (iii) using whole-community genome sequencing (i.e., metagenomics) (6, 8, 31). Recently, the advent of sequencing techniques like shotgun sequencing or pyrosequencing (38) has led to an increase in the number of metagenomics projects. The Global Ocean Sampling (GOS) Expedition has provided a unique opportunity to investigate viral diversity in different environments within the size fraction of 0.1 to 0.8 μm (39). The GOS data revealed highly abundant viral sequences (at least 3% of the predicted proteins had a viral origin) (53). In another study, the analysis of marine viromes from four oceanic regions suggested that the composition of viral assemblages depends on their geographic locations, but these authors conclude that similar viruses are widespread throughout the oceans (2). Despite these new methods and different ways to analyze viral diversity, we still do not really know if “everything is really everywhere” (7).The present study addresses a specific part of this problem: are viruses infecting a single host strain present at geographically distant locations? If several viral strains are identified and characterized, how closely do these viruses resemble one another on a phylogenetic scale? In order to answer these questions, we focused on a microalgal (Prasinophyceae)-virus (Prasinovirus) system. The studied hosts belong to the genus Ostreococcus, a ubiquitous prasinophyte picoeukaryotic alga abundant throughout the oceanic euphotic zone (55, 56). Several strains from this genus were isolated and assigned to four distinct ecotypes according to their growth parameters under different light regimens (22, 36), which correspond to four well-defined phylogenetic clades in an internal transcribed spacer (ITS)-based phylogeny (clades A to D). The complete genome sequences of two Ostreococcus species have been described: O. tauri (19) and O. lucimarinus (35). In the present study, viruses infecting specific host species (Ostreococcus spp.) have been screened from a variety of locations around the world.Among viruses infecting Ostreococcus, the genome of a single strain (OtV5) has been fully sequenced (18), and the phylogenetic relationships among several virus strains have been investigated (4). These viruses belong to the Prasinovirus group, a genus of the Phycodnaviridae family. Many viruses infecting phytoplankton are members of the Phycodnaviridae; they have double-stranded DNA genomes and large polyhedral capsids (20). In the prasinophyte-Prasinovirus system, the hosts and viruses can be grown on solid medium and are easily maintained in the laboratory. Ostreococcus viral strains have been isolated and characterized by phylogenetic analysis based on their B-family DNA polymerase (DNA pol) partial gene sequence (4). This DNA polymerase is a useful marker for phylogenetic analyses because its sequence is well conserved in all known members of nucleocytoplasmic large DNA viruses (NCLDVs) (26), including Phycodnaviridae. Furthermore, several previous studies have examined the abundance and the genetic diversity of marine eukaryotic viruses using environmental sequencing approaches and amplified DNA pol gene fragments (11, 12, 43-46), and Monier et al. (31) used this marker to describe the taxonomic distribution of large DNA viruses from the GOS data.The first stage of this study was to isolate Ostreococcus viruses from different worldwide geographic locations, by culturing on various host strains. In a second stage, these viral strains were characterized via the sequencing of their pol sequence (encoding a part of their DNA polymerase gene), and their specificity toward different host strains was assessed in order to assess the potential host range of the viral strains isolated and to gain a better understanding of their population dynamics and distribution. Finally we compared these new Prasinovirus DNA sequences with metagenomic sequence data (obtained from sampling all around the world) and environmental sequence data identified using BLAST similarity to assess the global distribution of similar Ostreococcus viruses.     

绿藻高效制氢影响因素的研究

绿藻作为生物能源的研究和开发具有诱人的发展前景。本文概述了绿藻制氢和产氢途径的研究进展,重点介绍了绿藻高效制氢的影响因素--绿藻[Fe]-氢化酶的研究和绿藻制氢的重要控制参数,同时,对绿藻制氢作为生物能源的开发应用前景进行了展望。     

Salicylhydroxamic Acid (SHAM) Inhibition of the Dissolved Inorganic Carbon Concentrating Process in Unicellular Green Algae

Rates of photosynthetic O₂ evolution, for measuring K_0.5(CO₂ + HCO₃⁻) at pH 7, upon addition of 50 micromolar HCO₃⁻ to air-adapted Chlamydomonas, Dunaliella, or Scenedesmus cells, were inhibited up to 90% by the addition of 1.5 to 4.0 millimolar salicylhydroxamic acid (SHAM) to the aqueous medium. The apparent K₁(SHAM) for Chlamydomonas cells was about 2.5 millimolar, but due to low solubility in water effective concentrations would be lower. Salicylhydroxamic acid did not inhibit oxygen evolution or accumulation of bicarbonate by Scenedesmus cells between pH 8 to 11 or by isolated intact chloroplasts from Dunaliella. Thus, salicylhydroxamic acid appears to inhibit CO₂ uptake, whereas previous results indicate that vanadate inhibits bicarbonate uptake. These conclusions were confirmed by three test procedures with three air-adapted algae at pH 7. Salicylhydroxamic acid inhibited the cellular accumulation of dissolved inorganic carbon, the rate of photosynthetic O₂ evolution dependent on low levels of dissolved inorganic carbon (50 micromolar Na-HCO₃), and the rate of ¹⁴CO₂ fixation with 100 micromolar [¹⁴C] HCO₃⁻. Salicylhydroxamic acid inhibition of O₂ evolution and ¹⁴CO₂-fixation was reversed by higher levels of NaHCO₃. Thus, salicylhydroxamic acid inhibition was apparently not affecting steps of photosynthesis other than CO₂ accumulation. Although salicylhydroxamic acid is an inhibitor of alternative respiration in algae, it is not known whether the two processes are related.     

New Insights into Evolution of the ABC Transporter Family in Mesostigma viride,a Unicellular Charophyte Algae

ATP-binding cassette (ABC) transporters play an important role in driving the exchange of multiple molecules across cell membranes. The plant ABC transporter family is among the largest protein families, and recent progress has advanced our understanding of ABC classification. However, the ancestral form and deep origin of plant ABCs remain elusive. In this study, we identified 59 ABC transporters in Mesostigma viride, a unicellular charophyte algae that represents the earliest diverging lineage of streptophytes, and 1034 ABCs in genomes representing a broad taxonomic sampling from distantly related plant evolutionary lineages, including chlorophytes, charophytes, bryophytes, lycophytes, gymnosperms, basal angiosperms, monocots, and eudicots. We classified the plant ABC transporters by comprehensive phylogenetic analysis of each subfamily. Our analysis revealed the ancestral type of ABC proteins as well as duplication and gene loss during plant evolution, contributing to our understanding of the functional conservation and diversity of this family. In summary, this study provides new insight into the origin and evolution of plant ABC transporters.     

Scavenging of Hydrogen Peroxide in Prokaryotic and Eukaryotic Algae: Acquisition of Ascorbate Peroxidase during the Evolution of Cyanobacteria

Ascorbate (AsA) peroxidase was found in six species of cyanobacteriaamong ten species tested. Upon the addition of H₂¹⁸O₂ to thecells of AsA peroxidase-containing cyanobacteria, ¹⁶O₂ derivedfrom water and ¹⁸O₂ derived from H₂^I8O₂ were evolved in thelight. The evolution of ¹⁶O₂ was inhibited by DCMU and did notoccur in the dark, but ^I8O₂ was evolved even in the dark orin the presence of DCMU. Similar light-dependent evolution of¹⁶O₂ was observed in the cells of AsA peroxidase-containingEuglena and Chlamydomonas. However, the cells of AsA perox-idase-lackingcyanobacteria evolved only ¹⁸O₂ in either the light or dark.Furthermore, the quenching of chlorophyll fluorescence inducedby hydrogen peroxide was observed only in the cells of the AsAperoxidase-containing Synechocystis 6803, and not in the cellsof Anacystis nidulans which lacks AsA peroxidase. Thus, cyanobacteriacan be divided into two groups, those that has and those thatlacks AsA peroxidase. The first group scavenges hydrogen peroxidewith the peroxidase using a photoreductant as the electron donor,and the second group only scavenges hydrogen peroxide with catalase. (Received July 23, 1990; Accepted October 18, 1990)     

Ultrastructure of the Cell Wall and Cell Division of Unicellular Blue-green Algae

The fine structure of the cell wall and the process of cell division were examined in thin sections of two unicellular blue-green algae grown under defined conditions. Unilateral invagination of the photosynthetic lamellae is the first sign of cell division in the rod-shaped organism, Anacystis nidulans. Symmetrical invagination of the cytoplasmic membrane and inner wall layers follows. One wall layer, which appears to be the mucopolymer layer, is then differentially synthesized to form the septum; the outer wall layers are not involved in septum formation. Centripetal splitting of the inner layer separates the two daughter cells. A second division, in a plane parallel to the first, usually occurs before the first daughter cells are separated. In the coccoid organism, Gleocapsa alpicola, the features of cell division are broadly similar; however, unilateral invagination of the lamellae is not observed and the second division takes place in a plane perpendicular to the plane of the previous division.     

Carbon and Hydrogen Isotopic Fractionation during Anaerobic Biodegradation of Benzene

Compound-specific isotope analysis has the potential to distinguish physical from biological attenuation processes in the subsurface. In this study, carbon and hydrogen isotopic fractionation effects during biodegradation of benzene under anaerobic conditions with different terminal-electron-accepting processes are reported for the first time. Different enrichment factors () for carbon (range of −1.9 to −3.6‰) and hydrogen (range of −29 to −79‰) fractionation were observed during biodegradation of benzene under nitrate-reducing, sulfate-reducing, and methanogenic conditions. These differences are not related to differences in initial biomass or in rates of biodegradation. Carbon isotopic enrichment factors for anaerobic benzene biodegradation in this study are comparable to those previously published for aerobic benzene biodegradation. In contrast, hydrogen enrichment factors determined for anaerobic benzene biodegradation are significantly larger than those previously published for benzene biodegradation under aerobic conditions. A fundamental difference in the previously proposed initial step of aerobic versus proposed anaerobic biodegradation pathways may account for these differences in hydrogen isotopic fractionation. Potentially, C-H bond breakage in the initial step of the anaerobic benzene biodegradation pathway may account for the large fractionation observed compared to that in aerobic benzene biodegradation. Despite some differences in reported enrichment factors between cultures with different terminal-electron-accepting processes, carbon and hydrogen isotope analysis has the potential to provide direct evidence of anaerobic biodegradation of benzene in the field.