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PubMed1994

Evolutionary relationships of bacterial and archaeal glutamine synthetase genes.

Glutamine synthetase (GS), an essential enzyme in ammonia assimilation and glutamine biosynthesis, has three distinctive types: GSI, GSII and GSIII. Genes for GSI have been found only in bacteria (eubacteria) and archaea (archaebacteria), while GSII genes only occur in eukaryotes and a few soil-dwelling bacteria. GSIII genes have been found in only a few bacterial species. Recently, it has been suggested that several lateral gene transfers of archaeal GSI genes to bacteria may have occurred. In order to study the evolution of GS, we cloned and sequenced GSI genes from two divergent archaeal species: the extreme thermophile Pyrococcus furiosus and the extreme halophile Haloferax volcanii. Our phylogenetic analysis, which included most available GS sequences, revealed two significant prokaryotic GSI subdivisions: GSI-alpha and GSI-beta. GSI-alpha-genes are found in the thermophilic bacterium, Thermotoga maritima, the low G+C Gram-positive bacteria, and the Euryarchaeota (includes methanogens, halophiles, and some thermophiles). GSI-beta-type genes occur in all other bacteria. GSI-alpha- and GSI-beta-type genes also differ with respect to a specific 25-amino-acid insertion and adenylylation control of GS enzyme activity, both absent in the former but present in the latter. Cyanobacterial genes lack adenylylation regulation of GS and may have secondarily lost it. The GSI gene of Sulfolobus solfataricus, a member of the Crenarchaeota (extreme thermophiles), is exceptional and could not be definitely placed in either subdivision.

Amino Acid Sequence↗
PubMed1995

Pyruvate: ferredoxin oxidoreductase from the sulfate-reducing Archaeoglobus fulgidus: molecular composition, catalytic properties, and sequence alignments.

Archaeoglobus fulgidus is a hyperthermophilic sulfate-reducing archaeon. In this communication we describe the purification and properties of pyruvate: ferredoxin oxidoreductase from this organism. The catabolic enzyme was purified 250-fold to apparent homogeneity with a yield of 16%. The native enzyme had an apparent molecular mass of 120 kDa and was composed of four different subunits of apparent molecular masses of 45, 33, 25, and 13 kDa, indicating an alpha beta gamma delta structure. Per mol, the enzyme contained 0.8 mol thiamine pyrophosphate, 9 mol non-heme iron, and 8 mol acid-labile sulfur. FAD, FMN, lipoic acid, and copper were not found. The purified enzyme showed an apparent Km for coenzyme A of 0.02 mM, for pyruvate of 0.3 mM, and for clostridial ferredoxin of 0.01 mM, an apparent Vmax of 64 U/mg (at 65 degrees C) with a pH optimum near 7.5 and an Arrhenius activation energy of 75 kJ/mol (between 30 and 70 degrees C). The temperature optimum was above 90 degrees C. At 90 degrees C, the enzyme lost 50% activity within 60 min in the presence of 2 M KCl. The enzyme did not catalyze the oxidation of 2-oxoglutarate, indolepyruvate, phenylpyruvate, glyoxylate, and hydroxypyruvate. The N-terminal amino acid sequences of the four subunits were determined. The sequence of the alpha-subunit had similarities to the N-terminal amino acid sequence of the alpha-subunit of the heterotetrameric pyruvate: ferredoxin oxidoreductase from Pyrococcus furiosus and from Thermotoga maritima, and unexpectedly, to the N-terminal amino acid sequence of the homodimeric pyruvate:ferredoxin oxidoreductase from proteobacteria and from cyanobacteria. No sequence similarities were found, however, between the alpha-subunits of the enzyme from A. fulgidus and the heterodimeric pyruvate:ferredoxin oxidoreductase from Halobacterium halobium.

Amino Acid Sequence↗
PubMed1995

Chromosomal organization and nucleotide sequence of the genes for elongation factors EF-1 alpha and EF-2 and ribosomal proteins S7 and S10 of the hyperthermophilic archaeum Desulfurococcus mobilis.

The Desulfurococcus mobilis genes fus (encoding EF-2) and tuf (for EF-1 alpha) were cloned and sequenced together with genes for ribosomal proteins S10 (rps10) and S7 (rps7). Unlike Methanococcus, which displays the bacterial-like fus and tuf gene context 5'-rps12-rps7-fus-tuf-3', and similar to Sulfolobus and Pyrococcus, the Desulfurococcus fus gene (734 codons) has a distinct chromosomal location. Moreover, tuf (441 codons) is the promoter-proximal unit of a three-gene cluster comprising the genes rps10 (98 codons) and tRNA(Ser); the arrangement of the cluster is 5'-tuf-91 bp spacer -rps10-138 bp spacer -tRNA(Ser)-3' and the tuf gene is preceded by a canonical archaeal promoter. The D. mobilis gene rps7 (198 codons) is located further upstream from tuf (535 bp 'silent' intergenic spacing) and no rps12 homolog occurs in its immediate vicinity. Also, judging from putative promoter and transcription termination sequences, rps7 appears to be separately transcribed. Analysis of the predicted fus and tuf gene products revealed the three consensus motifs characteristic of GTP-binding proteins, and the fus-encoded EF-2 protein also displayed the consensus sequence required for ADP-ribosylation by Diphtheria toxin. Both EF sequences were definitely crenarchaeal by comparison with available homologs from other Archaea. Outgroup-rooted phylogenies derived from the sequences of ribosomal proteins S10 and S7 yielded the Sulfolobus-Desulfurococcus association at a high bootstrap confidence level.

Amino Acid Sequence↗
PubMed1999

DNA repair systems in archaea: mementos from the last universal common ancestor?

DNA repair in the Archaea is relevant to the consideration of genome maintenance and replication fidelity in the last universal common ancestor (LUCA) from two perspectives. First, these prokaryotes embody a mix of bacterial and eukaryal molecular features. Second, DNA repair proteins would have been essential in LUCA to maintain genome integrity, regardless of the environmental temperature. Yet we know very little of the basic molecular mechanisms of DNA damage and repair in the Archaea in general. Many studies on DNA repair in archaea have been conducted with hyperthermophiles because of the additional stress imposed on their macromolecules by high temperatures. In addition, of the six complete archaeal genome sequences published so far, five are thermophilic archaea. We have recently shown that the hyperthermophile Pyrococcus furiosus has an extraordinarily high capacity for repair of radiation-induced double-strand breaks and we have identified and sequenced several genes involved in DNA repair in P. furiosus. At the sequence level, only a few genes share homology with known bacterial repair genes. For instance, our phylogenetic analysis indicates that archaeal recombinases occur in two paralogous gene families, one of which is very deeply branched, and both recombinases are more closely related to the eukaryotic RAD51 and Dmc1 gene families than to the Escherichia coli recA gene. We have also identified a gene encoding a repair endo/exonuclease in the genomes of several Archaea. The archaeal sequences are highly homologous to those of the eukaryotic Rad2 family and they cluster with genes of the FEN-1 subfamily, which are known to be involved in DNA replication and repair in eukaryotes. We argue that there is a commonality of mechanisms and protein sequences, shared between prokaryotes and eukaryotes for several modes of DNA repair, reflecting diversification from a minimal set of genes thought to represent the genome of the LUCA.

Amino Acid Sequence↗
PubMed2000

Investigation of exchange couplings in [Fe3S4]+ clusters by electron spin-lattice relaxation.

We have studied four proteins containing oxidized 3Fe clusters ([Fe3S4]+, S=1/2, composed of three, antiferromagnetically coupled high-spin ferric ions) by continuous wave (CW) and pulsed EPR techniques: Azotobacter vinelandii ferredoxin I, Desulfovibrio gigas ferredoxin II, and the 3Fe forms of Pyrococcus furiosus ferredoxin and aconitase. The 35 GHz (Q-band) CW EPR signals are simulated to yield experimental g tensors, which either had not been reported, or had been reported only at X-band microwave frequency. Pulsed X- and Q-band EPR techniques are used to determine electron spin-lattice (T1, longitudinal) relaxation times at several positions on the samples' EPR envelope over the temperature range 2-4.2 K. The T1, values vary sharply across the EPR envelope, a reflection of the fact that the envelope results from a distribution in cluster properties, as seen earlier as a distribution in g3 values and in 57 Fe hyperfine interactions, as detected by electron nuclear double resonance spectroscopy. The temperature dependence of 1/T1 is analyzed in terms of the Orbach mechanism, with relaxation dominated by resonant two-phonon transitions to a doublet excited state at approximately 20 cm(-1) above the doublet ground state for all four of these 3Fe proteins. The experimental EPR data are combined with previously reported 57Fe hyperfine data to determine electronic spin exchange-coupling within the clusters, following the model of Kent et al. Their model defines the coupling parameters as follows: J13=J, J12=J(1+epsilon'), J23=J(1+epsilon), where Jij is the isotropic exchange coupling between ferric ions i and j, and epsilon' and epsilon' are measures of coupling inequivalence. We have extended their theory to include the effects of epsilon' not equal to 0 and thus derived an exact expression for the energy of the doublet excited state for any epsilon, epsilon'. This excited state energy corresponds roughly to epsilonJ and is in the range 5-10 cm(-1) for each of these four 3Fe proteins. This magnitude of the product epsilonJ, determined by our time-domain relaxation studies in the temperature range 2-4 K, is the same as that obtained from three other distinct types of study: CW EPR studies of spin relaxation in the range 5.5-50 K, NMR studies in the range 293-303 K, and static susceptibility measurements in the range 1.8-200 K. We suggest that an apparent disagreement as to the individual values of J and epsilon be resolved in favor of the values obtained by susceptibility and NMR (J > or approximately 200 cm(-1) and epsilon> or =0.02 cm(-1)). as opposed to a smaller J and larger r as suggested in CW EPR studies. However, we note that this resolution casts doubt on the accepted theoretical model for describing the distribution in magnetic properties of 3Fe clusters.

Aconitate Hydratase↗
PubMed1997

Purification and properties of an extremely thermostable NADP+-specific glutamate dehydrogenase from Archaeoglobus fulgidus.

NADP+-specific glutamate dehydrogenase (EC 1.4.1.4) was purified to homogeneity from the extremely thermophilic, strictly anaerobic, sulfate-reducing archaeon Archaeoglobus fulgidus strain 7324. The native enzyme (263 kDa) is composed of subunits of mol. mass 46 kDa, suggesting a hexameric structure. The temperature optimum for enzyme activity was > 95 degrees C. The enzyme was highly thermostable, having a half-life of 140 min at 100 degrees C. Potassium phosphate, KCl, and NaCl enhanced the thermal stability and increased the rate of activity three- to fourfold. The N-terminal 26-amino-acid sequence showed a high degree of similarity to glutamate dehydrogenases from Pyrococcus spp. and Thermococcus spp.

Amino Acid Sequence↗
PubMed1999

Thermococcus waiotapuensis sp. nov., an extremely thermophilic archaeon isolated from a freshwater hot spring.

An extremely thermophilic, sulfur-dependent archaeon, strain WT1, was isolated from a freshwater hot spring in the Lake Taupo area of North Island, New Zealand. The cells are flagellated, strictly anaerobic cocci that grow optimally at 85 degrees C and 5.4 g NaCl l(-1). The strain grows heterotrophically on complex proteinaceous substrates or on appropriate salts plus amino acid mixtures and is also able to utilize maltose, starch, and pyruvate. Elemental sulfur could be replaced by cystine or thioglycollate. The range of temperatures allowing growth is from 60 to 90 degrees C; the pH supporting growth ranges from 5 to 8 (optimum, pH 7). Strain WT1 grew in a defined medium containing amino acids as the sole carbon and energy sources. The required amino acids were: Arg, His, Ile, Leu, Phe, Ser, Thr, Trp, Tyr, and Val. Strain WT1 showed sensitivity to rifampicin. DNA G+C content was 50.4 mol%. Phylogenetic analysis of the sequence encoding the 16S rRNA gene indicated that this isolate is a member of the Thermococcales. DNA/DNA hybridization studies revealed no similarity to several species of Thermococcus and Pyrococcus, with the exception of Thermococcus zilligii. Based on the reported results, we propose strain WT1 as a new species to be named Thermococcus waiotapuensis sp. nov.

Bacterial Typing Techniques↗
PubMed2005

Horizontal transfer of two operons coding for hydrogenases between bacteria and archaea.

Using a phylogenetic approach, we discovered three putative horizontal transfers between bacterial and archaeal species involving large clusters of genes. One transfer involves an operon of 13 genes, called mbx, which probably was transferred into the genome of Thermotoga maritima from a species belonging or close to the Pyrococcus genus. The two others implied an operon of six genes, called ech, transferred independently to the genomes of Thermoanaerobacter tengcongensis and Desulfovibrio gigas, from a species belonging or close to the Methanosarcina genus. All these transfers affected operons coding for multisubunit membrane-bound (NiFe) hydrogenases involved in the energy metabolism of the donor genomes. The functionality of the transferred operons has not been experimentally demonstrated for T. maritima, whereas in D. gigas and T. tengcongensis the encoded multisubunit hydrogenase could have a role in energy conservation. This report adds several cases of horizontal gene transfers among hydrogenases already described.

Archaea↗
PubMed2001

Both pH and carbon flux influence the level of rubredoxin in Clostridium butyricum.

The rubredoxin expression level in Clostridium butyricum DSM 5431 grown in continuous culture was monitored using primer extension analyses of the rub gene and a specific enzymatic assay of the iron-sulfur protein. In this way, we showed that variations in rubredoxin content and in rub mRNA level were influenced by the pH of the culture and were directly dependent on the carbon flux. The maximum rubredoxin level reached 1227.3 pmol (mg of proteins)(-1) (i.e. 0.7% of the total protein content) under strictly anaerobic conditions when cells grew at pH 6.5 with an excess of glucose. In addition, primer extension analyses established that the control for all the variations observed operates at the level of gene transcription. Altogether, these results suggested a main function of rubredoxin in Clostridium butyricum independent of the protection against oxygen as has already been reported for Desulfovibrio gigas and Pyrococcus furiosus.

Bacterial Proteins↗
PubMed1996

A RecA/RAD51 homologue from a hyperthermophilic archaeon retains the major RecA domain only.

A gene encoding a RecA/RAD51 homologue from a hyperthermophilic archaeon, Pyrococcus sp. KOD1 (Pk), was cloned, sequenced and expressed in Escherichia coli. The deduced 210-amino acid sequence was compared to homologues from bacteria (RecA), eukaryotes (RAD51, DMC1) and archaea (RadA). The entire protein from Pk (Pk-REC) basically corresponds to the essential central domain of its counterparts and lacks the two smaller RecA subdomains at the N- and C-termini. The sequence comparison suggests that Pk-REC represents a common prototype of RecA, RAD51, DMC1 and RadA, with higher enzymatic activity. Recombinant Pk-REC was fully active and complemented the ultraviolet light sensitivity of an E. coli recA mutant strain.

Amino Acid Sequence↗
PubMed2001

Conservation of the basic pattern of cellular amino acid composition of archaeobacteria during biological evolution and the putative amino acid composition of primitive life forms.

Previous studies showed that the cellular amino acid composition obtained by amino acid analysis of whole cells, differs such as eubacteria, protozoa, fungi and mammalian cells. These results suggest that the difference in the cellular amino acid composition reflects biological changes as the result of evolution. However, the basic pattern of cellular amino acid composition was relatively constant in all organisms examined. In the present study, we examined archaeobacteria, because they are considered important in understanding the relationship between biological evolution and cellular amino acid composition. The cellular amino acid compositions of Archaeoglobus fulgidus, Pyrococcus horikoshii, Methanobacterium thermoautotrophicum and Methanococcus jannaschii differed slightly from each other, but were similar to those determined from codon usage data, based on the complete genomes. Thus, the cellular amino acid composition reflects biological evolution. We suggest that primitive forms of life appearing on earth at the end of prebiotic evolution had a similar-cellular amino acid composition.

Amino Acids↗
PubMed2004

Contribution of the [FeII(SCys)4] site to the thermostability of rubredoxins.

The thermostabilities of Fe(2+) ligation in rubredoxins (Rds) from the hyperthermophile Pyrococcus furiosus (Pf) and the mesophiles Clostridium pasteurianum (Cp) and Desulfovibrio vulgaris (Dv) were compared. Residue 44 forms an NH.S(Cys) hydrogen bond to one of the cysteine ligands to the [Fe(SCys)(4)] site, and substitutions at this location affect the redox properties of the [Fe(SCys)(4)] site. Both Pf Rd and Dv Rd have an alanine residue at position 44, whereas Cp Fd has a valine residue. Wild-type proteins were examined along with V44A and A44V "exchange" mutants of Cp and Pf Rds, respectively, in order to assess the effects of the residue at position 44 on the stability of the [Fe(SCys)(4)] site. Stability of iron ligation was measured by temperature-ramp and fixed-temperature time course experiments, monitoring iron release in both the absence and presence of more thiophilic metals (Zn(2+), Cd(2+)) and over a range of pH values. The thermostability of the polypeptide fold was concomitantly measured by fluorescence, circular dichroism, and (1)H NMR spectroscopies. The A44V mutation strongly lowered the stability of the [Fe(II)(SCys)(4)] site in Pf Rd, whereas the converse V44A mutation of Cp Rd significantly raised the stability of the [Fe(II)(SCys)(4)] site, but not to the levels measured for wild-type Dv Rd. The region around residue 44 is thus a significant contributor to stability of iron coordination in reduced Rds. This region, however, made only a minor contribution to the thermostability of the protein folding, which was found to be higher for hyperthermophilic versus mesophilic Rds, and largely independent of the residue at position 44. These results, together with our previous studies, show that localized charge density, solvent accessibility, and iron site/backbone interactions control the thermostability of the [Fe(SCys)(4)] site. The iron site thermostability does make a minor contribution to the overall Rd thermostability. From a mechanistic standpoint, we also found that attack of displacing ions (H(+), Cd(2+)) on the Cys42 sulfur ligand at the [Fe(SCys)(4)] site occurs through the V8 side and not the V44 side of the iron site.

Amino Acid Sequence↗
PubMed2005

Purification and characterization of the tungsten enzyme aldehyde:ferredoxin oxidoreductase from the hyperthermophilic denitrifier Pyrobaculum aerophilum.

A tungsten-containing aldehyde:ferredoxin oxidoreductase (AOR) has been purified to homogeneity from Pyrobaculum aerophilum. The N-terminal sequence of the isolated enzyme matches a single open reading frame in the genome. Metal analysis and electron paramagnetic resonance (EPR) spectroscopy indicate that the P. aerophilum AOR contains one tungsten center and one [4Fe-4S](2+/1+) cluster per 68-kDa monomer. Native AOR is a homodimer. EPR spectroscopy of the purified enzyme that has been reduced with the substrate crotonaldehyde revealed a W(V) species with g(zyx) values of 1.952, 1.918, 1.872. The substrate-reduced AOR also contains a [4Fe-4S](1+) cluster with S=3/2 and zero field splitting parameters D=7.5 cm(-1) and E/D=0.22. Molybdenum was absent from the enzyme preparation. The P. aerophilum AOR lacks the amino acid sequence motif indicative for binding of mononuclear iron that is typically found in other AORs. Furthermore, the P. aerophilum AOR utilizes a 7Fe ferredoxin as the putative physiological redox partner, instead of a 4Fe ferredoxin as in Pyrococcus furiosus. This 7Fe ferredoxin has been purified from P. aerophilum, and the amino acid sequence has been identified using mass spectrometry. Direct electrochemistry of the ferredoxin showed two one-electron transitions, at -306 and -445 mV. In the presence of 55 microM ferredoxin the AOR activity is 17% of the activity obtained with 1 mM benzyl viologen as an electron acceptor.

Aldehyde Oxidoreductases↗
PubMed2006

The first crystal structure of class III superoxide reductase from Treponema pallidum.

Superoxide reductase (SOR) is a metalloprotein containing a non-heme iron centre, responsible for the scavenging of superoxide radicals in the cell. The crystal structure of Treponema pallidum (Tp) SOR was determined using soft X-rays and synchrotron radiation. Crystals of the oxidized form were obtained using poly(ethylene glycol) and MgCl2 and diffracted beyond 1.55 A resolution. The overall architecture is very similar to that of other known SORs but TpSOR contains an N-terminal domain in which the desulforedoxin-type Fe centre, found in other SORs, is absent. This domain conserves the beta-barrel topology with an overall arrangement very similar to that of other SOR proteins where the centre is present. The absence of the iron ion and its ligands, however, causes a decrease in the cohesion of the domain and some disorder is observed, particularly in the region where the metal would be harboured. The C-terminal domain exhibits the characteristic immunoglobulin-like fold and harbours the Fe(His)4(Cys) active site. The five ligands of the iron centre are well conserved despite some disorder observed for one of the four molecules in the asymmetric unit. The participation of a glutamate as the sixth ligand of some of the iron centres in Pyrococcus furiosus SOR was not observed in TpSOR. A possible explanation is that either X-ray photoreduction occurred or there was a mixture of redox states at the start of data collection. In agreement with earlier proposals, details in the TpSOR structure also suggest that Lys49 might be involved in attraction of superoxide to the active site.

Amino Acid Sequence↗
PubMed2000

Structural evidence for a common zinc binding domain in archaeal and eukaryal transcription factor IIB proteins.

X-ray absorption spectroscopy has been used to compare the metal coordination of the N-terminal zinc binding domain of eukaryal human transcription factor (TF) IIB to the previously reported structure of archaeal Pyrococcus furiosus (Pf) TFB. Full length and N-terminal fragments for both PfTFB and human TFIIB were cloned, expressed, and purified. The [C10H] variant of PfTFB was constructed to resemble the metal binding motif of higher eukaryal TFIIB proteins by mutating the second cysteine ligand to a histidine. All five proteins bind zinc in a 1:1 ratio. Zn X-ray absorption spectroscopy of human TFIIB and [C10H]PfTFB mutant are consistent with ZnS3(N,O) ligation, and further suggest that the N/O ligand is an imidazole.

Absorptiometry, Photon↗
PubMed2004

Revealing gene transcription and translation initiation patterns in archaea, using an interactive clustering model.

An interactive clustering model based on positional weight matrices is described and results obtained using the model to analyze gene regulation patterns in archaea are presented. The 5' flanking sequences of ORFs identified in four archaea, Sulfolobus solfataricus, Pyrobaculum aerophilum, Halobacterium sp. NRC-1, and Pyrococcus abyssi, were clustered using the model. Three regular patterns of clusters were identified for most ORFs. One showed genes with only a ribosome-binding site; another showed genes with a transcriptional regulatory region located at a constant location with respect to the start codon. A third pattern combined the previous two. Both P. aerophilum and Halobacterium sp. NRC-1 exhibited clusters of genes that lacked any regular pattern. Halobacterium sp. NRC-1 also presented regular features not seen in the other organisms. This group of archaea seems to use a combination of eubacterial and eukaryotic regulatory features as well as some unique to individual species. Our results suggest that interactive clustering may be used to examine the divergence of the gene regulatory machinery in archaea and to identify the presence of archaea-specific gene regulation patterns.

Archaea↗
PubMed2004

The first evidence of anaerobic CO oxidation coupled with H2 production by a hyperthermophilic archaeon isolated from a deep-sea hydrothermal vent.

From 24 samples of hydrothermal venting structures collected at the East Pacific Rise (13 degrees N), 13 enrichments of coccoid cells were obtained which grew on CO, producing H2 and CO2 at 80 degrees C. A hyperthermophilic archaeon capable of lithotrophic growth on CO coupled with equimolar production of H2 was isolated. Based on its 16S rRNA sequence analysis, this organism was affiliated with the genus Thermococcus. Other strains of Thermococcales species ( Pyrococcus furiosus, Thermococcus peptonophilus, T. profundus, T. chitonophagus, T. stetteri, T. gorgonarius, T. litoralis, and T. pacificus) were shown to be unable to grow on CO. Searches in sequence databases failed to reveal deposited sequences of genes related to CO metabolism in Thermococcales. Our work provides the first evidence of anaerobic CO oxidation coupled with H2 production performed by an archaeon as well as the first documented case of lithotrophic growth of a Thermococcales representative.

Anaerobiosis↗
PubMed2006

Composition of archaeal, bacterial, and eukaryal RuBisCO genotypes in three Western Pacific arc hydrothermal vent systems.

We studied the diversity of all forms of the RuBisCO large subunit-encoding gene cbbL in three RuBisCO uncharacterized hydrothermal vent communities. This diversity included the archaeal cbbL and the forms IC and ID, which have not previously been studied in the deep-sea environment, in addition to the forms IA, IB and II. Vent plume sites were Fryer and Pika in the Mariana arc and the Suiyo Seamount, Izu-Bonin, Japan. The cbbL forms were PCR amplified from plume bulk microbial DNA and then cloned and sequenced. Archaeal cbbL was detected in the Mariana samples only. Both forms IA and II were amplified from all samples, while the form IC was amplified only from the Pika and Suiyo samples. Only the Suiyo sample showed amplification of the form ID. The form IB was not recorded in any sample. Based on rarefaction analysis, nucleotide diversity and average pairwise difference, the archaeal cbbL was the most diverse form in Mariana samples, while the bacterial form IA was the most diverse form in the Suiyo sample. Also, the Pika sample harbored the highest diversity of cbbL phylogenetic lineages. Based on pairwise reciprocal library comparisons, the Fryer and Pika archaeal cbbL libraries showed the most significant difference, while Pika and Suiyo showed the highest similarity for forms IA and II libraries. This suggested that the Fryer supported the most divergent sequences. All archaeal cbbL sequences formed unique phylogenetic lineages within the branches of anaerobic thermophilic archaea of the genera Pyrococcus, Archaeoglobus, and Methanococcus. The other cbbL forms formed novel phylogenetic clusters distinct from any recorded previously in other deep-sea habitats. This is the first evidence for the diversity of archaeal cbbL in environmental samples.

Archaea↗