Introduction

Whole-genome amplification (WGA) based on phi29 polymerase-mediated multiple displacement amplification (Dean et al., 2001, 2002) holds great promise in the field of microbial ecology (Hutchison and Venter, 2006; Binga et al., 2008; Ishoey et al., 2008). The multiple displacement amplification reaction results in a billion-fold amplification of DNA even from femtogram amounts, thus making it possible to generate genomic DNA suitable for shotgun sequencing from single microbial cells. This technique is especially well suited for the study of environmental microbial samples in which <1% of microorganisms have been cultivated, and are thus not accessible by conventional techniques (Rappe and Giovannoni, 2003). Since the introduction of single-cell genomics to microbiology (Raghunathan et al., 2005), few studies have succeeded in the reconstruction of genomes from single uncultivated bacterial cells (Marcy et al., 2007; Mussmann et al., 2007; Rodrigue et al., 2009; Woyke et al., 2009; Woyke et al., 2010). The powerful combination of multiple displacement amplification with new sequencing technologies can thus provide comprehensive genomic insights into the metabolic capacities and environmental adaptations of single microbial cells independent of their cultivation.

Sponges (phylum Porifera) are the most ancient of multicellular animals with a fossil record dating back at least 580 million years (Li et al., 1998). In addition to their evolutionary significance, many marine sponges are noteworthy for their intimate associations with diverse and dense microbial communities (Taylor et al., 2007a, 2007b). Members of 22 bacterial phyla, the candidate phylum Poribacteria, and two archaeal lineages were identified in sponges so far, many of them forming monophyletic, sponge-specific 16S rRNA sequence clusters (Hentschel et al., 2002; Webster et al., 2009). The majority of these phylogenetically highly diverse and yet sponge-specific microbial consortia remain unculturable. It is generally believed that symbionts contribute significantly to the host's metabolism and biochemical repertoire and possibly also to the evolutionary success of their ancient hosts.

Of special interest is a novel candidate phylum termed ‘Poribacteria’ (Fieseler et al., 2004), which belongs to the Planctomycetes–Verrucomicrobia–Chlamydiae superphylum (Wagner and Horn, 2006). Poribacteria were thus far identified in more than a dozen sponge species from different oceans, suggesting their widespread distribution (Lafi et al., 2009). Vertical transmission, a hallmark of ancient symbioses, of the Poribacteria to the next sponge generation through the reproductive stages has been demonstrated (Schmitt et al., 2008; Webster et al., 2009). Although they were long found exclusively in sponges, some recent studies have reported on the presence of poribacterial DNA in seawater (Pham et al., 2008; Webster et al., 2009). Fluorescence in situ hybridization studies using Poribacteria-specific 16S rRNA-targeting probes showed high abundances of members of this phylum in the mesohyl extracellular matrix and in sponge larvae (Fieseler et al., 2004; Webster et al., 2009). The unusual ring-shaped appearance of poribacterial fluorescence in situ hybridization signals is highly suggestive of cell compartmentation. Indeed, nucleoid-containing bacterial cells were previously visualized by electron microscopy studies of the sponge mesohyl, and the presence of DNA in the compartment was confirmed by immunogold labeling (Fuerst et al., 1999). In this context, the finding of membrane coat-like proteins, which were previously considered exclusive to eukaryotes, in several members of the Planctomycetes–Verrucomicrobia–Chlamydiae superphylum and their localization to inner membranes of the planctomycete Gemmata obscuriglobus is especially noteworthy (Santarella-Mellwig et al., 2010). The first functional genomic information on Poribacteria was obtained by library construction from the microbial consortium of the sponge Aplysina aerophoba (Fieseler et al., 2006; Siegl and Hentschel, 2009). In the present study, we applied WGA to a single poribacterial cell that was obtained from the sponge A. aerophoba by fluorescence-activated cell sorting. This strategy provides nearly 1.9 Mb (Table 1) of poribacterial sequence information, and thus reveals unprecedented insights into the lifestyle of this elusive bacterial phylum. Comprehensive genomic insights regarding poribacterial primary and secondary metabolism, structure of the cell envelope, interaction of Poribacteria with the sponge host and the putative significance of Poribacteria for metazoan evolution are presented.

Table 1 General information about the 454 FLX run and assembly of a poribacterial SAG

Materials and methods

Sponge microbial community extraction and single-cell sorting

The marine sponge A. aerophoba (Verongida, Aplysinidae) was collected in April 2008 by scuba diving offshore Rovinj, Croatia (45°05′N, 13°38′E) at depths of 2–15 m. Sponge-associated prokaryotes were extracted from freshly obtained sponges following an established protocol based on tissue disintegration and differential centrifugation (Fieseler et al., 2004). Purified sponge-associated prokaryotes were subsequently used for single-cell sorting using the fluorescence-activated cell sorting Vantage SE flow cytometer with FACSDiVa option (Becton Dickinson, Heidelberg, Germany) as described previously (Siegl and Hentschel, 2009).

Whole-genome amplification

Fluorescence-activated cell sorting-isolated single microbial cells were disrupted by three cycles of freezing and thawing (−80 and 70 °C; 10 min each) and additional alkaline lysis (Lasken et al., 2005). WGA reactions based on phi29 polymerase-mediated multiple displacement amplification were performed using the REPLI-g Midi kit (Qiagen, Hilden, Germany) according to the manufacturer's recommendations. For the identification of single amplified genomes (SAGs), amplicons were subjected to PCR screenings targeting rRNA genes (bacterial 16S, archaeal 16S, poribacterial 16S, eukaryotic 18S) with subsequent cloning, restriction fragment length polymorphism and sequencing as described previously (Siegl and Hentschel, 2009).

Pyrosequencing of a SAG

The SAG of a member of the candidate phylum Poribacteria was treated with S1-nuclease as recommended (Zhang et al., 2006). Digestion was terminated by adding 2 μl 0.5 M EDTA and heating (at 70 °C for 10 min). The amplified DNA was purified using the QIAamp DNA Mini kit (Qiagen) following the manufacturer's supplementary protocol. Eluted DNA was then subjected to spectrophotometrical DNA quantification. Pyrosequencing was performed by AGOWA GmbH, Berlin, Germany, using the Genome Sequencer FLX System (Roche, Branford, CT, USA). Sequencing reads were assembled using the 454 Newbler assembler version 1.1.03.24.

Sequence annotation

Gene prediction was carried out using the Metagene software (University of Tokyo, Tokyo, Japan; Noguchi et al., 2006). Distributed job processing was performed by a refined version of the GenDB v2.2 system (GenDB, CiBiTec, Bielefeld, Germany) (Meyer et al., 2003). For each predicted open reading frame (ORF), the system retrieves observations from similarity searches against sequence databases NCBI-nr, Swiss-Prot, Kegg (release February 2009), as well as protein family databases Pfam (release 23) and InterPro (release 18, InterProScan 4.3.1). Annotation and data mining was performed by using JCoast (Max Planck Institute for Marine Microbiology, Bremen, Germany), version 1.5 (Richter et al., 2008). Predicted protein-coding sequences were automatically annotated by the MicHanThi software (Max Planck Institute for Marine Microbiology; Quast, 2006). The MicHanThi software predicts gene functions based on similarity searches using the NCBI-nr (including Swiss-Prot) and InterPro database. tRNA genes were identified using tRNAScan-SE (Lowe and Eddy, 1997). The annotation of each protein highlighted within the scope of this study was subjected to manual inspection. For all observations regarding putative protein functions, an e-value cutoff of 10−4 was considered.

Phylogenetic analysis

Sequence alignment and tree construction were conducted using the ARB program package (Technical University Munich, Munich, Germany; Ludwig et al., 2004) and the SILVA 16S rRNA database, version 93 (Pruesse et al., 2007), with all additionally available poribacterial sequences at the SILVA databases in November 2009. Sequence alignment was performed automatically and manually refined using the ARB alignment tool. Phylogenetic trees were constructed using sequences 1100 bp (n=146) only. Shorter sequences (n=8) were added without changing the tree topology through the parsimony interactive tool in ARB. Trees were rooted with 20 sequences belonging to the Deltaproteobacteria. We used three tree construction methods (namely maximum likelihood, maximum parsimony and neighbor joining) in combination with sequence conservation filters for the Planctomycetes–Verrucomicrobia–Chlamydiae superphylum and bootstrap analysis (100 resamplings). Trees constructed with different methods were compared and the maximum likelihood tree is shown. All trees showed the same topology on a phylum level.

Accession numbers

This Whole-Genome Shotgun project has been deposited at DDBJ/EMBL/GenBank under the accession ADFK00000000. The version described in this paper is the first version, ADFK01000000.

Results and Discussion

SAG sequencing

WGAs of single sponge symbiont cells resulted in the identification of the SAG of a member of the candidate phylum Poribacteria (Figure 1). Approximately 28 μg of amplified genomic DNA was obtained as revealed by spectrophotometrical measurement. SAG pyrosequencing generated 105 Mb of raw sequence data, and 1.88 Mb of genomic information organized in 1597 contigs were assembled (Table 1). Two data sets were generated. The first set of 455 contigs harbors at least one ORF per contig and encompasses almost 1.6 Mb of sequence information. A further set of 1142 contigs contains only gene fragments with neither a start nor a stop codon, and therefore these contigs were translated into all six reading frames. References to these partial gene sequences are named by contig name instead of locus tag in this publication.

Figure 1
figure 1

16S rRNA-based phylogenetic tree of the Candidatus phylum Poribacteria and the sister phyla within the PVC superphylum. The sequence obtained during this study is shown in bold. Bootstrap support 75% is illustrated as open circles and bootstrap support 90% is indicated by filled circles. Dashed lines indicate sequences <1100 bp, which were added using the parsimony interactive tool in ARB. Sequence sources (marine sponges and seawater, respectively) are given in brackets. Scale bar represents 10% sequence divergence.

Contamination is a major concern with the amplification of single genomes. PCR screenings of the amplicon from well A3 using primer pairs targeting different rRNA genes (eukaryotic 18S, bacterial 16S, archaeal 16S; Siegl and Hentschel, 2009) were negative (it must be noted that poribacterial 16S rDNA cannot be amplified with the universal eubacterial primers 27f/1492r because of mismatches in the primer-binding region). After WGA product cleanup, a second round of PCR screenings with the primers 27f/1492r led to the detection of a weak PCR product that was due to Delftia DNA, a previously described reagent contaminant (Stepanauskas and Sieracki, 2007). The JCoast genomesDB statistics tool (Richter et al., 2008) showed that DNA contamination is <0.1% (1378 bp/1503 489 bp) and is therefore considered negligible. The following results further support that only a single poribacterial genome was obtained by WGA: (1) A survey of 55 known single copy genes (Mussmann et al., 2007) showed that none of the 29 detected were present in multiple copies in the 454 data set (Supplementary Table S1). (2) Only a single copy 16S rRNA gene was identified, which might additionally point to a slow growing state of the Poribacteria. (3) The calculation of a GC plot with unassembled 454 reads led to a unimodal distribution with a mean of 54%, which is suggestive of a single genotypic sequence source (Supplementary Figure S1).

General genomic features

The poribacterial genome is at least 1.88 Mb in size (Table 2). Overall, 19 tRNA genes and 14 tRNA synthetase genes and gene fragments were identified with specificities for 14 out of the 20 canonical amino acids, suggesting that approximately two-third of the poribacterial genome sequence was obtained. The average GC content of the poribacterial genome is 53%, which is close to the GC content of the metagenomic poribacterial fosmid clone 64K2 (50%; Fieseler et al., 2006). Altogether, 1585 protein-coding genes were recovered from the 454 assembly, 40% of them with unknown function (Table 2). Approximately 24% are hypothetical proteins without any similarities to database entries (Table 2). This low value reflects their distinct phylogenetic position in the eubacterial tree. Analysis of clusters of orthologous groups (Wheeler et al., 2007) distribution indicated that all three major categories (namely metabolism, cellular processes, information storage and processing) and all groups within these are present in our data set (Supplementary Figure S2).

Table 2 General properties of the assembled Poribacteria single amplified genome (SAG)

Primary metabolism

The Poribacteria contain the genomic capacity for aerobic, heterotrophic metabolism. Major parts of glycolysis, tricarboxylic acid cycle and the pentose phosphate pathway (Supplementary Figures S3, S4 and S5), as well as of oxidative phosphorylation (23 complete ORFs) were reconstructed from the 454 data set. Several enzymes involved in purine and pyrimidine metabolism, as well as for all amino-acid biosynthesis pathways are present, thus indicating no auxotrophy at this level. A number of genes coding for degradative metabolism was found. These include nine sulfatases with N-acetylglucosamine-6-sulfate, N-acetylgalactosamine-6-sulfate, choline, mucine and heparane as putative substrates, as well as several peptidases and other enzymes responsible for the degradation of N-glycan. The Poribacteria appear as commensalistic symbionts that aid in, and at the same time benefit from the digestion of food particles.

Two intermediate enzymes of the anaerobic respiratory chain, the nitrite reductase (EC 1.7.2.1) and the nitric oxide reductase (EC 1.7.99.7), were identified. These data provide genomic evidence for denitrification in a sponge symbiont, thus endowing the Poribacteria with the ability to maintain a functional respiratory chain under oxygen-limiting conditions. Whether the complete reduction from nitrate to N2 is possible remains to be investigated. With respect to oxygen, the A. aerophoba mesohyl is well aerated (Hoffmann et al., 2008). However, microaerobic or even anaerobic microhabitats can principally be generated by active microbial metabolism, that is, when the oxygen demand exceeds the oxygen supply. Furthermore, it has been shown that the A. aerophoba mesohyl turns anaerobic during periods of nonpumping. The Poribacteria contain two further assimilatory nitrite reductases (EC 1.7.1.4 and 1.7.7.1), thus reflecting their genomic potential to assimilate nitrite, which might be useful under conditions of seasonal ammonia limitation (Bayer et al., 2008). Furthermore, a 10 ORF containing urease gene cluster was identified including various ABC-transporter components, three urease subunits UreA, UreB, UreC, as well as three accessory proteins (Contig c02128). Therefore, the Poribacteria are capable of using urea to cover their nitrogen needs. Urea is formed in nature by bacterial degradation of nucleic and amino acids, and is therefore a likely product to be encountered in the sponge mesohyl.

The Poribacteria have the genomic repertoire for carbon autotrophy. Autotrophic carbon assimilation has previously been shown for Cenarchaeum symbiosum, a crenarchaeote symbiotically associated with axinellid sponges and the only sequenced sponge symbiont genome to date (Hallam et al., 2006a, 2006b). C. symbiosum was shown to use a modified 3-hydroxypropionate cycle for carbon fixation (Hallam et al., 2006b). Genes encoding for the reductive tricarboxylic acid cycle and the reductive acetyl CoA pathway, also referred to as the Wood–Ljungdahl pathway, were identified on the poribacterial genome (Figure 2). Four partial fragments of the key enzyme of the reductive tricarboxylic acid cycle, citrate lyase (EC number 2.3.3.8), were recovered from the 454 data. All fragments share significant homologies to citrate lyases from Chlorobi, which also use the reverse tricarboxylic acid cycle for carbon fixation. The Wood–Ljungdahl pathway constitutes the most basic way of obtaining organic carbon by the joining of two inorganic carbon molecules (Drake and Daniel, 2004; Ragsdale and Pierce, 2008). In evolutionary terms, the Wood–Ljungdahl pathway can probably be regarded as the most ancient metabolic pathway that might already have been present in bacteria inhabiting the anoxic earth several billion years ago (Ragsdale and Pierce, 2008). The key enzyme of the Wood–Ljungdahl pathway, the oxygen-sensitive acetyl-CoA synthase, also referred to as carbon monoxide dehydrogenase, was identified in multiple copies. Further crucial enzymes within the Wood–Ljungdahl pathway are cobalamin-dependent methyltransferases. In total, three of such enzymes were identified in the poribacterial data set (POR_0033, POR_0034 and POR_0549). The best blastp hits of POR_0033 and POR_0034 originate from Kuenenia stuttgartiensis and of POR_0549 from Desulfococcus oleovorans, both of which are known to be capable of carbon fixation using the Wood–Ljungdahl pathway. All of the three identified methyltransferases possess radical S-adenosylmethionine for methylation and B12-binding domains. Interestingly, a gene cluster containing 11 ORFs affiliated with the metabolism of vitamin B12, the most prominent member of cobalamins, was identified on contig c02038. Therefore, it seems likely that the Poribacteria are capable of vitamin B12 biosynthesis, which in turn serves as a cofactor for one of the key enzymes (methyltransferase) of the Wood–Ljungdahl pathway.

Figure 2
figure 2

Reconstruction of the Wood–Ljungdahl pathway for carbon fixation. Filled circles represent complete ORFs and dashed circles gene fragments. Open circles indicate enzymes absent from the data set. Pathway modeled after studies by Drake and Daniel (2004) and Ragsdale and Pierce (2008).

Polyketide metabolism

The previously known unusually small and phylogenetically distinct Sup-type polyketide synthases (PKSs) are widely distributed in sponge microbiota (Fieseler et al., 2007). The poribacterial 454 data set revealed 11 genomic fragments with homologies to the supA gene, encoding together 48% of the entire PKS (Figure 3). Moreover, two accessory members of the Sup-PKS operon were identified in fragments, that is, two supD gene fragments and five supE gene fragments (Figure 3). The assignment of this elusive Sup-PKS clade to the Poribacteria, as has recently been proposed (Siegl and Hentschel, 2009), was thus proven in this study. In addition, a second putative PKS system was identified (Figure 3). Two ORFs (POR_0547 and POR_0548) show high similarities to the lipopolysaccharide type I PKS WcbR from Nitrosomonas and Burkholderia, as well as to RkpA from Sinorhizobium fredii (Parada et al., 2006). These PKS types are regularly found in sponge metagenomes (Fieseler et al., 2007) and are, in free-living bacteria, usually embedded within lipopolysaccharide gene clusters. Therefore, we can conclude that the Poribacteria are the original producers of at least two different types of PKS systems. Interestingly, homologs of both were shown to be major symbiosis and virulence factors in S. fredii and Mycobacterium tuberculosis, respectively (Minnikin et al., 2002; Parada et al., 2006), and this raises the intriguing possibility that the poribacterial PKS gene products might fulfill a similarly relevant function in the sponge–microbe interaction.

Figure 3
figure 3

Features of the polyketide metabolism in Poribacteria. Display to scale. Abbreviations of PKS functional domains covered: KS, ketosynthase; AT, acyltransferase; DH, dehydratase; ER, enoylreductase; KR, ketoreductase; ACP, acyl carrier protein; R, thioester reductase; ST, sulfotransferase. For both SupE and SupA, two fragments covering the same region were detected (indicated as 3+4). This finding could indicate the presence of multiple copies of the Sup genes on the poribacterial genome. Alternatively, a multimodular organization is conceivable like shown for the PKS from an uncultured bacterial symbiont of Discodermia dissoluta (SA1_PKSA; AAY00025). Upper part: recovery of gene fragments (gray) affiliated with the Sup-PKS system (SupE, SupA, SupD) mapped against fosmid clone pAPKS18 (white) from A. aerophoba (Fieseler et al., 2007). Average homologies (positives on the amino-acid level) were as follows: 75% for SupE and 77% for SupD (both compared with pAPKS18 from A. aerophoba, Fieseler et al., 2007) and 75% for SupA (compared with cosmid clone 1k6 from A. aerophoba, Siegl and Hentschel, 2009). Lower part: recovery of a WcbR-like operon, which is a part of the contig c00157 (26,267 bp). POR_0549 is a radical SAM domain protein, and could therefore be an auxiliary PKS domain with methyltransferating (MT) properties.

Sterol biosynthesis

Sterol biosynthesis is almost exclusively restricted to eukaryotes (for exceptions, see Bode et al., 2003; Pearson et al., 2003; Lamb et al., 2007). This evolutionarily ancient process is believed to have evolved very early in earth history shortly after the evolution of oxygenic photosynthesis. The most primitive sterol pathway exists in G. obscuriglobus (Love et al., 2009). Our data indicate that Poribacteria are capable of sterol formation. Two gene fragments of the key enzyme oxidosqualene cyclase (osc) with homologies to the enzyme from G. obscuriglobus were found (Figure 4). Both fragments possess the specific domain TIGR03463 and one of the fragments additionally covers an intact protosteryl cation-binding region (Pearson et al., 2003). As both G. obscuriglobus and Poribacteria, positioned as sister phyla in phylogenetic trees, most likely possess DNA-containing organelles, it is tempting to speculate that sterols have a key role in the formation of these unusual bacterial structures. In addition, parts of a 24-sterol C-methyltransferase were recovered from our data set (Figure 4). Interestingly, these fragments possess homologies only to those of plants and fungi, which is consistent with the finding that C-24 side-chain modifications were so far exclusively found in eukaryotes (Pearson et al., 2003). However, sponges contain a multitude of C-24-alkylated sterols, some of which are established fossil biomarkers for these animals (Figure 4) (Love et al., 2009). One such important molecule is 24-isopropyl-cholestane, which is virtually resistant to bacterial breakdown and has been used to document the presence of Demospongiae as early as 635 million years ago (Love et al., 2009). This hydrocarbon is derived from 24-isopropyl-sterols, the biosynthesis of which requires the methylation of the sterol side chain catalyzed by a 24-sterol methyltransferase (Kodner et al., 2008). Interestingly, 24-isopropyl-sterols are so far exclusively found in demosponge groups known to harbor Poribacteria (Bergquist et al., 1980). Our findings raise the fascinating possibility that 24-isopropyl steroids may in fact be of poribacterial origin.

Figure 4
figure 4

Putative sterol biosynthesis pathway in Poribacteria. Upper part: recovery of gene fragments (gray) homologous to oxidosqualene cyclase from Gemmata obscuriglobus (white), which is necessary for lanosterol biosynthesis. Average homologies (positives on the amino-acid level) were 57%. Both fragments possess a TIGR03463 domain (2,3-oxidosqualene cyclase). Fragment 1 harbors the protosteryl cation-binding region (PSCS; Bode et al., 2003). Lower part: recovery of gene fragments (gray) homologous to 24-sterol C-methyltransferase from Vitis vinifera (white). Average homologies (positives on the amino-acid level) were 62%. Fragments 2 and 3 do not share significant similarities on the nucleotide level. This finding could indicate that multiple copies of this gene are present. Conserved domains that are covered by the fragments are displayed. We hypothesize that this enzyme is involved in the formation of the demosponge biomarker 24-isopropyl-cholestane by repeated methylation of carbon C24.

Cell envelope

The Poribacteria appear to be derived from a Gram-negative ancestor. Besides genes involved in peptidoglycan biosynthesis, lipopolysaccharide biosynthesis genes were identified. The presence of a periplasm is suggested by the observation that five out of six substrate-binding proteins of ABC transporters do not require anchoring. The finding of a TonB-dependent outer membrane receptor (POR_0881), the TonB protein itself (POR_0882) and the preprotein translocase subunit SecA (POR_0883) further indicates the existence of a periplasm. Besides SecA, several additional translocase subunits were found (for example, YajC, SecD, SecF), as well as the Sec-independent Tat-pathway, which is, to our knowledge, known from Gram-negative and Gram-positive bacteria. With respect to cell division, solely the FtsH protease was detected. This finding is in agreement with the genomic survey of the planctomycete Rhodopirellula baltica (Glöckner et al., 2003). Finally, genes encoding for flagellar assembly and chemotaxis were entirely missing.

Host–symbiont interaction

Several putative host-interaction factors were recovered, that is, cell surface proteins with bacterial Ig-like domains and laminin G domain proteins, which are possibly involved in adhesion. The existence of eukaryotic domains (such as ankyrin, Sel1, fibronectin type III, leucin-rich repeat) provides further support that interactions between Poribacteria and their hosts take place (Taylor et al., 2007a, 2007b). The identification of 23 full or partial genes with tetratricopeptide repeat domains (cl0020) is noteworthy. Interestingly, an abundance of ankyrin and tetratricopeptide repeat proteins was also identified in the microbial metagenome of the sponge Cymbastela concentrica (Thomas et al., 2010). These domains are not only involved in eukaryote–prokaryote interactions but also in mitochondrial and peroxisomal transport in eukaryotes. To elucidate the function of these proteins with respect to the poribacterial intracellular compartment and to symbiosis will be a challenge for future studies.

Conclusions

Sequencing of a SAG derived from a member of the candidate phylum Poribacteria provided detailed insights into the lifestyle of a possibly ancient bacterium symbiotically associated with marine sponges (Figure 5). With regard to primary metabolism, the Poribacteria are mixotrophic bacteria with autotrophic capabilities of CO2 fixation through the Wood–Ljungdahl pathway. They are capable of aerobic and anaerobic respiration. The cell wall resembles that of Gram-negative bacteria. Chemotaxis and flagellar genes are absent from our data set. Analysis of secondary metabolism revealed two PKSs that are frequently found in sponge metagenomic libraries, and we can document in this study the first time their unequivocal appointment to Poribacteria as the producing microorganism. Several putative symbiosis factors such as adhesins and eukaryotic domain-containing proteins were identified, which may be involved in mediating microbe–sponge interactions. The discovery of sterol biosynthesis genes suggests that sterols may be involved in the function of the poribacterial cellular organelle. Furthermore, the presence of a specific gene encoding for sterol methylation might require reevaluation of fossil sponge biomarkers (24-isopropyl-cholestane) used to date the origins of metazoan life on earth.

Figure 5
figure 5

A schematic overview of poribacterial metabolism as deduced from SAG sequencing.