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From an evolutionary point of view, sponges are ideal targets to study marine symbioses as they are the most ancient living metazoans and harbour highly diverse microbial communities. A recently discovered association between the sponge Hemimycale columella and an intracellular bacterium that generates large amounts of calcite spherules has prompted speculation on the possible role of intracellular bacteria in the evolution of the skeleton in early animals. To gain insight into this purportedly ancestral symbiosis, we investigated the presence of symbiotic bacteria in Mediterranean and Caribbean sponges. We found four new calcibacteria OTUs belonging to the SAR116 in two orders (Poecilosclerida and Clionaida) and three families of Demospongiae, two additional OTUs in cnidarians and one more in seawater (at 98.5% similarity). Using a calcibacteria targeted probe and CARD-FISH, we also found calcibacteria in Spirophorida and Suberitida and proved that the calcifying bacteria accumulated at the sponge periphery, forming a skeletal cortex, analogous to that of siliceous microscleres in other demosponges. Bacteria-mediated skeletonization is spread in a range of phylogenetically distant species and thus the purported implication of bacteria in skeleton formation and evolution of early animals gains relevance.
Symbiosis, whereby different biological species live together in intimate, long-term interactions, is regarded as a major source of evolutionary innovation1. Symbiotic associations of animals and microbes are widespread in marine ecosystems and play key ecological roles by contributing in an important, and often cryptic, way to the ecosystem biodiversity and stability. For example, shifts in symbiotic bacterial communities have been attributed to recurrent mass mortalities of corals and sponges2,3,4,5.
From an evolutionary point of view, sponges are ideal targets to study marine microbial symbioses, as they are the most ancient living metazoans on Earth and harbour highly diverse microbial communities6. The establishment of symbiotic relationships between sponges and prokaryotes has been traced back to the pre-Cambrian period7. However, despite the abundance of available sequences from sponge-associated bacteria and their long history, the evolutionary origins of these associations and the adaptive traits of the species involved are only beginning to be understood8,9,10,11.
Recently, a symbiotic association between the Atlanto-Mediterranean sponge Hemimycale columella (Bowerbank, 1874) and an unidentified calcifying bacterium, has been shown to produce thousands of calcite spherules12. The calcifying bacteria are contained within vacuoles in amoeboid, archaeocyte-like cells13, or ‘calcibacteriocytes’, where they divide by bipartition before becoming enclosed within a 100-nm thick calcite envelope. The calcifying bacterium is vertically transmitted to the sponge progeny12 via phagocytosis of maternal calcibacteriocytes as embryos grow14. Uriz et al.12 speculated that this type of eukaryote-prokaryote symbiosis might represent a relict mechanism involved in the evolution of skeletons in Lower Metazoa. Later, Blanquer et al.15 used pyrosequencing to retrieve a dominant alpha-proteobacterium in H. columella that represented up to 67% of the total sequences in the sponge and was similar to that obtained from the sponge Cliona viridis (Schmidt, 1862).
To gain insight into this newly identified symbiosis and its possible role in the evolution of skeletons in Lower Metazoa, we investigated whether the dominant alpha-proteobacteria reported by Blanquer et al.15 corresponded to the extremely abundant calcifying bacteria that form calcareous spherules in the sponge tissues12. We also explored the molecular diversity of the symbiotic calcibacteria, and their presence in other sponge species, to assess the occurrence of this symbiosis across sponges and oceans. Moreover, we explored whether the calcibacterium of H. columella is evenly distributed within the sponge tissues or accumulate in particular sponge zones, thus, fulfilling a potential skeletal function, and analyse the purported costs and benefits for the symbiotic partners.
To achieve these objectives, we performed ultrastructure studies using transmission electron microscopy (TEM) and scanning electron microscopy (SEM), and designed a molecular probe based on the dominant bacterial species of H. columella. We also conducted CARD-FISH experiments and cloned the 16S rRNA gene of the calcibacterium from H. columella and C. viridis to examine their phylogenetic relationships.
Morphologically similar calcareous spherules, 1μm in size, were observed in the sponges Hemimycale columella, Cliona viridis, Prosuberites sp., Crella cyathophora (Carter, 1869) (Fig. 1), and Cinachyrella alloclada (Uliczka, 1929) (not shown). Profuse numbers of spherules were released from the squeezed tissues of all the sponge species examined, except in C. viridis and C. alloclada, where they were less abundant.
The calcareous spherules were concentrated at the periphery of whitish individuals of H. columella (Fig. 2a,b). Moving sponge cells (calcibacteriocytes) full of calcified calcibacteria were recorded immediately after sponge disaggregation (Fig. 2c), which confirmed the amoeboid-like properties of these cells and their capacity to transport calcibacteria across the sponge tissues.
SEM images of H. columella (whitish morph) showed huge numbers of calcareous spherules that had been released into the sponge mesohyl (Fig. 2b), as well as abundant, 10–15μm calcibacteria-full calcibacteriocytes (Fig. 2d). The calcareous spherules were accumulated at the sponge periphery (Fig. 2b) forming a 2–3mm thick layer, which concurred with light microscope observations (Fig. 2a). Some calcibacteriocytes showed hemispherical, ca. 1μm in diameter holes, which corresponded to the space previously occupied by released calcibacteria (Fig. 2d). There were frequent images of calcibacteria enclosed within the calcareous coat as they divided (Fig. 3c).
TEM pictures of calcibacteriocytes showed abundant cellular vacuoles containing single or dividing calcibacteria (Fig. 3a). Most vacuoles contained a single bacterium, but several bacteria were also observed enclosed within a common calcareous coat after successive incomplete divisions (Fig. 3c). Calcified calcibacteria degraded in most cases, as indicated by the scarce or absent organic content within the calcareous crusts, but also formed condensed bodies, ca. 200nm in size, that might correspond to starved forms (Fig. 3b). Uncalcified calcibacteria were spherical and relatively small (ca. 0.2–0.8μm in cross-section), showed a thin bacterial wall and were found abundantly in the mesohyl of sponge larvae, after being released from engulfed maternal cells (Fig. 3f). There, they divided profusely by bipartition (Fig. 3g). Archaeocyte-like embryo cells (newly differentiated calcibacteriocytes) contained calcified calcibacteria (Fig. 3e). The calcareous crust that surrounded calcibacteria was clearly visible in SEM images of samples that were fixed for just 2h (see methods) (Fig. 3h).
Table 1 shows the best 18 nt. long probe that targeted the prevalent alpha-proteobacteria sequence in H. columella (CAL32), as well as the 5′–3′ helpers, and competitors.
The non-sense probe, which was used as a negative control, did not hybridize in the samples (images not shown), and no hybridization occurred when the specific probe was assayed in the species Crambe crambe (Schmidt, 1862) (negative sponge control, images not shown), which confirmed that the hybridization signal observed was not an artefact and corresponded to the target calcibacteria.
CARD-FISH using the designed probe (CAL32L), helpers, and competitors allowed us to detect the presence of the target Ca. Calcibacterium at high densities within the tissues of H. columella, (adults and larvae) and Prosuberites sp. and at lower densities in C. alloclada and C. viridis (Fig. 4). There were numerous hybridization points in the sponge mesohyl and within sponge cells (calcibacteriocytes) (Fig. 4g,h,i). Similarly, isolated calcibacteria from H. columella tissue on filters also hybridized in high numbers (Fig. 4a,b). This confirmed that the bacteria, which form the calcareous spherules within calcibacteriocytes, corresponded to the dominant alpha-proteobacteria sequence of H. columella.
The DAPI staining showed two discrete cell sizes, corresponding to DNA material from sponge cells and calcibacteria. Strong hybridization signals that overlapped with the majority of the DAPI-stained small points were observed with the CAL32L specific probe (Fig. 4a,b) in both tissue sections and extracted calcified calcibacteria, which proved the correspondence of the target bacteria with the calcareous spherules and the abundance of calcibacteria in the sponge tissues and cells. Negative controls, including the non-sense probe, a confirmed calcibacteria-free sponge, and a non-probe control yielded no hybridization signals confirming the precision of the hybridization and a lack of endogenous peroxidases in the sponge tissue. However, a few other non-hybridized bacteria were also DAPI stained in the sponge tissues. Moreover, although targeting cyanobacteria CARD-FISH was not performed, sporadic red/orange fluorescence was observed under green excitation (Fig. 4), indicating the occasional presence of photosynthetic bacteria in the sponge tissues.
Two-way ANOVA with colour morph and sponge zone as orthogonal factors (5 replicates per zone and colour morph) showed significant differences (N=5, F=12.14, p<0.05) in the number of calcibacteria extracted from H. columella tissues and recorded through epifluorescence microscopy (EM) (Fig. 5a). However, the interaction between colour morph and sponge zone was also significant (p<0.05), so that the abundance of calcibacteria in the two colour morphs depended on the sponge zone considered. T-tests on colour morph and sponge zone separately showed that whitish morphs had significantly higher numbers of calcibacteria (i.e. hybridized points) in the ectosomal region than pinkish morphs (t-value=−3.98, p<0.001), whereas there were no differences in calcibacteria density between the choanosomes of both colour-morphs (t-value=0.52, p=0.67). Confocal microscopy of sponge sections confirmed the significant differences in calcibacteria density in the extracted spherules observed using EM (N=3 each colour, Z=−1.96, p<0.05, Mann-Whitney test) (Fig. 5b). Together, these results confirmed that calcified calcibacteria accumulated in large numbers at the sponge ectosome, conferring a whitish tinge to some individuals of H. columella, and that bacterial DNA remained within the calcareous spherules for an undetermined time after bacteria became calcified.
Larvae contained lower numbers of calcibacteria than adult tissue as non-reproductive individuals showed higher fluorescence values per tissue unit (Z=7.32, p<0.001, Mann-Whitney test) than sponges harbouring abundant larvae (Fig. 5c). The presence of larvae in reproductive individuals decreased the total integrated fluorescence of the sponge sections.
Cloning 16S rRNA gene of the bacterial symbionts present in H. columella and C. viridis allowed us to recover two sequences, ca. 1,400 nt. long, that contained the 273 nt. calcibacterium fragment.
Bayesian phylogenetic reconstruction using the cloned sequences, plus their closest neighbouring sequences in the 16S SILVA database and several outgroup sequences, retrieved a well-supported calcibacteria clade (1, posterior probability) that clustered bacteria from sponges harbouring calcareous spherules similar to those of H. columella along with sequences from two corals and two tropical seawater bacteria (Fig. 6). The calcibacteria clade contained 17 sequences, belonging to seven distinct calcibacteria OTUs with >98.5% intra-OTU similarity, which would correspond to seven calcibacteria species according to Kim et al.16. The calcifying bacterium of C. cyathophora differed from our cloned sequences of C. viridis and H. columella, in >5% and likely belonged to a different genus17.
According to the Bayesian phylogeny, the calcibacteria clade belonged to SAR116 (Alpha-proteobacteria), which appeared as a sister clade of some Rhodospirillales. It was split in two well supported subclades (1, posterior probability): subclade A contained the clone of H. columella (GenBank ID:KU985279), and that of the Alcyonacea coral Erythropodium caribaeorum (Duchassaing & Michelotti, 1860), and another clade with two bacterial sequences from tropical marine waters; subclade B clustered the C. viridis clone (GenBank ID: KU985280) with a clone from the Alcyonacea coral Scleronephthya gracillimum (Kükenthal, 1906) (previously Alcyonium gracillimum) from the North Pacific. This subclade was a sister clade of the C. cyathophora clone from the Indo-Pacific.
Ultrastructure images combined with molecular analyses have significantly improved our understanding of the symbiosis first discovered between Hemimycale columella sponges and calcibacteria. The specific probe designed enabled us to confirm the identity of the endosymbiont calcifying bacteria, which was surrounded by a calcareous crust, to quantify their abundance within the sponge tissues of H. columella, and to prove their accumulation at the sponge periphery, which suggest an exoskeleton function. A thin bacterial wall was made evident through TEM in healthy bacteria, which contradicts the lack of bacterial wall suggested by Uriz et al.12. The phylogenetic reconstruction of near-complete 16S sequences from cloned H. columella and Cliona viridis classified the calcibacteria within the SAR116, close to one of the three Rhodospirillales clades18.
Altogether, the results from CARD-FISH and bacterial phylogeny indicate a temperate-warm geographical distribution of this symbiosis, which comprises at least seven bacterial OTUs and two potential genera, and appears to include demosponges and cnidarian hosts. The inclusion of two bacteria sequences from tropical waters within the calcibacteria clade suggests the presence of calcibacteria stocks in the water from which sponges and cnidarians might acquire them. Indeed, the symbiosis may be propagated by two mechanisms: vertical transmission from maternal tissues to the progeny, as evident in our study, and horizontal transmission from the environment, as suggested by the presence of free calcibacteria in seawater. Redundant mechanisms for assuring a relevant biological function are frequent in nature19 and two acquisition modes of symbiotic microbes have also been reported for other sponges20.
In marine environments, calcium carbonates and calcium phosphates are the most commonly precipitated minerals and have formed most invertebrate skeletons since the Cambrian explosion21. Particular metabolisms of both autotrophic and heterotrophic bacteria are known to induce mineralisation22,23,24,25,26,27,28,29. However, only a few cases of calcium precipitation mediated by endosymbiotic microorganisms have been reported so far in marine eukaryotes: calcification is facilitated by symbiotic microalgae (Phaeocystis) in the radiolarian Acantharia30, and by bacteria in the Foraminifera31.
Increased pH, which may result from bacterial metabolism, could promote calcium precipitation. Significant increases in pH have been recorded during the growth of Escherichia coli32, and an increased pH of at least one unit above seawater pH fostered calcification in Foraminifera vacuoles, even at high Mg2+and low Ca2+concentrations and low temperature33.
In our target symbiosis, calcification occurred within sponge cell vacuoles. We propose that the vacuole microenvironment changed over the course of bacterial growth, as nutrients are removed from the medium and bacteria expel waste products into the medium (Fig. 7). As a consequence, the pH of the vacuole may increase, and calcium carbonate nucleation and precipitation on the bacteria membrane is biologically induced34. A similar process of calcification has been observed in experimental studies of Chromohalobacter marismortui28.
In general, sponge skeletons are either siliceous or calcareous35. Only a few relict sponges (the sclerosponges), which formed sponge reefs during the late Palaeozoic and Mesozoic eras36, have a double mineralisation system. Some parallels can be drawn between sclerosponges and the sponge species in this study. Both have siliceous spicules and a complementary calcareous skeleton layer. In both cases, spherules (spherulites in sclerosponges) are produced within the vacuoles of sponge cells (sclerocytes in sclerosponges or calcibacteriocytes in sponges in this study), which are then excreted and accumulate at the sponge periphery. However, some differences between the calcareous bodies produced by the two sponge types should be noted. In the sclerosponge Astrosclera willeyana Lister, 1900, calcareous bodies are solid, and 5μm in diameter, and become cemented forming a mass skeleton at the sponge base37, whereas those of the sponges in this study are hollow and 1μm in size, and remain free forming a cortical layer analogous to the siliceous, microsclere-constructed cortex of some Astrophorida demosponges35.
Studies on the formation of intracellular spherulites in the sclerosponge A. willeyana also report parallel traits with the bacteria-mediated calcareous spherules. Jackson et al.38 proposed that sponge genes of bacterial origin promoted calcification. Later, Jackson and Wörheide39 suggested that sponge cells use the remains of intracellular bacteria as a framework on which to initiate calcification. In both cases, the bacterial wall may act as a nucleation centre for the precipitation of calcium carbonate. Calcification, resulting in either 5μm spherulites or 1μm spherules, appears to be caused by the particular conditions (e. g. host enzymes or increased pH) in the sponge vacuoles, as it occurs within cell vacuoles.
It has been reported that many symbiotic microorganisms do not grow unconstrained in hosts40. Conversely, it is generally accepted that for mutualistic symbioses to become evolutionaryly fixed, benefits at the species level should compensate for the costs to the associated partners41. The most obvious benefit to sponges from their association with calcifying bacteria is the ‘low cost’ construction of an exoskeleton, which may serve as structural purpose and deter potential sponge predators better than secondary metabolites42. Protection against an increase in predators has been proposed as an evolutionary driver of exoskeletons in ancient animals during the Cambrian explosion43. By assuming that calcium precipitation around the bacteria is spontaneously triggered by increases in pH within the vacuole, the only cost of formation of the sponge exoskeleton would be the transport of calcified calcibacteria to the sponge peripheral zone.
However, the sponge mechanism of particle capture and transport may have not evolved primarily for bacteria. Calcibacteriocytes do not differ significantly from archaeocytes, which are moving cells that are genetically programmed to remove debris and undesired substances from the sponge mesohyl14. Archaeocyte-like cells pack bioactive metabolites in the form of spherules to prevent sponge self-toxicity44,45. These spherule-containing cells, or spherulous cells from their ultrastructural aspects46, have been observed to migrate to the sponge surface where toxins are released to the sponge boundaries to function in deterrent and/or allelochemical roles44.
In contrast, the benefits for calcibacteria are more difficult to ascertain. It has been experimentally demonstrated that some symbiotic microorganisms have an increased reproductive capacity and higher fitness within hosts relative to non-host environments47. Sponge tissues might offer protection from pathogens and predators, which are abundant in non-host environments40, and buffer nutrient ocean fluctuations that prevent the steady growth of bacteria over long periods48. However, considering the detrimental consequence of calcification for the bacteria, calcibacteria may also be more akin to ‘prisoners’ or ‘farmed crops’ than equal partners as in other bacteria-invertebrate symbioses40. Benefits might therefore be related to the propagation of the species. Symbiosis ensures that calcibacteria persist across sponge generations via the vertical transmission to sponge progeny. Moreover, the presence of free calcibacteria in seawater also suggests that viable calcibacteria are released back into the environment, which would allow the bacteria to form a species reservoir to facilitate dispersal and colonization of new invertebrate hosts.
Symbiotic relationships have been observed to be mostly stable over the lifetime of an individual host, from generation to generation, and over evolutionary time49. Thus, mechanisms must have evolved to correct potential deviations from the necessary holobiont homeostasis. In the calcibacteria-sponge association, the host should predominantly maintain proliferation of the dominant bacteria to a level compatible with host survival. Calcification appears to be the cost to bacteria for living in a more stable, predator-free, nutrient-rich environment. Once calcification prevents metabolic exchange between the bacteria and the vacuole medium, the calcibacteria may degrade or become starved. However, according to our TEM images, calcified calcibacteria recovered a steady growth phase as calcibacteriocytes broke and released purported resistant forms into the nutrient-rich mesohyl of sponge larvae. Then larval archaeocyte-like cells may engulf and transport them into cell vacuoles where calcification occurred (Fig. 7). This interpretation is based on H. columella observations but it can be safety extrapolated to other calcibacteria-bearing sponge species, as the cellular types involved in the process are similar in all of them (images not shown).
The current-day animal-bacteria symbioses, which likely existed when animals first appeared50, can provide key insights into Metazoa evolution. The reporting of bacteria-mediated calcification mechanisms in phylogenetically apart sponges suggests the implication of bacteria in the early evolution of the skeleton in the pre-Cambrian metazoans51. Although several molecular mechanisms are responsible for calcium precipitation and skeleton formation in Lower Metazoa52, those involving bacteria might be evolutionarily older and, thus, acquire new relevance in the light of these results. Paleogenomics approaches may help in the near future to confirm the presence of calcifying bacteria in early animals.
The sponge species studied all harboured 1μm diameter calcareous spherules, similar to those reported in Hemimycale columella12 (Fig. 1). From one to three samples per species (depending on the species availability) were collected by SCUBA diving between 10 and 30m depth in several seas: H. columella (whitish and pinkish morphs) and Cliona viridis from the Northwestern Mediterranean (Arenys de Mar, Spain); Protosuberites sp., and Cinachyrella alloclada from the Caribbean Sea (Florida, USA), and Crella cyatophora Carter from the Red Sea (Sharm el-Sheikh, Egypt).
Samples were preserved and treated according to the study purposes:
Different analyses were performed on different sub-sets of sponge species (see Supplementary Table S1).
We quantified the calcibacteria in the same set of H. columella individuals by two procedures to confirm that the calcibacteria were inside the calcareous spherules and to avoid possible biases in bacteria quantification in hybridized sponge sections due to signal overlapping in Epiflourescence Microscopy (EM):
Calcibacteria spherules were exhaustively extracted from fresh H. columella pieces. Pieces of ca. 1g of fresh sponge (three individuals per colour morph and two regions per individual) were disaggregated and homogenized. Siliceous spicules were precipitated and then the pellet was discarded. The spicule-free homogenates were subjected to a series of centrifugations and re-suspensions42. One aliquot of the each final spherule suspensions (three per individual) was filtered through 0.2μm pore filters and filters were CARD-FISH treated (Table 1).
An oligonucleotide probe targeting the prevalent alpha-proteobacteria sequence in the sponge H. columella was designed using ARB software (http://www.arb-home.de/). The target sequence matched with two alpha-proteobacteria from the water column (GenBank ID: KC425597.1; GenBank ID: EF471706) and another from the cnidarian Erytropodium caribaeorum (GenBank ID:889934.1). The best probe was checked in silico with the online software MathFish (http://mathfish.cee.wisc.edu/) and its efficacy confirmed using the probe match tool in ARB. We also designed two ‘competitor sequences’ to avoid non-specific hybridizations, and two ‘helper sequences’ (Table 1) to hybridize the flanking regions of the specific probe. A non-sense probe (Non-EUB 338-I 5′-ACTCCTACGGGAGGCAGC-3′)55 was used as a negative control (Table 1). All the probes were synthesized using Biomers (http://www.biomers.net/).
We used CARD-FISH with the designed probe to verify whether the dominant sequence in the species H. columella corresponded to the abundant intracellular calcifying bacteria, observed using TEM and SEM, and to detect its presence in other sponge species harbouring 1μm diameter calcareous spherules: H. columella (Poecilosclerida, Hymedesmiidae), C. viridis (Hadromerida, Clionaidae), Protosuberites sp. (Hadromerida, Suberitidae), and C. alloclada (Spirophorida, Tetillidae). CARD-FISH was also used to quantify calcibacteria within the main sponge regions (ectosome and choanosome) of whitish and pinkish morphs of H. columella (N=3) and in two stages of the sponge life cycle: reproductive individuals incubating larvae and non-reproductive individuals.
Tissue samples that were fixed in 4% paraformaldehyde were dehydrated, embedded in paraffin, cut, deparaffined, and subjected to membrane permeabilization and inactivation of endogeneous peroxidases following procedures listed in Table 1 (modified from Pernthaler & Pernthaler56). Filters containing the extracted calcareous spherules were directly subjected to bacteria membrane permeabilization and inhibition of endogenous peroxidases. The optimum formamide concentration for the specific probe (i.e. 45%) was determined from assays at concentrations of 55%, 45%, and 35%. Following CARD-FISH, the sponge sections and the isolated spherules were DAPI stained to observe DNA. Dehydrated samples were mounted using Citifluor.
To discount self-fluorescence from the hybridized tissue, three sponge sections were treated according to the CARD-FISH protocol without adding the probe. Moreover, hybridization was assayed in tissues of the sponge Crambe crambe, a species that does not harbour the target calcibacteria57, to confirm that the hybridization signal observed was not an artefact.
Hybridization was conducted on extracted calcibacteria from the sponge ectosome and choanosome of whitish and pinkish morphs. The resulting calcibacteria were re-suspended in sterilized seawater and an aliquot of this suspension was filtered through a 0.2μm polycarbonate filter. Filters containing the calcibacteria were hybridized using CARD-FISH and observed using an epifluorescence microscope (EM) (Axioimager, Zeiss). Pictures were captured from 10 randomly selected fields at 100×magnification using an Axiocam MR3 (Zeiss) digital camera (820ms exposure time) attached to the microscope. We divided each field into 16 quadrats and counted the number of calcibacteria (hybridization points) in four randomly selected quadrats using Adobe Photoshop. The average number of calcibacteria per quadrat was multiplied by a factor related to the spherule concentration in the initial suspension.
We quantified calcibacteria in whitish and pinkish morphs of H. columella (N=3) using a Leica TCS-SP5 confocal spectral microscope (Leica Microsystems Heidelberg GmbH, Universitat Autònoma of Barcelona) with a Plan-Apochromatic 63 ¥ 1.4 (oil HC ¥ PL APO lambda blue objective). A series of images (three fields per section) were taken every 1μm (axis-z) across 6μm thick histological sections to observe the emission signals of Alexa 488 and DAPI. The images were processed using Metamorph Imaging software (Universal Imaging Corporation, West Chester, PA, USA). We measured the integrated fluorescence intensity of the signal emitted by hybridized bacteria after removing the background fluorescence from the control samples.
Samples of C. viridis and H. columella were submersed in absolute ethanol immediately after collection and taken to the laboratory in a cooled container. H. columella was extracted using Qiamp DNA stool kit (Qiagen) and C. viridis with DNeasy blood and tissue kit (Qiagen). One 16S rRNA gene fragment, ca. 1,450 nt. in size, was amplified using universal primers 26F and 1492R58. PCR conditions were as described previously59. PCR products were purified using QIAquick PCR Purification kit (Qiagen) and cloned using TOPO® TA Cloning® Kit for sequencing using One Shot® TOP10 Chemically Competent E. coli (Invitrogen), according to the manufacturer instructions. Following colony growth, correct-size inserts were identified using PCR with T3–T7 primers, and purified and sequenced using the Sanger method (Macrogen Europe). Sequences containing the 273 nt. calcibacteria fragment15 were selected and aligned with the SILVA database using SINA web aligner. The alignment was merged into ARB software and improved using the Fast Aligner tool according to the secondary structure.
Normality and homoscedasticity of data was verified60. Differences in calcibacteria abundance between sponge zones in different colour morphs were analysed using two-way ANOVA, with sponge colour (whitish or pinkish) and zone (ectosome or choanosome) as fixed orthogonal factors. Integrated fluorescence intensities obtained using CLSM were analysed using the Mann Whitney U-test, since data did not meet the assumptions of normality and/or homoscedasticity. Cloned sequences containing the 273 nt. calcibacterium fragment5, and the closest sequences were exported from ARB and used to construct a Bayesian phylogenetic tree using MrBayes 3.2 software. The GTR evolutionary model was used. Four Markov Chains were run with ten million generations sampled every 1000 generations. The chains converged significantly and the average standard deviation of split frequencies was less than 0.01 at the end of the run. Early tree generations were discarded by default (25%) until the probabilities reached a stable plateau (burn-in) and the remaining trees were used to generate a 50% majority-rule consensus tree.
The threshold used for considering a group of sequences belonging to the same “species” (now OTU) was a sequence similarity higher than 98.5% 16 while similarities >95% suggest same genus17.
How to cite this article: Garate, L. et al. Endosymbiotic calcifying bacteria across sponge species and oceans. Sci. Rep. 7, 43674; doi: 10.1038/srep43674 (2017).
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We thank K. Rützler, E. Ballesteros, M. Bolivar, C. Diaz, and J. Lopez for providing sponge samples, J. C. Auguet, C. Restrepo and S. Merbt for helping with probe design and CARD-FISH, C. Huete-Stauffer for cloning help, and M. Roldan for Confocal Microscopy technical support. The research has been funded by MARSYMBIOMICS project (Spanish MINECO, CTM2013-43287-P) BluePharmTrain (FP7 People-INT, Ref. 2013- 667786), and Grup Consolidat SGR-120, to MJU. LG benefited from a fellowship within the Benthomics project (Spanish MICINN, CTM-2010-22218-C02-01).
The authors declare no competing financial interests.
Author Contributions L.G. performed sampling, microscope observation, CARD-FISH, cloning, phylogenetic reconstructions and wrote the manuscript. J.S. designed the calcibacteria probe and conducted sampling and CARD-FISH experiments, and contributed to the manuscript writing. G.A., helped with probe design and CARD-FISH, participated in microscope observation and analyses, and contributed to the manuscript writing. M.J.U. designed the study, interpreted the results, led manuscript writing and integration.