ORIGINAL RESEARCH article

Front. Mar. Sci., 05 June 2019

Sec. Microbial Symbioses

Volume 6 - 2019 | https://doi.org/10.3389/fmars.2019.00297

Prokaryotic Diversity and Community Patterns in Antarctic Continental Shelf Sponges

  • 1. Institute for Chemistry and Biology of the Marine Environment, Carl von Ossietzky University of Oldenburg, Oldenburg, Germany

  • 2. Genomic and Applied Microbiology and Göttingen Genomics Laboratory, Institute of Microbiology and Genetics, University of Göttingen, Göttingen, Germany

  • 3. Senckenberg Research Institute and Nature Museum, Frankfurt, Germany

  • 4. Department of Earth and Environmental Sciences and GeoBio-Center, Ludwig-Maximilians-Universität München, Munich, Germany

  • 5. Helmholtz Institute for Functional Marine Biodiversity, Carl von Ossietzky University of Oldenburg, Oldenburg, Germany

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Abstract

Marine sponges (Phylum Porifera) are globally distributed within marine and freshwater ecosystems. In addition, sponges host dense and diverse prokaryotic communities, which are potential sources of novel bioactive metabolites and other complex compounds. Those sponge-derived natural products can span a broad spectrum of bioactivities, from antibacterial and antifungal to antitumor and antiviral compounds. However, most analyses concerning sponge-associated prokaryotes have mainly focused on conveniently accessible relatively shallow sampling locations for sponges. Hence, knowledge of community composition, host-relatedness and biotechnological potential of prokaryotic associations in temperate and cold-water sponges from greater depths (mesophotic to mesopelagic zones) is still scarce. Therefore, we analyzed the prokaryotic community diversity of four phylogenetically divergent sponge taxa from mesophotic to mesopelagic depths of Antarctic shelf at different depths and locations in the region of the South Shetland Islands using 16S rRNA gene amplicon-based sequencing. In addition, we predicted functional profiles applying Tax4Fun from metagenomic 16S rRNA gene data to estimate their biotechnological capability and possible roles as sources of novel bioactive compounds. We found indications that cold and deep-water sponges exhibit host-specific prokaryotic communities, despite different sampling sites and depths. Functional prediction analysis suggests that the associated prokaryotes may enhance the roles of sponges in biodegradation processes of xenobiotics and their involvement in the biosynthesis of secondary metabolites.

Introduction

Marine sponges (Phylum Porifera) are taxonomically highly diverse with so far ∼ 9115 accepted species, which are distributed within marine and freshwater ecosystems (van Soest et al., 2012, 2018). Along with the vast phylogenetic diversity of the Porifera phylum, sponges are also known to host a dense and diverse microbiota, consisting of prokaryotes, uni- and multicellular eukaryotes (Taylor et al., 2007). Recent advances in sequencing technologies and the collaborative effort of a global sponge microbiome sequencing project found 63–72 prokaryotic phyla (including candidate phyla) among 268 sponge species (Moitinho-Silva et al., 2017b). However, most analyses concerning diversity and host-relatedness of sponge-associated microorganisms, such as bacteria or archaea, focused mainly on relative conveniently accessible sampling locations. Hence, most prokaryotic diversity studies account for sponges collected in relatively shallow coastal locations, with an additional tendency toward tropical and subtropical sponge species (Webster et al., 2010; Schmitt et al., 2012; Steinert et al., 2016; Thomas et al., 2016). Consequently, the knowledge of community composition, host-relatedness and potential functions of prokaryotic associations in temperate and cold-water sponges from greater depths is still scarce. The technical complexities and financial costs, which are related to the goal to reach the seafloor beyond technical diving depths, makes thorough sampling and methodological fieldwork either very challenging or even impossible. Therefore, the sparse existing sponge-associated prokaryotic diversity studies that encompass mesophotic to mesopelagic zones in various temperate and cold-water environments were often constrained by either only a few available sponge species, low or missing replication or the collection along large depth gradients and geographic locations (Webster et al., 2004; Xin et al., 2011; Jackson et al., 2013; Schöttner et al., 2013; Kennedy et al., 2014; Reveillaud et al., 2014). To the best of our knowledge, only two prokaryotic diversity characterization studies have been conducted in the Antarctic region with marine sponges collected from two coastal shallow sampling sites using high throughput sequencing (Rodríguez-Marconi et al., 2015; Cárdenas et al., 2018). Therefore, most of the prokaryotic diversity in Antarctic sponges from greater depths and the potential prokaryotic metabolic functions still remain unknown.

Closing this knowledge gap is crucial considering that sponges in general are prolific sources of secondary metabolites (Blunt et al., 2016; Indraningrat et al., 2016) and that the marine fauna in greater depths can also be considered as a rich source of novel natural products (Skropeta, 2008; Schupp et al., 2009; Skropeta and Wei, 2014). While results are still scarce emerging evidence indicates that North-Atlantic (Jackson et al., 2013; Kennedy et al., 2014) or Antarctic (Webster et al., 2004; Xin et al., 2011; Rodríguez-Marconi et al., 2015) cold- and/or deep-water sponges harbor diverse prokaryotic communities. Moreover, deep-sea sponges from the Atlantic exhibited novel secondary metabolite synthetic gene clusters of potential prokaryotic origin (Borchert et al., 2016), and Antarctic deep-water sponges proved to be rich sources of bioactive natural compounds (Turk et al., 2013; Berne et al., 2016; Botić et al., 2017; Angulo-Preckler et al., 2018; Mangano et al., 2018). Consequently, further studies on sponge-microbe associations from rarely accessed environments, such as the Antarctic shelf have the potential to lead to the discovery of novel metabolic mechanisms and bioactive natural compounds for a vast range of biotechnological applications (Sipkema, 2016).

Still overlooked are the xenobiotics degradation and metabolism capacities of the sponge-associated microbiota. The related pathway class comprises a set of metabolic pathways, which are involved in the metabolic breakdown of drugs and pollutants or the degradation of secondary metabolites foreign to the organisms degrading these compounds. Although research on marine sponges indicated already their capability in the biodegradation of xenobiotics, the presence of multixenobiotic resistance mechanisms or their ability to act as bioindicators for xenobiotic-related environmental stress has only been investigated for sponge-associated microbes to a very limited extent (Müller et al., 1996, 1998; Wagner et al., 1998; Krasko et al., 2001; Perez et al., 2002). The role of the sponge microbiota in some of these processes has mostly been restricted to reports on the presence of xenobiotics biodegradation pathways derived from the available sequence data (Lesser et al., 2016). However, there is a need for an initial evaluation of the bioremediation capabilities of marine sponges and their associated prokaryotic communities due to an increased awareness of a widespread marine pollution problem and its possible impact on the Antarctic marine environment (Goerke et al., 2004; Narayanaswamy et al., 2014; Courtene-Jones et al., 2017).

In the present study 16S rRNA gene amplicon data from sponge-associated prokaryotic communities was used to investigate two aims. First, we analyzed the diversity and composition of prokaryotic communities of four sponge taxa, Antarctotetilla leptoderma, Haliclona sp., Homaxinella balfourensis, and Isodictya bentarti, collected at the Antarctic shelf around the South Shetland Islands from various depths (96–469 m) (Figure 1). In addition, we investigated the influence of sponge-host identity on the prokaryotic community variance. Secondly, by applying the Tax4Fun functional gene profile prediction software with sponge prokaryotic community 16S rRNA gene data as input, we predicted functional profiles using 16S rRNA gene data to estimate the biotechnological capability and especially the potential roles of the associated prokaryotic communities as sources for novel bioactive compounds and in the degradation of xenobiotics. Corresponding with the present prokaryotic diversity and community, to our knowledge, only little or nothing is known about metabolic functions and secondary metabolites produced by the present sponges and / or their associated prokaryotic community. On the basis of the taxonomic status of the present Haliclona sp. specimens a comprehensive assessment regarding its known bioactivity is difficult. Nonetheless, different Haliclona taxa are already identified as hosts of several bioactive bacteria and sources of secondary metabolites (Erickson et al., 1997; Santalova et al., 2007; Kennedy et al., 2009; Khan et al., 2011; Turk et al., 2013; Viegelmann et al., 2014). In contrast, for the remaining three sponge taxa information is scarce, with only H. balfourensis known to contain stanols (Santalova et al., 2007). However, the here predicted metabolic functions remain to be validated by metagenomic or whole genome sequencing in future sponge microbiome studies. Nonetheless, predictive functional profiling from 16S rRNA gene sequence data can serve as a complementary and cost-effective metagenomic pre-study.

FIGURE 1

Materials and Methods

Sample Processing and Sponge Taxonomy

During the expedition of the research vessel “Polarstern” to the Southern Ocean in the Antarctic Peninsula in 2012 (ANT-XXVIII/4), 15 sponge specimens, comprising four sponge taxa, were collected by dredging from different depths (96–469 m) and sites located near the South Shetland Islands (Table 1). Collection of each specimen via dredging could have caused contamination with the surrounding sediments. To minimize the risk of such environmental contamination dissected specimens were rinsed with 0.2 μm filtered seawater. The sponges were photographed and subsequently dissected (Figure 1). Smaller tissue samples were stored in EtOH (70%) for molecular analyses, while larger tissue parts were stored in EtOH (70%) as vouchers for morphological identification. All samples were stored at -20°C until further processing. In addition, 12 seawater samples were collected at several stations from the same area at 20 m depth using Niskin bottles attached to a conductivity-temperature-depth sensor. Approximately 1000 ml of each seawater sample were filtered using 0.2 μm pore size filters and stored at -80°C until further processing. Sponge species were identified by morphological and molecular taxonomic methods (see Supplementary Material Section 1 and Supplementary Table 1). Specimens for the present study were selected and further processed if a minimum of two replicates per sponge taxon were collected. The research described refers to several Antarctic sponge species. It conforms to Antarctic Treaty legislation and to the SCAR Code of Conduct for the Use of Animals for Scientific Purposes in Antarctica (ATCM XXXIV, 2011).

Table 1

SamplesSampleIDStationDateDepthLatitudeLongitude# OTUsCoverageD-1PDFTU
A. leptodermaTB05Station 20020.03.201214061°09.82’S55°59.12’W510.999.81.80.04
A. leptodermaTB11Station 21422.03.201214861°00.70’S55°45.00’W690.9925.32.10.28
A. leptodermaTB16Station 24026.03.201246961°38.43’S57°08.83’W870.9829.12.60.40
A. leptodermaTB18Station 24728.03.201235362°23.72’S61°24.45’W1520.9925.22.50.01
A. leptodermaTB19Station 24728.03.201235362°23.72’S61°24.45’W2300.9941.23.10.02
A. leptodermaTB21Station 25129.03.201243462°09.78’S60°49.44’W2850.9935.52.70.01
A. leptodermaTB22Station 25129.03.201243462°09.78’S60°49.44’W2010.9919.42.00.01
Haliclona sp.TB01Station 19619.03.201211661°16.88’S55°37.35’W1530.9670.14.50.06
Haliclona sp.TB27Station 26431.03.201218961°50.01’S58°36.33’W1760.9876.13.70.08
H. balfourensisTB10Station 20721.03.201213760°53.75’S55°40.16’W1030.9646.54.10.10
H. balfourensisTB20Station 24828.03.201214162°28.15’S61°21.92’W2140.9955.03.40.10
I. bentartiTB31Station 28204.04.20129661°12.24’S55°41.59’W610.9911.31.70.01
I. bentartiTB32Station 29005.04.201233361°01.96’S54°56.54’W1720.9837.53.40.04
I. bentartiTB13Station 22924.03.20129760°59.33’S55°42.32’W990.9728.12.60.05
I. bentartiTB14Station 22924.03.20129760°59.33’S55°42.32’W790.9818.92.20.01
Seawaterpkl23Station 19318.03.20122061°33.86’S55°01.96’W850.9940.42.20.13
Seawaterpkl24Station 24124.03.20122061°38.13’S57°07.91’W890.9933.32.00.09
Seawaterpkl30Station 26701.04.20122061°58.09’S56°38.71’W1481.0047.82.40.14
Seawaterpkl32Station 21722.03.20122061°04.27’S55°48.87’W1241.0052.42.70.22
Seawaterpkl33Station 23224.03.20122061°05.60’S55°49.23’W1160.9954.62.90.17
Seawaterpkl34Station 23525.03.20122061°17.45’S56°11.24’W1350.9958.12.50.19
Seawaterpkl35Station 24427.03.20122061°38.19’S57°33.14’W1330.9957.82.60.23
Seawaterpkl36Station 24728.03.20122062°23.86’S61°23.78’W1170.9952.82.40.11
Seawaterpkl37Station 25129.03.20122062°17.38’S61°09.80’W1271.0045.62.20.15
Seawaterpkl38Station 26230.03.20122061°39.06’S59°14.06’W1580.9957.13.10.14
Seawaterpkl39Station 28103.04.20122062°08.77’S54°59.79’W1540.9960.72.70.14
Seawaterpkl40Station 27702.04.20122062°19.51’S56°27.99’W1340.9945.72.10.25

Sample information with sample identifiers, station, date, depth, coordinates, and OTU statistics, such as number of OTUs per sample, OTU coverage, phylogenetic diversity (PD), and fraction of unmapped tax4fun OTUs (FTU).

Pyrosequencing and Prokaryote 16S rRNA Gene Amplicon Processing

Whole genomic DNA was extracted using a modified protocol by bead beating, phenol:chloroform:isoamyl alcohol purification, isopropanol/sodium acetate precipitation and ethanol washing (Zhou et al., 1996). Extracted DNA from all specimens was subjected to PCR of the variable regions V3 to V5 of bacterial 16S rRNA genes. Each reaction mixture (50 μl) contained 25 μl of Phusion High-Fidelity PCR Master Mix with HF buffer (Thermo Scientific, Waltham, MA), 0.5 μM of each primer, 3% dimethylsulfoxide, 30 μg BSA and 50 ng template. Primers used for V3 forward were 5′-MID-TACGGRAGGCAGCAG-3′ (Liu et al., 2007) and for V5 reverse 5′-CCGTCAATTCMTTTGAGT-3′ (Wang and Qian, 2009). Forward primer sequences included also the variable multiplex identifier (MID) consisting of 10 bases. DNA from each sample was amplified in three parallel PCR runs (95°C for 4 min; 30 cycles of 45 s at 95°C, 1 min at 58°C, and 45 s at 72°C; 5 min at 72°C). Products were electrophoresed for 1 h at 80 V and gel-purified using the PeqGold Gel Extraction Kit (Peqlab, Erlangen, Germany). PCR products from parallel runs were pooled and quantified using the Quant-iT dsDNA HS assay kit and a Qubit fluorometer (Invitrogen, Carlsbad, CA, United States). 16S rRNA gene amplicons were sequenced using the GS-FLX 454 pyrosequencer and titanium chemistry as recommended by the manufacturer (Roche, Branford, CT, United States). The raw data have been deposited in the Sequence Read Archive with BioProject number: PRJNA471833.

Sequences were processed using mothur v.1.37.6 (Schloss et al., 2009, 2011). Pyrosequencing flowgrams were filtered and denoised using the mothur implementation of AmpliconNoise (Quince et al., 2009). Sequences were removed from the analysis if they were <300 bp or contained ambiguous characters, homopolymers longer than 8 bp, more than one MID mismatch, or more than two mismatches to the primer sequence. After chimera removal with UCHIME (Edgar et al., 2011), unique sequences were aligned and identified using the SILVA128 taxonomy1. Non-target sequences (e.g., chloroplasts, mitochondria, eukaryotic 18S rRNA) were removed prior to operational taxonomic unit (OTU) clustering. After raw data processing, mothur was used to cluster the obtained sequences into OTUs at 97% genetic identity (species level).

Prokaryotic Community Analyses

The OTU statistics / alpha-diversity calculations and subsequent diversity analyses, if not stated otherwise, were performed in R v.3.3.3 using the picante v.1.6 package (Kembel et al., 2010; R Development Core Team, 2018). In order to compare the (dis)similarity of OTU compositions between communities the OTU abundance table was standardized using decostand (method = “hellinger”) and pairwise Bray–Curtis dissimilarities were calculated using vegdist (method = “bray”) (Bray and Curtis, 1957; Ramette, 2007; Anderson and Walsh, 2013). For univariate and multivariate analyses (e.g., Kruskal–Wallis rank sum test or analysis of variance using distance matrices – adonis) all samples were arranged into sample groups (i.e., host-identity or seawater). Please note that due to the uneven sample size and low number of replicates (n = 2) for two sponge species (i.e., Haliclona sp. and H. balfourensis) these statistical results should be interpreted cautiously. Univariate relationships between alpha-diversity indices (i.e., OTU richness, coverage, Simpson’s inverse index of diversity D-1, Faith’s phylogenetic diversity PD) and sample groups were analyzed by the Kruskal-Wallis rank sum test using kruskal test (R stats package v.3.3.3) followed by Dunn’s Kruskal-Wallis multiple comparisons test using dunnTest (FSA package v.0.8.21) and the Benjamini–Hochberg p-value correction for multiple testing (Benjamini and Hochberg, 1995; Ogle, 2018). Multivariate beta-diversity analysis based on the host-identity and non-metric multidimensional scaling (nMDS) was performed using adonis and metaMDS functions of the vegan package v.2.5.3 (Oksanen et al., 2012). Hierarchical cluster analysis was performed using hclust (method = “averag”e). The heatmap was created using JColorGrid v.1.86 (Joachimiak et al., 2006). NCBI blastn search was performed against two NCBI databases (i.e., “rRNA type strains/prokaryotic 16S ribosomal RNA” and “Nucleotide collection – nt”) using the standard settings. The 16S rRNA 97% OTU table including the SILVA128 taxonomy for each individual OTU can be accessed via the Figshare online repository2.

Functional profiles were predicted using Tax4Fun, which is a software package that predicts the functional capabilities of prokaryotic communities based on 16S rRNA datasets (Aßhauer et al., 2015). Analyses were performed with short read mode disabled. To assess the quality of the predictions, the Fraction of Taxonomic units Unexplained (FTU) value was obtained. The FTU measures the fraction of sequences assigned to taxonomic units that cannot be mapped to KEGG organisms using the Tax4Fun association matrix. The KEGG Orthology (KO) abundance profile was visualized using metaMDS in R. Subsequently, LEfSe v.1 was used to identify KEGG pathways as significant biomarkers for the individual sponge-hosts by calculating the linear discriminant analysis effect size (LDA) (Segata et al., 2011). Note that results from predictive functional profiling using 16S rRNA marker genes can deviate from metagenomic profiling and functional gene annotation. In addition, because of functional overlap, some KOs can be assigned to more than one pathway. The KEGG Orthologs relative abundance table can be accessed via the Figshare online repository3. The KEGG Orthologs pathway relative abundance table can be accessed via the Figshare online repository4.

Results

Sponge Taxonomy

We morphologically assigned four taxa to the 15 collected demosponge specimens: A. leptoderma (Order Tetractinellida), Haliclona sp. (Haplosclerida), H. balfourensis (Suberitida), and I. bentarti (Poecilosclerida) (Figure 1 and Table 1). The molecular taxonomic results corroborate the morphological results. The resulting phylogenetic tree (Supplementary Figure 1) reflects the phylogenetic distances of the four taxa.

Prokaryotic Diversity and Community Patterns

The sequencing of sponge-associated prokaryotic communities and additional seawater samples yielded 1287 OTUs (Table 1). Coverage for all samples was >0.98, with one exception (sample TB01; coverage >0.96). Sponge specimens belonging to A. leptoderma (OTUs n = 153.6 ± 88.9), Haliclona sp. (164.5 ± 16.3), and H. balfourensis (158.5 ± 78.5), exhibited a higher average OTU richness compared to seawater samples (126.7 ± 22.8). The I. bentarti OTU richness was on average lower (102.8 ± 48.7) than seawater samples and all other sponges. We measured the shared phylogenetic history among prokaryotic OTUs in all samples using Faith’s PD index (Faith, 1992). Obtained values almost reflect OTU richness with high PD for Haliclona sp. (4.1 ± 0.6) and H. balfourensis (n = 3.8 ± 0.5) and low PD for I. bentarti (2.5 ± 0.7) and seawater (2.5 ± 0.3). Only the A. leptoderma PD values (2.4 ± 0.4) do not correspond with the observed relatively high OTU richness.

In total, 31 prokaryotic phyla, including the candidate phylum Berkelbacteria and two archaeal phyla Euryarchaeota and Thaumarchaeota were found within the present four sponge taxa and seawater samples (Figure 2 and Supplementary Table 2). Phylum richness ranged from 14 phyla in Haliclona sp., H. balfourensis, and I. bentarti, over 15 phyla in seawater samples, to 22 phyla in A. leptoderma. The most abundant prokaryotic phyla among all sponges and seawater samples were Proteobacteria (mainly Alpha- and Gammaproteobacteria) and Bacteroidetes (Figure 2). Compared to all the samples, Actinobacteria contributed a substantial share to the A. leptoderma (65.6%) and seawater (18.2%) microbiota. In addition, Firmicutes were considerably abundant only in I. bentarti (50%), whereas Marinimicrobia was only relatively well represented in seawater (68.6%). Altogether, these phyla made up the most dominant taxonomic groups (93.1%) responsible for the characteristic differences between the present sponge- and seawater-associated prokaryotic community patterns (Figure 2). Noteworthy is also the presence of typical sponge-associated prokaryotic phyla such as Nitrospinae (2.1%, n = 75 reads), Planctomycetes (1.7%, n = 62), Acidobacteria (0.6%, n = 22), Chloroflexi (0.6%, n = 21), Verrucomicrobia (0.4%, n = 13), Gemmatimonadetes (0.3%, n = 11), and Spirochaetae (0.3%, n = 10), which were still found in higher numbers among all samples compared to the taxonomically rich (n = 19 phyla) but rare prokaryotic community that accounted only for minuscule parts of the individual sponge and seawater microbiota (reads n ≤ 9) in the present study (Supplementary Table 2).

FIGURE 2

The most abundant OTUs were predominantly present within particular sponge-hosts or seawater samples (Figure 3). The two most abundant OTUs belong to the Sva0996 marine group family and were almost exclusively present within A. leptoderma. Moreover, this sponge species also exhibited two additional rather host-specific OTUs, which belong to the E01-9C-26 marine group and Flavobacteriaceae NS3a marine group families (Figure 3). In contrast, the genus Candidatus Branchiomonas was only present in I. bentarti, and besides a second OTU (SAR11 clade), the only abundant bacterium among all top OTUs in this sponge taxon. In contrast to the rather sponge-host specific OTU patterns, Haliclona sp. and H. balfourensis shared many predominant OTUs with the abundant seawater microbiota (Figure 3). Especially the phylum Bacteroidetes with the order Flavobacteriales was well represented among those shared OTUs (i.e., OTUs 9, 10, 12, 16, 18, 24, 26, 28, 30, 36) belonging to seawater, Haliclona sp. and H. balfourensis samples. Finally, H. balfourensis exhibits one apparently abundant and host-specific OTU (OTU0011, unclassified gammaproteobacterium), which was only classified to class level using the SILVA128 taxonomy. The subsequent NCBI blastn search revealed that the closest similar sequence in the NCBI 16S bacterial / archaeal database belongs to the gammaproteobacterial Spongiispira norvegica species (sequence similarity 86%; GenBank accession number: NR_042453), which was isolated from the boreal sponge identified as Geodia phlegraei. An additional blastn search against the nucleotide collection yielded as best match (sequence similarity 94%; GenBank accession number: JQ435988) also a sponge-associated, yet uncultured bacterial clone that was isolated from the marine sponge identified as Hymeniacidon perlevis.

FIGURE 3

Multivariate beta-diversity 16S rRNA gene community analyses using Bray–Curtis dissimilarities consolidated the preceding phylum and OTU patterns and underlined the influence of sponge-host identity on the prokaryotic community composition (Figure 2, 4A). The analysis of variance (i.e., adonis) revealed significant correlation (F4,22 = 11, R2= 0.67, p < 0.001) between community structure and host-identity. In addition, all seawater samples were clearly separated from the sponge specimens in the observed nMDS ordination and cluster analysis. Correspondingly, Simpson’s inverse alpha-diversity indices were also significantly different between seawater and A. leptoderma (p adjusted = 0.012) and I. bentarti (p adjusted = 0.017) sample groups, which are the two sponge taxa with the highest distances to seawater samples observed in the multivariate analyses (Supplementary Table 3 and Figure 2, 4A). Conversely, no significant correlation has been observed between the Haliclona sp. and H. balfourensis derived Simpson’s inverse diversity indices and seawater samples. Finally, no significant pairwise differences were found for the two remaining indices (observed OTUs and Phylogenetic Diversity PD) after corrections for multiple tests (Supplementary Table 3).

FIGURE 4

Predicted Functional Profiles

The potential functional roles of the sponge-associated prokaryotic community were predicted using Tax4Fun, which is a software package that predicts the functional capabilities of prokaryotic communities based on 16S rRNA gene datasets (Aßhauer et al., 2015). Compared to the PICRUSt tool, which is also a software package that predicts functional profiles of prokaryotic communities using 16S rRNA gene sequences, Tax4Fun showed higher correlations of predicted profiles with corresponding functional profiles obtained from whole metagenome sequence data (Langille et al., 2013; Aßhauer et al., 2015). Additionally, in direct comparison Tax4Fun predicted almost 15% more KEGG Orthologs than PICRUSt (Koo et al., 2017). However, due to the predictive nature of 16S rRNA gene based functional profiling this approach cannot substitute whole metagenome profiling completely (Aßhauer et al., 2015; Weigel and Erwin, 2017). Nonetheless, in broad prokaryotic community ecology surveys, like the present study, predictive functional profiling from 16S rRNA gene sequence data can serve as a complementary and cost-effective metagenomic pre-study.

The FTU value, as a measure of the quality of the predictions, was relatively low for most of the samples and reached only >0.20 for five out of 27 samples (Table 1). A low FTU indicates that the majority of OTUs were included in the functional prediction, which further indicates that most OTUs were represented by at least one KEGG organism in the reference data of Tax4Fun. Hence, the FTU value can serve as an indirect measure of quality, because a low FTU value is usually associated with a higher correlation to real metagenomic data. For instance, FTU values for the Guerrero Negro microbial mat were up to 0.5 for some samples, but still a correlation coefficient of around 0.65 between functional prediction made with Tax4Fun and the functional profile derived from metagenome sequencing were obtained (Aßhauer et al., 2015). Moreover, for the HMP data, all FTU values were >0.1 and Spearman correlation coefficients were around 0.85 (for further details see5). As a consequence of habitat and ecosystem related differences in microbiome functions the quality of predicted functional profiles is influenced by the presence of marine derived prokaryotic genes and genomes in the provided pre-computed metabolic reference file (Arrigo, 2005; Sunagawa et al., 2015). Therefore, it is important to emphasize that the predicted metagenomic functional pathways and implied synthesis of metabolites can deviate from actual functional capabilities of the present sponge-associated microbiomes assessed by metagenomic shotgun sequencing.

In total, 6323 KEGG Orthologs (KOs; i.e., sets of homologous sequences) were predicted to be present among all samples. Using the relative KO abundances samples are arranged similar to the 16S rRNA gene profile (Figure 4A,B). Furthermore, the correlation between the KO abundance profile and the sample groups was even higher (F4,22 = 47.6, R2= 0.9, p < 0.001) compared to the 16S rRNA gene OTU profile. In total, 278 pathways were found, which resulted in 161 significantly different pathways using LEfSe (Supplementary Table 4).

In the sponge taxa A. leptoderma, H. balfourensis, and I bentarti three different predicted energy metabolism pathways, comprising the oxidation and reduction reactions of the respective pathway-associated compounds, were significantly enriched [i.e., methane (ko00680), sulfur (ko00920), and nitrogen (ko00910), respectively] (Table 2). Besides energy metabolism, we focused on specific metabolic pathway classes involved in the synthesis of bioactive compounds and in the degradation of xenobiotics, which were identified as significant biomarkers among the four present sponge taxa (Table 2). Especially, the two sponges A. leptoderma and I. bentarti featured many predicted metabolic pathways within the biosynthesis of other secondary metabolites, like terpenoids and polyketides metabolism, and xenobiotics biodegradation and metabolism classes (Table 2). For instance, in A. leptoderma the predicted secondary metabolite pathways streptomycin (ko00521), neomycin, kanamycin and gentamicin (ko00524), and phenylpropanoid (ko00940) were significantly enriched. Furthermore, in A. leptoderma certain xenobiotics biodegradation and metabolism pathways were enriched, inter alia, styrene (ko00643), caprolactam (ko00930), and steroid (ko00984) degradation (Table 2). The number of significantly enriched predicted xenobiotics biodegradation pathways was even higher in I. bentarti, which comprised a wide range of potential (chlorinated) hydrocarbon degradation capabilities: e.g., toluene (ko00623), ethylbenzene (ko00642), naphthalene (ko00626), chloroalkane and chloroalkene (ko00625), chlorocyclohexane and chlorobenzene (ko00361), dioxin (ko00621), and atrazine (ko00791) degradation (Table 2).

Table 2

SpongePathwayKEGG Pathway nameKEGG Pathway ClassLDAp-value
A. leptodermako00521Streptomycin biosynthesisBiosynthesis of Other Secondary Metabolites2.830.001
ko00524Neomycin, kanamycin and gentamicin biosynthesisBiosynthesis of Other Secondary Metabolites2.030.004
ko00940Phenylpropanoid biosynthesisBiosynthesis of Other Secondary Metabolites2.72<0.001
ko00680Methane metabolismEnergy Metabolism3.34<0.001
ko00710Carbon fixation in photosynthetic organismsEnergy Metabolism2.68<0.001
ko00281Geraniol degradationMetabolism of Terpenoids and Polyketides2.710.010
ko00522Biosynthesis of 12-, 14- and 16-membered macrolidesMetabolism of Terpenoids and Polyketides2.66<0.001
ko00523Polyketide sugar unit biosynthesisMetabolism of Terpenoids and Polyketides2.270.029
ko00900Terpenoid backbone biosynthesisMetabolism of Terpenoids and Polyketides3.070.003
ko00909Sesquiterpenoid and triterpenoid biosynthesisMetabolism of Terpenoids and Polyketides2.66<0.001
ko01051Biosynthesis of ansamycinsMetabolism of Terpenoids and Polyketides2.89<0.001
ko01057Biosynthesis of type II polyketide productsMetabolism of Terpenoids and Polyketides2.000.002
ko00364Fluorobenzoate degradationXenobiotics Biodegradation and Metabolism2.230.001
ko00643Styrene degradationXenobiotics Biodegradation and Metabolism2.430.002
ko00930Caprolactam degradationXenobiotics Biodegradation and Metabolism2.110.032
ko00984Steroid degradationXenobiotics Biodegradation and Metabolism2.450.020
Haliclona sp.ko00401Novobiocin biosynthesisBiosynthesis of Other Secondary Metabolites2.180.022
ko00624Polycyclic aromatic hydrocarbon degradationXenobiotics Biodegradation and Metabolism2.370.006
ko00980Metabolism of xenobiotics by cytochrome P450Xenobiotics Biodegradation and Metabolism2.360.002
H. balfourensisko00920Sulfur metabolismEnergy Metabolism3.10<0.001
ko00253Tetracycline biosynthesisMetabolism of Terpenoids and Polyketides2.340.001
ko01053Biosynthesis of siderophore group non-ribosomal peptidesMetabolism of Terpenoids and Polyketides2.840.001
ko00982Drug metabolism – cytochrome P450Xenobiotics Biodegradation and Metabolism2.470.001
I. bentartiko00960Tropane, piperidine and pyridine alkaloid biosynthesisBiosynthesis of Other Secondary Metabolites2.340.009
ko00190Oxidative phosphorylationEnergy Metabolism3.37<0.001
ko00910Nitrogen metabolismEnergy Metabolism3.67<0.001
ko01054Non-ribosomal peptide structuresMetabolism of Terpenoids and Polyketides3.310.001
ko00361Chlorocyclohexane and chlorobenzene degradationXenobiotics Biodegradation and Metabolism2.210.014
ko00621Dioxin degradationXenobiotics Biodegradation and Metabolism2.320.007
ko00622Xylene degradationXenobiotics Biodegradation and Metabolism2.310.005
ko00623Toluene degradationXenobiotics Biodegradation and Metabolism2.70<0.001
ko00625Chloroalkane and chloroalkene degradationXenobiotics Biodegradation and Metabolism2.600.001
ko00626Naphthalene degradationXenobiotics Biodegradation and Metabolism2.390.013
ko00642Ethylbenzene degradationXenobiotics Biodegradation and Metabolism2.500.001
ko00791Atrazine degradationXenobiotics Biodegradation and Metabolism2.330.003

KEGG pathways information sorted by sponge taxa with pathway identifier, pathway name and class, the linear discriminant analysis effect size (LDA), and corresponding p-values.

In contrast, the predicted bioactive potential of the associated prokaryotic community in Haliclona sp. and H. balfourensis seems to be rather low considering the number of significant predicted secondary metabolite and xenobiotics pathways. Both sponges exhibited significant P450 xenobiotics metabolism pathways, metabolism of xenobiotics by cytochrome P450 (ko00980) and drug metabolism – cytochrome P450 (ko00982), which are pathways involved in a multitude of metabolic processes. Furthermore, in Haliclona sp. only novobiocin secondary metabolite biosynthesis (ko00401), together with polycyclic aromatic hydrocarbon degradation (ko00624) pathways were enriched.

Discussion

The investigated cold-water sponges from the Antarctic shelf host diverse prokaryotic communities, which feature several bacterial phyla, such as Proteobacteria (Alpha-, Beta-, and Gamma-), Actinobacteria, or Bacteroidetes, that are usually enriched in marine sponges (Hentschel et al., 2012; Thomas et al., 2016; Moitinho-Silva et al., 2017c). In particular, most of these phyla are significantly enriched in low microbial abundance (LMA) sponges, whereas typical phyla of high microbial abundance (HMA) sponges, such as Chloroflexi, Acidobacteria, Gemmatimonadetes, are underrepresented in the present sponges (Moitinho-Silva et al., 2017c). While it is possible to utilize prokaryotic diversity patterns to predict the LMA or HMA status of sponge species, only one recent study confirmed the reliability of HMA-LMA dichotomy for cold-water sponges using microscopic cell counts (Schöttner et al., 2013). However, the present potential host-specific prokaryotic community patterns indicate that all four sponges belong to the LMA group.

Our results showed that the prokaryotic communities of the sponges were distinctly different from those in surface waters. A comparison to data of a study conducted during the same cruise, which assessed bacterial communities in mesopelagic and bathypelagic waters, showed that the sponge-associated bacterial communities are also different from bacterial communities in mesopelagic waters (Milici et al., 2017). Even though Gammaproteobacteria also dominated the mesopelagic bacterial communities, other taxa than those prevalent in the sponges were dominant, such as Pseudoalteromonas, SAR86 and ZD0417 (Milici et al., 2017). Furthermore, a plethora of prokaryotic community studies demonstrated consistent apparent differences between either various sponge-associated communities or individual sponge-specific bacteria and seawater communities, independent of spatial distances between sponge and seawater sampling locations (Blanquer et al., 2013; Taylor et al., 2013; Reveillaud et al., 2014; Thomas et al., 2016; Steinert et al., 2017). However, a recent study that utilized 98 sponge specimens and corresponding seawater samples suggested that horizontal acquisition is an important mechanism for the establishment and maintenance of sponge-species specific prokaryotic communities (Turon et al., 2018). Consequently, seawater samples should be collected close to the related sponges in order to improve the accuracy of sponge-seawater microbiota comparisons.

To our knowledge, of the present four sponge taxa, only the prokaryotic community associated with H. balfourensis has been investigated using culture-dependent and independent methods (Webster et al., 2004; Xin et al., 2011). Especially alphaproteobacterial clones, and cultured isolates belonging to several Gram-positive bacteria, such as Pseudonocardia sp., Bacillus sp., or Virgibacillus picturae, were part of the H. balfourensis microbiota in these two studies. For Haliclona sp. one Antarctic specimen from the same genus has been screened using high-throughput-sequencing and several phyla, such as Proteobacteria (Alpha-, Beta-, and Gamma-), Actinobacteria or Planctomycetes were present in relatively high abundances, which is similar to the results obtained with the specimens in the present study (Rodríguez-Marconi et al., 2015). Moreover, in different Haliclona taxa from other locations, these bacterial phyla were also found in high abundances (Kennedy et al., 2009; Sipkema et al., 2009; Thomas et al., 2016). However, the apparent large fraction of OTUs assigned to Bacteroidetes in the present study appears to be novel considering the available literature that studied Haliclona spp. specimens.

In general, sponges from deep-sea and/or cold-water habitats exhibit a diverse range of prokaryotic taxa, which are known to be associated with sponges to a greater or lesser extent. Prokaryotic phyla, such as Acidobacteria, Bacteroidetes, Chloroflexi, PAUC34f, Planctomycetes, Poribacteria, Proteobacteria (Alpha-, Beta-, Gamma-, and Delta-), Thaumarchaeota, or Verrucomicrobia, were detected in several phylogenetically divergent sponge species (Radax et al., 2012; Jackson et al., 2013; Kennedy et al., 2014; Rodríguez-Marconi et al., 2015). Correspondingly, the present study also identified most of these taxa as major part of the sponge-associated microbiota. However, on the basis of the differences in the abundance and composition of the individual communities, apparently host-identity significantly influences the prokaryotic composition; this is a defining pattern of the complex sponge-prokaryote and fungal relationships with strong supportive evidence from multiple sponge species inhabiting environmentally diverse marine habitats and climate zones (Pita et al., 2013; Easson and Thacker, 2014; Steinert et al., 2016; Thomas et al., 2016; Chaib De Mares et al., 2017).

Besides the here indicated host-specificity of prokaryotic communities, also the predominance of one single taxon, or even single OTUs, is an often observed circumstance in sponge-symbiont relationships (Croué et al., 2013; Giles et al., 2013; Jackson et al., 2013; Simister et al., 2013; Hardoim and Costa, 2014). Likewise, also the present sponge specimens possessed OTUs that made up large fractions of their potential host-specific microbiota. This includes the two most abundant bacterial OTUs, both belonging to the same taxon Sva0996 marine group (Phylum Actinobacteria), which has been recovered from various environments/organisms such as Red Sea sponges (Moitinho-Silva et al., 2014), tropical ascidians (Steinert et al., 2015), Arctic and Atlantic ocean bacterioplankton assemblages (Bano and Hollibaugh, 2002; Milici et al., 2016), or Arctic marine sediment (Ravenschlag et al., 1999). While this taxon seems to be a cosmopolitan, the enrichment in just one sponge species hints to a putative symbiotic relationship between the host and this bacterium. The presence of Candidatus Branchiomonas (order Nitrosomonadales) among the most abundant OTUs is also noteworthy. To the best of our knowledge this taxon has not been found to be present in sponges so far. However, recent research provided evidence that “ammonia oxidizing” Nitrosomonadales representatives might contribute to the nitrogen cycling in sponges and are often present in high abundances in several sponge taxa, such as Crambe crambe (Croué et al., 2013) or in one Clathria sp. individual from the Antarctic (Rodríguez-Marconi et al., 2015). In addition, the order Nitrosomonadales has also been detected in deep-sea coral and sponge communities, although at relatively low abundances (Kennedy et al., 2014; Simister et al., 2016). Finally, the presence of a potentially novel and sponge-specific bacterium (i.e., low BLAST similarity to known bacterial 16S rRNA gene sequences), which is predominant in H. balfourensis, suggests that certain bacterial symbionts are potentially highly adapted to their specific sponge-host and its metabolic as well as chemical environment. In fact, in recent years ‘omics-related analyses started to reveal the complexity of metabolic interactions between symbionts and sponge-hosts (Thomas et al., 2010; Liu et al., 2012; Radax et al., 2012; Moitinho-Silva et al., 2017a; Slaby et al., 2017).

Functional metabolic profiling by a predictive approach using PICRUSt (Langille et al., 2013) has been successfully applied in several recent sponge-microbiota studies either by investigating individual sponges and their functional potential (de Voogd et al., 2015; Cleary et al., 2017), comparing predicted profiles with shotgun sequenced metagenomic data (Weigel and Erwin, 2017), correlating predicted functions with ocean acidification and elevated seawater temperature (Lesser et al., 2016), or focusing on predicted functions of individual key symbionts (Morrow et al., 2015). We applied a similar approach with a different predictive program, Tax4fun (Aßhauer et al., 2015), which was successfully applied for bacterioplankton communities and providing valid correlations of functional profiles to microbial and environmental parameters (Wemheuer et al., 2017). The present study demonstrates that this approach can provide first insights into potential functional aspects of sponge-associated prokaryotic communities. Similar to the differences observed here in community composition among different sponge and seawater samples, the predicted functional KO profiles also resulted in a clear distinction between the four sponge-hosts and/or seawater samples. So far, comparative metagenomic functional analyses between different sponge species are scarce (Pita et al., 2016). Only one metagenomic study, which investigated the microbiomes of six phylogenetically divergent sponge species, has shown that host-specific symbiont communities exhibited apparent core functions despite maintaining sponge species-specific gene composition patterns (Fan et al., 2012). Apart from the presence of energy metabolism classes (e.g., carbon or nitrogen metabolism) or symbiosis factors (e.g., eukaryotic-like proteins, ankyrin repeats, or tetratricopeptide repeats), potential prokaryotic symbionts often also synthesize secondary metabolites and bioactive natural products for which sponges are widely acknowledged (Hentschel et al., 2012; Reynolds and Thomas, 2016; Bhushan et al., 2017; Lackner et al., 2017). Here, the predicted pathway analysis found first indications that the four Antarctic sponge species may possess significantly different secondary metabolite biosynthesis pathways. Predicted significant secondary metabolism biosynthesis pathways of known antibiotics, such as streptomycin, butirosin and neomycin in A. leptoderma, and novobiocin in Haliclona sp. suggest that these sponge species may possess host-specific antimicrobial activity. So far, a broad range of antibacterial compounds and activities has been reported for phylogenetically divergent sponges from different marine habitats (Laport et al., 2009; Indraningrat et al., 2016), including the Southern Ocean (Berne et al., 2016; Angulo-Preckler et al., 2018). In the present study, certain predicted xenobiotics-related degradation pathways are significantly enriched in all four sponges, especially in A. leptoderma and I. bentarti. For instance, styrene and its derivatives are aromatic compounds that pose environmental risks due to their toxicity (O’Leary et al., 2002; Mooney et al., 2006). In addition, the degradation process of steroids, a rich class of organic molecules in all natural environments, can utilize steroids as growth substrates for prokaryotes (Bergstrand et al., 2016; Holert et al., 2018). Hence, the predicted presence of the styrene and steroid degradation pathways may indicate a potential role in bioremediation processes and the biotechnological potential of the A. leptoderma microbiota. Finally, the sponge I. bentarti exhibited a wide range of predicted xenobiotic degradation pathways that encompass several organic compound classes, such as alkylbenzenes, chlorinated alkenes, chloroarenes, organochlorides, or naphtalenes. Many derivatives of these compound classes are known contaminants and pollutants due to their (geno)toxic properties (Singh, 2012). Local enrichment of pollutants could explain the predicted differential xenobiotic degradation pathway patters. However, the sponge specimens that belonged to the same species were mostly collected at different sites and depths. Hence, it seems unlikely that certain predicted degradation pathways may reflect the local enrichment of pollutants. On the other hand, genomic analyses indicated that prokaryotes possess a broad range of detoxifying functions within the sponge-holobiont (Hoffmann et al., 2009; Konoki et al., 2010; Fan et al., 2012; Uriz et al., 2012; Tian et al., 2014; Karimi et al., 2017; Keren et al., 2017). Therefore, a host-specific microbiota that is adapted to the host-intrinsic chemistry and metabolism could have shaped the distribution patterns of the predicted xenobiotic degradation pathways.

However, it should be emphasized that the performed functional metabolic predictions are no substitute for metabolic gene and gene cluster analyses. For instance, a direct comparison between predicted and shotgun sequenced metagenome derived nitrogen cycling genes revealed relatively similar KO counts and abundances, though with noticeable deviations (Weigel and Erwin, 2017). Moreover, prokaryotic secondary metabolism can be highly strain and environment-specific (Jensen et al., 2007; Romano et al., 2018), and 90% of the marine prokaryotic genes detected by the TARA Oceans project had no match in public databases at the time when the survey was conducted (Sunagawa et al., 2015). Therefore, it remains to be validated by metagenomic or whole genome sequencing if specific sponge-associated prokaryotic taxa are responsible for the metabolic functions predicted in the present study.

Conclusion

We could find indications that cold and deep-water sponges exhibit host-specific prokaryotic communities, despite different sampling sites and depths. This is similar to the conclusions regarding host-specificity from studies of sponge-prokaryotic communities from several (sub)tropical and temperate regions (Pita et al., 2013; Easson and Thacker, 2014; Steinert et al., 2016, 2017). Finally, predictive functional analysis suggests that sponge-associated prokaryotes may also enhance the roles of sponges in bioremediation processes of environmental pollutants, besides their acknowledged involvement in the biosynthesis of secondary metabolites and detoxification of metabolic waste products.

Statements

Author contributions

PS and GS designed and conceived the study. MS and TB collected samples during the ANT-XXVIII/4 Polarstern cruise. DJ and DE classified the sponge samples and wrote the Supplementary Section 1: Sponge barcoding and morphological taxonomy. BW undertook the laboratory work and sequencing, and generated data. RD contributed reagents and materials for sequencing. GS analyzed and interpreted the data and wrote the first draft of the manuscript. All authors contributed to manuscript corrections and improved the final version. The authors greatly appreciate the thoughtful and insightful comments by the reviewers.

Funding

TB, RD, MS, and BW were supported by the Transregional Collaborative Research Center Roseobacter (TRR51) funded by Deutsche Forschungsgemeinschaft (DFG). DJ thanks the Deutsche Forschungsgemeinschaft (DFG) for financial support to our Antarctic Porifera research (JA-1063/17 1). DE thanks Gabriele Büttner, Simone Schätzle, and Gert Wörheide, LMU Munich for support in various aspects of the molecular investigations. Additionally, we acknowledge support by DFG and the Open Access Publication Funds of the Carl-von-Ossietzky University of Oldenburg.

Acknowledgments

We are grateful for the excellent support of captain Thomas Wunderlich and his crew on board RV Polarstern.

Conflict of interest

The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

Supplementary material

The Supplementary Material for this article can be found online at: https://www.frontiersin.org/articles/10.3389/fmars.2019.00297/full#supplementary-material

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Summary

Keywords

16S rRNA, Antarctic shelf, functional prediction, host-specificity, prokaryotic diversity, sponge microbiota

Citation

Steinert G, Wemheuer B, Janussen D, Erpenbeck D, Daniel R, Simon M, Brinkhoff T and Schupp PJ (2019) Prokaryotic Diversity and Community Patterns in Antarctic Continental Shelf Sponges. Front. Mar. Sci. 6:297. doi: 10.3389/fmars.2019.00297

Received

08 February 2019

Accepted

20 May 2019

Published

05 June 2019

Volume

6 - 2019

Edited by

Zhiyong Li, Shanghai Jiao Tong University, China

Reviewed by

Angelina Lo Giudice, National Research Council (CNR), Italy; Marinella Silva Laport, Federal University of Rio de Janeiro, Brazil

Updates

Copyright

*Correspondence: Georg Steinert, Peter J. Schupp,

Present address: Georg Steinert, Marine Symbioses, GEOMAR – Helmholtz Centre for Ocean Research Kiel, Kiel, Germany Bernd Wemheuer, Centre for Marine Bio-Innovation, School of Biological, Earth and Environmental Sciences, University of New South Wales, Sydney, NSW, Australia

This article was submitted to Microbial Symbioses, a section of the journal Frontiers in Marine Science

Disclaimer

All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.

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