Hopanoids in marine cyanobacteria: probing their phylogenetic distribution and biological role

Cyanobacteria are key players in the global carbon and nitrogen cycles and are thought to have been responsible for the initial rise of atmospheric oxygen during the Neoarchean. There is evidence that a class of membrane lipids known as hopanoids serve as biomarkers for bacteria, including many cyanobacteria, in the environment and in the geologic record. However, the taxonomic distributions and physiological roles of hopanoids in marine cyanobacteria remain unclear. We examined the distribution of bacteriohopanepolyols (BHPs) in a collection of marine cyanobacterial enrichment and pure cultures and investigated the relationship between the cellular abundance of BHPs and nitrogen limitation in Crocosphaera watsonii, a globally significant nitrogen‐fixing cyanobacterium. In pure culture, BHPs were only detected in species capable of nitrogen fixation, implicating hopanoids as potential markers for diazotrophy in the oceans. The enrichment cultures we examined exhibited a higher degree of BHP diversity, demonstrating that there are presently unaccounted for marine bacteria, possibly cyanobacteria, associated with the production of a range of BHP structures. Crocosphaera watsonii exhibited high membrane hopanoid content consistent with the idea that hopanoids have an important effect on the bulk physical properties of the membrane. However, the abundance of BHPs in C. watsonii did not vary considerably when grown under nitrogen‐limiting and nitrogen‐replete conditions, suggesting that the role of hopanoids in this organism is not directly related to the physiology of nitrogen fixation. Alternatively, we propose that high hopanoid content in C. watsonii may serve to reduce membrane permeability to antimicrobial toxins in the environment.     

Palaeoecology of a billion‐year‐old non‐marine cyanobacterium from the Torridon Group and Nonesuch Formation

A new chroococcalean cyanobacterium is described from approximately 1‐billion‐year‐old non‐marine deposits of the Torridonian Group of Scotland and the Nonesuch Formation of Michigan, USA. Individual cells of the new microfossil, Eohalothece lacustrina gen. et sp. nov., are associated with benthic microbial biofilms, but the majority of samples are recovered in palynological preparations in the form of large, apparently planktonic colonies, similar to extant species of Microcystis. In the Torridonian, Eohalothece is associated with phosphatic nodules, and we have developed a novel hypothesis linking Eohalothece to phosphate deposition in ancient freshwater settings. Extant cyanobacteria can be prolific producers of extracellular microcystins, which are non‐ribosomal polypeptide phosphatase inhibitors. Microcystins may have promoted the retention and concentration of sedimentary organic phosphate prior to mineralization of francolite and nodule formation. This has a further implication that the Torridonian lakes were nitrogen limited as the release of microcystins is enhanced under such conditions today. The abundance and wide distribution of Eohalothece lacustrina attests to the importance of cyanobacteria as oxygen‐producing photoautotrophs in lacustrine ecosystems at the time of the Mesoproterozoic–Neoproterozoic transition.     

Cellular interactions: lessons from the nitrogen‐fixing cyanobacteria

Marine nitrogen‐fixing cyanobacteria play a central role in the open‐ocean microbial community by providing fixed nitrogen (N) to the ocean from atmospheric dinitrogen (N₂) gas. Once thought to be dominated by one genus of cyanobacteria, Trichodesmium, it is now clear that marine N₂‐fixing cyanobacteria in the open ocean are more diverse, include several previously unknown symbionts, and are geographically more widespread than expected. The next challenge is to understand the ecological implications of this genetic and phenotypic diversity for global oceanic N cycling. One intriguing aspect of the cyanobacterial N₂ fixers ecology is the range of cellular interactions they engage in, either with cells of their own species or with photosynthetic protists. From organelle‐like integration with the host cell to a free‐living existence, N₂‐fixing cyanobacteria represent the range of types of interactions that occur among microbes in the open ocean. Here, we review what is known about the cellular interactions carried out by marine N₂‐fixing cyanobacteria and where future work can help. Discoveries related to the functional roles of these specialized cells in food webs and the microbial community will improve how we interpret their distribution and abundance patterns and contributions to global N and carbon (C) cycles.     

The microbe–mineral environment and gypsum neogenesis in a weathered polar evaporite

Evaporitic deposits are a globally widespread habitat for micro‐organisms. The microbe–mineral environment in weathered and remobilized gypsum from exposed mid‐Ordovician marine evaporite beds in the polar desert of Devon Island, Nunavut, Canadian High Arctic was examined. The gypsum is characterized by internal green zones of cyanobacterial colonization (dominated by Gloeocapsa/Aphanothece and Chroococcidiopsis spp. morphotypes) and abundant black zones, visible from the surface, that contain pigmented cyanobacteria and fungi. Bioessential elements in the gypsum are primarily provided by allochthonous material from the present‐day polar desert. The disruption, uplift and rotation of the evaporite beds by the Haughton meteorite impact 39 Ma have facilitated gypsum weathering and its accessibility as a habitat. No cultured cyanobacteria, bacteria and fungi were halophilic consistent with the expectation that halophily is not required to persist in gypsum habitats. Heterotrophic bacteria from the evaporite were slightly or moderately halotolerant, as were heterotrophs isolated from soil near the gypsum outcrop showing that halotolerance is common in arctic bacteria in this location. Psychrotolerant Arthrobacter species were isolated. No psychrophilic organisms were isolated. Two Arthrobacter isolates from the evaporite were used to mediate gypsum neogenesis in the laboratory, demonstrating a potential role for microbial biomineralization processes in polar environments.     

Lipid biomarkers in ooids from different locations and ages: evidence for a common bacterial flora

Ooids are one of the common constituents of ancient carbonate rocks, yet the role that microbial communities may or may not play in their formation remains unresolved. To search for evidence of microbial activity in modern and Holocene ooids, samples collected from intertidal waters, beaches and outcrops in the Bahamas and in Shark Bay in Western Australia were examined for their contents of lipid biomarkers. Modern samples from Cat and Andros islands in the Bahamas and from Carbla Beach in Hamelin Pool, Western Australia, showed abundant and notably similar distributions of hydrocarbons, fatty acids (FAs) and alcohols. A large fraction of these lipids were bound into the carbonate matrix and only released on acid dissolution, which suggests that these lipids were being incorporated continuously during ooid growth. The distributions of hydrocarbons, and their disparate carbon isotopic signatures, were consistent with mixed input from cyanobacteria together with small and variable amounts of vascular plant leaf wax [C₂₇–C₃₅; δ¹³C ?25 to ?32‰Vienna Pee Dee Belemnite (VPDB)]. The FAs comprised a complex mixture of C₁₂–C₁₈ normal and branched short‐chain compounds with the predominant straight‐chain components attributable to bacteria and/or cyanobacteria. Branched FA, especially 10‐MeC₁₆ and 10‐MeC₁₇, together with the prevalence of elemental sulfur in the extracts, indicate an origin from sulfate‐reducing bacteria. The iso‐ and anteiso‐FA were quite variable in their ¹³C contents suggesting that they come from organisms with diverse physiologies. Hydrogen isotopic compositions provide further insight into this issue. FAs in each sample show disparate δD values consistent with inputs from autotrophs and heterotrophs. The most enigmatic lipid assemblage is an homologous series of long‐chain (C₂₄–C₃₂) FA with pronounced even carbon number preference. Typically, such long‐chain FA are thought to come from land plant leaf wax, but in this case, their ¹³C‐enriched isotopic signatures compared to co‐occurring n‐alkanes (e.g., Hamelin Pool TLE FA C₂₄–C₃₂; δ¹³C ?20 to ?24.2‰ VPDB; TLE n‐alkanes δ¹³C ?24.1 to ?26.2 ?‰VPDB) indicate a microbial origin, possibly sulfate‐reducing bacteria. Lastly, we identified homohopanoic acid and bishomohopanol as the primary degradation products of bacterial hopanoids. The distributions of lipids isolated from Holocene oolites from the Rice Bay Formation of Cat Island, Bahamas were very similar to the beach ooids described above and, in total, these modern and fossil biomarker data lead us to hypothesize that ooids are colonized by a defined microbial community and that these microbes possibly mediate calcification.     

Diversity and bioactive potential of endospore-forming bacteria cultured from the marine sponge Haliclona simulans

Aims: Despite the frequent isolation of endospore‐formers from marine sponges, little is known about the diversity and characterization of individual isolates. The main aims of this study were to isolate and characterize the spore‐forming bacteria from the marine sponge Haliclona simulans and to examine their potential as a source for bioactive compounds. Methods and Results: A bank of presumptive aerobic spore‐forming bacteria was isolated from the marine sponge H. simulans. These represented c. 1% of the total culturable bacterial population. A subgroup of thirty isolates was characterized using morphological, phenotypical and phylogenetic analysis. A large diversity of endospore‐forming bacteria was present, with the thirty isolates being distributed through a variety of Bacillus and Paenibacillus species. These included ubiquitous species, such as B. subtilis, B. pumilus, B. licheniformis and B. cereus group, as well as species that are typically associated with marine habitats, such as B. aquimaris, B. algicola and B. hwajinpoensis. Two strains carried the aiiA gene that encodes a lactonase known to be able to disrupt quorum‐sensing mechanisms, and various isolates demonstrated protease activity and antimicrobial activity against different pathogenic indicator strains, including Clostridium perfringens, Bacillus cereus and Listeria monocytogenes. Conclusions: The marine sponge H. simulans harbours a diverse collection of endospore‐forming bacteria, which produce proteases and antibiotics. This diversity appears to be overlooked by culture‐dependent and culture‐independent methods that do not specifically target sporeformers. Significance and Impact of Study: Marine sponges are an as yet largely untapped and poorly understood source of endospore‐forming bacterial diversity with potential biotechnological, biopharmaceutical and probiotic applications. These results also indicate the importance of combining different methodologies for the comprehensive characterization of complex microbial populations such as those found in marine sponges.     

Discovery of a SAR11 growth requirement for thiamin's pyrimidine precursor and its distribution in the Sargasso Sea

Vitamin traffic, the production of organic growth factors by some microbial community members and their use by other taxa, is being scrutinized as a potential explanation for the variation and highly connected behavior observed in ocean plankton by community network analysis. Thiamin (vitamin B₁), a cofactor in many essential biochemical reactions that modify carbon–carbon bonds of organic compounds, is distributed in complex patterns at subpicomolar concentrations in the marine surface layer (0–300 m). Sequenced genomes from organisms belonging to the abundant and ubiquitous SAR11 clade of marine chemoheterotrophic bacteria contain genes coding for a complete thiamin biosynthetic pathway, except for thiC, encoding the 4-amino-5-hydroxymethyl-2-methylpyrimidine (HMP) synthase, which is required for de novo synthesis of thiamin''s pyrimidine moiety. Here we demonstrate that the SAR11 isolate ‘Candidatus Pelagibacter ubique'', strain HTCC1062, is auxotrophic for the thiamin precursor HMP, and cannot use exogenous thiamin for growth. In culture, strain HTCC1062 required 0.7 zeptomoles per cell (ca. 400 HMP molecules per cell). Measurements of dissolved HMP in the Sargasso Sea surface layer showed that HMP ranged from undetectable (detection limit: 2.4 pM) to 35.7 pM, with maximum concentrations coincident with the deep chlorophyll maximum. In culture, some marine cyanobacteria, microalgae and bacteria exuded HMP, and in the Western Sargasso Sea, HMP profiles changed between the morning and evening, suggesting a dynamic biological flux from producers to consumers.     

Alkali-labile precursors of dimethyl sulfide in marine benthic cyanobacteria

By the method of cold alkali hydrolysis, 29 marine benthic cyanobacteria were screened for production of alkali-labile precursors of dimethyl sulfide (DMS) including dimethylsulfoniopropionate (DMSP), a compound of significant importance in marine environments. Concentrations of DMS precursors ranged from undetectable to 0.8 mmol (g Chl a)^–1. The data correspond to some previous investigations concerning DMSP content of marine cyanobacteria and suggest that marine benthic cyanobacteria are only minor producers of DMSP. Received: 3 July 1997 / Accepted: 21 October 1997     

Roles of the acidic lipids sulfoquinovosyl diacylglycerol and phosphatidylglycerol in photosynthesis: their specificity and evolution

Sulfoquinovosyl diacylglycerol (SQDG) and phosphatidylglycerol (PG) are lipids with negative charges, distributed among membranes of chloroplasts of plants and their postulated progenitors, cyanobacteria, and also widely among membranes of anoxygenic photosynthetic bacteria. Thus, these acidic lipids are of great interest in terms of their roles in the function and evolution of the photosynthetic membranes. The physiological significance of these lipids in photosynthesis has been examined through characterization of mutants defective in their abilities to synthesize SQDG or PG, and through characterization of isolated thylakoid membranes or photosynthetic particles, the acidic lipid contents of which were manipulated in vitro, for example, on treatment with phospholipase to degrade PG. Responsibility of SQDG or PG has been clarified so far in terms of the structural and/or functional integrity of photosystems I and/or II in cyanobacterial, green algal, and higher plant species. Also implied were distinct levels of the responsibility in the different photosynthetic organisms. Extreme cases involved the indispensability of SQDG for photosynthesis and growth in two prokaryotic, photosynthetic organisms and the contribution of PG to construction of the photosystem-I trimer exclusively in cyanobacteria. Here, roles of these acidic lipids are discussed with a focus on their specificity and the evolution of photosynthetic membranes.Norihiro Sato is the recipient of the Botanical Society Award for Young Scientist, 2003.     

Influence of thylakoid membrane lipids on the structure of aggregated light‐harvesting complexes of the diatom Thalassiosira pseudonana and the green alga Mantoniella squamata

The study investigated the effect of the thylakoid membrane lipids monogalactosyldiacylglycerol (MGDG), digalactosyldiacylglycerol (DGDG), sulphoquinovosyldiacylglycerol (SQDG) and phosphatidylglycerol (PG) on the structure of two algal light‐harvesting complexes (LHCs). In contrast to higher plants whose thylakoid membranes are characterized by an enrichment of the neutral galactolipids MGDG and DGDG, both the green alga Mantoniella squamata and the centric diatom Thalassiosira pseudonana contain membranes with a high content of the negatively charged lipids SQDG and PG. The algal thylakoids do not show the typical grana–stroma differentiation of higher plants but a regular arrangement. To analyze the effect of the membrane lipids, the fucoxanthin chlorophyll protein (FCP) complex of T. pseudonana and the LHC of M. squamata (MLHC) were prepared by successive cation precipitation using Triton X‐100 as detergent. With this method, it is possible to isolate LHCs with a reduced amount of associated lipids in an aggregated state. The results from 77 K fluorescence and photon correlation spectroscopy show that neither the neutral galactolipids nor the negatively charged lipids are able to significantly alter the aggregation state of the FCP or the MLHC. This is in contrast to higher plants where SQDG and PG lead to a strong disaggregation of the LHCII whereas MGDG and DGDG induce the formation of large macroaggregates. The results indicate that LHCs which are integrated into thylakoid membranes with a high amount of negatively charged lipids and a regular arrangement are less sensitive to lipid‐induced structural alterations than their counterparts in membranes enriched in neutral lipids with a grana–stroma differentiation.     

Family 34 glycosyltransferase (GT34) genes and proteins in Pinus radiata (radiata pine) and Pinus taeda (loblolly pine)

Using a functional genomics approach, four candidate genes (PtGT34A, PtGT34B, PtGT34C and PtGT34D) were identified in Pinus taeda. These genes encode CAZy family GT34 glycosyltransferases that are involved in the synthesis of cell‐wall xyloglucans and heteromannans. The full‐length coding sequences of three orthologs (PrGT34A, B and C) were isolated from a xylem‐specific cDNA library from the closely related Pinus radiata. PrGT34B is the ortholog of XXT1 and XXT2, the two main xyloglucan (1→6)‐α‐xylosyltransferases in Arabidopsis thaliana. PrGT34C is the ortholog of XXT5 in A. thaliana, which is also involved in the xylosylation of xyloglucans. PrGT34A is an ortholog of a galactosyltransferase from fenugreek (Trigonella foenum‐graecum) that is involved in galactomannan synthesis. Truncated coding sequences of the genes were cloned into plasmid vectors and expressed in a Sf9 insect cell‐culture system. The heterologous proteins were purified, and in vitro assays showed that, when incubated with UDP‐xylose and cellotetraose, cellopentaose or cellohexaose, PrGT34B showed xylosyltransferase activity, and, when incubated with UDP‐galactose and the same cello‐oligosaccharides, PrGT34B showed some galactosyltransferase activity. The ratio of xylosyltransferase to galactosyltransferase activity was 434:1. Hydrolysis of the galactosyltransferase reaction products using galactosidases showed the linkages formed were α‐linkages. Analysis of the products of PrGT34B by MALDI‐TOF MS showed that up to three xylosyl residues were transferred from UDP‐xylose to cellohexaose. The heterologous proteins PrGT34A and PrGT34C showed no detectable enzymatic activity.     

The microbiome associated with two Synechococcus ribotypes at different levels of ecological interaction

Planktonic cyanobacteria belonging to the genus Synechococcus are ubiquitously distributed in marine and fresh waters, substantially contributing to total carbon fixation on a global scale. While their ecological relevance is acknowledged, increasing resolution in molecular techniques allows disentangling cyanobacteria's role at the micro‐scale, where complex microbial interactions may drive the overall community assembly. The interplay between phylogenetically different Synechococcus clades and their associated bacterial communities can affect their ecological fate and susceptibility to protistan predation. In this study, we experimentally promoted different levels of ecological interaction by mixing two Synechococcus ribotypes (MW101C3 and LL) and their associated bacteria, with and without a nanoflagellate grazer (Poterioochromonas sp.) in laboratory cultures. The beta‐diversity of the Synechococcus‐associated microbiome in laboratory cultures indicated that the presence of the LL ribotype was the main factor determining community composition changes (41% of total variance), and prevailed over the effect of protistan predation (18% of total variance). Our outcomes also showed that species coexistence and predation may promote microbial diversity, thus highlighting the underrated ecological relevance of such micro‐scale factors.     

Diversity of hopanoids and squalene-hopene cyclases across a tropical land-sea gradient

Bacterial hopanoids are ubiquitous in Earth surface environments. They hold promise as environmental and ecological biomarkers, if the phylogeny and physiological drivers of hopanoid biosynthesis can be linked with the distribution of hopanoids observed across a breadth of samples. Here we survey the diversity of hopanoid cyclases from a land‐sea gradient across the island of San Salvador, in the easternmost part of the Bahamas. The distribution of lipids was determined for the same sites, for the first time overlaying quantification of bacteriohopanepolyols with sqhC phylogeny. The results are similar to previous reports: environmental sqhCs average < 65% translated amino acid identity to their closest named relatives, and sequences from putative Proteobacteria dominate. Additionally, a new and apparently ubiquitous group of marine hopanoid producers is identified; it has no identifiable close relatives. The greatest diversity of hopanoid lipids occurs in soil, but hopanoids represent a minor fraction of total soil‐derived lipids. Marine samples contain fewer identifiable hopanoids, but they are more abundant as a fraction of the total extractable lipids. In soil, the dominant compounds are 35‐aminobacteriohopane‐32,33,34‐triol and adenosylhopane. In an upper estuarine sample, bacteriohopanetetrol and 32,35‐anhydrobacteriohopanetetrol dominate; while in lower estuarine and open marine samples, the most abundant are bacteriohopanetetrol and bacteriohopaneribonolactone. Cyclitol ethers are trace components in the soil, absent in the estuary, and of moderate abundance in the open marine setting, suggesting a dominant marine source. Conversely, aminotriol and aminotetrol decrease in abundance or disappear completely from land to ocean, while 2‐methyldiplopterol shows the opposite trend. Small quantities of 2‐methylbacteriohopanepolyols are detectable in all samples. The overall hopanoid distributions may correlate to the major phylogenetic families of hopanoid producers or to the environments in which they are found.     

Underestimated biodiversity as a major explanation for the perceived rich secondary metabolite capacity of the cyanobacterial genus Lyngbya

Marine cyanobacteria are prolific producers of bioactive secondary metabolites responsible for harmful algal blooms as well as rich sources of promising biomedical lead compounds. The current study focused on obtaining a clearer understanding of the remarkable chemical richness of the cyanobacterial genus Lyngbya. Specimens of Lyngbya from various environmental habitats around Curaçao were analysed for their capacity to produce secondary metabolites by genetic screening of their biosynthetic pathways. The presence of biosynthetic pathways was compared with the production of corresponding metabolites by LC‐ESI‐MS² and MALDI‐TOF‐MS. The comparison of biosynthetic capacity and actual metabolite production revealed no evidence of genetic silencing in response to environmental conditions. On a cellular level, the metabolic origin of the detected metabolites was pinpointed to the cyanobacteria, rather than the sheath‐associated heterotrophic bacteria, by MALDI‐TOF‐MS and multiple displacement amplification of single cells. Finally, the traditional morphology‐based taxonomic identifications of these Lyngbya populations were combined with their phylogenetic relationships. As a result, polyphyly of morphologically similar cyanobacteria was identified as the major explanation for the perceived chemical richness of the genus Lyngbya, a result which further underscores the need to revise the taxonomy of this group of biomedically important cyanobacteria.     

The distribution of active iron‐cycling bacteria in marine and freshwater sediments is decoupled from geochemical gradients

Microaerophilic, phototrophic and nitrate‐reducing Fe(II)‐oxidizers co‐exist in coastal marine and littoral freshwater sediments. However, the in situ abundance, distribution and diversity of metabolically active Fe(II)‐oxidizers remained largely unexplored. Here, we characterized the microbial community composition at the oxic‐anoxic interface of littoral freshwater (Lake Constance, Germany) and coastal marine sediments (Kalø Vig and Norsminde Fjord, Denmark) using DNA‐/RNA‐based next‐generation 16S rRNA (gene) amplicon sequencing. All three physiological groups of neutrophilic Fe(II)‐oxidizing bacteria were found to be active in marine and freshwater sediments, revealing up to 0.2% anoxygenic photoferrotrophs (e.g., Rhodopseudomonas, Rhodobacter, Chlorobium), 0.1% microaerophilic Fe(II)‐oxidizers (e.g., Mariprofundus, Hyphomonas, Gallionella) and 0.3% nitrate‐reducing Fe(II)‐oxidizers (e.g., Thiobacillus, Pseudomonas, Denitromonas, Hoeflea). Active Fe(III)‐reducing bacteria (e.g., Shewanella, Geobacter) were most abundant (up to 2.8%) in marine sediments and co‐occurred with cable bacteria (up to 4.5%). Geochemical profiles of Fe(III), Fe(II), O₂, light, nitrate and total organic carbon revealed a redox stratification of the sediments and explained 75%–85% of the vertical distribution of microbial taxa, while active Fe‐cycling bacteria were found to be decoupled from geochemical gradients. We suggest that metabolic flexibility, microniches in the sediments, or interrelationships with cable bacteria might explain the distribution patterns of active Fe‐cycling bacteria.     

Molecular architectures of Pen and Pal: Key enzymes required for CMP‐pseudaminic acid biosynthesis in Bacillus thuringiensis

Bacillus thuringiensis is a soil‐dwelling Gram positive bacterium that has been utilized as a biopesticide for well over 60 years. It is known to contain flagella that are important for motility. One of the proteins found in flagella is flagellin, which is post‐translationally modified by O‐glycosylation with derivatives of pseudaminic acid. The biosynthetic pathway for the production of CMP‐pseudaminic acid in B. thuringiensis, starting with UDP‐N‐acetyl‐d ‐glucosamine (UDP‐GlcNAc), requires seven enzymes. Here, we report the three‐dimensional structures of Pen and Pal, which catalyze the first and second steps, respectively. Pen contains a tightly bound NADP(H) cofactor whereas Pal is isolated with bound NAD(H). For the X‐ray analysis of Pen, the site‐directed D128N/K129A mutant variant was prepared in order to trap its substrate, UDP‐GlcNAc, into the active site. Pen adopts a hexameric quaternary structure with each subunit showing the bilobal architecture observed for members of the short‐chain dehydrogenase/reductase superfamily. The hexameric quaternary structure is atypical for most members of the superfamily. The structure of Pal was determined in the presence of UDP. Pal adopts the more typical dimeric quaternary structure. Taken together, Pen and Pal catalyze the conversion of UDP‐GlcNAc to UDP‐4‐keto‐6‐deoxy‐l ‐N‐acetylaltrosamine. Strikingly, in Gram negative bacteria such as Campylobacter jejuni and Helicobacter pylori, only a single enzyme (FlaA1) is required for the production of UDP‐4‐keto‐6‐deoxy‐l ‐N‐acetylaltrosamine. A comparison of Pen and Pal with FlaA1 reveals differences that may explain why FlaA1 is a bifunctional enzyme whereas Pen and Pal catalyze the individual steps leading to the formation of the UDP‐sugar product. This investigation represents the first structural analysis of the enzymes in B. thuringiensis that are required for CMP‐pseudaminic acid formation.     

Unique Microbial Signatures of the Alien Hawaiian Marine Sponge Suberites zeteki

Invasive species poses a threat to the world’s oceans. Alien sponges account for the majority of introduced marine species in the isolated Hawaiian reef ecosystems. In this study, cultivation-dependent and cultivation-independent techniques were applied to investigate microbial consortia associated with the alien Hawaiian marine sponge Suberites zeteki. Its microbial communities were diverse with representatives of Actinobacteria, Firmicutes, α- and γ-Proteobacteria, Bacteroidetes, Chlamydiae, Planctomycetes, and Cyanobacteria. Specifically, the genus Chlamydia was identified for the first time from marine sponges, and two genera (Streptomyces and Rhodococcus) were added to the short list of culturable actinobacteria from sponges. Culturable microbial communities were dominated by Bacillus species (63%) and contained actinobacterial species closely affiliated with those from habitats other than marine sponges. Cyanobacterial clones were clustered with free-living cyanobacteria from water column and other environmental samples; they show no affiliation with other sponge-derived cyanobacteria. The low sequence similarity of Planctomycetes, Chlamydiae, and α-Proteobacteria clones to other previously described sequences suggested that S. zeteki may contain new lineages of these bacterial groups. The microbial diversity of S. zeteki was different from that of other studied marine sponges. This is the first report on microbial communities of alien marine invertebrate species. For the first time, it provides an insight into microbial structure within alien marine sponges in the Hawaiian marine ecosystems.