Microbial diversity in the coralline sponge Vaceletia crypta

Coralline sponges of the genus Vaceletia are regarded as ‘living fossils’, the only recent members of the so-called ‘sphinctozoan-type’ sponges that contributed to reef-building during the Palaeozoic and Mesozoic eras. Vaceletia species were thought to be extinct until the discovery of Vaceletia crypta in the 1970s. Here, we used molecular methods to provide first insights into the microbial diversity of these coralline sponges. Both denaturing gradient gel electrophoresis (DGGE) analyses of 19 Vaceletia specimens and the analysis of 427 clones from a bacterial 16S rRNA gene clone library of a specimen of V. crypta from the Great Barrier Reef (Australia) revealed high diversity and a complex composition with a relatively uniform phylogenetic distribution. Only a single archaeal 16S rRNA phylotype was recovered. The most abundant bacteria were the Chloroflexi (35 %). Of the microbial community, 58 % consisted of the Gammaproteobacteria, Gemmatimonadetes, Actinobacteria, Nitrospira, Deltaproteobacteria, Deferribacteres and Acidobacteria, with nearly equal representation. Less abundant members of the microbial community belonged to the Alphaproteobacteria (3 %), as well as to the Poribacteria, Betaproteobacteria, Cyanobacteria, Spirochaetes, Bacteroidetes, Deinococcus-Thermus and Archaea (all together 4 %). Of the established 96 OTUs, 88 % were closely related to other sponge-derived sequences and thereof 71 OTUs fell into sponge- or sponge-coral specific clusters, which underscores that the “living fossil” coralline sponge Vaceletia shares features of its microbial community with other sponges. The DGGE cluster analysis indicated distinct microbial communities in the different growth forms (solitary and colonial) of Vaceletia species.     

Photosynthesis versus Exopolymer Degradation in the Formation of Microbialites on the Atoll of Kiritimati,Republic of Kiribati,Central Pacific

Aragonitic microbialites, characterized by a reticulate fabric, were discovered beneath lacustrine microbial mats on the atoll of Kiritimati, Republic of Kiribati, Central Pacific. The microbial mats, with cyanobacteria as major primary producers, grow in evaporated seawater modified by calcium carbonate and gypsum precipitation and calcium influx via surface and/or groundwaters. Despite the high aragonite supersaturation and a high photosynthetic activity, only minor aragonite precipitates are observed in the top parts of the microbial mats. Instead, major aragonite precipitation takes place in lower mat parts at the transition to the anoxic zone. The prokaryotic community shows a high number of phylotypes closely related to halotolerant taxa and/or taxa with preference to oligotrophic habitats. Soil- and plant- inhabiting bacteria underline a potential surface or subsurface influx from terrestrial areas, while chitinase-producing representatives coincide with the occurrence of insect remains in the mats. Strikingly, many of the clones have their closest relatives in microorganisms either involved in methane production or consumption of methane or methyl compounds. Methanogens, represented by the methylotrophic genus Methanohalophilus, appear to be one of the dominant organisms in anaerobic mat parts. All this points to a significant role of methane and methyl components in the carbon cycle of the mats. Nonetheless, thin sections and physicochemical gradients through the mats, as well as the ¹²C-depleted carbon isotope signatures of carbonates indicate that spherulitic components of the microbialites initiate in the photosynthesis-dominated orange mat top layer, and further grow in the green and purple layer below. Therefore, these spherulites are considered as product of an extraordinary high photosynthesis effect simultaneous to a high inhibition by pristine exopolymers. Then, successive heterotrophic bacterial activity leads to a condensation of the exopolymer framework, and finally to the formation of crevice-like zones of partly degraded exopolymers. Here initiation of horizontal aragonite layers and vertical aragonite sheets of the microbialite occurs, which are considered as a product of high photosynthesis at decreasing degree of inhibition. Finally, at low supersaturation and almost lack of inhibition, syntaxial growth of aragonite crystals at lamellae surfaces leads to thin fibrous aragonite veneers. While sulfate reduction, methylotrophy, methanogenesis and ammonification play an important role in element cycling of the mat, there is currently no evidence for a crucial role of them in CaCO₃ precipitation. Instead, photosynthesis and exopolymer degradation sufficiently explain the observed pattern and fabric of microbialite formation.     

Phylogenetic Diversity and Community Structure of the Symbionts Associated with the Coralline Sponge Astrosclera willeyana of the Great Barrier Reef

The coralline sponge Astrosclera willeyana, considered to be a living representative of the reef-building stromatoporoids of the Mesozoic and the Paleozoic periods, occurs widely throughout the Indo-Pacific oceans. We aimed to examine, for the first time, the phylogenetic diversity of the microbial symbionts associated with A. willeyana using molecular methods and to investigate the spatial variability in the sponge-derived microbial communities of A. willeyana from diverse sites along the Great Barrier Reef (GBR). Both denaturing gradient gel electrophoresis (DGGE) analyses of 12 Astrosclera specimens and sequencing of a 16S rRNA gene clone library, constructed using a specimen of A. willeyana from the Yonge Reef (380 clones), revealed the presence of a complex microbial community with high diversity. An assessment of the 16S rRNA gene sequences to the particular phylogenetic groups showed domination of the Chloroflexi (42 %), followed by the Gammaproteobacteria (14 %), Actinobacteria (11 %), Acidobacteria (8 %), and the Deferribacteres (7 %). Of the microbes that were identified, a further 15 % belonged to the Deltaproteobacteria, Alphaproteobacteria, and Nitrospirae genera. The minor phylogenetic groups Gemmatimonadetes, Spirochaetes, Cyanobacteria, Poribacteria, and the Archaea composed 3 % of the community. Over 94 % of the sequences obtained from A. willeyana grouped together with other sponge- or coral-derived sequences, and of these, 72 % formed, with nearest relatives, 46 sponge-specific or sponge–coral clusters, highlighting the uniqueness of the microbial consortia in sponges. The DGGE results showed clear divisions according to the geographical origin of the samples, indicating closer relationships between the microbial communities with respect to their geographic origin (northern vs. southern GBR).