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A new genus and species of hypercalcified calcareous sponge, Gzhelistella cornigera gen. et sp. nov., is described from the Kosherovo Formation (Gzhelian Stage) of the Moscow region. The new genus is the first representative of hypercalcified calcareous sponges from the Upper Carboniferous with an "inozoan-like" internal structure and a characteristic spicular organization of the skeleton. [ABSTRACT FROM AUTHOR]

Sponges-associated microorganisms play important roles in their health and ecology; consequently, they may be crucial in the successful adaptation of exotic species to novel environments. However, few studies have focused on the microbial diversity of exotic sponges, especially those with calcium carbonate spicules (class Calcarea). Therefore, this is the first in situ characterization of the microbiota of the exotic calcareous sponges Sycettusahastifera and Paraleucillamagna. Our results suggest that S. hastifera has a more stable microbiota than P. magna, as there were no differences in its beta diversity among sampling sites. Conversely, P. magna showed significant differences in its microbial communities, perhaps related to its adhesion to artificial substrate and/or shellfish mariculture activities. Each sponge species presented a single dominant proteobacterial OTU potentially active in the nitrogen cycle, which could help sponge detoxification, especially in polluted areas where exotic species usually establish. Our results show the importance of assessing the microbial diversity to unveil host-microorganism relationships and suggest that these associated nitrogen-cycling microorganisms could favor the success of exotic sponges in new environments. [ABSTRACT FROM AUTHOR]

Abstract—: The Middle-Late Permian reefs were formed in two paleogeographic realms: North Pangaea and Tethyan Realm. The basic reef builders in the first realm were representatives of Calcispongiae and Bryozoa; in the second realm, sphinctozoans, corals, and stromatoporoids. In these realms, various algae and cyanobacteria communities were of importance. Reef construction in the first realm associated with arid climatic conditions, isolation of water basins, and accumulation of salt-bearing sequences came to the end in the early Late Permian. Reef construction in the Tethyan Realm occurred in the Late Permian up to the Permian-Triassic boundary. The termination of reef construction was due to features of the reef ecosystem, which turned out to be unstable against the background of variations in the conditions and mass extinction at the Permian-Triassic boundary and dissociated before the termination of this extinction. [ABSTRACT FROM AUTHOR]

Fertilization is an important factor influencing the chemical structure of soil organic carbon (SOC) and soil microbial communities; however, whether any connection exists between the two under different fertilization regimes remains unclear. Soils from a 27-year field experiment were used to explore potential associations between SOC functional groups and specific bacterial taxa, using quantitative multiple cross-polarization magic-angle spinning 13C nuclear magnetic resonance and 16S rRNA gene sequencing. Treatments included balanced fertilization with organic materials (OM) and with nitrogen (N), phosphorus (P), and potassium (K) mineral fertilizers (NPK); unbalanced fertilization without one of the major elements (NP, PK, or NK); and an unamended control. These treatments were divided into four distinct groups, namely OM, NPK, NP plus PK, and NK plus control, according to their bacterial community composition and SOC chemical structure. Soil total P, available P, and SOC contents were the major determinants of bacterial community composition after long-term fertilization. Compared to NPK, the OM treatment generated a higher aromatic C-O and OCH3 and lower alkyl C and OCH abundance, which were associated with the enhanced abundance of members of the Acidobacteria subgroups 6 and 5, Cytophagaceae, Chitinophagaceae, and Bacillus sp.; NP plus PK treatments resulted in a higher OCH and lower aromatic C-C abundance, which showed a close association with the enrichment of unclassified Chloracidobacteria, Syntrophobacteraceae, and Anaerolineae and depletion of Bacillales; and NK plus control treatments resulted in a higher abundance of aromatic C-C, which was associated with the enhanced abundance of Bacillales. Our results indicate that different fertilization regimes changed the SOC chemical structure and bacterial community composition in different patterns. The results also suggest that fertilization-induced variations in SOC chemical structure were strongly associated with shifts in specific microbial taxa which, in turn, may be affected by changes in soil properties. [ABSTRACT FROM AUTHOR]

Calcaronean sponges are acknowledged to be taxonomically difficult, and generally, molecular data does not support the current morphology-based classification. In addition, molecular markers that have been successfully employed in other sponge taxa (e.g., COI mtDNA) have proven challenging to amplify due to the characteristics of calcarean mitochondrial genomes. A short fragment of the 28S rRNA gene (C-region) was recently proposed as the most phylogenetically informative marker to be used as a DNA barcode for calcareous sponges. In this study, the C-region and a fragment of the 18S rRNA gene were sequenced for a wide range of calcareous taxa, mainly from the subclass Calcaronea. The resulting dataset includes the most comprehensive taxon sampling of Calcaronea to date, and the inclusion of multiple specimens per species allowed us to evaluate the performance of both markers, as barcoding markers. 18S proved to be highly conserved within Calcaronea and does not have sufficient signal to resolve phylogenetic relationships within the subclass. Although the C-region does not exhibit a “proper” barcoding gap, it provides good phylogenetic resolution for calcaronean sponges. The resulting phylogeny supports previous findings that the current classification of the subclass Calcaronea is highly artificial, and with high levels of homoplasy. Furthermore, the close relationship between the order Baerida and the genus Achramorpha suggest that the order Baerida should be abandoned. Although the C-region currently represents the best available marker for phylogenetic and barcoding studies in Calcaronea, it is necessary to develop additional molecular markers to improve the classification within this subclass. [ABSTRACT FROM AUTHOR]

The Red Sea is a biodiversity hotspot with a considerable percentage of endemic species for many marine animals. Little is known about the diversity and distribution of calcareous sponges (Porifera, Class Calcarea) in this marginal sea. Here we analysed calcareous sponges of the subclass Calcinea that were collected between 2009 and 2013 at 20 localities in the Red Sea, ranging from the Gulf of Aqaba in the north to the Farasan Islands in the south, to document the species of this region. For this, we applied an integrative approach: We defined OTUs based on the analyses of a recently suggested standard DNA marker, the LSU C-region. The analysis was complemented with a second marker, the internal transcribed spacer, for selected specimens. Ten OTUs were identified. Specimens of each OTU were morphologically examined with spicule preparations and histological sections. Accordingly, our ten OTUs represent ten species, which cover taxonomically a broad range of the subclass. By combining molecular and morphological data, we describe four new species from the Red Sea: Soleneiscus hamatus sp. nov., Ernstia arabica sp. nov., Clathrina rotundata sp. nov., and Clathrina rowi sp. nov.. One additional small specimen was closely related to 'Clathrina' adusta, but due to the small size it could not be properly analysed morphologically. By providing the DNA sequences for the morphologically documented specimens in the Sponge Barcoding Database () we facilitate future DNA-assisted species identification of Red Sea Calcinea, even for small or incomplete samples, which would be insufficient for morphological identification. Application of DNA barcode methods in the subclass will help to further investigate the distribution of Calcinea in the Red Sea and adjacent regions. [ABSTRACT FROM AUTHOR]

Calcareous sponges are taxonomically difficult, and their morpho-systematic classification often conflicts with molecular phylogenies. Consequently, species descriptions that rely solely on morphological characters,and taxonomic revisions appear to provide little to no information about phylogenetic affiliations and integrative approaches, combining DNA and morphological data, are applied more frequently. However, a standardized database that combines DNA sequence and morphological specimen information is still missing for calcareous sponges. The mitochondrial cytochrome oxidase subunit 1 gene (COI) is the marker of choice for rapid species identification in many other animal taxa, including demosponges, for which COI sequences and morphological information have been compiled in the sponge barcoding database (). But due to the peculiarities of calcarean mitochondrial genomes, sequencing COI in Calcarea is methodologically challenging. We here propose the use of one more commonly used DNA marker, the C-region of the 28S gene (LSU), as standard barcoding marker for Calcarea, after also considering the internal transcribed spacer (ITS) region for such proposes. Especially in the subclass Calcaronea, we observed severe problems of high intra- and intergenomic variation that impedes pan-calcarean ITS alignments. In contrast, the C-region of LSU provides a short but phylogenetically informative DNA sequence, alignable across both subclasses with the help of a newly developed secondary structure and which also can be used to address exemplary taxonomic questions. With our work, we start to close the gap of Calcarea in the sponge barcoding project () and provide a resource for biodiversity studies and potentially for DNA-guided species identification. [ABSTRACT FROM AUTHOR]

Calcareous fens have a high conservation priority in the European Union. They are very unique, very sensitive and very rare habitats in Latvia as well as in many other European countries. Because of their rarity, many organisms living in calcareous fens are nowadays considered threatened. The same is applied to spiders. Spiders have been suggested as good biodiversity indicators because they have numerous direct and indirect relationships with other organisms. Only few investigations have been carried out on fen inhabiting spiders. The knowledge of grass-dwelling spiders is especially lacking. Thus the aim of this study was to evaluate grass-dwelling spider diversity in several calcareous fens of Latvia, compare these fens and to find out the habitat features that might affect grass-layer inhabiting spiders. The research was carried out in eight calcareous fens located in the Coastal Lowland of Latvia. A total of 760 spiders from nine families and 20 species were collected with a sweep net. Two of the most abundant spider species were Dolomedes fimbriatus (Clerck, 1757) and Tibellus maritimus (Menge, 1875). Diversity indices suggested that the grass-dwelling spider community consists of few abundant species and numerous rare species. Correlation analysis as well as DCA showed that plant species diversity did not significantly affect spider species richness and diversity, although at the same time there were a lot of significant associations between spiders and individual plant species. It was shown that various spider species responded very differently to the presence of particular plant species, and thus habitat structural heterogeneity emerges to be an important factor influencing the grass-dwelling spider diversity and community structure. Correlation analysis also revealed that spider abundance was negatively affected by the vegetation height and wind speed. [ABSTRACT FROM AUTHOR]

The taxonomy of the class Calcarea has long relied on histological and morphological characters, with a few molecular studies done. In character-poor genera, such as Clathrina, an integrative taxonomy, associating morphological and molecular tools, greatly aids in the species identification. In this study, we describe four Clathrina species from the northern Adriatic Sea using morphology and DNA sequences together with observations on their ecology. Clathrina clathrus and Clathrina blanca have been previously reported for the Adriatic Sea; however, it is the first time that a DNA sequence of C. blanca has been obtained. Clathrina cf. hondurensis, a Caribbean species, is being reported in the Adriatic Sea for the first time, and we present the first description and DNA sequence of Clathrina rubra, a red species originally mentioned from Naples. [ABSTRACT FROM AUTHOR]

The problem of the origin of Metazoa has been one of the most discussed for nearly the last one and a half centuries. Some 20 years ago, morphological approaches were replaced with molecules, but the problem then became more complex. At the same time, morphological data were incomplete, and therefore, this approach can still help in comparison with choanoflagellates and sponges—two sister groups having uniflagellated cells with a collar. The structure of the flagellar apparatus has phylogenetic significance, but sponge choanocytes are poorly studied in this respect, and we still do not know what the ancestral kinetid of Porifera looks like. The kinetid structure of choanocytes in Sycon sp. is investigated here for the first time, and a 3D reconstruction of the kinetid provided. It is composed of a flagellar kinetosome with a nuclear fibrillar root and a basal foot with a few microtubules; the accessory centriole lies orthogonal to and just below the foot of the kinetosome, and a dictyosome is near the centriole. This kinetid is similar to that of the choanocyte of Corticium candelabrum (Homoscleromorpha) and is considered to be the ancestral type for the whole branch Calcarea + Homoscleromorpha. [ABSTRACT FROM AUTHOR]

The process of inversion observed during the development of Calcaronea (Calcarea, Porifera) species is a unique and remarkable event in the Metazoa. However, few studies have focused on the embryogenesis of Calcaronea species or on the ultrastructure of their larva and its accessory epithelium, the so-called placental membrane. Herein, using light and electron microscopy, we describe the embryogenesis and ultrastructure of the amphiblastula of Paraleucilla magna (Porifera, Calcarea, Calcaronea). It was observed that the cleavage in this species is of the table-like palyntomy type, typical of calcaroneans. Cleavage leads to the formation of a stomoblastula, which becomes inverted in the mesohyl. At the same time, the accessory epithelium (here called epilarval trophocyte epithelium) rises, isolating and nursing the early larva. The amphiblastula is formed by an epithelium composed of ciliated cells, granular cells, and cross-cells, this latter persisting even after larval release. Some degenerating amoeboid cells and bacteria were found in the larval cavity, possibly helping with larval nutrition. The possibility of cross-cells being precursors of the germ cell lineage and the vertical transmission of bacteria found in the larva are discussed. [ABSTRACT FROM AUTHOR]

In most animals mitochondrial DNA (mtDNA) evolves much faster than nuclear DNA. Therefore, and because of its shorter coalescent time, mitochondrial (mt) markers provide better resolution to trace more recent evolutionary events compared to nuclear DNA. But in contrast to most other Metazoa, previous studies suggested that in sponges mitochondrial sequence evolution is much slower, making mtDNA less suitable for studies at the intraspecific level. However, these observations were made in the class Demospongiae and so far no data exist for calcareous sponges (Class Calcarea). We here provide the first study that evaluates intraspecific mt sequence variation in Calcarea. We focus on arguably the best-studied species Leucetta chagosensis, for which three nuclear DNA marker datasets existed previously. We here sequenced the partial mitochondrial cytochrome oxidase subunit III gene ( cox3). Our analyses reveal an unexpected variability of up to 8.5% in this mitochondrial marker. In contrast to other sponges where this marker evolves considerable slower than the nuclear internal transcribed spacer region ( ITS), we found that cox3 in L. chagosensis evolves about five times as fast as ITS. The variability is similar to that of nuclear intron data of the species. The phylogeny inferred with cox3 is congruent with other markers, but separates earlier reported genetic groups much more distinctively than nuclear DNA. This provides further evidence for cryptic speciation in L. chagosensis. All these features make calcarean mtDNA exceptional among sponges and show its suitability for phylogeographic studies and potential as a species-specific (DNA barcoding) marker to distinguish morphologically identical cryptic species. [ABSTRACT FROM AUTHOR]

The aquiferous system is an essential character of poriferans and supports their monophyly. Within the Calcarea, this system displays its greatest variety and traditionally is classified as: asconoid, syconoid, sylleibid, and leuconoid. Species of Leucascus, however, present a different type of aquiferous system composed of anastomosed (interconnected) choanocyte tubes and have an atrium lacking choanoderm. There is such confusion about the classification of the aquiferous system of Leucascus that, depending on the author, it has been classified as asconoid, syconoid, or leuconoid. Therefore, in the present work, we describe a new type of aquiferous system for Leucascus: the solenoid aquiferous system. This new aquiferous system is defined by the presence of anastomosed tubes internally lined by choanocytes and atrium without choanoderm. Although no deep phylogenetic significance has been attributed to the aquiferous system, the solenoid system raises important evolutionary questions about the variety of systems found among the poriferans. [ABSTRACT FROM AUTHOR]

Gametogenesis in Calcarea is still poorly known; therefore, in this work, we describe the gametogenesis of Paraleucilla magna (Porifera, Calcarea) using light and electron microscopy. Male and female gametes derived from choanocytes. Oocytes grew inside a follicle-like structure composed of pinacocyte-like cells and choanocytes. They were nourished through nutrient transfer from nurse cells and through bacteria phagocytosis, which was never documented for a calcarean species. Mature oocytes were typical, spherical, with nucleolated nuclei and a cytoplasm filled with different types of inclusions and digestive vesicles. Nuage was also found. Spermatogenesis occurred in the lumen of differentiated choanocyte chambers, and spermatic cysts were never formed. Spherical spermatogonia without flagellum or collar were derived from hourglass-shaped primordial germ cells. Spermatozoa were of the 'aberrant type', showed a compact electron-dense nucleus and a homogeneous granulated body in its cytoplasm. The gametogenesis of P. magna is similar to what has been observed for other Porifera and Eumetazoa. [ABSTRACT FROM AUTHOR]

Aerobic and anaerobic microbial key processes were quantified and compared to microbial numbers and morphological structure in Mediterranean sponges. Direct counts on histological sections stained with DAPI showed that sponges with high microbial abundances (HMA sponges) have a denser morphological structure with a reduced aquiferous system compared to low microbial abundance (LMA) sponges. In Dysidea avara, the LMA sponge, rates of nitrification and denitrification were higher than in the HMA sponge Chondrosia reniformis, while anaerobic ammonium oxidation and sulfate reduction were below detection in both species. This study shows that LMA sponges may host physiologically similar microbes with comparable or even higher metabolic rates than HMA sponges, and that anaerobic processes such as denitrification can be found both in HMA and LMA sponges. A higher concentration of microorganisms in the mesohyl of HMA compared to LMA sponges may indicate a stronger retention of and, hence, a possible benefit from associated microbes. [ABSTRACT FROM AUTHOR]

In recent years, reports of sponge bleaching, disease, and subsequent mortality have increased alarmingly. Population recovery may depend strongly on colonization capabilities of the affected species. The giant barrel sponge Xestospongia muta is a dominant reef constituent in the Caribbean. However, little is known about its population structure and gene flow. The 5 ′-end fragment of the mitochondrial gene cytochrome oxidase subunit I is often used to address these kinds of questions, but it presents very low intraspecific nucleotide variability in sponges. In this study, the usefulness of the I3-M11 partition of COI to determine the genetic structure of X. muta was tested for seven populations from Florida, the Bahamas and Belize. A total of 116 sequences of 544 bp were obtained for the I3- M11 partition corresponding to four haplotypes. In order to make a comparison with the 5 ′-end partition, 10 sequences per haplotype were analyzed for this fragment. The 40 resulting sequences were of 569 bp and corresponded to two haplotypes. The nucleotide diversity of the I3-M11 partition (π = 0.00386) was higher than that of the 5 ′-end partition (π = 0.00058), indicating better resolution at the intraspecific level. Sponges with the most divergent external morphologies (smooth vs. digitate surface) had different haplotypes, while those with the most common external morphology (rough surface) presented a mixture of haplotypes. Pairwise tests for genetic differentiation among geographic locations based on FST values showed significant genetic divergence between most populations, but this genetic differentiation was not due to isolation by distance. While limited larval dispersal may have led to differentiation among some of the populations, the patterns of genetic structure appear to be most strongly related to patterns of ocean currents. Therefore, hydrological features may play a major role in sponge colonization and need to be considered in future plans for management and conservation of these important components of coral reef ecosystems. [ABSTRACT FROM AUTHOR]

Abstract  Larval development and follicle structure of a representative of the Calcinea (Calcispongiae) Guancha arnesenae from the White Sea have been studied for the first time at the ultrastructural level. The follicle in G. arnesenae has an unusual structure: it consists of trapezoid cells rich in phagosomes and a surrounding dense collagen layer. Follicular cells differentiate from choanocytes. Cleavage results in formation of a hollow, equal, non-polarized coeloblastula. Larval morphogenesis occurs by means of direct hollow blastula formation without any individual cell or cell layer movements. The coeloblastula (calciblastula) larva of G. arnesenae is completely ciliated. The larva also contains rare non-ciliated cells: vacuolar cells, bottle-shaped cells and free cells in a central cavity. The basal ciliary apparatus of larval cells includes the basal body, an accessory centriole oriented perpendicularly to it, the basal foot, and two cross-striated rootlets. A bundle of microtubules emerges from the side of the basal body, opposite to the basal foot, running parallel to the outer surface. All bundles of cells are parallel to each other and oriented towards the posterior larval pole, forming a transverse cytoskeletal system. Specialized intercellular junctions in the apical regions of all ciliated cells are revealed for the first time in a Calcispongiae larva. The central larval cavity contains symbiotic bacteria, which are included inside the embryo at the blastula stage. [ABSTRACT FROM AUTHOR]

The new calcisponges Regispongia fluegeli n. sp., and Iranospongia circulara n. gen. n. sp., are described from central Iran. These are the first heteractinid sponges reported from the Permian of the region. These wewokellid sponges are large, irregularly cylindrical forms with a distinct axial spongocoel. The calcareous spicular skeletons of both taxa have been overgrown and are recrystallized. However, the preserved skeleton of Regispongia fluegeli does include large polyactines in the main endosomal layer and small octactines and possibly other polyactine spicules in both the relatively massive dermal layer and the distinct, delicately spiculed, gastral layer. Iranospongia is characterized by a discontinuous ring of vertical exhalant canals interior to the dense dermal layer, and by an interior skeleton net that includes common coarse vertical fibers. Individual spicules in Iranospongia are commonly obscured, but locally some remnants of possible polyactines occur in outer parts of the skeleton. [ABSTRACT FROM AUTHOR]

Recent pharetronid sponges were regarded as relict species in tropical and subtropical waters, inhabiting cryptic habitats on coral reefs and in caves. More recent findings of a new species of the genus Plectroninia off northern Norway, with an inner fused skeleton have changed that view. Recent investigations on the sponge fauna of the “Propeller Mound”, northern Porcupine Seabight, focusing on sponges growing on the azooxanthellate cold-water coral Lophelia pertusa (Linné 1758) and Madrepora oculata Linné 1758, established the presence of a species of Plectroninia new to science. Its status as a common species within this deep-water coral habitat and the general status of the genus Plectroninia are discussed. [ABSTRACT FROM AUTHOR]

Sponges display a variety of reproductive strategies that have the potential to influence population genetic structure. Histological examination of ten reproductive individuals of the Western Australian spongeHaliclonasp. showed that this species broods embryonic larvae that are potentially limited in dispersal capabilities. Because sponges have the potential to propagate in a number of modes, allozyme electrophoresis was used to assess the relative importance of asexual and sexual reproduction to recruitment, and to quantify genetic subdivision over different spatial scales. Tissue samples from 227 sponges were collected from reefs within two areas 400 km apart: Hamelin Bay and Rottnest Island. Contrary to expectations for highly clonal populations, genotypic diversity within sites was high, no linkage disequilibrium was found, and there was no evidence of genotypic clustering within reefs. There was no genetic evidence that asexual reproduction is important for the maintenance of populations. Genetic comparisons were consistent with mixing of sexually produced recruits within reefs, on a scale up to a few hundred metres, but significant genetic subdivision between reefs (FST=0.069 at Hamelin Bay, 0.130 at Rottnest Island) indicated that water gaps of several hundred metres are effective at preventing dispersal. Subdivision between the two areas, separated by 400 km, was moderately greater (FST=0.142) than within, but the same alleles were predominant in the two areas. These genetic patterns are consistent with limited dispersal capabilities of brooded larvae. [ABSTRACT FROM AUTHOR]

Biologically-active substances were investigated from 35 demosponge species and 5 calcareous sponge species collected from intertidal or shallow subtidal habitats near San Diego, California, USA, from 1978 to 1980. Crude methanolic extracts of each species were tested for suppression of growth by bacteria (7 species) and a yeast. Antimicrobial activity was found in 26 Demospongiae and 2 Calcarea. Strong activity was found in 11 demosponges and, subsequently, 38 natural products with antimicrobial activity were isolated from 8 of these species ( Aplysina fistularis, Dysidea amblia, Leiosella idia, Euryspongia sp., Toxadocia zumi, Axinella sp., Haliclona?cinerea and ? Pachychalina lunisimilis). Twenty-eight of these natural products (usually as pure compounds) were assayed for: (1) suppression of growth of marine fungi (3 spp.) and a red alga; (2) behavior modifications of invertebrate adults (4spp.); (3) toxicity to a goldfish; (4) inhibition of sexual reproduction of a brown alga; (5) inhibition of settlement and/or metamorphosis of late larvae or invertebrate juveniles (4spp.). Many of the natural products were also incorporated into pelleted fish food and tested for feeding-behavior modifications of fishes (5 spp.). Three of the compounds from Dysidea amblia were inactive in all tests. All other natural products were active in at least one assay, although none was active in all assays. The discussion relates the possession of biologically-active substances to the ecology of each sponge species; for example, sponges with antimicrobial substances are rarely overgrown. [ABSTRACT FROM AUTHOR]

The endolithic and endopsammic habits in sponges promote similar morphologies and offer similar ecological niches of being protected and anchored. We assessed whether this also induces similar functions, i.e., whether the commonly endopsammic sponge Coelocarteria singaporensis (Carter, 1883) shares bioerosion capabilities with clionaid endopsammic sponges such as some Spheciospongia species, enabling it to inhabit and also to expand within calcareous substrates. We studied a range of traits that are commonly accepted as evidence for bioerosion. C. singaporensis has a globular or irregular body from which fistules arise, but the fistules never penetrated calcareous substrate, and while endopsammic specimens were able to agglutinate and incorporate particles, their bodies were not embedded within calcareous rock. Tough tissue filled small cavities in adjacent rock, but only in a few exceptions did we find sponge chips in it. We encountered the only indication for possible active bioerosion in the form of sponge scars and canals in some of the substrate the sponge touched or had embedded, but these areas lacked fresh erosion fissures and well-defined erosion scars and may have been made by other species. If C. singaporensis is able to bioerode, it does not seem to cut out chips to produce a regular shagreen pattern. The sponge clearly has the ability to insinuate into pre-existing cavities, but overall we regard the evidence for its bioerosion capability as circumstantial or unreliable. At this stage, we can neither confirm nor reject that this sponge may be able to bioerode calcareous material, but it appears to be unlikely. [ABSTRACT FROM AUTHOR]