Can the morphology of the integumentary spicules be used to distinguish genera and species of phyllidiid nudibranchs (Porostomata: Phyllidiidae)?

Thirty-eight specimens belonging to four genera and 15 species of the nudibranch family Phyllidiidae were examined to investigate whether the morphology of their integumentary calcareous spicules and/or the occurrence of the spicules within the regions of the body could be used to distinguish genera and species. The spicules were studied separately from five regions of the body of each specimen—the foot, gills, mantle, dorsal pustules (or ridges in Reticulidia) and rhinophores. The mantle itself plus its pustules were found to possess the full complement of spicules in every individual. Four types of spicules were recorded overall—smooth diactines, centro-polytylote diactines, triactines and tetractines. Different regions of the body were found to possess different spicule types: (a) only smooth diactines in the gills, (b) both smooth diactines and triactines in the foot and (c) all of smooth diactines, centro-polytylote diactines and triactines in the mantle, dorsal pustules and the rhinophores. Among the genera, three types of spicules (smooth diactine, triactine, and tetractine) are present in Phyllidia, Phyllidiopsis and Reticulidia, but the form of the spicules is not diagnostic between these genera or between the constituent species. The fourth type of spicule (centro-polytylote diactine) is present exclusively in Phyllidiella, and is diagnostic for that genus. However, we failed to find any difference in spicule form, or composition, or location in the body between the three (closely related) species of Phyllidiella we investigated. Therefore, our key conclusion is that spicule morphology is an extremely important character to tell the genus Phyllidiella apart from all the other genera of the family, but it is not taxonomically informative at the level of species.     

Structural investigations of octocoral sclerites

A common structural pattern (as observed under the SEM) in the main body of sectioned sclerites of the family Alcyoniidae, and octocorals in general, is the arrangement of acicular crystals in concentric layers. The crystals roughly follow the direction of the spicule axis, however, the sectioned tubercles of large Sinularia spicules have the acicular crystals oriented in the direction of the tubercles (i.e. perpendicular to the spicule axis), contrary to the sectioned tubercles of Sarcophyton and Lobophytum spicules. They reveal some rod-like structures, furcating the acute processes at the top of the tubercles. Sectioned small, club-like Sinularia sclerites show numerous tiny acicular crystals, oriented with their long axes at a fairly constant degree of inclination around a central axis. SEM studies of sectioned Cladiella sclerites show a granulate structure organized in concentric layers, but lacking acicular crystals. The Silurian Atractosella cataractaca show important characters in common with Recent alcyoniid species.     

Silica deposition in Demosponges: spiculogenesis in Crambe crambe

Transmission electron-microscopy images coupled with dispersive X-ray analysis of the species Crambe crambe have provided information on the process of silica deposition in Demosponges. Sclerocytes (megasclerocytes) lie close to spicules or surround them at different stages of growth by means of long thin enveloping pseudopodia. Axial filaments occur free in the mesohyl, in close contact with sclerocytes, and are triangular in cross section, with an internal silicified core. The unit-type membrane surrounding the growing spicule coalesces with the plasmalemma. The axial filament of a growing spicule and that of a mature spicule contain 50%-70% Si and 30%-40% Si relative to that contained in the spicule wall, respectively. The extracellular space between the sclerocyte and the growing spicule contains 50%-65%. Mitochondria, vesicles and dense inclusions of sclerocytes exhibit less than 10%. The cytoplasm close to the growing spicule and that far from the growing spicule contain up to 50% and less than 10%, respectively. No Si has been detected in other parts of the sponge. The megascleres are formed extracellularly. Once the axial filament is extruded to the mesohyl, silicification is accomplished in an extracellular space formed by the enveloping pseudopodia of the sclerocyte. Si deposition starts at regularly distributed sites along the axial filament; this may be related to the highly hydroxylated zones of the silicatein-alpha protein. Si is concentrated in the cytoplasm of the sclerocyte close to the plasmalemma that surrounds the growing spicules. Orthosilicic acid seems to be pumped, both from the mesohyl to the sclerocyte and from the sclerocyte to the extracellular pocket containing the growing spicule, via the plasmalemma.     

Socket cells mediate spicule morphogenesis in Caenorhabditis elegans males.

Caenorhabditis elegans male spicule morphogenesis requires the coordinated cellular behaviors of several types of cells. We found that the spicule neurons and sheath cells, although important for spicule function, are dispensable for spicule morphology. In contrast, the spicule socket cells are essential for both spicule elongation and formation of spicule cuticle. The socket cells are not only necessary but also sufficient to produce spicule cuticle. This functional aspect of socket cells is genetically separable from their function in mediating spicule elongation: elongated spicules with defective spicule cuticle can be formed. During spicule morphogenesis, the expression of an egl-17::GFP reporter gene is found in the spicule socket cells and its expression appears to be regulated in the socket cells. Mutants defective in TGF-beta signaling display a crumpled spicules phenotype as a result of failure of socket cell movement during spicule morphogenesis. These observations suggest that both the FGF and the TGF-beta signaling pathways might be involved in spicule elongation.     

Ancestors and homology

Current issues concerning the nature of ancestry and homology are discussed with reference to the evolutionary origin of the tetrapod limb. Homologies are argued to be complex conjectural inferences dependant upon a pre-existing phylogenetic analysisand a theoretical model of the evolutionary development of ontogenetic information. Ancestral conditions are inferred primarily from character (synapomorphy/homology) distributions within phylogeny, because of the deficiencies of palaeontological data. Recent analyses of tetrapod limb ontogeny, and the diverse, earliest morphologies known from the fossil record, are inconsistent with typological concepts such as fixed ancestral patterns or bauplans, emphasising the incompatibility of these with evolutionary continuity. The evolutionary origin of the tetrapod limb is also examined in the light of its recent discussion in developmental genetics. While this field promises to reveal more of the fundamental ontogenetic content of homology (identity), at present it is concerned mostly with the abstraction of a new set of types, rather than investigating diversity and change.     

Skeletal morphology of two controversial Poecilosclerid genera (Porifera,Demospongiae):Discorhabdella andCrambe

The generaDiscorhabdella andCrambe are characterized by bearing uncommon spicule types, i.e. pseudoastrose acanthostyles and sphaeroclones, respectively. They have traditionally been considered to be unrelated taxa, but the present reexamination made evident that an important amount of skeletal features are shared by both. Some of these morphological features, such as the ornamentation on the point of the ectosomal subtylostyles, are reported for the first time. The study also revealed that a tuberose nature of the tyles of the main choanosomal megascleres could be a common ancestral condition in both genera. The morphology of the multi-toothed anchorate chelae showed a gradual transition across the species, suggesting that the morphological diversity in chelae was generated in these genera through a “palmate-anchorate-arcuate” evolutionary sequence. However, the forward or backward direction of this sequence remained unclear from the available evidence. Important levels of skeletal variability were found to affect many of the skeletal characters, especially in the genusCrambe. In some cases, this variability transgressed the limits theoretically defining a species, making evident that the traditional procedure just based on comparison of the skeletons becomes unreliable when tackling the taxonomy of these genera. Most of the skeletal variability seemed to correspond to genetic polymorphisms, except in the case ofC. acuata. In this taxon, the skeletal variability could be a result of the existence of a cryptic species, originated by a misconceived synonymy betweenC. acuata andC. chelastra. Besides the skeletal variability, the obscure taxonomic meaning of many skeletal features favored the existence of conflicting taxonomic proposals for the suprageneric location of these genera, depending on the author’s criteria. This study made evident that any subsequent attempt of phylogenetic inference should be based on an unweighted analysis of the available skeletal information.     

Extracellular Formation of Body and Tunic Spicules in the New Zealand Solitary Ascidian Pyura pachydermatina (Urochordata, Ascidiacea)

The New Zealand ascidian Pyura pachydermatina has a 7–10 cm long body at the end of a stalk up to 1 m long and 1–2 cm in diameter. Two different spicule types are present: dumbbell-shaped spicules of calcite in the fibrous tunic that covers the body and stalk, and antler-shaped spicules of amorphous calcium carbonate in the soft body tissues. Both types form extracellularly within a closed compartment surrounded by an epithelium of sclerocytes. In adults the tunic spicules form in 2–3 weeks in the lumen of the tunic blood vessels, as determined by calcein uptake studies. They add mineral only while surrounded by the sclerocyte epithelium, which is anchored to the vessel wall. Ultimately the sclerocytes rupture at one or more leading points on the spicule. The blood vessel epithelium also becomes very thin at these points and either ruptures or the cells separate. allowing the spicules to migrate out into the tunic. The sclerocytes degenerate and the blood vessel closes behind the migrating spicule, thus maintaining the vessel's integrity. Tunic spicules accumulate in the subcuticular region of the stalk, but the outermost layer of tunic covering the body is periodically sloughed off along with some spicules. This gives the "neck" between body and stalk a flexibility that allows it to orient to currents, and prevents an accumulation of epizoic organisms on the body. The antler spicules form within blood sinuses of the body tissues. The mineral and organic material are arranged in concentric layers. In the branchial sac, oral tentacles, gut and endostyle, where antler spicules occur most densely, the branches interlock, providing support to the soft tissues. They are of many sizes and apparently remain where they form, increasing in number and size throughout the animal's lifespan.     

Plasticity and constraints in development and evolution

Morphological similarities between organisms may be due to either homology or homoplasy. Homologous structures arise by common descent from an ancestral form, whereas homoplasious structures are independently derived in the respective lineages. The finding that similar ontogenetic mechanisms underlie the production of the similar structures in both lineages is not sufficient evidence of homology, as such similarities may also be due to parallel evolution. Parallelisms are a class of homoplasy in which the two lineages have come up with the same solution independently using the same ontogenetic mechanism. The other main class of homoplasy, convergence, is superficial similarity in morphological structures in which the underlying ontogenetic mechanisms are distinct. I argue that instances of convergence and parallelism are more common than is generally realized. Convergence suggests flexibility in underlying ontogenetic mechanisms and may be indicative of developmental processes subject to phenotypic plasticity. Parallelisms, on the other hand, may characterize developmental processes subject to constraints. Distinguishing between homology, parallelisms and convergence may clarify broader taxonomic patterns in morphological evolution.     

Ultrastructural Aspects of Spicule Formation in the Solitary Ascidian Herdmania momus (Urochordata,Ascidiacea)

The solitary stolidobranch ascidian Herdmania momus contains numerous calcium carbonate spicules in its tunic and body tissues. The slender body spicules form inside complex sheaths in the body wall and branchial basket, where they remain for the life of the animal. The much smaller tunic spicules form inside the tunic blood vessels and then migrate to the tunic surface, where they become anchored by their spiny base. This paper is an ultrastructural investigation of the formation of the body spicules; the tunic spicules, which apparently form quite differently, will be the focus of a future study. The body spicules are composed of rows of closely packed acicular spines which form completely extracellularly. The spine tips are covered by flattened, highly pseudopodial sclerocytes bound together by tightly interdigitating cell processes. The basal regions of contiguous spines are covered by very thin sclerocyte cell processes. An organic matrix is present within the spines; its exact nature is not clear. A very dense extracellular inter-spine matrix is located between the spine tips and the contiguous basal regions. Presclerocytes within the sheaths between the spicules are probably responsible for formation of the extracellular structures of the sheaths. The presclerocytes appear to aggregate and transform into sclerocytes at the apical end of the spicule. New spines are added at the apical end of the spicule as well as between larger spines. Comparisons are made between body spicule formation in H. momus and skeletogenesis in echinoids.     

Cellular control over spicule formation in sea urchin embryos: A structural approach

The spicules of the sea urchin embryo form in intracellular membrane-delineated compartments. Each spicule is composed of a single crystal of calcite and amorphous calcium carbonate. The latter transforms with time into calcite by overgrowth of the preexisting crystal. Relationships between the membrane surrounding the spiculogenic compartment and the spicule mineral phase were studied in the transmission electron microscope (TEM) using freeze-fracture. In all the replicas observed the spicules were tightly surrounded by the membrane. Furthermore, a variety of structures that are related to the material exchange process across the membrane were observed. The spiculogenic cells were separated from other cell types of the embryo, frozen, and freeze-dried on the TEM grids. The contents of electron-dense granules in the spiculogenic cells were shown by electron diffraction to be composed of amorphous calcium carbonate. These observations are consistent with the notion that the amorphous calcium carbonate-containing granules contain the precursor mineral phase for spicule formation and that the membrane surrounding the forming spicule is involved both in transport of material and in controlling spicule mineralization.     

Intra-epithelial spicules in a homosclerophorid sponge

Attempts to understand the intricacies of biosilicification in sponges are hampered by difficulties in isolating and culturing their sclerocytes, which are specialized cells that wander at low density within the sponge body, and which are considered as being solely responsible for the secretion of siliceous skeletal structures (spicules). By investigating the homosclerophorid Corticium candelabrum, traditionally included in the class Demospongiae, we show that two abundant cell types of the epithelia (pinacocytes), in addition to sclerocytes, contain spicules intracellularly. The small size of these intracellular spicules, together with the ultrastructure of their silica layers, indicates that their silicification is unfinished and supports the idea that they are produced "in situ" by the epithelial cells rather than being incorporated from the intercellular mesohyl. The origin of small spicules that also occur (though rarely) within the nucleus of sclerocytes and the cytoplasm of choanocytes is more uncertain. Not only the location, but also the structure of spicules are unconventional in this sponge. Cross-sectioned spicules show a subcircular axial filament externally enveloped by a silica layer, followed by two concentric extra-axial organic layers, each being in turn surrounded by a silica ring. We interpret this structural pattern as the result of a distinctive three-step process, consisting of an initial (axial) silicification wave around the axial filament and two subsequent (extra-axial) silicification waves. These findings indicate that the cellular mechanisms of spicule production vary across sponges and reveal the need for a careful re-examination of the hitherto monophyletic state attributed to biosilicification within the phylum Porifera.     

Phylogenetic comparison of spicule networks in cryptobranchiate dorid nudibranchs (Gastropoda, Euthyneura, Nudibranchia, Doridina)

Many dorid nudibranchs possess large numbers of calcareous spicules in their mantle, gill, rhinophores and foot. However, the arrangements of these structures and their differences among taxa are poorly known. Spicule networks were stained with Alizarin red and compared among 12 species of cryptobranchiate dorid nudibranchs and four outgroups. Three general types of networks were found: a cobweb-like, unbraced framework of one or few spicules per side; a ramifying system of thick, spiculated tracts; and a lattice-like arrangement of distinct radial and circumferential tracts. The Discodorididae species investigated shared a cobweb-like network and papillae supported by a ring of spicules, while the Porostomata showed consistent characters leading to a lattice-like network with larger spicules in the central notum. The Dorididae studied were not cohesive, but each species shared characters with the aforementioned groups. Therefore, spicule network form may provide new characters to help resolve the phylogeny of Doridina.     

Analysis of the axial filament in spicules of the demosponge Geodia cydonium: different silicatein composition in microscleres (asters) and megascleres (oxeas and triaenes)

The skeleton of the siliceous sponges (Porifera: Hexactinellida and Demospongiae) is supported by spicules composed of bio-silica. In the axial canals of megascleres, harboring the axial filaments, three isoforms of the enzyme silicatein (-alpha, -beta and -gamma) have been identified until now, using the demosponges Tethya aurantium and Suberites domuncula. Here we describe the composition of the proteinaceous components of the axial filament from small spicules, the microscleres, in the demosponge Geodia cydonium that possesses megascleres and microscleres. The morphology of the different spicule types is described. Also in G. cydonium the synthesis of the spicules starts intracellularly and they are subsequently extruded to the extracellular space. In contrast to the composition of the silicateins in the megascleres (isoforms: -alpha, -beta and -gamma), the axial filaments of the microscleres contain only one form of silicatein, termed silicatein-alpha/beta, with a size of 25kDa. Silicatein-alpha/beta undergoes three phosphorylation steps. The gene encoding silicatein-alpha/beta was identified and found to comprise the same characteristic sites, described previously for silicateins-alpha or -beta. It is hypothesized, that the different composition of the axial filaments, with respect to silicateins, contributes to the morphology of the different types of spicules.     

An aplacophoran postlarva with iterated dorsal groups of spicules and skeletal similarities to Paleozoic fossils

Abstract. A tiny neomenioid postlarva (Neomeniomorpha, or Solenogastres) collected from the water column 3 to 6 m above the east Pacific seamount Fieberling Guyot has 6 iterated, transverse groups of spicules and 7 regions devoid of spicules between the transverse groups and the anterior-and posteriormost spicules. Three pairs of ventral, longitudinal zones with columns of single spicules, each pair with its own distinctive spicule morphology, lack transverse iteration. The 7 regions bare of spicules are compared to shell fields in developing polyplacophorans, and spicule arrangement is compared to sclerite arrangement on the Cambrian fossils Wiwaxia corrugata and Halkieria evangelista and to the spines and shell plates of the Silurian Acaenoplax hayae. The term iteration is used to denote processes that result in both metameric segments and repeated ectodermal skeletal structures. Iterative morphogenesis was probably present in bilateral animals before the Cambrian. Comparisons of iterated ectodermal skeletal structures among fossil and extant forms are suggested to indicate evolutionary relationship.     

Scleroblast cultures from the gorgonianLeptogorgia virgulata (Lamarck) (Coelenterata: Gorgonacea)

Summary Scleroblasts were separated from fragmented tissue of growing tips ofLeptogorgia virgulata and cultured using a modification of the technique of Rannou. Replacement of fetal bovine serum with horse serum seemed to increase scleroblast viability. Cell adhesion occurred from 14 to 43 d. Cultured scleroblasts demonstrated cell aggregation, spicule formation, and extrusion of spicules into the external medium. Cells showing spicules in the process of being extruded appeared on the average after 24 d of culture. Variability among cultures was marked with respect to both division and spicule formation. Healthy cultures were maintained for more than 4 mo. This work was supported by National Science Foundation grants PCM8201389 and DCB8502698. This is contribution No. 674 of Belle W. Baruch Institute for Marine Biology and Coastal Research, University of South Carolina.     

Evidence for spicule homology in calcareous and siliceous sponges: biminerallic spicules in Lenica sp. from the Early Cambrian of South China

Botting, J.P., Muir, L.A., Xiao, S., Li, X. & Lin, J.‐P. 2012: Evidence for spicule homology in calcareous and siliceous sponges: biminerallic spicules in Lenica sp. from the Early Cambrian of South China. Lethaia, Vol. 45, pp. 463–475. The relationships of the extant sponge classes, and the nature of the last common ancestor of all sponges, are currently unclear. Early sponges preserved in the fossil record differ greatly from extant taxa, and therefore information from the fossil record is critical for testing hypotheses of sponge phylogenetic relationships that are based on modern taxa. New specimens of the enigmatic sponge Lenica sp., from the Early Cambrian Hetang Biota of South China, exhibit an unusual spicule structure. Each spicule consists of a siliceous core with an axial canal, an organic outer layer and a middle layer interpreted to have been originally calcium carbonate. This finding confirms previous work suggesting the existence of biminerallic spicules in early sponges. Combined with data from other early sponges, the new findings imply that the two fundamental spicule structures of modern sponges were derived from a compound, biminerallic precursor. Spicules are therefore homologous structures in Calcarea and Silicea, and if sponges are paraphyletic with respect to Eumetazoa, then spicules may also have been a primitive feature of Metazoa. □Calcarea, Early Cambrian, Hetang Biota, phylogeny, Silicea, taphonomy.     

Ontogenetic systematics: The synthesis of taxonomy, phylogenetics, and evolutionary developmental biology

The main purpose of the present review is to draw attention to growing problems in the modern systematics and phylogenetics which are presently underestimated by the professional community. The dramatic reduction of the importance of ontogeny and morphology in phylogenetic studies of the second part of the 20th century is considered among the major factors of the modern taxonomic and evolutionary paradigm. The deep contradiction of modern approaches, which either merely consider systematics and phylogeny as genealogy or even in a neotypolgical manner irrespective of the evolutionary idea, is demonstrated. Thus, despite the widespread opinion that the evolutionary theory is the major basis for taxonomy, the processes, which in fact caused the origin and formation of the systematic hierarchy are often considered as redundant for the procedure of classification. In this respect, the classical, but well forgotten statement that evolution is a modification of ontogeny is specially highlighted. Tight relationships between evolution, ontogeny, systematics, and phylogenetics are prima facie obvious, but also presently underestimated, although the field of the evo-devo is continuously growing. Paradoxically, even despite the outburst of various molecular ontogenetic approaches, the commonly accepted evolutionary paradigm still lacks a general theory for changes in the shape of organisms. As a step towards the development of such a theory, a synthesis (or more exactly, resynthesis) of still largely independently developing major biological fields, i.e., ontogenetic and evolutionary studies, on the one hand, and traditional taxonomy, on the other hand, a new concept of ontogenetic systematics is proposed. The new concept is intended for integration of supposedly ??immobile?? traditional taxonomy with the dynamics, but predominantly considered as hypothetical, evolutionary field based on the process of ontogeny, which, in contrast to the evolution itself, can be observed in the real time. Therefore, it is concluded that, for instance, the evolution of the main group of living organisms Metazoa, is primarily the evolution of a very limited number of ontogenetic cycles that were formed as early as the Early Cambrian. A significant underestimation of cyclic properties of ontogeny in the evolution and systematics is shown. Using two model groups, echinoderms of the class Ophiuroidea and dorid nudibranch mollusks (Gastropoda: Doridacea), practical importance of the integrative approach developed here is demonstrated. The ??disruption?? of the ancestral ontogenetic cycle and further formation of a new descendant cycle (which implies some continuity of ancestral and descendant characters) is considered to be a major evolutionary pattern. The model proposed implies either progressive (addition of stages and characters) or regressive (reduction of already existing stages and structures) modification of ancestral taxon, the diagnosis of which corresponds to the model of its ontogenetic cycle. In the extreme cases of disruption of the ancestral ontogenetic cycle, adult characters of descendants are substituted by juvenile ancestral features, demonstrating paedomorphoses in the narrow sense. Within the framework of the approach proposed, the evolutionary and ontogenetic models of ancestral ontogenetic cycles of brittle stars and dorid nudibranchs are developed and discussed. Based on the original material of the extinct Paleozoic ophiuroid group Oegophiurida, the origin of key evolutionary novelties is discussed. A major conclusion of the present review is the high necessity of integration of new molecular data with already well-established taxonomic hierarchy and ontogenetic information as a basis for the development of the general theory of transformations of organisms, i.e., the theory of evolution in its true sense.     

Loss of phospholipid asymmetry in dilauroylphosphatidylcholine induced plasma membrane vesicles from human platelets

Incubation of human platelets with unilamellar vesicles composed of dilauroylphosphatidylcholine (DLPC) induces shedding of small vesicular structures from the platelet plasma membrane. No significant cell lysis is observed during the process of shedding. Isolated spicules contain the major membrane glycoproteins, Ib, IIb, and IIIa, which are used to define the sidedness of the spicule membrane. These glycoproteins are completely susceptible to chymotrypsin treatment, whereas cytoskeletal proteins are inaccessible towards this enzyme. This demonstrates that the spicule membranes have a right-side-out orientation in as far as membrane proteins are concerned. Isolated spicules were 30-fold more active than platelets in stimulating prothrombin conversion to thrombin by the prothrombinase complex (factors Xa, Va and Ca2+). The increased prothrombinase activity reflects an increased amount of phosphatidylserine in the outer leaflet of the spicule membrane. Protein analysis of platelet spicules and native platelets reveals a number of differences, the most conspicuous of which is the virtual absence of myosin in the spicule preparations. It is proposed that a lack of myosin produces a different cytoskeletal organization in the spicules. This enables phosphatidylserine to become exposed at the outer surface of the spicule membrane.     

The biology of the marine sponge Microciona prolifera (Ellis and Solander). III. Spicule secretion and the effect of temperature on spicule size

The secretion of siliceous spicules in the marine demosponge Microciona prolifera (Ellis and Solander) is by three different means. Styles are secreted by sclerocytes with archeocyte characteristics (nucleolate nucleus, phagosomes). chelas are formed by small sclerocytes with anucleolate nuclei, and toxas are apparently formed extracellularly within membranous material. Genetically and physiologically equivalent explants of this sponge were grown at 15, 20, and 25 C for four weeks. Analyses of spicule dimensions show little correlation of temperature with spicule length, except in the case of toxas. but a clear inverse relationship of spicule width with temperature. It is suggested that thicker spicules are formed at lower temperatures due to the more efficient entrapment of silicon rather than to effects upon silicon transport. Chela dimensions are very uniform implying an all or none process in their secretion. Differences in spicule dimensions between individual sponges grown at these temperatures may be due to the highly complex pathways of silicon transport and/or to genetic differences.