²⁶Mg labeling of the sea urchin regenerating spine: Insights into echinoderm biomineralization process

This paper reports the results of the first dynamic labeling experiment with regenerating spines of sea urchins Paracentrotus lividus using the stable isotope ²⁶Mg and NanoSIMS high-resolution isotopic imaging, which provide a direct information about the growth process. Growing spines were labeled twice (for 72 and 24 h, respectively) by increasing the abundance of ²⁶Mg in seawater. The incorporation of ²⁶Mg into the growing spines was subsequently imaged with the NanoSIMS ion microprobe. Stereom trabeculae initially grow as conical micro-spines, which form within less than 1 day. These micro-spines fuse together by lateral outgrowths and form a thin, open meshwork (inner stereom), which is subsequently reinforced by addition of layered thickening deposits (outer stereom). The (longitudinal) growth rate of the inner stereom is ca. 125 μm/day. A single (ca. 1 μm) thickening layer in the stereom trabeculae is deposited during 24 h. The thickening process is contemporaneous with the formation micro-spines and involves both longitudinal trabeculae and transverse bridges to a similar degree. Furthermore, the skeleton-forming cells remain active in the previously formed open stereom for at least 10 days, and do not migrate upwards until the end of the thickening process. The experimental capability presented here provides a new way to obtain detailed information about the skeleton formation of a multitude of marine, calcite producing organisms.     

Spine skeleton morphogenesis during regeneration in clypeasteroid and camarodont sea urchins

The process of skeleton morphogenesis is described for broken and totally removed spines in clypeasteroid (hollow spine) and camarodont (solid spine) sea urchins. Spine regeneration after total spine removal is completed in 40–45 days in clypeasteroids and in 60–70 days in camarodont sea urchins. Along with common stages of formation of longitudinal ribs in both hollow and solid spines, fundamental differences were found between the initial stages of reparative growth of the spine shaft. The spine shaft is formed from a single median process in clypeasteroids and from many simultaneously growing processes in camarodont sea urchins. Reparative morphogenesis of totally removed and partly broken spines in clypeasteroid sea urchins and totally removed spines in camarodont sea urchins leads to the formation of a skeletal structure identical to the intact spine. However, during the regeneration of broken camarodont spines, lateral growth is markedly retarded. As a result, the regenerated part of the spine shaft has a smaller diameter when the initial spine length is achieved. A hypothesis is proposed on a paedomorphic origin of spines in the clypeasteroid sea urchins on the basis of the juvenile stage of definitive spines in the camarodont sea urchins.     

Ultrastructural studies of regenerating spines of the sea urchin Strongylocentrotus purpuratus I. Cell types without spherules

The fine structure of regenerating tips of spines of the sea urchin Strongylocentrotus purpuratus was investigated. Each conical tip consisted of an inner dermis, which deposits and contains the calcite skeleton, and an external layer of epidermis. Although cell types termed spherulecytes containing large, intracellular membrane bound spherules were also present in spine tissues, only epidermal and dermal cell types lacking such spherules are described in this paper. The epidermis was composed largely of free cells representing several functional types. Over the apical portion of the tip these cells occurred in groups, while proximally they were distributed within longitudinal grooves present along the periphery of the spine from the base to the tip. The terminal portions of apical processes extending from some of the epidermal cells formed a thin, contiguous outer layer consisting of small individual islands of cytoplasm bearing microvilli. Adjacent islands were connected around the periphery by a junctional complex extending roughly 200 Å in depth in which the opposing plasma membranes were separated by a narrow gap about 145 Å in width bridged by amorphous material. Other epidermal cells were closely associated with the basal lamina, which was 900 Å in thickness and delineated the dermoepidermal junction; some of these cells appeared to synthesize the lamina, while others may be sensory nerve cells. The dermis at the spine tip also consisted of several functional types of free cells; the most interesting of these was the calcoblast, which deposits the skeleton. Calcoblasts extended a thin, cytoplasmic skeletal sheath which surrounded the tips and adjacent proximal portions of each of the longitudinally oriented microspines comprising the regenerating skeleton, and distally, formed a conical extracellular channel ahead of the mineralizing tip. The intimate relationship between calcoblasts and the growing mineral surface strongly suggests that these cells directly control both the kinetics of mineral deposition and morphogenesis of the skeleton. Other cell types in the dermis were precalcoblasts and phagocytes. Precalcoblasts may function as fibroblasts and are possible precursors of calcoblasts. Closely associated with the basal lamina at the dermoepidermal junction were extracellular unbanded anchoring fibrils 150 Å to 200 Å in diameter. Scattered proximally among dermal cells were other extracellular fibrils, presumably collagenous, about 300 Å in diameter with a banding periodicity of 210 Å.     

Structure and function of clypeasteroid miliary spines (Echinodermata,Echinoides)

Summary Histological and ultrastructural techniques have been used to describe the functional morphology of clypeasteroid miliary spines, with special reference to their supposed mucus-secreting role. Mucus cells were not found in the miliary spines of any members of the Arachnoididae, Fibulariidae, Laganidae, Echinarachniidae, Dendrasteridae, Astriclypeidae, or Mellitidae examined in this study. Only members of the Clypeasteridae have mucus-secreting cells in these spines. Characteristics of the skeleton, ultrastructure of the nervous system, and histology of the musculature and epithelia of the base, shaft and tip are also discussed. Miliary spines have two bands of cilia running along the entire length of opposite sides of the shaft. The geometric packing of cilium-bearing cells in these bands is described for the first time, as is the remarkable form of the sacs found at the tips of dendrasterid, astriclypeid, and mellitid miliary spines. These sacs are definitely not mucous sacs, as previously described, but are balloons of single-celled epithelium internally tethered to the skeletal tip by copious quantities of collagenous connective tissue. Miliary spines prevent obstruction of aboral nutritive and ventilatory ciliary currents caused by substrate particles falling to the test surface during burrowing. They do this in two ways: (1) they help generate ciliary currents that sweep finer material off the test, and (2) they contribute to the formation of a spine canopy that mechanically blocks larger particles from falling between the spines. Members of the Clypeasteridae secrete an interspine mucous tent that traps potentially clogging material. The miliary spine sacs of sand dollars are deformable space-fillers that plug holes between primary spines in the aboral canopy, even as the spines rock on their tubercles to push sand backwards over the test. Allometry of spines from Echinarachnius parma suggests that aboral military spines and club-shaped spines exhibit co-ordinated growth that maintains the aboral canopy throughout post-metamorphic ontogeny, and that aboral spins have an overall lower growth rate than spines on the oral surface.     

Stereom morphogenesis and differentiation during regeneration of adambulacral spines of Asterias rubens (Echinodermata,Asteroida)

Summary The very first mineral deposits appearing in regenerating fractured adambulacral spines of Asterias rubens are minute polyhedrons that cover the surface of fractured trabeculae. Polyhedrons fuse together forming a fold from which a microspine differentiates. Microspines develop into long linear trabeculae which send out lateral processes at regular length intervals. Lateral processes from adjacent trabeculae fuse together, bridging the trabeculae and giving the regenerate the typical meshwork structure of stereom. Most of the regenerate is built up according to this growth pattern which ensures its longitudinal growth. Simultaneously, the initial fascicular stereom of the stub sends out short radial processes which branch into upward and downward directed subprocesses. The latter fuse with their equivalents located above or below, building up longitudinal rows of stereom meshes. These rows then bridge together by additional branched or unbranched lateral processes, so forming a new stereom layer which progressively covers the whole stub. Up to three new layers of stereom are formed in this way at the stub periphery. These become continuous with the stereom layers of the regenerate by fusion of reciprocal subprocesses, so ensuring the continuity between the stub and the regenerate. In both structures the first stage of mineralization results in an open stereom. Stereom thickening occurs in a second stage of mineralization (that is chronologically separated from the formation of the open stereom) and results in the differentiation of the original stereom fabrics (i.e. fascicular stereom). Regeneration of removed spines starts with the formation of a new spine base made of labyrinthic stereom. The development of the latter mostly relies on short branched and unbranched processes which fuse with each other or with predifferentiated meshes. After completion of its base, the regenerating spine lengthens and thickens similarly to the regenerating fractured spines. The diversity of the stereom growth processes observed in the present work may be reduced to the combination of one to three elementary events, viz. the development of long linear processes, of short unbranched processes and of short branched processes. A survey of the literature allows the suggestion that the implementation of these elementary events is sufficient to describe most types of stereom morphogenesis.Senior research assistant NFSR (Belgium)     

Partial regeneration of a genal spine by the trilobite Ceraurus plattinensis

A slender extension of a rounded stump on the proximal portion of the left genal spine of Ceraurus plattinensis Foerste, 1920 from the Middle Ordovician of Ontario, Canada records the partial regeneration of a genal spine. The regenerated spine possesses almost normal prosopon of fine granules and resembles the distal portion of the normal right genal spine. It demonstrates the following aspects about this trilobite's physiology: partial regeneration of genal spines could take place even if severed proximally. partial regeneration of genal spines could take place even in late holaspid individuals and the pattern of regeneration took place in a distoproximal order.     

REDUCTION OF THE PECTORAL SPINE AND GIRDLE IN DOMESTICATED CHANNEL CATFISH IS LIKELY CAUSED BY CHANGES IN SELECTION PRESSURE

Locked pectoral spines of the Channel Catfish Ictalurus punctatus more than double the fish's width and complicate ingestion by gape‐limited predators. The spine mates with the pectoral girdle, a robust structure that anchors the spine. This study demonstrates that both spine and girdle exhibit negative allometric growth and that pectoral spines and girdles are lighter in domesticated than in wild Channel Catfish. This finding could be explained by changes in selection pressure for spine growth during domestication or by an epigenetic effect in which exposure to predators in wild fish stimulates pectoral growth. We tested the epigenetic hypothesis by exposing domesticated Channel Catfish fingerlings to Largemouth Bass Micropterus salmoides predators for 13 weeks. Spines and girdles grow isometrically in the fingerlings, and regression analysis indicates no difference in proportional pectoral growth between control and predator‐exposed fish. Therefore a change in selection pressure likely accounts for smaller pectoral growth in domesticated Channel Catfish. Decreasing spine growth in older fish suggests anti‐predator functions are most important in smaller fish. Additionally, growth of the appendicular and axial skeleton is controlled differentially, and mechanical properties of the spine and not just its length are an important component of this defensive adaptation.     

Sea Urchin Spines as a Model-System for Permeable, Light-Weight Ceramics with Graceful Failure Behavior. Part I. Mechanical Behavior of Sea Urchin Spines under Compression

The spines of pencil and lance urchins Heterocentrotus mammillatus and Phyllacanthus imperialis were studied as a modelof light-weight material with high impact resistance.The complex and variable skeleton construction ("stereom") of body andspines of sea urchins consists of highly porous Mg-bearing calcium carbonate.This basically brittle material with pronouncedsingle-crystal cleavage does not fracture by spontaneous catastrophic device failure but by graceful failure over the range of tensof millimeter of bulk compression instead.This was observed in bulk compression tests and blunt indentation experiments onregular,infiltrated and latex coated sea urchin spine segments.Microstructural characterization was carried out using X-raycomputer tomography,optical and scanning electron microscopy.The behavior is interpreted to result from the hierarchicstructure of sea urchin spines from the rnacroscale down to the nanoscale.Guidelines derived from this study see ceramics withlayered porosity as a possible biomimetic construction for appropriate applications.     

Pectoral spine size in Synodontis schall (Teleostei: Mochokidae) from Asa Lake, Ilorin, Nigeria

The pectoral spines of Synodontis schall (n = 813) were examined for 24 months. Mean length for the right (3.2 cm) and left (3.1 cm) pectoral spines were not significantly different [P > 0.05]. However, the male and female pectoral spine lengths were significantly different (P < 0.05). A fractured pectoral spine in one of the specimens was shorter than the other. The fracture which could be deleterious to balancing, feeding and reproductive activities was attributed to an injury rather than to genetic or epigenetic defects.     

Vertebral end-plate fractures as a result of high rate pressure loading in the nucleus of the young adult porcine spine

In a healthy spine, end-plate fractures occur from excessive pressurization of the intervening nucleus. Younger spines are most susceptible to such type of injury due to the highly hydraulic nature of their intervertebral discs. The purpose of this paper was to confirm this fracture mechanism of the healthy spine through the pressurization of the nucleus in the absence of external compressive loading. Sixteen functional porcine spine units were dissected and both injection and pressure transducer needles were inserted into the nucleus of the intervertebral disc. Hydraulic fluid was rapidly injected into the nucleus until failure occurred. Peak pressure and rate of pressure development were monitored. Spine units were dissected to determine the type and location of fracture. Fifteen of the 16 spine units fractured (the remaining unit had a degenerated disc). Of the 15 fractures, 13 occurred at the posterior margin of the end-plate along the lines of the growth plates. A slightly exponential relationship was found between peak pressure and its rate of development (R(2) = 0.544). Also, in each of the growth-plate fractured specimens, nuclear material was forcefully emitted, during fracture, from the intervertebral disc into the vertebral foramen. The posterior end-plate fractures produced here are similar to those often seen in young adult humans. This provides insight into a mechanism of fracture development through pressurization of the nucleus that might be seen in older adolescents and younger adults during athletic events or mild trauma.     

Histochemical study of jaw muscle fibers in the American alligator (Alligator mississippiensis)

The ontogenetic development of caudal vertebrae and associated skeletal elements of salmonids provides information about sequence of ossification and origin of bones that can be considered as a model for other teleosts. The ossification of elements forming the caudal skeleton follows the same sequence, independent of size and age at first appearance. Dermal bones like principal caudal rays ossify earlier than chondral bones; among dermal bones, the middle principal caudal rays ossify before the ventral and dorsal ones. Among chondral bones, the ventral hypural 1 and parhypural ossify first, followed by hypural 2 and by the ventral spine of preural centrum 2. The ossification of the dorsal chondral elements starts later than that of ventral ones. Three elements participate in the formation of a caudal vertebra: paired basidorsal and basiventral arcocentra, chordacentrum, and autocentrum; appearance of cartilaginous arcocentra precedes that of the mineralized basiventral chordacentrum, and that of the perichordal ossification of the autocentrum. Each ural centrum is mainly formed by arcocentral and chordacentrum. The autocentrum is irregularly present or absent. Some ural centra are formed only by a chordacentrum. This pattern of vertebral formation characterizes basal teleosts and primitive extant teleosts such as elopomorphs, osteoglossomorphs, and salmonids. The diural caudal skeleton is redefined as having two independent ural chordacentra plus their arcocentra, or two ural chordacentra plus their autocentra and arococentra, or only two ural chordacentra. A polyural caudal skeleton is identified by more than two ural centra, variably formed as given for the diural condition. The two ural centra of primitive teleosts may result from early fusion of ural centra 1 and 2 and of ural centra 3 and 4, or 3, 4, and 5 (e.g., elopomorphs), respectively. The two centra may corespond to ural centrum 2 and 4 only (e.g., salmonids). Additionally, ural centra 1 and 3 may be lost during the evolution of teleosts. Additional ural centra form late in ontogeny in advanced salmonids, resulting in a secondary polyural caudal skeleton. The hypural, which is a haemal spine of a ural centrum, results by growth and ossification of a single basiventral ural arococentrum and its haemal spine. The proximal part of the hypural always includes part of the ventral ural arcocentrum. The uroneural is a modification of a ural neural arch, which is demonstrated by a cartilaginous precursor. The stegural of salmonids and esocids originates from only one paired cartilaginous dorsal arcocentrum that grows anteriorly by a perichondral basal ossification and an anterodorsal membranous ossification. The true epurals of teleosts are detached neural spines of preural and ural neural arches as shown by developmental series; they are homologous to the neural spines of anterior vertebrae. Free epurals without any indication of connection with the dorsal arococentra are considered herein as an advanced state of the epural. Caudal distal radials originate from the cartilaginous distal portion of neural and haemal spines of preural and ural (epurals and hypurals) vertebrae. Therefore, they result from distal growth of the cartilaginous spines and hypurals. Cartilaginous plates that support rays are the result of modifications of the plates of connective tissue at the posterior end of hypurals (e.g., between hypurals 2 and 3 in salmonids) and first preural haemal spines, or from the distal growth of cartilaginous spines (e.g., epural plates in Thymallus). Among salmonids, conditions of the caudal skeleton such as the progressive loss of cartilaginous portions of the arcocentra, the progressive fusion between the perichondral ossification of arcocentra and autocentra, the broadening of the neural spines, the enlargement and interdigitation of the stegural, and other features provide evidence that Prosopium and Thymallus are the most primitive, and that Oncorhynchus and Salmo are the most advanced salmonids respectively. This interpretation supports the current hypothesis of phylogenetic relationships of salmonids. © 1992 Wiley-Liss, Inc.     

Occipital spine of Orthacanthus (Xenacanthidae,Elasmobranchii): Structure and growth

The morphology of 16 occipital spines of the xenacanthid Orthacanthus from Upper Carboniferous deposits of Robinson (Kansas, USA), Nýřan (Czech Republic) and Puertollano (Spain) is described. The nonreplaced spines reveal the growth pattern of the shark. Moreover, the relationship between growth and paleoenvironmental conditions can be used to determine paleoecological conditions. Both external and internal morphology indicate that the spine was superficially inserted in the skin. During growth, the spine moved from a deep position in the dermis, in which trabecular dentine is formed, to a more superficial location in which centrifugally growing lamellar dentine was formed. Centripetally growing lamellar dentine was deposited more slowly than the centrifugally growing dentine; it obliterated the pulp cavity. The denticles are independent dermal elements formed by a dermal papilla and secondarily attached by dentine to the spine proper. The number of denticles per annual cycle and the density of denticulation vary with the growth rate. Moreover, the ratio of length of denticulated region to total length of the spine changes throughout ontogeny. In consequence, those features cannot be used for systematic purposes without a careful analysis of the variability. Centrifugally growing lamellar dentine in spines from Robinson shows a regular alternation of layers, suggesting tidal conditions in the environment in which the sharks lived. Monthly and seasonal cycles also occur. Tidal (lunar) cyclicity is also observed in the denticles: size and distance between denticles increase and decrease gradually, forming waves that are considered seasonal and yearly cycles. The observed regularity could be related to the variation in calcium phosphate deposition following the cyclical changes in water temperature produced in the tidal zone. Monthly and seasonal cycles are the result of the interaction of the solar and tidal (lunar) cycles. The cyclical pattern of growth is used to determine the age and growth rates. Orthacanthus was a fast‐growing shark like the Recent sharks Isurus, Mustelus, and Negaprion. J. Morphol. 242:1–45, 1999. © 1999 Wiley‐Liss, Inc.     

Mechanical defensive adaptations of three Mediterranean sea urchin species

In the Mediterranean, Paracentrotus lividus and Sphaerechinus granularis are important drivers of benthic ecosystems, often coexisting in sublittoral communities. However, the introduction of the invasive diadematoid Diadema setosum, which utilizes venomous spines, may affect these communities. To describe the mechanical properties of the test and spines of these three species, specimens were collected in winter of 2019 from the sublittoral zone of the Dodecanese island complex, southeastern Aegean Sea. This region serves as a gateway for invasive species to the Mediterranean Sea. Crushing test was conducted on live individuals, while 3‐point bending test was used to estimate spine stiffness. Porosity and mineralogy of the test and spine, thickness of the test, and breaking length of the spine were measured and compared, while the microstructural architecture was also determined. The test of S. granularis was the most robust (194.35 ± 59.59 N), while the spines of D. setosum (4.76 ± 2.13 GPa) exhibited highest flexibility. Increased porosity and thickness of the test were related to increased robustness, whereas increased flexibility of the spine was attributed to high porosity, indicating that porosity in the skeleton plays a key role in preventing fracture. The spines of S. granularis exhibited highest length after fracture % (71.54 ± 5.5%). D. setosum exhibited higher values of Mg concentration in the test (10%) compared with the spines (4%). For the first time, the mineralogy of an invasive species is compared with its native counterpart, while a comparison of the mechanical properties of different species of the same ecosystem also takes place. This study highlights different ways, in which sea urchins utilize their skeleton and showcases the ecological significance of these adaptations, one of which is the different ways of utilization of the skeleton for defensive purposes, while the other is the ability of D. setosum to decrease the Mg % of its skeleton degrading its mechanical properties, without compromising its defense, by depending on venomous bearing spines. This enables this species to occupy not only tropical habitats, where it is indigenous, but also temperate like the eastern Mediterranean, which it has recently invaded.     

Activity-dependent regulation of dendritic spine density on cortical pyramidal neurons in organotypic slice cultures

In order to examine the effects of activity on spine production and/or maintenance in the cerebral cortex, we have compared the number of dendritic spines on pyramidal neurons in slices of PO mouse somatosensory cortex maintained in organotypic slice cultures under conditions that altered basal levels of spontaneous electrical activity. Cultures chronically exposed to 100 μM picrotoxin (PTX) for 14 days exhibited significantly elevated levels of electrical activity when compared to neurons in control cultures. Pyramidal neurons raised in the presence of PTX showed significantly densities of dendritic spines on primary apical, secondary apical, and secondary basal dendrites when compared to control cultures. The PTX-induced increase in spine density was dose dependent and appeared to saturate at 100 μM. Cultures exhibiting little or no spontaneous activity, as a result of growth in a combination of PTX and tetrodotoxin (TTx), showed significantly fewer dendritic spines compared to cultures maintained in PTX alone. These results demonstrate that the density of spines on layers V and VI pyramidal neurons can be modulated by growth conditions that alter the levels of spontaneous electrical activity. 1994 John Wiley & Sons, Inc.     

Dynamic microtubules promote synaptic NMDA receptor-dependent spine enlargement

Most excitatory synaptic terminals in the brain impinge on dendritic spines. We and others have recently shown that dynamic microtubules (MTs) enter spines from the dendritic shaft. However, a direct role for MTs in long-lasting spine plasticity has yet to be demonstrated and it remains unclear whether MT-spine invasions are directly influenced by synaptic activity. Lasting changes in spine morphology and synaptic strength can be triggered by activation of synaptic NMDA receptors (NMDARs) and are associated with learning and memory processes. To determine whether MTs are involved in NMDAR-dependent spine plasticity, we imaged MT dynamics and spine morphology in live mouse hippocampal pyramidal neurons before and after acute activation of synaptic NMDARs. Synaptic NMDAR activation promoted MT-spine invasions and lasting increases in spine size, with invaded spines exhibiting significantly faster and more growth than non-invaded spines. Even individual MT invasions triggered rapid increases in spine size that persisted longer following NMDAR activation. Inhibition of either NMDARs or dynamic MTs blocked NMDAR-dependent spine growth. Together these results demonstrate for the first time that MT-spine invasions are positively regulated by signaling through synaptic NMDARs, and contribute to long-lasting structural changes in targeted spines.     

Evolution of venom delivery structures in madtom catfishes (Siluriformes: Ictaluridae)

The use of venom to subdue prey or deter predators has evolved multiple times in numerous animal lineages. Catfishes represent one of the most easily recognized, but least studied groups of venomous fishes. Venom glands surround spines on the dorsal and pectoral fins that serve as venom delivery structures. Species of madtom catfishes in the genus Noturus were found to each have one of four venom delivery morphologies: (1) smooth spine with no venom gland; (2) smooth spine with venom gland associated with shaft of spine; (3) serrated spine with venom gland associated with shaft of spine; and (4) serrated spine with venom gland associated with shaft of spine and posterior serrations. Analyses accounting for the phylogenetic history of Noturus species suggest that a serrated pectoral spine with a venom gland is the ancestral condition for the genus. The presence of serrations and a venom gland have been largely conserved among Noturus species, but sting morphology has changed at least five times within the genus. Four of these changes have resulted in a loss of morphological complexity, including the loss of posterior serrations, loss of venom glands associated with the posterior serrations, and one complete loss of the venom gland. © 2010 The Linnean Society of London, Biological Journal of the Linnean Society, 2011, 102 , 115–129.     

Periodic shedding and replacement of venomous caudal spines,with special reference to South American freshwater stingrays,Potamotrygon spp.

Synopsis The number of venomous caudal spines and their length and position relative to one another were determined in seven species of South American freshwater rays (Potamotrygonidae) and eight marine or euryhaline species of four families from the Caribbean Coast of South and Central America. Most species have two visible spines at certain stages in the shedding-replacement cycle and only one visible spine at other stages (following shedding). If we include the embryological beginnings of the spines before they erupt and become visible, the spine counts of most rays are actually 2 rather than 1 or 2. Since most species apparently follow this pattern, spine counts are of little use in distinguishing between species except in the relatively few that may have only one, or no spines. Eight captive Potamotrygon specimens maintained in simulated tropical temperature conditions over 12 months showed periodic shedding and replacement of spines. The molts were biannual for a given ray but annual for a given spine. They alternated between two spine loci and their cycles were approximately six months out of phase with each other. Recent studies on Dasyatis sabina by others report only one molt per year, with replacement spines forming always posterior to the primary spine rather than alternating between posterior and anterior. Supernumerary spines (counts of more than two, up to five) are also discussed, as are counts of one and zero.     

Skeleton resorption in echinoderms: Regression of pedicellarial stalks inSphaerechinus granularis (Echinoida)

Summary When a globiferous pedicellaria ofSphaerechinus granularis injects its venom, the head autotomizes whereas the stalk remains on the test and enters a regression process with concomitant resorption of its supporting ossicle (i.e. the rod). Scanning electron microscope investigations of the morphological changes undergone by the stereom of resorbing rods show that: (1) resorption proceeds both axially and laterally, and leads to a reduction of approximately 80% of the original length of the rod, (2) secondary growth of new stereom processes occurs concomitantly with resorption but never ensures even a partial regeneration of the rod, and (3) resorption and secondary growth stop before the rod is totally destroyed leaving a static stump that remains in place up to 190 days. Particular resorption figures result from either the axial or the lateral resorption of the rod shaft. These consist chiefly of terraced conical cupules, dense cylinders and concentric lamellae whose walls or edges are typically made of closely piled and/or aligned subprismatic crystallites. Whatever their location along the rod, these crystallites always organize strictly parallel to the rod axis. Whether the crystallites are mosaic blocks composing larger monocrystalline units or discrete monocrystals themselves is for the moment unclear. A growth model, which accounts for the observed resorption figures, is proposed for the shaft of pedicellarial rods. According to this model, the early growth of the shaft would produce elongated, interconnected trabeculae (initial trabeculae) made of densely piled and perfectly aligned crystallites. Thickening and coalescence of adjoining trabeculae would progressively occur by adjunction around the initial trabeculae of successive and concentric layers of similarly arranged crystallites. Coalescent trabeculae would then be cemented together in a perforate stereom layer by the final deposition of larger crystallite layers surrounding the whole shaft periphery. Growth of secondary stereom processes occurs both in the resorbing rod (here the newly formed processes are resorbed soon after they have been produced) and in rods where resorption has stopped. These are always irregular processes that localize near or on the actual sites of resorption. It is suggested these processes result from an uncontrolled activation of the skeleton-forming cells in areas where the concentration of calcium ions increases as a consequence of calcite resorption.     

Bomb dating and age validation using the spines of spiny dogfish (Squalus acanthias)

Bomb radiocarbon has previously been used to validate the age of large pelagic sharks based on incorporation into vertebrae. However, not all sharks produce interpretable vertebral growth bands. Here we report the first application of bomb radiocarbon as an age validation method based on date-specific incorporation into spine enamel. Our results indicate that the dorsal spines of spiny dogfish, Squalus acanthias, recorded and preserved a bomb radiocarbon pulse in growth bands formed during the 1960s with a timing which was very similar to that of marine carbonates. Using radiocarbon assays of spine growth bands known to have formed in the 1960s and 1970s as a dated marker, we confirm the validity of spine enamel growth band counts as accurate annual age indicators to an age of at least 45 year. Radiocarbon incorporation into northeast Atlantic dogfish spines occurred in similar years as those in the northwest Atlantic and northeast Pacific, although the amount of radiocarbon differed in keeping with the radiocarbon content of the different water masses. Published reports suggesting that Pacific dogfish are longer lived and slower growing than their Atlantic counterparts appear to be correct, and are not due to errors in interpreting the spine growth bands. Radiocarbon assays of fin spine enamel appears to be well suited to the age validation of sharks with fin spines which inhabit the upper 200 m of the ocean.     

Geometric shell growth and mode of life of a Devonian chonetoidean brachiopod

Morphological and statistical analysis of the chonetoid species Kentronetes variabilis from the Lower Devonian (Lochkovian) of the Argentine Precordillera demonstrate ontogenetic changes and allometric relationships between characters. A special study was made of spine distribution, morphology, and growth, compared to valve growth. The first, inner, developed spines (pairs 1–1'and 2–2') continued to grow after development of the following outer pairs. The spacing of spines, their diameter, and the density of growth rings vary from beak to posterolateral margins following a specific 2ⁿ geometric growth factor, compared to the regular, almost linear growth of the valves, attested by growth lines. The linear growth rate of outer spines (pairs 3–3'and 4–4') can be 6–8 times more rapid than that of the shell on the valve margin. Ontogenetic changes in spine morphology are interpreted as a response to changes in the mode of life.