Effects of Germanium (Ge) on the silica spicules of the marine sponge Suberites domuncula: Transformation of spicule type

Germanium (Ge), in the form of germanic acid, at a Ge/Si molar ratio of 1.0 inhibits gemmule development and silica deposition in the marine demosponge Suberites domuncula. Lower Ge/Si ratios inhibit the growth in length of the silica spicules (tylostyles) producing short structures, but with relatively normal morphology and close to normal width; spherical protuberances occasionally occur on these spicules. A few of the short spicules possess completely round rather than pointed tips. Many of the latter develop when Ge is added (pulsed) to growing animals, thus inducing a change in spicule type. These results indicate that the growth in length of the axial filament is more sensitive to Ge inhibition than is silica deposition and that pointed spicule tips normally develop because the growth of the axial filament at the spicule tip is more rapid than silica deposition. Newly formed spicules initiate silica deposition at the spicule head but the absence of Ge-induced bulbs as in freshwater spicules (oxeas) leaves open the question of whether there is a silicification center(s) present in Suberites tylostyles. The morphogenesis of freshwater oxeas and of marine tyolstyles appears fundamentally different-bidirectional growth in the former and unidirectional growth in the latter. X-ray analysis demonstrate relatively uniform Ge incorporation into the silica spicules with considerable variation from spicule to spicule in the incorporated level. Increased silicic acid concentration induces the formation of siliceous spheres, suggesting that the axial filament becomes prematurely encased in silica.     

Interaction of germanium (Ge) with biosilicification in the freshwater sponge Ephydatia mülleri: evidence of localized membrane domains in the silicalemma

In the presence of germanium (Ge) the needle-shaped silica spicules of the freshwater sponge Ephydatia m ulleri are very short and thin and possess bulbs with large spines. SEM-coupled X-ray analyses confirm the incorporation of Ge into the silica. A small number of bulbs are susceptible to erosion by HNO3 and hypochlorite and although the chemical basis of such erosion is presently unknown it suggests the presence of an organic matrix within the bulbs and/or an incomplete polymerization of the silica. Addition of Ge to control media in which silicification is newly initiated increases the incidence of erosion and results in centrally located eroded areas of the silica and discontinuities in its deposition. Removal of Ge from such newly forming structures results in a partial recovery of normal morphology (spine development and thickening of the silica) but only in the central region surrounding the bulbs. Both results establish the presence of a central, active region for silicification and further support the view that there is a distal spreading, away from this center, of transported forms of silica. Secondary centers may also be present. The newly assembled organic core of control structures is associated with tubular elements possibly derived from the surrounding membrane. In such newly silicifying structures the spicule tips contain oriented material in the form of "rays." Both of these new observations increase the likelihood of the presence of an organic matrix within the silica.     

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.     

Does germanium interact with radular morphogenesis and biomineralization in the limpet Lottia gigantea?

Specimens of Lottia gigantea were incubated in germanium enriched seawater [( Ge]/[Si] = 0.2-783) for 1-8 days. The siliceous radulae were examined histologically. No visible changes, degenerations or deformations were found in all 62 experimental radulae, although germanium is known to be a competitive inhibitor of silicon. In high concentrations, germanium was toxic to the limpets and killed them. Germanium was incorporated into the radular teeth in a distribution similar to silicon. Two suggestions are discussed for the apparent noninhibitory result.     

Comparison of spiculogenesis in in vitro ADCP-primmorph and explants culture of marine sponge Hymeniacidon perleve with 3-TMOSPU supplementation

This study aims to test the feasibility of introducing functional chemical groups into biogenic silica spicules by examining the effect of supplementing a silican coupler [3-(trimethoxysilyl)propyl]urea (3-TMOSPU) as silica source in the cultures of archaeocytes-dominant-cell-population (ADCP) primmorphs and explants of the marine sponge Hymeniacidon perleve. Analysis by Fourier Transform Infrared Spectroscopy (FT-IR) confirmed that the organic group in 3-TMOSPU was introduced into silica spicules. By comparing ADCP-primmorph cultures when supplemented with Na2SiO3, 3-TMOSPU supplementation showed no notable effect on the primmorphs development and cell locomotion behaviors. A decline in silicatein expression quantified by real-time RT-PCR was, however, observed during spiculogenesis. The decline was slower for the 3-TMOSPU group whereas significantly fewer spicules were formed. When sponge papillae explants were cultured, 3-TMOSPU supplementation had no negative effect on sponge growth but inhibited the growth biofouling of the diatom Nitzschia closterium. By monitoring the detectable Si concentration, it seemed that 3-TMOSPU was converted by the sponge and its conversion was related to spiculogenesis. Analysis of spicule dimensional changes indicated that the inhibition of spiculogenesis by 3-TMOSPU supplementation was less in ADCP-primmorphs culture due to lower 3-TMOSPU/detectable Si ratio in the media.     

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.     

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.     

Aberration of morphogenesis of siliceous frustule elements of the diatom <Emphasis Type="Italic">Synedra acus</Emphasis> in the presence of germanic acid

Addition of germanic acid into the culture medium of the diatom Synedra acus subsp. radians (Kutz.) Skabitsch. had nearly no influence on the culture growth at the Ge/Si molar ratio 0.01, but stopped it at ratios 0.05 and higher. It was shown by mass-spectrometry that at the Ge/Si ratio 0.01 germanium was incorporated in both the cytoplasm and siliceous valves, whereas at Ge/Si 0.05 it was incorporated into the cytoplasm but almost failed to accumulate in the valves. At Ge/Si 0.1 germanium was accumulated in the cytoplasm, but its incorporation into the valves terminated. Studies on the cell morphology by light, epifluorescence, and transmission electron microscopy showed that high concentrations of germanic acid induced disorders in morphogenesis of the siliceous frustule and accumulation of large rhodamine-stainable electron-dense inclusions. Model chemical experiments with over-saturated solutions of silicic acid in the presence of polyallylamine revealed that addition of 5% germanic acid considerably accelerated coagulation of silica. Hence, the toxic effect of germanic acid on diatoms could be caused by changes in coagulation of silica.     

Dynamics of spicule production in the marine sponge <Emphasis Type="Italic">Hymeniacidon perlevis</Emphasis> during in vitro cell culture and seasonal development in the field

To characterize the formation of silica spicules, the dynamics of spiculogenesis of an intertidal marine sponge Hymeniacidon perlevis (Montagu 1818) (Porifera: Demospongiae) were investigated by measuring the gene expression of silicatein (the enzyme responsible for spicule silicification) and the dimensional changes of spicules during the developmental process of individual sponges and in cell cultures of primmorphs of archaeocyte-dominant cell populations. The different developmental stages of spicules were documented by time-lapse microscopy and observed by transmission electron microscopy during a 1-month culture period. During its annual life cycle, H. perlevis has four different developmental stages: dormancy, resuscitation, bloom, and decline. Field-grown individual sponge samples at different stages were collected over 7 months (March to September 2005). The dimensions of the silica spicules from these samples were microscopically measured and statistically analyzed. This analysis and the material properties of the spicules allowed them to be classified into four groups representing the different developmental stages of spiculogenesis. Silicatein expression in the bloom stage was more than 100 times higher than that in the other stages and was correlated with the spicule developmental stage. The trend of spicule formation in field-grown sponges was consistent with the trend in cell culture. A new parameter, the maturation degree (MD) of spicules (defined as the ratio of actual to theoretical silica deposition of mature spicules), was introduced to quantify spicule development. Silica spiculogenesis during H. perlevis development was delineated by comparing MD and silicatein expression.     

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.     

Magnetic resonance imaging of the siliceous skeleton of the demosponge Lubomirskia baicalensis

The skeletal elements (spicules) of the demosponge Lubomirskia baicalensis were analyzed; they are composed of amorphous, non-crystalline silica, and contain in a central axial canal the axial filament which consists of the enzyme silicatein. The axial filament, that orients the spicule in its longitudinal axis exists also in the center of the spines which decorate the spicule. During growth of the sponge, new serially arranged modules which are formed from longitudinally arranged spicule bundles are added at the tip of the branches. X-ray analysis revealed that these serial modules are separated from each other by septate zones (annuli). We describe that the longitudinal bundles of spicules of a new module originate from the apex of the earlier module from where they protrude. A cross section through the oscular/apical-basal axis shows that the bundle rays are organized in a concentric and radiate pattern. High resolution magnetic resonance microimaging studies showed that the silica spheres of the spicules in the cone region contain high amounts of 'mobile' water. We conclude that the radiate accretive growth pattern of sponges is initiated in the apical region (cones) by newly growing spicules which are characterized by high amounts of 'mobile' water; subsequently spicule bundles are formed laterally around the cones.     

Spicules of hexactinellid sponges (Hexactinellida: Porifera) as natural composite materials

This paper reviews studies on the hexactinellid glass sponges (Hexactinellida: Porifera) that have organic silica spicules. According to its physical properties (microdensity, Young’s modulus, and light transmission), the material of the spicules is similar to amorphous silica; however, sponge spicules are birefringent, which suggests that they have a highly ordered crystal-like nature. Mineralized remnants of siliceous spicules composed of chemically inert materials are preserved in sedimentary rocks and provide evidence of the ecological state of the ancient biosphere. Sponges occur in waters with low temperatures; therefore, they grow very slowly and live for hundreds of years. The organic silica spicules exhibit the capacity for triboluminescence. The generated light emission may be used by symbiotic bacteria on the spicule surface.     

Subcellular localization of silicon and germanium in grass root and leaf tissues by SIMS: evidence for differential and active transport

Silicon transport and incorporation into plant tissue is important to both plant physiological function and to the influence plants have on ecosystem silica cycling. However, the mechanisms controlling this transport have only begun to be explored. In this study, we used secondary ion mass spectrometry (SIMS) to image concentrations of Si in root and shoot tissues of annual blue grass (Poa annua L.) and orchard grass (Dactylis glomerata L.) with the goal of identifying control points in the plant silica uptake pathway. In addition, we used SIMS to describe the distributions of germanium (Ge); the element used to trace Si in biogeochemical studies. Within root tissue, Si and Ge were localized in the suberized thick-walled region of endodermal cells, i.e. the proximal side of endodermal cells which is in close association to the casparian strip. In leaves, Si was present in the cell walls, but Ge was barely detectable. The selective localization of Si and Ge in the proximal side of endodermal cell walls of roots suggests transport control is exerted upon Si and Ge by the plant. The absence of Si in most root cell walls and its presence in the cell walls of leaves (in areas outside of the transpiration terminus) suggests modifications in the chemical form of Si to a form that favors Si complexation in the cell walls of leaf tissue. The low abundance of Ge in leaf tissue is consistent with previous studies that suggest preferential transport of Si relative to Ge.     

Nanostructural features of demosponge biosilica

Recent interest in the optical and mechanical properties of silica structures made by living sponges, and the possibility of harnessing these mechanisms for the synthesis of advanced materials and devices, motivate our investigation of the nanoscale structure of these remarkable biomaterials. Scanning electron and atomic force microscopic (SEM and AFM) analyses of the annular substructure of demosponge biosilica spicules reveals that the deposited material is nanoparticulate, with a mean particle diameter of 74+/-13 nm. The nanoparticles are deposited in alternating layers with characteristic etchant reactivities. Further analyses of longitudinally fractured spicules indicate that each deposited layer is approximately monoparticulate in thickness and exhibits extensive long range ordering, revealing an unanticipated level of nanoscale structural complexity. NMR data obtained from differentially heated spicule samples suggest that the etch sensitivity exhibited by these annular domains may be related to variation in the degree of silica condensation, rather than variability in the inclusion of organics. In addition, AFM phase imaging in conjunction with results obtained from HF and alkaline etching experiments suggest that at various stages in spicule biosynthesis, regions of unusually low silica condensation are deposited, indicating a possible interruption in normal spicule formation. While this discovery of nanoparticulate silica aggregation in demosponge skeletal elements is likely to reflect the intrinsic kinetic tendency of silica to form such particles during polycondensation, the heirarchical organization of these nanoparticles is biologically unique.     

Spicule records of <Emphasis Type="Italic">Ephydatia fluviatilis</Emphasis> as a proxy for hydrological and environmental changes in the shallow Lake Trasimeno (Umbria,Italy)

This research shows the results of an analysis of siliceous spicules found in sediment cores collected in Lake Trasimeno (Umbria, Italy), a shallow lake that experienced an important water level lowering during the last century. A morphological analysis of sedimentary sponge records revealed that the spicules accumulated in the lake sediments over the last 150 years are attributable to Ephydatia fluviatilis, the only sponge species found in the lake in recent years. The stratigraphic analysis of the cores showed that the abundance and size of the sponge spicules (megascleres) have remarkably decreased, suggesting that a significant depletion of the sponge fauna occurred, particularly during the first half of the twentieth century. A correlation analysis has identified morpho-hydrological and related variables (the theoretical fraction of lake surface subjected to resuspension and the amount of total suspended solids) as the most significant factors explaining the change in density of sponge spicules. Two ecological explanations of the sponge decline are proposed, based on the sensitivity of the sponge both to the availability of suitable hard substrata for colonization, and to the amount of wind-resuspended solids. One-ended sigmoid response curves were obtained by regression and corresponding transfer functions were derived, which allow the mean water depth of the lake and total suspended solids to be inferred from spicule density records. The results support the use of sponge spicules as a paleohydrological and paleoecological proxy, application of which appears particularly promising for shallow-water systems.     

Axial growth of hexactinellid spicules: formation of cone-like structural units in the giant basal spicules of the hexactinellid Monorhaphis

The glass sponge Monorhaphis chuni (Porifera: Hexactinellida) forms the largest bio-silica structures on Earth; their giant basal spicules reach sizes of up to 3 m and diameters of 8.5 mm. Previously, it had been shown that the thickness growth proceeds by appositional layering of individual lamellae; however, the mechanism for the longitudinal growth remained unstudied. Now we show, that the surface of the spicules have towards the tip serrated relief structures that are consistent in size and form with the protrusions on the surface of the spicules. These protrusions fit into the collagen net that surrounds the spicules. The widths of the individual lamellae do not show a pronounced size tendency. The apical elongation of the spicule proceeds by piling up cone-like structural units formed from silica. As a support of the assumption that in the extracellular space silicatein(-like) molecules exist that associate with the external surface of the respective spicule immunogold electron microscopic analyses were performed. With the primmorph system from Suberites domuncula we show that silicatein(-like) molecules assemble as string- and net-like arrangements around the spicules. At their tips the silicatein(-like) molecules are initially stacked and at a later stay also organized into net-like structures. Silicatein(-like) molecules have been extracted from the giant basal spicule of Monorhaphis. Applying the SDS–PAGE technique it could be shown that silicatein molecules associate to dimers and trimers. Higher complexes (filaments) are formed from silicatein(-like) molecules, as can be visualized by electron microscopy (SEM). In the presence of ortho-silicate these filaments become covered with 30–60 nm long small rod-like/cuboid particles of silica. From these data we conclude that the apical elongation of the spicules of Monorhaphis proceeds by piling up cone-like silica structural units, whose synthesis is mediated by silicatein(-like) molecules.     

The ratio of germanium to silicon in plant phytoliths: quantification of biological discrimination under controlled experimental conditions

Slight differences in the chemical behavior of germanium (Ge) and silicon (Si) during soil weathering enable Ge/Si ratios to be used as a tracer of Si pathways. Mineral weathering and biogenic silicon cycling are the primary modifiers of Ge/Si ratios, but knowledge of the biogenic cycling component is based on relatively few studies. We conducted two sets of greenhouse experiments in order to better quantify the range and variability in Ge discrimination by plants. Graminoid species commonly found in North American grassland systems, Agropyron smithii, Schizachyrium scoparium, and Andropogon gerardii were grown under controlled hydroponic environmental conditions. Silicon leaf contents were positively correlated with solution Si and ambient temperature but not with nutrient solution pH, electrical conductivity, or species. The Ge/Si ratio incorporated into phytoliths shows a distribution coefficient [(Ge/Si)_phytolith/(Ge/Si)_solution] of about 0.2 and is remarkably invariant between species, photosynthetic pathway, and solution temperature. Ge seems to be discriminated against during the uptake and translocation of Si to the opal deposition sites by about a factor of five. In the second experiment, a wider range of graminoid species (Agropyron smithii, Bouteloua gracilis, Buchloe dactyloides, Oryzopsis hymenoides, Schizachyrium scoparium and Andropogon gerardii) were grown in two different soil mediums. Plant phytoliths showed a distribution factor of about 0.4 for field grown grasses, and 0.6 for potting soil grown grasses with no clear trends among the species. Evidence of the direction and degree of biological Ge discrimination during plant uptake provides a geochemical finger print for plants and improves the utility of Ge/Si ratios in studies of terrestrial weathering and links between Si cycles in terrestrial and marine systems.     

Differentiation of Sea Urchin Micromeres: Correlation between Specific Protein Synthesis and Spicule Formation

Sea urchin micromeres were isolated from the 16-cell stage embryos and cultured until they differentiated into spicule-forming cells. Electrophoretic analysis of proteins labeled with [³⁵S]-methionine showed that the differentiation accompanied the synthesis of five cell-specific proteins. These proteins appeared prior to spicule formation and were synthesized continuously or maintained stably while the cultured micromeres formed spicules. In contrast, these proteins were hardly detectable during development of the meso- and macromeres. Correlation between synthesis of the specific proteins and spicule formation was further examined in culture conditions which inhibit spicule formation. In Zn²⁺ -containing or serum-free medium, the micromere descendants failed to form spicules and exhibited markedly reduced synthesis of one of the specific proteins (32 K daltons). After removal of Zn²⁺, or addition of serum, however, spicules were formed with delay but concomitantly with an increase in the synthesis of this protein. This clear correlation suggests the participation of the 32 K protein in the process of spicule formation.     

Fine Structure of Silica Deposition and the Origin of Shell Components in a Testate Amoeba Netzelia tuberculata1

ABSTRACT Netzelia tuberculata secretes a test composed of siliceous particles cemented together by organic plaques forming a single-layered spheroidal shell. The siliceous particles are produced within cytoplasmic vacuoles by three mechanisms: 1) synthesis de novo by deposition of the silica on a matrix; 2) deposition of silica on particles remaining in digestive vacuoles, including starch grains and undigested walls of yeast cells; and 3) secretion of silica as a hollow sphere at the periphery of vacuoles enclosed by the silicasecreting membrane. The silicalemma (silica-secreting membrane) originates as fibril-containing vesicles (GFV) secreted by the Golgi body. Fusion of these vesicles with membranes surrounding digestive vacuoles or with membranes surrounding specialized vacuoles containing a silica-binding matrix apparently converts the vacuole into a silica-depositing organelle. Small spherules of silica occur on the vacuolar side of the membrane surrounding the developing test granules, marking the presence of silicalemma activity. These colloidal spherules become aggregated into larger spherules that condense to form the siliceous surface of the developing test particle. Other Golgi vesicles, designated Golgi plaque vesicles (GPV), produce the organic plaques that are deposited among the siliceous particles at the periphery of the cell during new test construction during cell division. The fine structure of the GFV and GPV and their role in test wall deposition are discussed in relation to other silica-biomineralizing protozoa, including radiolaria.     

Spicule Formation-Inducing Substance in Sea Urchin Embryo

Isolated micromeres of sea urchin produced spicules in sea water containing blastocoelic fluid (BCF) taken from embryos, or in a medium in which embryos had previously been dissociated (dissociated solution, DS). When isolated micromeres were cultured in vitro , their descendants initiated spicule formation only when BCF was added to the culture medium by the time when, in normal development, primary mesenchyme cells form two aggregates in the vegetal region. After the initiation of spicule formation, growth of spicules occurred under the continuous influence of DS. Spicule formation-inducing (SFI) activity in DS was first detected at the mesenchme blastula stage. The activity in BCF was heat-labile and was inactivated by trypsin.