Decay and mineralization of soft tissue in Early Devonian boring ctenostome bryozoans

The Early Devonian of Podolia, Ukraine, has yielded phosphatized colonies of the boring ctenostome bryozoan Podoliapora doroshivi with 3‐D preservation of soft tissues. However, the feeding zooids are not anatomically complete, their preserved soft tissues comprising decay‐resistant structures such as the protective cuticular polypide sacs with presumed parietal muscles inside the wall of the sacs, the setigerous collars, the membranous orificial walls and remains of the muscle tissues. Early diagenetic apatite mineralization occured in numerous feeding zooids of Podoliapora at different stages of decay and may be important for the interpretation of decay processes in these colonial soft‐bodied fossil organisms. A setigerous collar, which is a characteristic of extant ctenostomes, occurs in P. doroshivi in several stages of decay showing progressive collapse and eventual complete loss. This study indicates that the morphological changes of collars induced by decay often resulted in connection with the membranous orificial wall, producing false anatomical structures, unrelated to structures observed in the earlier stages of decay or to the anatomical structures of extant ctenostomes. The most decay‐resistant cuticular polypide sacs mineralized as cryptocrystalline apatite in early stage of decay became degraded in later stages of decay. These data provide evidence that the anatomical interpretation of soft‐bodied fossils preserved only in the later stages of decay may have led to imprecise morphological interpretations.     

Probable advanced hydroid from the Early Ordovician of China

A fossil of a colonial organism with pyritized soft tissues of elongated fusiform zooids, found in the middle part of the early Floian Fenxiang Formation in Hubei Province of China, probably represents the oldest reliable record of a hydroid cnidarian. The preservation of the fossil is sufficiently different from that of associated carbonized skeletons of graptolites to exclude affinities with this group. The fossil is unlikely to be a bryozoan because of the mode of budding from proximal, not distal, parts of parent zooids, which is typical rather of hydroids. Although no thecae are preserved, the fossil, named Sinobryon elongatum gen. et sp. nov., is suggested to be a thecate hydroid, possibly related to the Haleciidae. The apparent presence of an advanced member of the thecaphoran Macrocolonia clade in strata 470 Ma old means that much of the hydroid (and cnidarian) diversification preceded the Middle Ordovician.     

Hemichordate skeletal growth: shared patterns in Rhabdopleura and graptoloids

Rhabdopleura shows several features of skeleton growth that are also seen in graptoloids. The similarities between the growth patterns, in terms of the plan towards which the zooids aimed and of their response to environmental disturbance, are profound. Both demonstrate a high degree of genetic control, not only on the gross morphology of the tube or theca but also on the pattern of increments by which this must be achieved. The execution of this 'blueprint' is facilitated by spatial awareness in the zooids of both groups. The main variable left to the graptoloid zooid was the number of increments used in building a theca. Variations in the number of increments probably reflect differences in the productivity of the environment and hence the amount of spare energy in the colony budget. An important new observation is that mortality is common amongst zooids in both Rhabdopleura and graptoloids, with new animals taking over tube or thecal building from where the previous zooid left off. This is identifiable in the increment patterns of tubes and thecae. Several generations of zooids can inhabit a rhabdopleuran tube and can be demonstrated to have inhabited a graptolite theca. This means that innate senescence was not a major cause of death for graptolite colonies. It also means that all thecae might have been continuously occupied and that the colony could have survived significantly bleak environmental conditions by large-scale zooid mortality followed by regeneration. □ Graptolite, ecology, hemichordate, pterobranch, RHABDOPLEURA, growth.     

PHOSPHATIZED SOFT-TISSUE IN TRIASSIC BIVALVES

Abstract: Exceptionally preserved specimens of the genera Myophoria, Neoschizodus and Trigonodus (Bivalvia, Palaeoheterodonta, Trigonioida) from carbonate sediments of the Muschelkalk (Anisian, Ladinian) contain phosphatized soft‐tissues. This is the oldest record of soft‐tissue preservation in bivalves and the first from the German Muschelkalk. The phosphatized remains are here interpreted as relics of the originally chitinous gill supports, the gill axis, the labial palps (?), the adductor muscles, the pedal retractor muscles, the mantle margin including the radial mantle musculature, and the ‘siphons’. According to microprobe analysis, the mineral replacing the soft‐tissue is mainly apatite and, more rarely, francolite. Additionally, quartz filled voids within the gill supports, and in one sample it occurs in minute crystals in the phosphatized remains of the adductor muscle of Neoschizodus. Myophoria, Neoschizodus and Trigonodus were soft‐bottom dwellers and five of the specimens were discovered in life position. This is indicated by geopetal structures in three specimens.     

Senescence‐associated superoxide dismutase influences mitochondrial gene expression in budding tunicates

A recent study has shown that in the budding tunicate Polyandrocarpa misakiensis, the mitochondrial respiratory chain (MRC) dramatically attenuates the gene activity during senescence. In this study, we examined the possible involvement of superoxide dismutase (SOD) in the attenuation of gene expression of cytochrome c oxidase subunit 1 (COX1) in aged zooids. By RT‐PCR and in situ hybridization, Cu/Zn‐SOD (SOD1) was found to be expressed in most cells and tissues of buds and juvenile zooids but showed a conspicuous decline in senescent adult zooids, except in the gonad tissue in which the cytoplasm of juvenile oocytes was stained heavily. This expression pattern of SOD1 was similar to that of COX1. In contrast to SOD1, Mn‐SOD (SOD2) was expressed constitutively in both somatic and germline tissues of buds, juvenile zooids, and senescent adult zooids. Knockdown of SOD1 by RNAi diminished the gene activity of not only SOD1 but also of COX1. The resultant zooids had transient deficiencies in growth and budding, and they recovered from these deficiencies approximately 1 month later. Our results indicate that in P. misakiensis, SOD1 is a senescence‐associated nuclear gene and that the experimental decline in SOD1 gene expression accompanies the attenuation of MRC gene activity. Although it is uncertain how SOD1 is downregulated during tunicate senescence, the decreased SOD1 activity could be one of the main causes of MRC gene attenuation during normal senescence.     

Cephalodiscus reproductive biology (Pterobranchia,Hemichordata)

Sexually mature adults and embryos and larvae of Cephalodiscus nigrescens and C. gracilis were studied by light and electron microscopy. Contrary to claims in the literature, individual coenecial cavities are inhabited by colonies of up to 15 joined zooids and not by single individuals, which is important for the interpretation of the mode of life of the related fossil group the graptolites. Some aspects of the reproductive apparatus and reproduction in Cephalodiscus are reported. The ultrastructure of the spermatozoon is described for the first time. Coelom formation is by schizocoely. The structure of the larva at several developmental stages is illustrated. Not all fertilised eggs are destined to become motile larvae and some develop into zooids omitting the motile stage. The lumen of the oviduct is much larger than previously supposed. Spermatozoa are shed into the cavity of the coenecium. It is proposed that fertilisation takes place within the coenecium. The ultrastructure of the enigmatic black ‘Comma Body’ is described and a reproductive function is proposed. Budding takes place from a base common to several zooids. This base probably also serves as an attachment foot. Large masses of yolk have been discovered within the coelom of some zooids and muscle stalks. It is inconceivable that a colony of Cephalodiscus nigrescens could survive unless it spent most of its life outside the coenecium.     

Epistylis portoalegrensis n. sp. (Ciliophora,Peritrichia): A New Freshwater Ciliate Species from Southern Brazil

The peritrich ciliate Epistylis portoalegrensis n. sp. was found in two bodies of freshwater located in Porto Alegre, Southern Brazil. Morphological features were investigated using live and protargol‐stained specimens. The zooids presented a vase to cylindrical shape narrowed at the scopula, and a mean size of 131 × 37 μm in vivo. A C‐shaped macronucleus lay in the middle of the cell close to a single contractile vacuole. The oral infraciliature was typical for the genus, with all infundibular polykineties composed by three distinct rows of kinetosomes. Colonies are often nonbranched with no lateral stalk, carrying several zooids stemming from a single point. Specimens from the two sampling sites showed identical arrangement of the infraciliature, similar morphometry, identical 18S rDNA sequences, and a single nucleotide difference across the more variable ITS regions. Molecular phylogenetic analyses placed E. portoalegrensis in a well‐supported clade containing other Epistylis species, within the order Vorticellida.     

Systemic Invasion of Plum Seed and Fruit by Xanthomonas campestris pv. pruni through Stalks

Many fruits on Golden King plum trees inoculated through the stalks with Xanthomonas campestris pv. pruni developed unusual lesions extending from the exocarp to the endocarp. A few uninoculated, diseased fruits had similar lesions. The pathogen was isolated from both inoculated and uninoculated stalks and from seeds inside fruits. Scanning electron microscopy of inoculated stalks and mature fruits with unusual lesions revealed that vascular channels of the stalk, seed coat, stony endo, carp, and mesocarp were filled with masses of X. campestris pv. pruni. Bacterial colonies also occurred in other tissues of these fruit parts but were apparently absent from the starchy endosperm or surface of the diseased exocarp. This is the first full report of systemic movement of X. campestris pv. pruni to seed and fruit through stalks.     

Exceptionally preserved tadpoles from the Miocene of Libros,Spain: ecomorphological reconstruction and the impact of ontogeny upon taphonomy

McNamara, M.E., Orr, P.J., Kearns, S.L., Alcalá, L., Anadón, P. & Peñalver‐Mollá, E. 2010: Exceptionally preserved tadpoles from the Miocene of Libros, Spain: ecomorphological reconstruction and the impact of ontogeny upon taphonomy. Lethaia, Vol. 43, pp. 290–306. The Libros exceptional biota from the Upper Miocene of NE Spain includes abundant frog tadpoles (Rana pueyoi) preserved in finely laminated lacustrine mudstones. The tadpoles exhibit a depressed body, short tail, low tail fins, dorso‐laterally directed eyes and jaw sheaths; these features identify the Libros tadpoles as members of the benthic lentic ecomorphological guild. This, the first ecomorphological reconstruction of a fossil tadpole, supports phylogenetic evidence that this ecology is a conserved ranid feature. The soft‐tissue features of the Libros tadpoles are characterized by several modes of preservation. The space occupied previously by the brain is defined by calcium carbonate, the nerve cord is defined by calcium phosphate, and jaw sheaths and bone marrow are preserved as organic remains. Gut contents (and coprolites adjacent to specimens) comprise ingested fine‐grained sedimentary detritus and epiphyton. The body outline and the eyespots, nares, abdominal cavity, notochord, caudal myotomes and fins are defined by a carbonaceous bacterial biofilm. A similar biofilm in adult specimens of R. pueyoi from Libros defines only the body outline, not any internal anatomical features. In the adult frogs, but not in the tadpoles, calcium phosphate and calcium sulphate precipitated in association with integumentary tissues. These differences in the mode of preservation between the adult frogs and tadpoles reflect ontogenetic factors. □Anuran, ecology, soft‐tissue, tadpoles, taphonomy.     

The ciliate epibiont Epistylis pygmaeum: selection for zooplankton hosts, reproduction and effect on two rotifers

1. A clonal culture of the peritrich Epistylis pygmaeum was used for all observations and experiments. Motile cells preferentially attached to the eggs of three species of Brachionus but also attached to the body of adult B. angularis. Zooids on the transitory egg substratum developed only short stalks, while those on the body often developed long stalks and branched colonies. Selection for the eggs positions the ciliate near the cloaca, and thus high concentrations of fine particulate material excreted by the host. Settlement on eggs occurred equally well in the light and dark, and on moving and stationary eggs. 2. Motile Epistylis cells attached to a wide variety of rotifer and crustacean zooplankton, but exhibited some pronounced selectivity. They readily settled on the eggs of other rotifers (Epiphanes, Polyarthra), on the carapace of several cladocerans (Ceriodaphnia, Daphnia, Diaphanosoma), and on the egg sacs of a copepod (Tropocyclops). They settled less readily on the bodies of the rotifers Asplanchna and Synchaeta, and rarely or never settled on the rotifer Keratella, the cladocerans Bosmina and Scapholeberis, and the body of the copepod. 3. Epistylis populations initiated with a single zooid on Brachionus increased exponentially and often contained several hundred attached zooids and motile cells after 3 days at 20 °C. Observations of a culture initiated from a single telotroch provided new information about peritrich life cycles: (1) motile cells reproduced themselves at a rapid rate (λ = 4.26 day^?1); (2) telotrochs produced or transformed into swimming zooids and vice versa. Functions of the two types of motile cells remain to be clarified. Telotrochs likely are specialised for finding and attaching to hosts. Swimming zooids can feed and reproduce, producing both their own cell type and telotrochs. Together, they should enhance dispersal and population growth, especially when hosts are rare. 4. Life‐table experiments with two species of Brachionus showed that colonisation by Epistylis had no effect on adult survival but significantly decreased fecundity, by 29% in both cases. Zooids attached to eggs could be a weight burden, increase drag, and possibly inhibit egg development. Those on the body of B. angularis also could interfere with coronal cilia, inhibiting feeding and further slowing locomotion. The ability of E. pygmaeum to select and then interfere with its hosts indicates that this epibiont has the potential to influence the species structure of zooplankton communities.     

Mineralization of Alvinella polychaete tubes at hydrothermal vents

Alvinellid polychaete worms form multilayered organic tubes in the hottest and most rapidly growing areas of deep‐sea hydrothermal vent chimneys. Over short periods of time, these tubes can become entirely mineralized within this environment. Documenting the nature of this process in terms of the stages of mineralization, as well as the mineral textures and end products that result, is essential for our understanding of the fossilization of polychaetes at hydrothermal vents. Here, we report in detail the full mineralization of Alvinella spp. tubes collected from the East Pacific Rise, determined through the use of a wide range of imaging and analytical techniques. We propose a new model for tube mineralization, whereby mineralization begins as templating of tube layer and sublayer surfaces and results in fully mineralized tubes comprised of multiple concentric, colloform, pyrite bands. Silica appeared to preserve organic tube layers in some samples. Fine‐scale features such as protein fibres, extracellular polymeric substances and two types of filamentous microbial colonies were also found to be well preserved within a subset of the tubes. The fully mineralized Alvinella spp. tubes do not closely resemble known ancient hydrothermal vent tube fossils, corroborating molecular evidence suggesting that the alvinellids are a relatively recent polychaete lineage. We also compare pyrite and silica preservation of organic tissues within hydrothermal vents to soft tissue preservation in sediments and hot springs.     

PREPARATION AND CHARACTERIZATION OF PROTOPLASTS OBTAINED FROM THE PRASINOPHYTE SCHERFFELIA DUBIA (CHLOROPHYTA)1

The prasinophyte genera Scherffelia and Tetraselmis are the only genera that form a cell wall by an extracellular fusion of scales called a theca. We established a protocol for the production of protoplasts from Scherffelia dubia Pascher emend. Melkonian et Preisig using 3 mM Ellman's reagent (5,5′‐dithio‐bis‐2‐nitrobenozoic acid [DTNB]). Protoplasts analyzed by EM lacked flagella and thecae but were otherwise similar to control cells. In response to treatment with DTNB, many protoplasts synthesized new thecal scales in the Golgi apparatus, indicating that cells attempted to regenerate new cell walls. However, complete regeneration of the thecae only occurred once DTNB was washed out from the medium. At higher DTNB concentrations (5 mM), two protoplasts were found within the parental cell wall and scales accumulated between the plasma membrane of the protoplasts and the original theca but failed to form a new theca.     

Fossilization processes of graptolites: insights from the experimental decay of Rhabdopleura sp. (Pterobranchia)

Laboratory experiments documenting the decomposition pattern of extant organisms are used to reconstruct the anatomy and taphonomy of fossil taxa. The subclass Graptolithina (Hemichordata: Pterobranchia) is a significant fossil taxon of the Palaeozoic era, represented by just one modern genus, Rhabdopleura. The rich graptolite fossil record is characterized by an almost total absence of fossil zooids. Here we investigated the temporal decay pattern of Rhabdopleura sp. tubes, stolons and single zooids removed from the tubarium. Tubes showed decay after four days, when fuselli began to separate from the tube walls. This rapid loss may explain the absence of fuselli from some graptolite fossils. The black stolon did not show decay until day 155. One day after their removal, zooids quickly decomposed in the following temporal sequence: (1) tentacles; (2) ectoderm; (3) arms; (4) gut; (5) cephalic shield, leading to complete disappearance of recognizable body parts in the majority of experimental zooids within 64–104 h. The most resistant zooid features to decay (61 days) were black‐pigmented granules. These results indicate that tubes and the black stolon would persist for weeks across death, transport and burial, whereas a complete decay of zooid features occurs in few days, providing an explanation for the overall poor record of fossil graptolite zooids and suggesting that recorded silhouettes of fossil zooids may be attributed to fossil decay‐resistant pigments.     

Unconventional signalling in tunicates

The zooids in colonial tunicates do not appear to be directly interconnected by nerves, but this has not prevented the evolution of coordinated behaviour in several groups. In Botryllus and other colonial styelid asci‐dians the endothelium lining the blood vessels is excitable and transmits action potentials from cell to cell via gap junctions. These signals mediate protective contractions of the zooids and synchronize contractions of the vascular ampullae. In didemnid ascidians such as Diplosoma a network of myocytes in the tunic serves to transmit excitation and to cause contractions of the cloacal apertures. Individual zooids of Pyrosoma protect themselves by closing their siphons and arresting their branchial cilia when stimulated. At the same time a flash of light is emitted. Neighbouring zooids sense the flash with their photoreceptors and respond in turn with protective responses and light emission. Protective responses thus spread by photic signalling and propagate from zooid to zooid through the colony in a saltatory manner. In chains of Salpafusifortnis, changes in the direction and/or speed of swimming are transmitted from zooid to zooid via adhesion plaques. When a zooid is stimulated, its body‐wall epithelium conducts action potentials to the plaque connecting it to the next zooid, exciting receptor neurons in that zooid. These receptors have sensory processes that bridge the gap between the two zooids. The sensory neurons so excited in the second zooid conduct impulses to the brain where they alter the motor output pattern, and at the same time generate epithelial action potentials that travel to the next zooid in line, where the same thing happens.

It is not clear why these unconventional signalling methods have evolved but the tunic may be an inhospitable environment for nerves, making conventional nervous links impossible.     

Unveiling biases in soft‐tissue phosphatization: extensive preservation of musculature in the Cretaceous (Cenomanian) polychaete Rollinschaeta myoplena (Annelida: Amphinomidae)

The process of soft‐tissue phosphatization (the replication of labile tissues by calcium phosphate) is responsible for many instances of high‐resolution soft tissue preservation, often revealing anatomical insights into the animals that so preserved. However, while much work has gone into exploring key issues such as biases and micro‐controls, phosphatization remains poorly understood as a taphonomic process. Here, using camera lucida, plain‐light microscopy and SEM imagery, we address this issue by describing the taphonomy and fidelity of the musculature of Rollinschaeta myoplena Parry et al., a phosphatized annelid from the Cretaceous Konservat‐Lagerstätten of Hakel and Hjoula, Lebanon, with an unprecedented quantity of three‐dimensional soft‐tissue preservation. Analysis highlights two strong, previously recognized biases affecting the process of phosphatization: (1) a taxonomic bias restricted to R. myoplena that triggers unusually extensive phosphatization; and (2) a tissue bias whereby longitudinal and parapodial musculature show markedly higher fidelity in comparison to the musculature of the intestine and body wall circular muscles. Potential explanations for these biases include internal phosphate‐enrichment by relative muscle density, the relative rate of decay and the physiology of musculature. Incongruence between experimental decay series for polychaetes and the prevalence of labile tissue preservation over recalcitrant tissues in R. myoplena exposes the limits of decay experiments for understanding exceptional preservation.     

A New Flagship Peritrich (Ciliophora,Peritrichida) from the River Rhine,Germany: Apocarchesium arndti n. sp.

ABSTRACT. We discovered a free‐living peritrich ciliate with outstanding features in the River Rhine. Its morphology and 18S rRNA gene sequence were studied with standard methods. Apocarchesium arndti n. sp. has several peculiarities. (i) There are ordinary zooids, macrozooids, and microzooids, which form a hemispherical rosette on a discoidal base, the stalk dish, locking the ～18 μm wide and up to 2 mm long, spirally contracting colony stalk. (ii) The stalk myoneme is connected only to the microzooids. (iii) A rosette contains up to 50 zooids not connected to each other but individually attached to the stalk dish with the scopula. (iv) The ordinary zooids are epistylidid, trumpet‐shaped (～6:1 length:width), about 180 × 30 μm in size, and have an ellipsoidal macronucleus subapically between oral cavity and dorsal side. (v) The myoneme system of the zooids, which can contract individually, forms a tube‐like structure in the narrow posterior half of the cell. (vi) The silverline pattern belongs to the transverse‐striate type. (vii) The oral apparatus is of usual structure, with kinety 1 of peniculus 3 distinctly shortened proximally. (viii) The 18S rRNA places A. arndti n. sp. as a distinct lineage near Vorticella and Carchesium. These data are used to provide an improved diagnosis of the genus Apocarchesium. Features (i)–(iii) and the molecular data indicate that Apocarchesium could be the type genus of a new peritrich family.     

Developmental pattern of colonies in the polystyelid ascidian,Polyandrocarpa misakiensis

Summary

The growth pattern of zooids formed asexually by budding was studied in the colonial ascidian, Polyandrocarpa misakiensis. Each colony started from a blas- tozooid (the first generation) on the glass plate in two series of experiments. To evaluate the growth of colonies, lineage of all the zooids of three successive generations was traced on photographs which were taken once a week. The zooids of the first generation produced many buds from any basal margin of the zooidal body, and those of the second generation produced a small number of buds mainly from anterior parts of the zooidal body. The zooids of the second generation produced by early budding of mother zooids were clearly more prolific than those produced by late budding. Circular colonies which developed around a zooid of the first generation consisted of stratified zones of successive generations. Each zone was composed of two subzones; the outer one mainly containing early-produced zooids, and the inner one mainly containing late-produced zooids. The zooids in the marginal area of colony are early-produced ones from generation to generation. The seawater temperature may influence the growth of zooids and/or the frequency of budding.     

Ovarian structure of the marsupial frog Gastrotheca riobambae (Fowler)

The mature ovary of Gastrotheca riobambae presents large oocytes (3 mm in diameter) of pale yellow color. After ovulation and the beginning of embryonic incubation, the empty postovulatory follicles can be recognized in the ovary for about 30 days. The granulosa of these follicles never fills the follicular lumen and this cavity becomes filled with fluid during the first five days of incubation. Later, at 18 days of incubation, the lumen is mostly empty and contains few cells of the granulosa. Shrinkage results in the disappearance of the follicular cavity by approximately the thirtieth day of incubation. The thecae are thick and become separated by a space. This space is filled progressively with cells, blood capillaries and fluid. After the thirtieth to fortieth day of incubation, these follicles become regressive and disappear. The postovulatory follicles of Gastrotheca may correspond to corpora lutea. The evidence suggests that pouch vascularization and the formation of embryonic chambers of pouch tissue may be under ovarian control. In addition, the process of vitellogenesis is influenced by incubation, as most growth of the ovarian oocyte occurs after birth of the tadpoles. Follicular atresia is common and is similar to that of other frogs.     

Spicule structure and affinities of the Late Ordovician hexactinellid‐like sponge Cyathophycus loydelli from the Llanfawr Mudstones Lagerstätte,Wales

Exceptionally well‐preserved specimens of the reticulosan sponge Cyathophycus loydelli from the Sandbian (Late Ordovician) Llanfawr Mudstones Formation of Llandrindod, Waes, UK, have been examined using scanning electron microscopy (SEM). The specimens include exquisitely detailed pyritized spicules, and granular pyritization of surrounding soft tissues. Spicules frequently show axial canals of diameter similar to those of modern siliceous sponges, with hexagonal symmetry typical of modern demosponges rather than hexactinellids. In one case, the axial filament is also preserved. The largest spicules (ray diameter >20 μm) show a complex structure, with a laminar external region similar to that of the extant hexactinellid Monorhaphis. Some spicules preserve sub‐micron detail of the spicule surface, resembling the reticulate collagenous sheath of Monorhaphis. The hexagonal symmetry of the canal confirms that at least some Reticulosa are not crown‐group hexactinellids, but stem‐group Hexactinellida or Demospongea, or stem‐group Silicea. This suggests that a square canal is a sufficient diagnostic feature of total‐group Hexactinellida, but that hexagonal canals were more widely distributed among Early Silicea and were probably not restricted to demosponges. Alternatively, comparison with the structure of modern verongiid fibres suggests that these may be homologous with the outer layers of Cyathophycus spicules, and Cyathophycus may instead be a stem‐group demosponge. The preserved detail of the surface layer shows that pyritization can preserve certain material with extraordinarily fine resolution.     

Presumed postlarval pentacrinoids from the Lower Devonian Hunsrück Slate,Germany

Several tiny crinoids with crowns as small as 1 mm, or less, in width are newly recognized from the Hunsrück Slate of southwestern Germany. The presence of erect arms above an amorphous calyx in some specimens can be inferred. Based on comparison with the size and gross morphology of developmental stages in living crinoids, these tiny Hunsrück crinoids are judged to be at an early postlarval stage that is analogous to the pentacrinoid stage just after development from the stalked, but armless, smaller cystidean larval stage found in both living comatulids and isocrinids. Some of these tiny crinoids have a stalk up to 4 mm long attached to a now pyritized former substrate. Their clustered occurrence suggests gregarious settlement of larvae. Taxonomic identification of these presumed pentacrinoids is not possible, even to the sub‐class level, although they are preserved with larger juveniles of the cladids Propoteriocrinus and Lasiocrinus. These larger juveniles exhibit 3‐D pyritized calcite plates, whereas the probable pentacrinoids appear to be preserved as flattened, micro‐crystalline pyritized dermal tissues that enclosed lightly calcified, porous ossicles. The pentacrinoids were likely buried within weeks or months of hatching, based on developmental stages in similar‐sized living crinoids. These tiny crinoids, presumably pentacrinoids, are a further example of the extraordinarily detailed preservation of delicate tissues in pyrite from the Hunsrück Slate. They are most likely the pentacrinoid stage from one or more of the crinoid taxa (30 genera) present in the Hunsrück Slate. Assuming these are not microcrinoids, they are the first report of pentacrinoids from the fossil record and document that a Palaeozoic sister group to modern crinoids had similar developmental stages.