Bioapatite to calcite,an unusual transformation seen in fossil bones affected by aquatic bioerosion

A characteristic aquatic bioerosion, which peripherally penetrates the bone cortex, has previously been described from the 7‐million‐year‐old Cerro de la Garita calcareous lakeshore site (Concud, Teruel, Spain). This site has also yielded body fossils that appear to have been partly or entirely replaced by a delicate, white ‘crumbly substance’ that disaggregates upon touch. High‐resolution image and chemical analyses of the ‘crumbly substance’, bioeroded and non‐altered fossils, fresh bones and the site sediment are here described. The ‘crumbly substance’ was identified as calcite formed by non‐cemented micro‐crystals, preserving identical micro‐tunnelling than was observed in bioeroded fossil bones. This paper reports these results in detail and discusses how the original bone bioapatite may have been transformed. Results of these analyses have led us to propose that micro‐organisms, peripherally boring the bone, could also have influenced the transformation of bone bioapatite to calcite under specific micro‐environmental conditions.     

Trophic level and macronutrient shift effects associated with the weaning process in the Postclassic Maya

The weaning process was investigated at two Maya sites dominated by Postclassic remains: Marco Gonzalez (100 BC-AD 1350) and San Pedro (1400-AD 1650), Belize. Bone collagen and bioapatite were analyzed from 67 individuals (n < or = 6 years = 15, n > 6 years = 52). Five isotopic measures were used to reconstruct diet and weaning: stable nitrogen- and carbon-isotope ratios in collagen, stable carbon- and oxygen-isotope ratios in bioapatite, and the difference in stable carbon-isotope values of coexisting collagen and bioapatite. Nitrogen-isotope ratios in infant collagen from both sites are distinct from adult females, indicating a trophic level effect. Collagen-to-bioapatite differences in infant bone from both sites are distinct from adult females, indicating a shift in macronutrients. Oxygen-isotope ratios in infant bioapatite from both sites are also distinct from adult females, indicating the consumption of breast milk. Among infants, carbon- and nitrogen-isotope ratios vary, indicating death during different stages in the weaning process. The ethnohistoric and paleopathological literature on the Maya indicate cessation of breast-feeding between ages 3-4 years. Isotopic data from Marco Gonzalez and San Pedro also indicate an average weaning age of 3-4 years. Based on various isotopic indicators, weaning likely began around age 12 months. This data set is not only important for understanding the weaning process during the Postclassic, but also demonstrates the use of collagen-to-bioapatite spacing as an indicator of macronutrient shifts associated with weaning.     

The presence of mercury selenide in various tissues of the striped dolphin: evidence from μ-XRF-XRD and XAFS analyses

Marine mammals accumulate mercury in their tissues at high concentration and detoxify by forming mercury selenide (HgSe, tiemannite) mainly in the liver. We investigated the possibility of formation of HgSe in various tissues (liver, kidney, lung, spleen, pancreas, muscle and brain) other than the liver of the striped dolphin (Stenella coeruleoalba). We applied a combination method of micro-X-ray fluorescence (μ-XRF) imaging and micro-X-ray diffraction (μ-XRD) using a synchrotron radiation X-ray microbeam to analyze the tissue samples directly with minimal sample preparation. By this method, many accumulation points for Hg and Se on a micron scale were found in thin sections of the spleen and liver tissue and consequently, the XRF spectra and the XRD pattern of the hot spots confirmed the presence of tiemannite, HgSe. On the other hand, the insoluble fractions after enzyme digestion of the nuclear and mitochondrial fractions of all tissues were subjected to X-ray absorption fine structure (XAFS) analysis. XAFS analysis confirmed the presence of HgSe in all the tissues examined (liver, kidney, lung, spleen, pancreas, muscle and brain) of the striped dolphin. The presence of HgSe in all the tissues examined suggests that Se would be involved in the detoxification process of Hg in various tissues other than the liver. This contribution seems to be large especially in the liver and spleen but relatively small in the kidney, pancreas and brain, because the proportion of insoluble fraction containing HgSe was lower in these tissues (25 to 46%). This is the first report on the presence of tiemannite HgSe in various tissues of marine mammals.     

Ontogenetic variations in Sr/Ca and Ba/Ca ratios of dental bioapatites from Bos taurus and Odocoileus virginianus

Sr/Ca and Ba/Ca ratios of bone are commonly used as biochemical indicators of trophic level in modern and fossil mammals. Concerns over the effects of diagenesis on Sr/Ca and Ba/Ca ratios of bone led archaeologists and paleontologists to favor tooth enamel, which is less prone to alteration. Sr/Ca and Ba/Ca ratios of bone, enamel, and dentin from three farm-raised steers (Bos taurus) and five wild white-tailed deer (Odocoileus virginianus) from central Missouri were compared. Our results show that changes in diet, discrimination, and growth rate during ontogeny can lead to significant differences in Sr/Ca and Ba/Ca ratios of different bioapatite types as well as significant differences within the same bioapatite forming at different times. Early- and late-forming tooth enamel can have significant differences in Sr/Ca and Ba/Ca ratios equivalent to almost one full trophic step. Although differences between early- and late-forming dentin are typically not significant, dentin Sr/Ca and Ba/Ca ratios are significantly greater than enamel values. This difference in Sr/Ca or Ba/Ca ratios between enamel and dentin from the same tooth can be greater than one full trophic step. These results have profound implications for the use of dental bioapatites in trophic level reconstructions. They highlight the importance of consistency in bioapatite selection, tooth selection, and relative location of sampling within the enamel cap. Furthermore, this expected difference in Sr/Ca and Ba/Ca ratios could be used as another means of checking for diagenetic alteration in ancient samples.     

A quantitative bioapatite/collagen calibration method using Raman spectroscopy of bone

Numerous calibration models were developed and tested for the quantitative analysis of collagen and bioapatite in bone using Raman spectroscopy. The ν₁ phosphate vibration at 960 cm^–1 was used as indicator of the content of bioapatite while for collagen three markers were used: the C–H₂ band at 2940 cm^–1, the amide I band at 1667 cm^–1 and the vibrations of proline and hydroxyproline at 855 and 878 cm^–1, respectively. Also a calibration model based on the PLS algorithm was developed, too. Validation of the derived calibration models indicated that the model that makes use of the height ratio of the peaks 960/(855+878) exhibits the best accuracy. (© 2013 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)     

Stable isotope evidence (δ13C, δ18O) for winter feeding on seaweed by Neolithic sheep of Scotland

The antiquity of the use of seaweed to feed domestic animals was investigated through carbon ( δ ¹³C) and oxygen ( δ ¹⁸O) isotope analysis of tooth enamel bioapatite. The analysis was performed on sheep and cattle teeth from two Neolithic sites in Orkney (Scotland). At the Knap of Howar, c . 3600 bc , carbon isotopes reflect grazing on terrestrial plants throughout the year for both sheep and cattle, with no contribution of seaweed to their diet. At the Holm of Papa Westray North (HPWN), c . 3000 bc , significant contribution of seaweed to the sheep diet during winter is indicated by bioapatite δ ¹³C values as high as −5.7‰, far outside of the range of values expected for the feeding on terrestrial C₃ plants, and δ ¹⁸O values higher than expected during winter, possibly caused by ingestion of oceanic water with seaweed. Ingestion of seaweed by sheep at HPWN might have been necessitated by severe reduction of pastures during winter. Results suggest that sheep ingested fresh seaweed rather than dry fodder, perhaps directly on the shore as sheep do nowadays on North Ronaldsay. A significant difference between the two populations is the exclusive reliance on seaweed by the North Ronaldsay sheep, which have developed physiological adaptations to this diet. Contribution of seaweed to the sheep winter diet at HPWN might have been a first step towards this adaptation.     

New approaches for study of mechanisms of bone demineralization due to microgravity

Changes in nano-scale subsystems of rat femurs due to the axial unloading of hindlimbs are studied by means of electron paramagnetic resonance (EPR). After irradiation by 60Co isotopes, the results indicate that weightlessness simulation leads to formation of free radicals in tropocollagen molecules and to a reduction in the amount of CO2 radicals, located on the surface of bioapatite nanocrystals.     

The rocker bone: a new kind of mineralised tissue?

In some Ophidiiform fishes, the anterior part of the swimbladder is thickened into a hard structure called the "rocker bone", which is thought to play a role in sound production. Although this structure has been described as cartilage or bone, its nature is still unknown. We have made a thorough analysis of the rocker bone in Ophidion barbatum and compared it with both classical bone and cartilage. The rocker bone appears to be a new example of mineralisation. It consists of (1) a ground substance mainly composed of proteoglycans (mucopolysaccharide acid) and fibres and (2) a matrix containing small mineralised spherules composed of a bioapatite and fibrils. These spherules are embedded in mineralised cement of a similar composition to the spherules themselves. The rocker bone grows via the apposition of new apatite spherules at its periphery. These spherules are first secreted by the innermost fibroblast layer of the capsule contained in the rocker bone and then grow extracellularly. Blood vessels, which represent the only means of transport for matrix and mineral material, are numerous. They enter the rocker bone via the hyle and ramify towards the capsule. We propose to call this new kind of mineralised tissue constituting the rocker bone "frigolite" (the Belgian name for styrofoam) in reference to the presence of spherules of different sizes and the peculiarity of the rocker bone in presenting a smooth surface when fractured.     

Modern macaque dietary heterogeneity assessed using stable isotope analysis of hair and bone

Dietary variability might have been a major factor in the dispersal and subsequent persistence of the genus Macaca in both tropical and temperate areas. Macaques are found from northern Africa to Japan, yet there have been few systematic attempts to compare diets between different modern populations. Here we have taken a direct approach and sampled museum-curated tissues (hair and bone) of Macaca mulatta (rhesus macaques) for carbon and nitrogen stable isotope dietary analyses. Samples from India, Vietnam, and Burma (Myanmar) were taken, representing both tropical and temperate populations. The δ¹³C values obtained from hair show that the temperate macaques, particularly those from Uttar Pradesh, have a δ¹³C signature that indicates at least some use of C₄ resources, while the tropical individuals have a C₃-based diet. However, δ¹³C values from bone bioapatite indicate a C₃-based diet for all specimens and they do not show the C₄ usage seen in the hair of some animals, possibly because bone represents a much longer turnover period than that of hair. The results of δ¹⁵N analyses grouped animals by geographic region of origin, which may be related to local soil nitrogen values. The greatest variation in δ¹⁵N values was seen in the specimens from Burma, which may be partly due to seasonality, as specimens were collected at different times of year. We also investigated the relationship between the hair, bone collagen, and bone bioapatite δ¹³C results, and found that they are highly correlated, and that one tissue can be used to extrapolate results for another. However, our results also suggest that hair may pick up discrete feeding traces (such as seasonal usage), which are lost when only bone collagen and bioapatite are examined. This has important implications for dietary reconstructions of archaeological and paleontological populations.     

Tunable multicolor and white‐light upconversion luminescence in Yb3+/Tm3+/Ho3+ tri‐doped NaYF4 micro‐crystals

NaYF₄ micro‐crystals with various concentrations of Yb³⁺/Tm³⁺/Ho³⁺ were prepared successfully via a simple and reproducible hydrothermal route using EDTA as the chelating agent. Their phase structure and surface morphology were studied using powder X‐ray diffraction (XRD) and scanning electron microscopy (SEM). The XRD patterns revealed that all the samples were pure hexagonal phase NaYF₄. SEM images showed that Yb³⁺/Tm³⁺/Ho³⁺ tri‐doped NaYF₄ were hexagonal micro‐prisms. Upconversion photoluminescence spectra of Yb³⁺/Tm³⁺/Ho³⁺ tri‐doped NaYF₄ micro‐crystals with various dopant concentrations under 980 nm excitation with a 665 mW pump power were studied. Tunable multicolor (purple, purplish blue, yellowish green, green) and white light were achieved by simply adjusting the Ho³⁺ concentration in 20%Yb³⁺/1%Tm³⁺/xHo³⁺ tri‐doped NaYF₄ micro‐crystals. Furthermore, white‐light emissions could be obtained using different pump powers in 20%Yb³⁺/1%Tm³⁺/1%Ho³⁺ tri‐doped NaYF₄ micro‐crystals at 980 nm excitation. The pump power‐dependent intensity relationship was studied and relevant energy transfer processes were discussed in detail. The results suggest that Yb³⁺/Tm³⁺/Ho³⁺ tri‐doped NaYF₄ micro‐crystals have potential applications in optoelectronic devices such as photovoltaic, plasma display panel and white‐light‐emitting diodes. Copyright © 2014 John Wiley & Sons, Ltd.     

Oxygen and Carbon Isotope Variations in a Modern Rodent Community – Implications for Palaeoenvironmental Reconstructions

Background

The oxygen (δ¹⁸O) and carbon (δ¹³C) isotope compositions of bioapatite from skeletal remains of fossil mammals are well-established proxies for the reconstruction of palaeoenvironmental and palaeoclimatic conditions. Stable isotope studies of modern analogues are an important prerequisite for such reconstructions from fossil mammal remains. While numerous studies have investigated modern large- and medium-sized mammals, comparable studies are rare for small mammals. Due to their high abundance in terrestrial ecosystems, short life spans and small habitat size, small mammals are good recorders of local environments.

Methodology/Findings

The δ¹⁸O and δ¹³C values of teeth and bones of seven sympatric modern rodent species collected from owl pellets at a single locality were measured, and the inter-specific, intra-specific and intra-individual variations were evaluated. Minimum sample sizes to obtain reproducible population δ¹⁸O means within one standard deviation were determined. These parameters are comparable to existing data from large mammals. Additionally, the fractionation between coexisting carbonate (δ¹⁸O_CO3) and phosphate (δ¹⁸O_PO4) in rodent bioapatite was determined, and δ¹⁸O values were compared to existing calibration equations between the δ¹⁸O of rodent bioapatite and local surface water (δ¹⁸O_LW). Specific calibration equations between δ¹⁸O_PO4 and δ¹⁸O_LW may be applicable on a taxonomic level higher than the species. However, a significant bias can occur when bone-based equations are applied to tooth-data and vice versa, which is due to differences in skeletal tissue formation times. δ¹³C values reflect the rodents’ diet and agree well with field observations of their nutritional behaviour.

Conclusions/Significance

Rodents have a high potential for the reconstruction of palaeoenvironmental conditions by means of bioapatite δ¹⁸O and δ¹³C analysis. No significant disadvantages compared to larger mammals were observed. However, for refined palaeoenvironmental reconstructions a better understanding of stable isotope signatures in modern analogous communities and potential biases due to seasonality effects, population dynamics and tissue formation rates is necessary.     

Middle Pleistocene ecology and Neanderthal subsistence: Insights from stable isotope analyses in Payre (Ardèche,southeastern France)

The Middle Palaeolithic site of Payre in southeastern France yields abundant archaeological material associated with fossil hominid remains. With its long sequence of Middle Pleistocene deposits, Payre is a key site to study the Middle Palaeolithic chronology of this region. This study is the first to investigate carbon and oxygen isotope contents of Neanderthal tooth enamel bioapatite, together with a wide range of herbivorous and carnivorous species. The aim is to contribute to the understanding of hunting behaviour, resource partitioning, diet and habitat use of animals and Neanderthals through a palaeoecological reconstruction.     

Epithelial cell patterns on a PDMS polymer surface using a micro plasma structure

We developed a simple and reproducible epithelial cell-patterning tool on a PDMS (polydimethylsiloxane) polymer surface using a micro plasma structure that did not require chemical or biological treatment. The concept behind this novel approach was based on the fact that cells should easily adhere to the plasma-treated PDMS surface and not the inherent PDMS surface. The micro plasma structure consisted of copper and SU-8 photoresist on a glass substrate. A predetermined space (micro plasma chamber) was formed between the copper electrode layer on the upper part and the PDMS plate surrounded by the SU-8 photoresist structure. The single cell pattern was achieved by introducing a micro-plasma structure of 30 μm in width. Using this approach, a closed cell pattern was successfully developed using a micro chamber structure that was 200 μm in diameter with a microchannel that was 10 μm in width.     

Evidence-Based Nanoscopic and Molecular Framework for Excipient Functionality in Compressed Orally Disintegrating Tablets

The work investigates the adhesive/cohesive molecular and physical interactions together with nanoscopic features of commonly used orally disintegrating tablet (ODT) excipients microcrystalline cellulose (MCC) and D-mannitol. This helps to elucidate the underlying physico-chemical and mechanical mechanisms responsible for powder densification and optimum product functionality. Atomic force microscopy (AFM) contact mode analysis was performed to measure nano-adhesion forces and surface energies between excipient-drug particles (6-10 different particles per each pair). Moreover, surface topography images (100 nm²–10 µm²) and roughness data were acquired from AFM tapping mode. AFM data were related to ODT macro/microscopic properties obtained from SEM, FTIR, XRD, thermal analysis using DSC and TGA, disintegration testing, Heckel and tabletability profiles. The study results showed a good association between the adhesive molecular and physical forces of paired particles and the resultant densification mechanisms responsible for mechanical strength of tablets. MCC micro roughness was 3 times that of D-mannitol which explains the high hardness of MCC ODTs due to mechanical interlocking. Hydrogen bonding between MCC particles could not be established from both AFM and FTIR solid state investigation. On the contrary, D-mannitol produced fragile ODTs due to fragmentation of surface crystallites during compression attained from its weak crystal structure. Furthermore, AFM analysis has shown the presence of extensive micro fibril structures inhabiting nano pores which further supports the use of MCC as a disintegrant. Overall, excipients (and model drugs) showed mechanistic behaviour on the nano/micro scale that could be related to the functionality of materials on the macro scale.     

Mineralogical–geochemical characteristics of the bone detritus of Pleistocene mammals as a source of paleontological information

A complex mineralogical geochemical study of the bone detritus of large Pleistocene mammals inhabiting the Pechora Fore-Urals, the northernmost European part of their geographical range, is performed for the first time. The chemical composition, microstructure, content of 50 chemical elements are analyzed. The taphonomy of bones, extent of preservation of their initial properties, character and extent of fossilization are considered. The ultraporosity in the nanometer range is examined for the first time; it is established that it can be a marker of epigenetic changes in bones, beginning from the earliest stage of their fossilization. Based on X-ray structure and spectroscopic data, bone bioapatite is referred to carbonate–apatite of the B type. The results of thermal, chromatographic, and spectroscopic studies of collagen extracted from the bones of Pleistocene animals are discussed for the first time. The general trend of chemical degradation of bone proteins during fossilization is determined. The amino acid composition of bone collagen, the isotope composition of C, O, and N in biomineral and organic components of bones in the course of two-stage mass-spectrometer analysis of a complex sample are analyzed for the first time. Based on isotope-geochemical data conclusions concerning the diet and paleoclimatic and paleolandscape conditions of Pleistocene mammals are made.     

Technical Note: Calcium and carbon stable isotope ratios as paleodietary indicators

Calcium stable isotope ratios are hypothesized to vary as a function of trophic level. This premise raises the possibility of using calcium stable isotope ratios to study the dietary behaviors of fossil taxa and to test competing hypotheses on the adaptive origins of euprimates. To explore this concept, we measured the stable isotope composition of contemporary mammals in northern Borneo and northwestern Costa Rica, two communities with functional or phylogenetic relevance to primate origins. We found that bone collagen δ¹³C and δ¹⁵N values could differentiate trophic levels in each assemblage, a result that justifies the use of these systems to test the predicted inverse relationship between bioapatite δ¹³C and δ⁴⁴Ca values. As expected, taxonomic carnivores (felids) showed a combination of high δ¹³C and low δ⁴⁴Ca values; however, the δ⁴⁴Ca values of other faunivores were indistinguishable from those of primary consumers. We suggest that the trophic insensitivity of most bioapatite δ⁴⁴Ca values is attributable to the negligible calcium content of arthropod prey. Although the present results are inconclusive, the tandem analysis of δ⁴⁴Ca and δ¹³C values in fossils continues to hold promise for informing paleodietary studies and we highlight this potential by drawing attention to the stable isotope composition of the Early Eocene primate Cantius. Am J Phys Anthropol 154:633–643, 2014. © 2014 Wiley Periodicals, Inc.     

Bone demineralization mechanisms at level of free radicals and nanoscale subsystems of bone tissue

Influence of simulated microgravity on characteristics of rat bones was investigated by electron paramagnetic resonance (EPR). For simulation of microgravity condition the hanging of animal by tail was used. The main measurements were performed for diaphysis of femoral bones. The quantity of native radicals Rn, localized in an organic matrix, and carbonate radicals CO2-, localized on a surface of bioapatite nanocrystals, were determined. The decrease of CO2- radical quantity in bones of experimental animals have shown, that due to simulation of microgravity the decrease of "collagen-nanocrystals" interaction takes place. It is shown that the EPR method open possibilities to receive the unique information about bone demineralization processes at level of free radicals and nanoscale subsystems of bone tissue.     

Disulfide bonding among micro 1 trimers in mammalian reovirus outer capsid: a late and reversible step in virion morphogenesis

We examined how a particular type of intermolecular disulfide (ds) bond is formed in the capsid of a cytoplasmically replicating nonenveloped animal virus despite the normally reducing environment inside cells. The micro 1 protein, a major component of the mammalian reovirus outer capsid, has been implicated in penetration of the cellular membrane barrier during cell entry. A recent crystal structure determination supports past evidence that the basal oligomer of micro 1 is a trimer and that 200 of these trimers surround the core in the fenestrated T=13 outer capsid of virions. We found in this study that the predominant forms of micro 1 seen in gels after the nonreducing disruption of virions are ds-linked dimers. Cys679, near the carboxyl terminus of micro 1, was shown to form this ds bond with the Cys679 residue from another micro 1 subunit. The crystal structure in combination with a cryomicroscopy-derived electron density map of virions indicates that the two subunits that contribute a Cys679 residue to each ds bond must be from adjacent micro 1 trimers in the outer capsid, explaining the trimer-dimer paradox. Successful in vitro assembly of the outer capsid by a nonbonding mutant of micro 1 (Cys679 substituted by serine) confirmed the role of Cys679 and suggested that the ds bonds are not required for assembly. A correlation between micro 1-associated ds bond formation and cell death in experiments in which virions were purified from cells at different times postinfection indicated that the ds bonds form late in infection, after virions are exposed to more oxidizing conditions than those in healthy cells. The infectivity measurements of the virions with differing levels of ds-bonded micro 1 showed that these bonds are not required for infection in culture. The ds bonds in purified virions were susceptible to reduction and reformation in situ, consistent with their initial formation late in morphogenesis and suggesting that they may undergo reduction during the entry of reovirus particles into new cells.     

Development and validation of opioid ligand-receptor interaction models: the structural basis of mu vs delta selectivity.

Opioid receptor binding conformations for two structurally related, conformationally constrained tetrapeptides, JOM-6 ( micro receptor selective) and JOM-13 (delta receptor selective), were deduced using conformational analysis of these ligands and analogs with additional conformational restrictions. Docking of these ligands in their binding conformations to opioid receptor structural models, based upon the published rhodopsin X-ray structure, implicates specific structural features of the micro and delta receptor ligand binding sites as forming the basis for the micro selectivity of JOM-6 and the delta selectivity of JOM-13. In particular, the presence of E229 in the micro receptor (in place of the corresponding D210 of the delta receptor) causes an adverse electrostatic interaction with C-terminal carboxylate-containing ligands, resulting in the observed preference of ligands with an uncharged C-terminus for the micro receptor. In addition, the requirement that the Phe3 side chain of JOM-13 assume a gauche orientation for optimal delta binding, whereas the Phe3 side chain of JOM-6 must be in a trans orientation for high-affinity micro binding can be largely attributed to the steric effect of replacement of L300 of the delta receptor by W318 of the micro receptor. Testing this hypothesis by examining the binding of JOM-6 and several of its key analogs with specific micro receptor mutants is described. Our initial results are consistent with the proposed ligand-receptor interaction models.     

The integumental ultrastructure of Lamippe rubra Bruzelius and Enalcyonium rubicundum Olsson (Copepoda,Poecilostomatoida)

The integument of Lamippe rubra Bruzelius and of Enalcyonium rubicundum Olsson has been studied with the electron microscope.Most of the cuticle covering the body of Lamippe is represented by the epicuticle, which shows an average thickness of about 2.0 µm, but in sclerified zones it consists of a thin epicuticle (0.2 µm) and a stratified laminated procuticle (0.5–1.5 µm) without bow-shaped structure. A complex system of epithelial microvilli or a well-developed system of membranes running parallel to the cuticle is also present.The cuticle of Enalcyonium consists of a thin procuticle (0.4–0.5 µm) covered with a uniform fibrillar coat (0.5 µm), whereas in sclerotized areas it is composed of a stratified procuticle (0.7–3.5 µm) with bow-shaped structures.In both species, cuticular hairs and gland vents occur at the dorsal and ventral surfaces. Some of the hairs are considered to be sensory in nature.The cuticular ultrastructure of L. rubra and of E. rubicundum is compared with that of some other copepods.