Cytochemical, biochemical and molecular aspects of the process of keratinization in the epidermis of reptilian scales

The characteristics of scaled skin of reptiles is one of their main features that distinguish them from the other amniotes, birds and mammals. The different scale patterns observed in extant reptiles result from a long evolutive history that allowed each species to adapt to its specific environment. The present review deals with comparative aspects of epidermal keratinization in reptiles, chelonians (turtles and tortoises), lepidosaurian (lizards, snakes, sphenodontids), archosaurians (crocodilians). Initially the morphology and cytology of reptilian scales is outlined to show the diversity in the epidermis among different groups. The structural proteins (alpha-keratins and associated proteins), and enzymes utilized to form the corneous layer of the epidermis are presented. Aside cytokeratins (alpha-keratins), used for making the cytoskeleton, reptilian alpha-keratinocytes produce interkeratin (matrix) and corneous cell envelope proteins. Keratin bundles and degraded cell organelles constitute most of the corneous material of alpha-keratinocytes. Matrix, histidine-rich and sulfur-rich proteins are produced in the soft epidermis and accumulated in the cornified cell envelope. Main emphasis is given to the composition and to the evolution of the hard keratins (beta-keratins). Beta-keratins constitute the hard corneous material of scales. These small proteins are synthesized in beta-keratinocytes and are accumulated into small packets that rapidly merge into a compact corneous material and form densely cornified layers. Beta-keratins are smaller proteins (8-20 kDa) in comparison to alpha-keratins (40-70 kDa), and this size may determine their dense packing in corneocytes. Both glycine-sulfur-rich and glycine-proline-rich proteins have been so far sequenced in the corneous material of scales in few reptilian species. The latter keratins possess C- and N-amino terminal amino acid regions with sequence homology with those of mammalian hard keratins. Also, reptilian beta-keratins possess a central core with homology with avian scale/feather keratins. Multiple genes code for these proteins and their discovery and sequentiation is presently an active field of research. These initial findings however suggest that ancient reptiles already possessed some common genes that have later diversified to produce the specific keratin-associated proteins in their descendants: extant reptiles, birds and mammals. The evolution of these small proteins in lepidosaurians, chelonians and archosaurians represent the next step to understand the evolution of cornification in reptiles and derived amniotes (birds and mammals).     

Soft epidermis of a scaleless snake lacks beta-keratin

Beta-keratins are responsible for the mechanical resistance of scales in reptiles. In a scaleless crotalus snake (Crotalus atrox), large areas of the skin are completely devoid of scales, and the skin appears delicate and wrinkled. The epidermis of this snake has been assessed for the presence of beta-keratin by immunocytochemistry and immunoblotting using an antibody against chicken scale beta-keratin. This antibody recognizes beta-keratins in normal snake scales with molecular weights of 15-18 kDa and isoelectric points at 6.8, 7.5, 8.3 and 9.4. This indicates that beta-keratins of the stratum corneum are mainly basic proteins, so may interact with cytokeratins of the epidermis, most of which appear acidic (isoelectric points 4.5-5.5). A beta-layer and beta-keratin immunoreactivity are completely absent in moults of the scaleless mutant, and the corneous layer comprises a multi-layered alpha-layer covered by a flat oberhautchen. In conclusion, the present study shows that a lack of beta-keratins is correlated with the loss of scales and mechanical protection in the skin of this mutant snake.     

Embryonic keratinization in vertebrates in relation to land colonization

The embryogenesis and cytology of the epidermis in different vertebrates is variable in relation to the formation of a stratum corneum of different complexity. The latter process was essential for land colonization during vertebrate evolution and produced an efficient barrier in amniotes. Keratinocytes are made of cross‐linked keratins associated with specific proteins and lipids that are produced at advanced stages of embryogenesis when the epidermis becomes stratified. In these stages the epidermis changes from an aquatic to a terrestrial type, preadapted in preparation for the impact with the dry terrestrial environment that occurs at hatching or parturition. The epidermal barrier against water‐loss, mechanical and chemical stress, and microbe penetration is completely formed shortly before birth. Beneath the outer periderm, variably stratified embryonic layers containing glycine‐rich alpha‐keratins are formed in preparation for adult life. The following layers of the epidermis produce proteins for the formation of the cornified cell membrane and of the cornified material present in keratinocytes of the adult epidermis in reptiles, birds and mammals. The general features of the process of soft cornification in the embryonic epidermis of vertebrates are presented. Cornification in developing scales in reptiles, avian feathers and mammalian hairs is mainly related to the evolution of keratin‐associated proteins. The latter proteins form the resistant matrix of hard skin derivatives such as claws, beaks, nails and horns.     

Immuno-cross reactivity of transglutaminase and cornification marker proteins in the epidermis of vertebrates suggests common processes of soft cornification across species

In differentiating mammalian keratinocytes proteins are linked to the plasma membrane by epidermal transglutaminases through N-epsilon-(gamma-glutamyl)-lysine isopeptide bonds to form the cornified cell envelope. The presence of transglutaminases and their protein substrates in the epidermis of nonmammalian vertebrates is not known. The present study analyses the presence and localization of the above proteins in the epidermis using immuno-cross reactivity across different classes of amniotes. After immunoblotting, some protein bands appear labelled for loricrin, sciellin, and transglutaminase in most species. These proteins are scarce to absent in the epidermis of aquatic species (goldfish and newt) where a stratum corneum is absent or very thin. The molecular weight of transglutaminase immunoreactive bands generally varies between 40 to 62 kDa, with the most represented bands at 52-57 kDa in most species. The more intense loricrin- and sciellin-immunoreactive bands are seen at 50-55-62 kDa, but are weak or absent in aquatic vertebrates. Loricrine-like immunoreactivity is present in the epidermis where alpha-(soft)-keratinization occurs. Isopeptide bonds are mainly associated to bands in the range of 50-62 kDa. In vertebrates where hard-keratin is expressed (the beta-keratin corneous layer of sauropsids and in feathers) or in hair cortex of mammals, no loricrin-like, transglutaminase-, and isopeptide-bond-immunoreactivities are seen. Immunoblotting however shows loricrin-, sciellin-, and trasnsglutaminase-positive bands in the corneous layers containing beta-keratin. Histologically, the epidermis of most amniotes shows variable transglutaminase immunoreactivity, but isopeptide-bond and sciellin immunoreactivities are weak or undetactable in most species. The limitations of immunohistochemical methods are discussed and compared with results from immunoblotting. In reptilian epidermis transglutaminase is mainly localized in 0.15-0.3 microm dense granules or diffuse in transitional alpha-keratogenic cells. In beta-keratogenic cells few small dense granules show a weak immunolabeling. Transglutaminase is present in nuclei of terminal differentiating alpha- and beta-keratinocytes, as in those of mature inner and outer root sheath. The present study suggests that keratinization based on loricrin, sciellin and transglutaminase was probably present in the stratum corneoum of basic amniotes in the Carboniferous. These proteins were mainly maintained in alpha-keratogenic layers of amniotes but decreased in beta-keratogenic layers of sauropsids (reptiles and birds). The study suggests that similar proteins for the formation of the cornified cell envelope are present in alpha-keratinocytes across vertebrates but not in beta-keratinocytes.     

Distribution and characterization of keratins in the epidermis of the tuatara (Sphenodon punctatus; Lepidosauria, Reptilia)

Reptilian scales are mainly composed of alpha-and beta-keratins. Epidermis and molts from adult individuals of an ancient reptilian species, the tuatara (Sphenodon punctatus), were analysed by immunocytochemistry, mono- and bi-dimensional electrophoresis, and western blotting for alpha- and beta-keratins. The epidermis of this reptilian species with primitive anatomical traits should represent one of the more ancient amniotic epidermises available. Soft keratins (AE1- and AE3-positive) of 40-63 kDa and with isoelectric points (pI) at 4.0-6.8 were found in molts. The AE3 antibody was diffusely localised over the tonofilaments of keratinocytes. The lack of basic cytokeratins may be due to keratin alteration in molts, following corneification or enzymatic degradation of keratins. Hard (beta-) keratins of 16-18 kDa and pI at 6.8, 8.0, and 9.2 were identified using a beta-1 antibody produced against chick scale beta-keratin. The antibody also labeled filaments of beta-cells and of the mature, compact beta-layer. We have shown that beta-keratins in the tuatara resemble those of lizards and snakes, and that they are mainly basic proteins. These proteins replace cytokeratins in the pre-corneoum beta-layers, from which a hard, mechanically resistant corneoum layer is formed over scales. Beta-keratins may have both a fibrous and a matrix role in forming the hard texture of corneoum scales in this ancient species, as well as in more recently evolved reptiles.     

Formation of the corneous layer in the epidermis of the tuatara (Sphenodon punctatus, Sphenodontida, Lepidosauria, Reptilia)

The formation of the stratum corneum in the epidermis of the reptile Sphenodon punctatus has been studied by histochemical, immunohistochemical, and ultrastructural methods. Sulfhydryl groups are present in the mesos and pre-alpha-layer but disappear in the keratinized beta-layer and in most of the mature alpha-layer. This suggests a complete cross-linking of keratin filaments. Tyrosine increases in keratinized layers, especially in the beta-layer. Arginine is present in living epidermal layers, in the presumptive alpha-layer, but decreases in keratinized layers. Histidine is present in corneous layers, especially in the intermediate region between the alpha- and a new beta-layer, but disappears in living layers. It is unknown whether histidine-rich proteins are produced in the intermediate region. Small keratohyalin-like granules are incorporated in the intermediate region. The plane of shedding, as confirmed from the study on molts, is located along the basalmost part of the alpha-layer and may involve the degradation of whole cells or cell junctions of the intermediate region. A specific shedding complex, like that of lizards and snakes, is not formed in tuatara epidermis. AE1-, AE2-, or AE3-positive alpha-keratins are present in different epidermal layers with a pattern similar to that previously described in reptiles. The AE1 antibody stains the basal and, less intensely, the first suprabasal layers. Pre-keratinized, alpha- and beta-layers, and the intermediate region remain unlabeled. The AE2 antibody stains suprabasal and forming alpha- and beta-layers, but does not stain the basal and suprabasal layers. In the mature beta-layer the immunostaining disappears. The AE3 antibody stains all epidermal layers but disappears in alpha- and beta-layers. Immunolocalization for chick scale beta-keratins labels the forming and mature beta-layer, but disappears in the mesos and alpha-layer. This suggests the presence of common epitopes in avian and reptilian beta-keratins. Low molecular weight alpha-keratins present in the basal layer are probably replaced by keratins of higher molecular weight in keratinizing layers (AE2-positive). This keratin pattern was probably established since the beginning of land adaptation in amniotes.     

Immunocytochemistry and protein analysis suggest that reptilian claws contain small high cysteine-glycine proteins

The present study analyzes the structure and the main proteins of reptilian claws. Mature claws are formed by two to four layers of keratinocytes, a transitional layer of spindle-shaped cells and a thick corneous layer. Transitional cells elongate and merge into a compact corneous layer that is immunoreactive for beta-keratins, now indicated as sauropsid keratin-associated proteins (sKAPs). Most proteins extracted from claws in representative reptiles have a molecular weight of 13-20 kDa, an acidic to basic isoelectric point, and are identified from the positive immunoreactivity to beta-keratin antibodies. The comparative analysis between lizard and avian claw beta-keratins shows the presence of an internal region of 20 amino acids with the highest identity, indicated as core-box, within an extended 32-amino acid region with a prevalent beta-sheet secondary conformation. This region is structurally equivalent to a 32-amino acid region present in scale beta-keratins of most reptiles. Both reptilian and avian keratins contain glycine-rich regions for stabilization of the beta-keratin polymer. The N- and C-regions contain most cysteine for disulphide-bonds formation. Claw proteins contain higher amount of cysteine and glycine than other scale proteins, suggesting that claw proteins are specialized cysteine-glycine-rich proteins suited to produce a very hard corneous material.     

Alpha- and beta-keratins of the snake epidermis

Snake scales contain specialized hard keratins (beta-keratins) and alpha- or cyto-keratins in their epidermis. The number, isoelectric point, and the evolution of these proteins in snakes and their similarity with those of other vertebrates are not known. In the present study, alpha- and beta-keratins of snake molts and of the whole epidermis have been studied by using two-dimensional electrophoresis and immunocytochemistry. Specific keratins in snake epidermis have been identified by using antibodies that recognize acidic and basic cytokeratins and avian or lizard scale beta-keratin. Alpha keratins of 40-70 kDa and isoelectric point (pI) at 4.5-7.0 are present in molts. The study suggests that cytokeratins in snakes are acidic or neutral, in contrast to mammals and birds where basic keratins are also present. Beta keratins of 10-15 kDa and a pI of 6.5-8.5 are found in molts. Some beta-keratins appear as basic proteins (pI 8.2) comparable to those present in the epidermis of other reptiles. Some basic "beta-keratins" associate with cytokeratins as matrix proteins and replace cytokeratins forming the corneous material of the mature beta-layer of snake scales, as in other reptiles. The study also suggests that more forms of beta-keratins (more than three different types) are present in the epidermis of snakes.     

Identification of a rapidly labelled 350K histidine-rich protein in neonatal mouse epidermis

The major histidine-rich protein (HRP) found in the stratum corneum of neonatal mouse epidermis (band 2 protein, molecular weight 27,000) is a relatively late product of epidermal differentiation and incorporates labelled amino acids in vivo only after a 6-9 h lag period. A number of putative precursor HRPs in the 70-300 K molecular weight range were initially identified using short pulse labeling times and our previously described methods for isolation of epidermis and extraction of proteins. However, when steps were taken to minimise proteolysis during preparation, a single species of approximately 350 K molecular weight was the most strongly labelled protein following a 1 h in vivo pulse of [3H]-histidine. This protein was stable in sodium dodecyl sulphate dithiothreitol at 100 degrees C and in 4 M urea, suggesting a single covalently linked polypeptide. The kinetics of labelling and the localisation of the 350 K HRP in the lower granular layers suggest that it is a precursor of the stratum corneum HRP. The processing of the 350 K HRP to the stratum corneum species appears to involve a complex series of specific cleavage steps which give rise to a number of HRPs of intermediate molecular weight.     

Characterization of beta-keratins in lizard epidermis: electrophoresis, immunocytochemical and in situ-hybridization study

Lizard scales are composed of alpha-(cyto-) keratins and beta-keratins. The characterization of the molecular weight and isoelectric point (pI) of alpha- and beta-keratins of lizard epidermis (Podarcis sicula) has been done by using two-dimensional electrophoresis, immunoblotting, and immunocytochemistry. Antibodies against cytokeratins, against a chicken scale beta-keratin or against lizard beta-keratin bands of 15-16 kDa, have been used to recognize alpha- and beta-keratins. Acid and basic cytokeratins of 42-67 kDa show a pI from 5.0 to 8.9. This indicates the presence of specific keratins for the formation of the stratum corneum. Main protein spots of beta-keratin at 15-17 kDa, and pI at 8.5, 8.2, and 6.7, and one spot at 10 kDa and pI at 7.3 were recognized. Therefore, beta-keratins are mainly basic proteins, and are used for the formation of the hard corneous layer of the epidermis. Ultrastructural immunocytochemistry confirms that beta-keratin is packed into large and dense bundles of beta-keratin cells of lizard epidermis. The use of a probe against a lizard beta-keratin in situ-hybridization studies confirms that the mRNA for beta-keratins is present in beta-cells and is localized around or even associated with beta-keratin filaments.     

Hard (Beta-)keratins in the epidermis of reptiles: composition, sequence, and molecular organization

Beta-keratins form the hard corneous material of reptilian scales. In the present review, the distribution and molecular characteristics of beta-keratins in reptiles are presented. In lepidosaurians immunoreactive, protein bands at 12-18 kDa are generally present with less frequent proteins at higher molecular weight. In chelonians, bands at 13-18 and 22-24 kDa are detected. In crocodilians, bands at 14-20 kDa and weaker bands at 30-32 kDa are seen. Protein bands above 25 kDa are probably polymerized beta-keratins or aggregates. Two-dimensional gel electrophoresis shows that beta-keratins are mainly basic and that acidic-neutral keratins may derive from post-translational modifications. Beta-keratins comprise glycine-proline-rich and cystein-proline-rich proteins of 13-19 kDa. Beta-keratin genes may or may not contain introns and are present in multiple copies with a linear organization as in avian beta-keratin genes. Despite amino acid differences toward N- and C-terminals all beta-keratins share high homology in their central, beta-folded region of 20 amino acids, indicated as core-box. This region is implicated in the formation of beta-keratin filaments of scales, claws, and feathers. The homology of the core-box suggests that these proteins evolved from a progenitor sequence present in the stem of reptiles. Beta-keratins have diversified in their amino acid sequences producing secondary (and tertiary) conformations that suited them for their mechanical role in scales. In birds, a small beta-keratin has allowed the formation of feathers. It is suggested that beta-keratins represent the reptilian counterpart of keratin associated or matrix proteins present in mammalian hairs, claws, and horns.     

Identification of a Rapidly Labelled 350K Histidine-Rich Protein in Neonatal Mouse Epidermis

Abstract. The major histidine-rich protein (HRP) found in the stratum corneum of neonatal mouse epidermis (band 2 protein, molecular weight 27,000) is a relatively late product of epidermal differentiation and incorporates labelled amino acids in vivo only after a 6–9 h lag period. A number of putative precursor HRPs in the 70–300 K molecular weight range were initially identified using short pulse labelling times and our previously described methods for isolation of epidermis and extraction of proteins. However, when steps were taken to minimise proteolysis during preparation, a single species of approximately 350 K molecular weight was the most strongly labelled protein following a 1 h in vivo pulse of [³H]-histidine. This protein was stable in sodium dodecyl sulphate dithiothreitol at 100°C and in 4 M urea, suggesting a single covalently linked polypeptide. The kinetics of labelling and the localisation of the 350 K HRP in the lower granular layers suggest that it is a precursor of the stratum corneum HRP. The processing of the 350 K HRP to the stratum corneum species appears to involve a complex series of specific cleavage steps which give rise to a number of HRPs of intermediate molecular weight.     

Dermo-epidermal interactions in reptilian scales: speculations on the evolution of scales, feathers, and hairs

The dermal influence on the epidermis during scale formation in reptiles is poorly known. Cells of the superficial dermis are not homogeneously distributed beneath the epidermis, but are instead connected to specific areas of the epidermis. Dermal cells are joined temporarily or cyclically through the basement membrane, with the reactive region of the epidermis forming specific regions of dermo-epidermal interactions. In these regions morphoregulatory molecules may be exchanged between the dermis and the connected epidermis. Possible changes in the localization of these regions in the skin may result in the production of different appendages, in accordance with the genetic makeup of the epidermis in each species. Regions of dermo-epidermal interactions seem to move their position during development. A hypothesis on the development and evolution of scales, hairs, and feathers from sarcopterigian fish to amniotes is presented, based on the different localization and extension of regions of dermo-epidermal interactions in the skin. It is hypothesized that, during phylogenesis, possible variations in the localization and extension of these regions, from the large scales of basic amniotes to those of sauropsid amniotes, may have originated scales with hard (beta)-keratin. In extant reptiles, extended regions of dermo-epidermal interaction form most of the expanse of outer scale surface. It is hypothesized that the reduction of large regions of dermo-epidermal interactions into small areas in the skin were the origin of dermal condensations. In mammals, small regions of dermo-epidermal interactions have invaginated, forming the dermal papilla with the associated hair matrix epidermis. In birds, small regions of dermo-epidermal interactions have reduced the original scale surface of archosaurian scales, forming the dermal papilla. The latter has invaginated in association with the collar epidermis from which feathers were produced.     

Ontogenetic variation in the stratum granulosum of the epidermis of Chaetophractus vellerosus (Xenarthra,Dasypodidae) in relation to the development of cornified scales

The epidermis of mammals is characterized by having a stratum granulosum that produces an orthokeratotic stratum corneum, different from the typical reptilian parakeratotic stratum. Nonetheless, some mammals show distinct degrees of parakeratosis in epidermal regions with few or no pilose follicles (e.g., areas subjacent to cornified scales). With respect to the epidermis and the development of cornified scales in the Dasypodidae, previous studies have supported the presence of a continuous stratum granulosum without any variations during ontogeny. This condition, in which the cornified scales develop without a loss of the stratum granulosum, was interpreted as primitive for eutherians. The present contribution expands the knowledge on the epidermis of Chaetophractus vellerosus in distinct ontogenetic stages in order to determine whether the cornified scales show the same developmental pattern as in other eutherians. The presence of a stratum granulosum in C. vellerosus neonates and its reduction in more advanced ontogenetic stages, in direct relationship with cornified scale development, supports the hypothesis that the partial parakeratosis in the xenarthran integument is secondary, as in other eutherians, and can be interpreted as a derived character state.     

Immunocytochemical analysis of beta keratins in the epidermis of chelonians,lepidosaurians, and archosaurians

Beta (beta) keratins are present only in the avian and reptilian epidermises. Although much is known about the biochemistry and molecular biology of the beta keratins in birds, little is known for reptiles. In this study we have examined the distribution of beta keratins in the adult epidermis of turtle, lizard, snake, tuatara, and alligator using light and electron immunocytochemistry with a well-characterized antiserum (anti-beta(1) antiserum) made against a known avian scale type beta keratin. In lizard, snake, and tuatara epidermis this antiserum reacts strongly with the beta-layer, more weakly with the oberhautchen before it merges with the beta-layer, and least intensely with the mesos layer. In addition, the anti-beta(1) antiserum reacts specifically with the setae of climbing pads in gekos, the plastron and carapace of turtles, and the stratum corneum of alligator epidermis. Electron microscopic studies confirm that the reaction of the anti-beta(1) antiserum is exclusively with characteristic bundles of the 3-nm beta keratin filaments in the cells of the forming beta-layer, and with the densely packed electron-lucent areas of beta keratin in the mature bet- layer. These immunocytochemical results suggest that the 3-nm beta keratin filaments of the reptilian integument are phylogenetically related to those found in avian epidermal appendages.     

Local cutaneous water barrier in cold- and heat-acclimated pigeons (Columba livia) in relation to cutaneous water evaporation

The thermoregulatory function of the skin differs in adult cold-acclimated and heat-acclimated rock pigeons (Columba livia). In general, the cutaneous evaporative cooling mechanism is not activated by appropriate stimuli in cold-acclimated pigeons in contrast to heat-acclimated pigeons. We studied with electron microscopy whether the differences in the function of the skin are reflected in the structure of the epidermal water barrier of these two extreme acclimation states. The epidermis of cold-acclimated pigeons is attenuated, and the underlying dermis lacks any intimate vascularization. Both the extracellular and the intracellular domains in the stratum corneum contain organized lamellar lipids. At the stratum transitivum-stratum corneum interface, multigranular body secretion is indicated by the highly convoluted cell membranes and membraneous sacculae enclosing the multigranular bodies. Alternatively, multigranular bodies retain in the corneocytes, and the lipoid material originated from them is reprocessed to broad lamellae. The keratohyalin (KH) granules are spotlike and oriented as cortical bands beneath the plasma membrane. In heat-acclimated pigeons, the epidermis displays modified patches side by side with basic structural type of epidermis. The modified areas are characterized by hypertrophy and abundance of dermal capillaries adjacent to the hypertrophied patch. No lamellar lipids are discerned in the dilated extracellular space. The structure of multigranular bodies is abnormal, and the numbers of lipid droplets in the outer viable epidermis and stratum corneum are decreased. The transitional cells contain stellate KH granules, which form a network throughout the cell. It is concluded that cold-acclimated pigeons have a lamellar, extracellular water barrier, the cutaneous water evaporation is minimized, and heat is stored in the body core. Acclimation to heat leads to formation of structurally heterogeneous skin. The structurally modified skin patches show disruption of the barrier-forming machinery in the multigranular bodies and marked reorganization of fibrillar proteins and electron-dense KH masses in the transitional layer. Thus water barrier adjustments in cold- and heat-acclimated pigeons manifest the dynamic function of avian skin as a thermoregulatory organ.     

Morphological Characteristics of the Dorsal Skin of Two Hynobiids and Their Adaptive Role in Aquatic and Terrestrial Habitats

The morphological characteristics of the dorsal skin of trunk in two species of hynobiid salamanders, Batrachuperus pinchonii and Hynobius chinensis were examined by light microscopy. The basic structures of the skin in the two species are similar and consist of two layers: epidermis and dermis. The epidermis consists of stratum corneum, stratum intermedium and stratum germinativum, while the dermis is composed of a stratum spongiosum and stratum compactum. However, some species-specific variation has been identified(e.g., the distribution of capillary vessels and gland cells, and the thickness of skin). H. chinensis is a terrestrial species and only lives in water during breeding period, but B. pinchonii is aquatic and remains aquatic throughout its lifetime. The differences in the distribution of capillary vessels and gland cells are related to their different habitats, and show a morphological adaptation.     

Putative histidin-rich proteins in the epidermis of lizards

In the stratum granulosum of mammalian epidermis, histidin-rich proteins (filaggrins) determine keratin clumping and matrix formation into terminal keratinocytes of the stratum corneum. The nature of matrix, interkeratin proteins in the epidermis of nonmammalian vertebrates, and in particular in that of reptilian, mammalian progenitors are unknown. The present biochemical study is the first to address this problem. During a specific period of the renewal phase of the epidermis of lizards and during epidermal regeneration, keratohyalin-like granules are formed, at which time they take up tritiated histidine. The latter also accumulate in cells of the alpha-keratin layer (soft keratin). This pattern of histidine incorporation resembles that seen in keratohyalin granules of the stratum granulosum of mammalian epidermis. After injection of tritiated histidine, we have analysed the distribution of the radioactivity by histoautoradiography and electrophoretic gel autoradiography of epidermal proteins. Extraction and electrophoretic separation of interfilamentous matrix proteins from regenerating epidermis 3-48 hours post-injection reveals the appearance of protein bands at 65-70, 55-58, 40-43, 30-33, 25-27, and 20-22 kDa. Much weaker bands were seen at 100, 140-160, and 200 kDa. A weak band at 20-22 kDa or no bands at all are seen in the normal epidermis in resting phase and in the dermis. In regenerating epidermis at 22 and 48 hours post-injection, little variation in bands is detectable, but low molecular weight bands tend to increase slightly, suggesting metabolic turnover. Using anti-filaggrin antibodies against rat, human, or mouse filaggrins, some cross-reactivity was seen with more reactive bands at 40-42 and 33 kDa, but it was reduced or absent at 140, 95-100, 65-70, 50-55, and 25 kDa. This suggests that different intermediate degradative proteins of lizard epidermis may share some epitopes with mammalian filaggrins and are different from keratins with molecular weight ranging from 40 to 65-68 kDa. The immunocytochemical observation confirms that a weak filaggrin-like immunoreactivity characterizes differentiating alpha-keratogenic layers in normal and regenerating tail. A weak filaggrin labeling is discernable in small keratohyalin-like granules but is absent from the larger granules and from mature keratinocytes. The present results indicate, for the first time, that histidine-rich proteins are involved in the process of alpha-keratinization in reptilian epidermis. The cationic, interkeratin matrix proteins implicated may be fundamentally similar in both theropsid-derived and sauropsid amniotes.     

Immunolocalization and characterization of beta-keratins in growing epidermis of chelonians

Beta-keratins constitute most of the corneous material of carapace and plastron of turtles. The production of beta-keratin in the epidermis of a turtle and tortoise (criptodirians) and of a species of pleurodiran turtle was studied after injection of tritiated proline during the growth of carapace, plastron and claws. Growth mainly occurs near hinge regions along the margins of scutes and along most of the claws (growing regions). Proline incorporation occurs mainly in the growing centers, and is more specifically associated with beta-keratin synthesis. Proline-labeled bands of protein at 12-14 kDa and 25-27 kDa, and 37 kDa, in the molecular weight range of beta-keratins, were isolated from the soft epidermis of turtles 3 h after injection of the labeled amino acid. After extraction of epidermal proteins, an antibody directed against a chicken beta-keratin was used for immunoblotting. Bands of beta-keratin at 15-17 kDa, 22-24 kDa, and 36-38 kDa appear in all species. Beta-keratin is present in the growing and compact stratum corneum of the hard (shell) and soft (limbs, neck and tail) epidermis. This was confirmed using a specific antibody against a turtle beta-keratin band of 15-16 kDa. The latter antibody recognized epidermal protein bands in the range of 15-16 kDa and 29-33 kDa, and labels beta-keratin filaments. This result indicates that different forms of beta-keratins are produced from low molecular weight precursors or that larger aggregate form during protein preparation. The present study shows that beta-keratin is abundant in the scaled epidermis of tortoise but also in the soft epidermis of pleurodiran and cryptodiran turtles, indicating that this form of hard keratin is constitutively expressed in the epidermis of chelonians.     

Immunological characterization and fine localization of a lizard beta-keratin

Scales of lizards contain beta-keratin of poorly known composition. In the present study, a rat polyclonal serum against a lizard beta-keratin of 14-15 kDa has been produced and the relative protein has been immunolocalized in the epidermis. The observations for the first time show that the isolated protein band derives from the extraction of a protein component of the beta-keratin filaments of lizard epidermis. In immunoblots and immunocytochemistry, the antiserum recognizes most lizard beta-keratins, but produces a variable cross-reactivity with snake beta-keratins, and weak or no reactivity with beta-keratins isolated from tuatara, turtles, alligator and birds. In bidimensional immunoblots of lizard epidermis, three main spots at 15-16 kDa with isoelectric point at 7.0, 7.6 and 8.0, and an unresolved large spot at 29-30 kDa and with pI at 7.5-8.0, are obtained, may be derived from the aggregation of smaller beta-keratin proteins. The ultrastructural immunolocalization with the antibody against lizard beta-keratin shows that only small and large beta-keratin filaments of beta-cells of lizard epidermis are labeled. Keratin bundles in oberhautchen cells are less immunolabeled. Beta-keratin is rapidly polymerized into beta-packets that merge into larger beta-keratin filaments. No labeling is present over other cell organelles or cell layers of lizard epidermis, and is absent in non-epidermal cells. The antiserum recognizes epitope(s) characteristics for lizard beta-keratins, partially recognized in snakes and absent in non-lepidosaurian species. This result indicates that beta-keratins among different reptilian groups posses different immunoreactive regions.