QUICK SEARCH:   [advanced] Author: Keyword(s):
Home     Help     Feedback     Subscriptions     Archive     Search     Table of Contents

First published online January 3, 2006
Journal of Experimental Biology 209, 202-226 (2006)
Published by The Company of Biologists 2006
doi: 10.1242/jeb.02007

This Article Summary Figures Only Full Text (PDF) Alert me when this article is cited Alert me if a correction is posted Services Email this article to a friend Similar articles in this journal Similar articles in PubMed Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via HighWire Citing Articles via Google Scholar Google Scholar Articles by Lillywhite, H. B. Search for Related Content PubMed PubMed Citation Articles by Lillywhite, H. B.

Review

Water relations of tetrapod integument

Harvey B. Lillywhite^*

Department of Zoology, University of Florida, Gainesville, FL 32611-8525, USA

^* Author for correspondence (e-mail: hbl{at}zoo.ufl.edu)

Accepted 17 November 2005

	Summary

TOP Summary Introduction General features of vertebrate... Transepidermal water permeation Cellular junctions and the... Structural and secreted barriers Lipids and the evolution... Lipids and the evolution... Plasticity of the water... Conclusion References

 
The vertebrate integument represents an evolutionary compromise between the needs for mechanical protection and those of sensing the environment and regulating the exchange of materials and energy. Fibrous keratins evolved as a means of strengthening the integument while simultaneously providing a structural support for lipids, which comprise the principal barrier to cutaneous water efflux in terrestrial taxa. Whereas lipids are of fundamental importance to water barriers, the efficacy of these barriers depends in many cases on structural features that enhance or maintain the integrity of function. Amphibians are exceptional among tetrapods in having very little keratin and a thin stratum corneum. Thus, effective lipid barriers that are present in some specialized anurans living in xeric habitats are external to the epidermis, whereas lipid barriers of amniotes exist as a lipid-keratin complex within the stratum corneum. Amphibians prevent desiccation of the epidermis and underlying tissues either by evaporating water from a superficial aqueous film, which must be replenished, or by shielding the stratum corneum with superficial lipids. Water barrier function in vertebrates generally appears to be relatively fixed, although various species have `plasticity' to adjust the barrier effectiveness facultatively. While it is clear that both phenotypic plasticity and genetic adaptation can account for covariation between environment and skin resistance to water efflux, studies of the relative importance of these two phenomena are few. Fundamental mechanisms for adjusting the skin water barrier include changes in barrier thickness, composition and physicochemical properties of cutaneous lipids, and/or geometry of the barrier within the epidermis. While cutaneous lipids have been studied extensively in the contexts of disease and cosmetics, relatively little is known about the processes of permeability barrier ontogenesis related to adaptation and environment. Advances in such knowledge have didactic significance for understanding vertebrate evolution as well as practical application to clinical dermatology.

Key words: skin, vertebrate, permeability, lipids, evaporative water loss, phenotypic plasticity

	Introduction

TOP Summary Introduction General features of vertebrate... Transepidermal water permeation Cellular junctions and the... Structural and secreted barriers Lipids and the evolution... Lipids and the evolution... Plasticity of the water... Conclusion References

 
One of the dilemmas in the evolution of multicellular organization was how increasingly larger organisms might continue to sense, interact and exchange with their environment while simultaneously achieving protection from the mechanical, radiative and chemical hazards with which they came into contact. Hence, the integument evolved as a heterogeneous, pluristratified, multimembrane system providing physical protection while simultaneously regulating the exchange of energy and materials between the organism and its surroundings (Chuong et al., 2002). An impressive array of body coverings evolved, with collectively diverse mechanical properties, appendages and multiple diffusion pathways, but with rate-limiting barriers for specific molecules. While integumentary coverings are highly variable in their morphology, they nonetheless exhibit common themes of adaptation. An important aspect of vertebrate evolution was the orchestration of characters that rendered the skin increasingly less permeable to water as forms invaded and adapted to harsher and drier terrestrial environments.

Understanding water relations of vertebrate skin has been advanced by empirical knowledge and by perspectives based on several sources. These include descriptive studies of morphology, physiological studies of specific transport mechanisms and phenomena, physicochemical and physiological studies of integumentary lipids (thought to comprise the principal barrier to transepidermal water movement) and, generally, comparative investigations related to quantitative measures of water flux across the skin of animals adapted to specific environments. Holistic understanding of vertebrate adaptation to terrestrial environments requires considerable appreciation for the integration of characters that determine the water relations of integument per se, as well as the water budget for the whole organism.

	General features of vertebrate integument

TOP Summary Introduction General features of vertebrate... Transepidermal water permeation Cellular junctions and the... Structural and secreted barriers Lipids and the evolution... Lipids and the evolution... Plasticity of the water... Conclusion References

 
The integument is a complex structure comprised of epithelial cells derived from embryonic ectoderm and attached to an underlying fibrous and vascular dermis originating from mesoderm (Fig. 1). Epidermal-dermal interactions are critical for differentiation and specialization of cells. Mitotic activity takes place in the basal layer (stratum germinativum), which proliferates cells that are eventually lost from the animal's surface. All cell types that are present in the epidermis are represented by precursors in the basal layer. Localized cellular proliferation and differentiation produce appendages such as claws, glands, hair or feathers, which together with patterned folds or scales, contribute to integumentary form. Cellular renewal is a further characteristic of vertebrate skin and serves to maintain the integrity of structure and its various functions.

View larger version (49K): [in this window] [in a new window]   Fig. 1. Generalized features of integument in four major clades of vertebrates. and ß indicate alpha- and beta-type keratins, respectively. OG and IG indicate outer and inner epidermal generations that might be present in a squamate reptile prior to skin shedding. The mesos layer of squamates is a specialized cell type derived from keratins and contains extracellular, laminated lipids, comprising the principal water barrier in these species.

Keratin is a prevalent structural feature (Table 1) and is formed in epidermis of all living vertebrates by regulated processes involving synthesis of keratin filaments and cellular death. The synthesis of keratin polypeptides is known from epidermal cells of lampreys 450 million years ago (McLaughlin and Dayhoff, 1969). Subsequent evolution involved variable expression of genes to produce specific keratins and keratinized structures, as well as appropriate protective substances besides keratin. For example, cyclostomes, most osteichthyans, lissamphibians, and many larval or adult amphibians are protected principally by mucus (Maderson and Alibardi, 2000), and thus the body is covered by a largely non-keratinizing epidermis that suffices for aquatic life (e.g. Mittal and Banerjee, 1980). Additional mechanical protection is provided by a cytoskeleton and a terminal web of keratin filaments in superficial cells. During vertebrate evolution, elaboration of the keratinization process allowed adaptation to amphibious and eventually fully terrestrial life. Protection and movement on terrestrial substrates was facilitated by highly resistant cell envelopes encasing stabilized keratin frameworks in superficial cells. The formation of a corneous cell envelope is absent in fishes but occurs in epidermis of adult amphibians and forms in the periderm and first embryonic layers of amniotes, suggesting a primary role for terrestrial survival (Alibardi, 2003). Formation of a stratum corneum over the body surfaces evolved in adult amphibians about 350 million years ago (Matoltsy and Bereiter-Hahn, 1986).

Mucus became associated with the filament matrix and was also discharged to fill the extracellular spaces of the stratum corneum. However, the requirement for an efficient permeability barrier to reduce significantly the exchange of water between the body and environment was met by production of neutral and polar lipids as well as mucus to become components of the cellular matrix and intercellular spaces in differentiating epidermal cells. The participation of lipids to form a competent water barrier likely began in reptiles about 300 million years ago (Matoltsy and Bereiter-Hahn, 1986) and has evolved independently in at least four principal lineages: reptiles, birds, mammals (Maderson, 2003; Maderson and Alibardi, 2000; Menon and Menon, 2000) and amphibians (Lillywhite and Mittal, 1999). The composition of Golgi-derived organelles related to barrier function changed during evolution from mucus and glycoproteins (fishes, amphibians) to glycolipids and lipids (amniotes; see below).

Most functions of the epidermis can be considered protective or defensive in all vertebrates. The majority of these functions reside in the stratum corneum, and of these, the protective function of the water permeability barrier is paramount (Chuong et al., 2002). If mammalian skin is damaged or diseased, cutaneous water loss can increase by several orders of magnitude. The rate-limiting process of water diffusion across the epidermis normally resides in the stratum corneum. Accordingly, many cutaneous phenomena, including immune responses, inflammation and hyperplasia, are recruited directly or secondarily to maintain a competent permeability barrier. Thus, mechanisms that normalize the stratum corneum and competent barrier function can abrogate susceptibility to diseases such as psoriasis, atopic and contact dermatitis, which are triggered, sustained or exacerbated by external perturbations (Chuong et al., 2002).

	Transepidermal water permeation

TOP Summary Introduction General features of vertebrate... Transepidermal water permeation Cellular junctions and the... Structural and secreted barriers Lipids and the evolution... Lipids and the evolution... Plasticity of the water... Conclusion References

 
Fundamentally, the integument of vertebrates consists of a large number of cell membranes organized essentially in stratified series with heterogeneous structure and variable resistances to movement of water molecules in both intracellular and extracellular pathways. While there is good understanding of permeation processes in membranes generally, the complexity and diversity of vertebrate skin greatly complicates a generalized analysis. Transepidermal water loss (TEWL) (and cutaneous water loss, CWL), is a passive diffusion process that is not dependent on cellular metabolic energy (Pinnagoda, 1994; Wilson and Maibach, 1994; Chuong et al., 2002). Therefore, limitations are expected to relate to tractable morphological features. Key questions are: (1) what are the pathways of molecular movement across the skin, and (2) which steps in the permeation process are rate-limiting?

Limitations for water transport through the skin can be related to movement through cell membranes and cytosol of cells, diffusion in the cutaneous matrix between the membranes, and passage of molecules across the membrane/environment interface, neglecting unstirred layers or secreted substances at the skin surface (see Feder and Pinder, 1988). Attributes of integument affecting water movement contribute to resistance of the skin to water passage (R_s), and this property combines with resistance of any external boundary layer (R_bl) to determine the actual rates of TEWL to ambient air in terrestrial animals. Measurements of R_s (in s cm^-1) range from negligible (near zero) in various aquatic or terrestrial amphibians to several hundred in xerophilic arboreal or cocooned frogs, to over a thousand in desert reptiles, with more moderate values (10-300 s cm^-1) being characteristic of birds and mammals (Table 2). Most measurements of boundary layer resistance are near zero to a few s cm^-1 and thus constitute a negligible fraction of the whole-body R_s in most cases.

The ease of water movement through cell membranes can vary by orders of magnitude depending on the composition and physical state of the structure (Finkelstein, 1978; Carruthers and Melchior, 1983). Membranes that are in a liquid-crystalline state are far less permeable than are those that are fluid. In general, the relative diffusivity of molecules through cutaneous membranes will depend on their solubility and partition coefficients, as well as thermal mobility related inversely to molecular mass.

Cutaneous membranes are mosaic structures composed of lipid bilayers in addition to molecular channels or pores. Therefore, the penetration of water molecules into cutaneous cells will depend, in part, on the fractional membrane area that is occupied by channels and the characteristics of the channels (Finkelstein and Cass, 1968; Finkelstein, 1984). Various proteins that serve as membrane channels for specific ions may also facilitate the concomitant flux of water by means of processes that induce solvent drag and by forming a low resistance pathway between the protein and lipid. Solubility-diffusion mechanisms will depend on the degree of packing and thermal mobility of hydrocarbon chains and on the charge of phospholipid polar groups in the bilayer membrane. In addition to diffusion, water flow across skin may be related to concentration differences of impermeant solutes or a differential of hydrostatic pressure. In contrast to diffusion, bulk osmotic or hydrodynamic flow involves the vectorial movement of an assembly of molecules being driven by an imposed potential. Consequently, various permeability coefficients can differ quantitatively because of the physical nature of the water movement pathway (Schafer and Andreoli, 1972; Finkelstein, 1984).

Water appears to permeate lipid bilayers by interaction with lipid polar head groups rather than a mechanism involving solubility of water in hydrocarbons (Carruthers and Melchior, 1983). Driven by the transmembrane gradient of water concentration energy, water then diffuses (exchanges) between the various hydration shells of the polar group into the hydrocarbon core (Hauser and Phillips, 1979). Divalent cations potentially displace water molecules by competing for interaction with the negatively charged phospholipid groups (Hauser et al., 1976).

The number of ion channels in many cell membranes may be relatively too few to provide a significant pathway for water movement, and the bulk of transcellular water movement in cutaneous tissues appears to occur by a solubility-diffusion mechanism involving the lipid bilayer pathway (Finkelstein, 1984). However, aqueous pores do comprise a major route for water transport in certain epithelia including the skin of amphibians (Hevesy et al., 1935; Koefoed-Johnsen and Ussing, 1953). Moreover, if there is osmotic flow of water through a significant number of membrane-spanning channels, water transport is increased greatly because osmotic flux of water occurs by laminar or quasilaminar flow (Mauro, 1957). Water flow can also occur at the lipid/protein interface as well as via channels formed by protein, and thus water permeability may be governed significantly by the presence of membrane-spanning proteins and their interactions with the lipid bilayer. Diffusional movement of water through lipid bilayers is reduced by orders of magnitude when proteins are absent (Carruthers and Melchior, 1983).

	Cellular junctions and the extracellular diffusion pathway

TOP Summary Introduction General features of vertebrate... Transepidermal water permeation Cellular junctions and the... Structural and secreted barriers Lipids and the evolution... Lipids and the evolution... Plasticity of the water... Conclusion References

 
In addition to the cellular route of water movement across integument, water also can move between the lateral, intercellular spaces. Simple epithelia are often categorized according to the relative permeabilities of the intra- and intercellular pathways. So-called `leaky epithelia' are ones in which most diffusion occurs between cells, whereas `tight epithelia' have junctional contacts between cells that impose a high resistance such that most passive diffusion occurs through cell membranes and cytosol. These distinctions may become blurred in consideration of complex, multi-layered barriers such as skin. In the various layers, junctional contacts between cells have various organizations such that cells can adhere, interact and dissipate tensional stresses throughout the tissue.

Intercellular regions of membrane apposition may have junctional features that occlude the intercellular space. The term `tight junction' has been applied loosely to a broad range of such intimate contacts between plasma membranes, although the term was originally introduced to designate the zonula occludens (Farquhar and Palade, 1963). Generally, tight junctions join cells at their apical edges by a continuous belt of fusion with the adjoining plasma membranes. So-called tight epithelia can support large osmotic and ionic gradients and maintain large transepithelial potentials by limiting the diffusion of electrolytes rather than of water (Staehelin, 1974; Madara, 1998).

The sealing elements of tight junctions consist, in part, of diverse fibrils within the membranes. In some tissues the junctional permeability appears related to the number of intramembrane fibers (Claude and Goodenough, 1973), but the packing geometry should be important as well. Sometimes the fibrils are not continuous, and leak pathways might be related to interruptions that occur at more or less regular intervals. Ionic selectivity of junctional zones also suggest the chemical composition of molecules within the junctions are important, as well as the pH of the junction environment. Low pH, for example, weakens intercellular junctions and increases permeation of ions through extracellular spaces (Ferreira and Hill, 1982; Marshall, 1985). The permeability properties of cellular junctions also may depend on the osmotic and hydration status of cells which, in skin, will be determined by the total water barrier properties, their location, and their interaction with blood capillaries and the environment at the skin surface. Changes in cellular volume can alter active transport as well as the structure of intercellular spaces (Erlij and Ussing, 1978). Moreover, the osmotic flow of water within epithelia can induce dilation or collapse of the lateral extracellular spaces, depending on the flow direction, and thereby affect diffusion in a manner that is independent of cellular shrinking or swelling. Such changes in the dimensions of lateral spaces can produce asymmetry of water flow, and diffusion can become rate-limiting as such spaces collapse (Wright et al., 1972).

Tight junctions restrict the movement of both fluids and solutes between cells. While it is recognized that epithelia are selectively permeable, generally more than 90% of transepithelial ionic conductances appear to be localized in the paracellular pathways of leaky epithelia, whereas less than 10% of the total conductance is attributable to the paracellular route of tighter epithelia such as frog skin (Erlij and Martinez-Palomo, 1978). Some investigators believe that tight junctions also are effective in restricting water movement and estimate that hydraulic conductivity of the junctional pathway can account for only 10% of the entire epithelium (Wright et al., 1972). However, the junctional pathway can account for most of the water movement in leaky epithelia (Levitt, 1981).

The relative importance of paracellular vs transcellular pathways to diffusional water movement, and the significance of tight junctions in the overall resistance to water movement across multi-layered integuments, are unclear. There has been extensive use of amphibian skin and endothelial tissues as model systems for the study of membrane permeability, but little is known about the significance of tight junctions in skin from amniote species representing a broad range of requirements and morphologies. Tight junctions have been identified in skin of all classes of vertebrates, although they are considered to be sparse or absent in the skin of mammals (Matoltsy, 1984). Tight junctions joining cellular walls are present in the stratum corneum of adult anurans and possibly play a role in limiting transcutaneous water movement (Farquhar and Palade, 1965). However, these structures do not impede transcellular water flux and appear to be a general feature of anuran integument without variation among amphibian species from mesic and xeric habitats. Insofar as some anurans evaporate water from the skin at rates equivalent to a free water surface (Adolf, 1932; Spotila and Berman, 1976), it seems that tight junctions are not significant components of adaptation of R_s to desiccating environments. Moreover, skin permeability varies greatly among species that all possess these structures.

Thus, in a very broad sense, there is little evidence to suggest that the presence or nature of tight junctions is a significant determinant of the resistance of integument to transepidermal water flux. However, further research will be important to confirm or qualify this generalization. Recent studies implicate claudin-based cellular junctions to be important for barrier function in mammalian epidermis (Furuse et al., 2002). Claudins are integral membrane proteins that mediate cell-to-cell adhesion and are concentrated in the stratum granulosum of mouse skin. Genetic ablation of claudin-1 in mice induces rapid weight loss, increased TEWL, wrinkled skin and neonatal death, presumably attributable to dehydration. The deficient skin exhibits an impaired water barrier, although the organization of the stratum corneum appears to be normal. Genetic studies have demonstrated that absence of cross-linking molecules essential to organization of the cornified cell envelopes also results in a defective phenotype similar to that of claudin-1 deficiency (Matsuki et al., 1998). These studies draw attention to the possible importance of correct organization of cellular junctions in the stratum granulosum and of the cornified cell envelopes in the stratum corneum for permeability barrier function in mammalian skin. However, further investigations are required to understand the proposed as well as alternative, complex, and possibly indirect roles for claudins that might relate to permeability barrier function (Bazzoni and Dejana, 2002).

	Structural and secreted barriers

TOP Summary Introduction General features of vertebrate... Transepidermal water permeation Cellular junctions and the... Structural and secreted barriers Lipids and the evolution... Lipids and the evolution... Plasticity of the water... Conclusion References

 
Structural barriers
During the evolutionary radiation of vertebrates, a variety of factors related to body size, locomotion, endothermy and especially terrestrial life, necessitated structural and protective reinforcement of the skin (Maderson and Alibardi, 2000; Maderson, 2003). On the one hand, terrestrial locomotion by tetrapods required loose connective tissues in the hypodermis and mechanical decoupling of the skin from underlying muscles. Exceptions are found among animals where skin is directly involved in transmission of locomotory forces, so in birds, for example, skin has extensive attachments to the underlying skeleton. On the other hand, fibrous keratins evolved as heterogeneous complexes of proteins containing sulphydryl (SH) and disulphide (SS) linkages of cystine. These provided variable protection from physical elements in the environment and formed the principal constituents of dead horny cells in the superficial layers of the epidermis and in derived hair or feathers (Figs 1, 2). Importantly, keratins provided mechanically resistant but relatively lightweight organic material in comparison with calcified dermal shields that were present in some earlier ancestral lineages (Alibardi, 2003).

View larger version (51K): [in this window] [in a new window]   Fig. 2. Schematic illustrations of the water permeability barrier in relation to the stratum corneum of the epidermis in four principal lineages of vertebrates. The images on the left depict the morphology of generalized integument, and drawings to the right illustrate the stylized arrangement of barrier lipids (dark bars) in relation to horny layers of stratum corneum (thin broken lines). The stratum germinativum is represented by the thick broken lines. The features shown are not to scale.

Various conformations of ß-keratin polypeptides played a principal role in the evolution of strong armament among reptiles and made possible the aerial locomotion of birds by means of stiff feathers. Wide variation in structure and mechanical properties are provided by association of keratins with fibrous globular proteins and by mineralization that involves calcium, usually bonded to phospholipid within the keratin complex. In both turtles and crocodilians, ß-keratin forms thick, mechanically resistant corneous layers and may be mineralized with calcium. Scales in these animals are tough, dry and relatively non-pliable, except in the skin of the neck, limbs, and tail of chelonians where a softer corneous layer contains only -keratin. Calcified structures are virtually impermeable to water, depending on thickness. At the other extreme, keratins of amphibians may form thin, transparent membranes, generally only 1-2 cell layers thick.

Desquamation of corneous cells results from wear and is a gradual and slow process. However, in the scales of lepidosaurs, deposition of ß-keratin alternates with -keratin to form a specialized, pluristratified `shedding complex' that facilitates ecdysis (Maderson, 1984, 1985; Maderson et al., 1998). In both lepidosaurian reptiles and amphibians, periodic cellular proliferation (renewal phases) alternates with periods of inactivity (resting phases) and allows the skin to follow seasonal periods of rapid body growth or to restore skin functions such as gas exchange.

Issues of thickness
In very general terms, the permeability of a fibrous structure correlates with length of the diffusion pathway, or thickness, and where hard and soft tissues occur on the body surface, the important sites of exchange are at the softer sites. However, thickness is not an absolute predictor of permeability because the dimension is not independent of the tissue composition (Lillywhite and Maderson, 1982). The thickness of a diffusion barrier contributes to overall R_s across a structure, so overall thickness, and especially the number of keratinized cell layers in series, might have importance for water relations of skin. In this context, the location of blood capillaries determines the `effective thickness' of skin, so vascularization of skin is an important related property.

Generally, in the majority of amniotes the outermost cutaneous capillaries occur within the dermal layers, sometimes just beneath the epidermis or at the dermis-epidermis boundary. However, capillaries penetrate the epidermis in certain fishes and amphibians where their presence is associated with cutaneous gas exchange (Mittal and Datta Munshi, 1971; Guimond and Hutchison, 1973; Hutchison et al., 1976; Toledo and Jared, 1993). The skin of the pelvic region ('seat patch') of anuran amphibians is especially thin and richly vascularized, features regarded as specializations for water uptake from moist surfaces (Toledo and Jared, 1993). Such pelvic integuments also bear specialized structures, `verrucae hydrophylicae', which are provided with vascular plexa and are sensitive to peptide hormones that influence permeability (Drewes et al., 1977; Hillyard, 1999). There is some evidence that Angiotensin II increases rates of blood flow through the seat patch of anurans (Slivkoff and Warburton, 2001), but observations also demonstrate that mere water exposure of the seat patch in dehydrated toads rapidly induces large increments of blood flow independent from hormonal influence (Viborg and Hillyard, 2005). These specialized features of integument are important in contexts of water gain ('cutaneous drinking'; Hillyard, 1999) involving ventral integument that is normally not exposed to atmospheric conditions. As in other vascular systems, cutaneous blood vessels are no doubt responsive to neuronal as well as endocrine control.

Studies of anurans suggest that overall skin thickness is related to habitat and is important for water balance in some species (for references, see Toledo and Jared, 1993). However, among amphibians as well as vertebrates generally, the thickness of skin per se does not constitute the principal barrier to the diffusion of water. Moreover, the keratinized surfaces of amphibian skin are typically no more than a few cell layers thick, and heavily keratinized integument does not appear to be an adaptive response of amphibian integument.

The periodic production of `cocoons' in certain amphibian taxa is an exception to these statements. These structures impose considerable resistance to water passage (Table 2) and allow burrowing anurans to establish themselves at shallower depths during drought than do species without cocoons (Lee and Mercer, 1967; Ruibal and Hillman, 1981; McClanahan et al., 1983; Withers, 1998). Cocoons consist of multiple superimposed -cell layers of stratum corneum resulting from multiple shedding of skin layers during periods of dormancy in drying soils. The phenomenon is present in the anuran families of Bufonidae, Hylidae, Leptodactylidae and Ranidae, as well as in a few urodeles. A cocoon may consist of some 40-60 layers of cornified cells with secreted lipids and proteinaceous materials sandwiched between them (McClanahan et al., 1976; Ruibal and Hillman, 1981; Withers, 1995a; Christian and Parry, 1997).

The presence of osteoderms or `co-ossified' regions in skin where bone tissue occurs in the dermis is potentially significant for regional enhancement of R_s, and this subject has been given limited attention principally in amphibians (Seibert et al., 1974; Ruibal and Shoemaker, 1984; De Andrade and Abe, 1997; Navas et al., 2002; Jared et al., 2005). The integument of co-ossified regions of skin contains collagen fibres with reduced presence of blood vessels and mucous glands. Co-ossified head regions provide mechanical protection from predators and are used to seal off entries to refugia in plants where frogs seclude themselves (Duellmann and Trueb, 1986). Thickened or mineralized structures in the skin of various terrestrial amniotes no doubt increase regional R_s of the skin (Seibert et al., 1974), but few studies of regional differences in TEWL have quantified such contributions.

Water permeation in keratins
How do the structural features of keratin influence its resistance to water movement? Generally, structural features that alter the free volume (equivalent to pores or channels) should alter the permeation of water molecules accordingly. Resistance to diffusion is affected by the molecular mass of side chains and tends to increase with cross-linking beyond certain critical levels (Lieberman et al., 1972). However, proteins with bulky, globular side chains may inhibit close packing of molecules and thereby diminish the resistance of a complex membrane. Proteins with generally smaller and non-polar amino acids are able to pack more closely together, thereby permitting formation of many van der Waals forces. The stability of cross-linkages is dependent on a large number of intermolecular forces, including covalent, ionic, and hydrogen bonding in addition to van der Waals attractive forces between non-polar amino acid side chains. All of these act to influence the mobility and free volumes of the structure.

Water itself influences the molecular structure of fibrous protein polymers, and the hydrated status of the skin is an important property. Proteins, in general, bind water very strongly at low relative humidities, and the water content increases in proportion to humidity exposure. As water content increases, it enters between protein molecules and thereby increases the mobility of side chains and the distance between them, potentially reducing the degree of crystallinity. Thus, introduction of water molecules into the polymer structure increases the available free volume as well as the mobility of cross-linkage groups. Dehydration reduces permeability not only by reversing these effects but also by promoting non-covalent bondings between protein chains (Vincent and Hillerton, 1979). Consequently, the permeability of dry protein films can be extremely low (Lieberman et al., 1972), presumably enhancing water resistance in comparatively dry tissue.

Recently it was shown that the `natural' hydration level of human stratum corneum in vivo is about 30-50% of dry mass (Caspers et al., 2001). When the stratum corneum is equilibrated over water, its mass increases to 300-400% of dry mass. At low hydration levels the stratum corneum is relatively brittle and fragile, whereas when water levels exceed a value of around 10-15% of dry mass, the tissue softens markedly. Hydration of the stratum corneum enhances the flux of hydrophilic as well as lipophilic substances (Bouwstra et al., 2003a).

Models of cutaneous water movement are subject to uncertainties related to the phase state of water moving through epidermal tissues and the potential effects of hydration and temperature (Scheuplein and Blank, 1971; Mautz, 1982; Marder and Ben-Asher, 1983). Webster et al. (1985) properly note that if liquid water moves into the superficial layers of the skin, water in the vapor phase might diffuse across a shorter pathway and, hence, reduced resistance. Studies of human skin have indeed demonstrated that gradients of water exist in the stratum corneum (Warner et al., 1988; Bommannan et al., 1990; Caspers et al., 2001; Bouwstra et al., 2003a). Fourier transform infrared spectroscopy has demonstrated that free water content in stratum corneum is greater in central regions relative to superficial and deeper cell layers at moderate levels of hydration (57%-87%, w/w), whereas at higher levels of hydration (300% w/w) water swells corneocytes in a direction perpendicular to the skin surface except for the deepest cell layers adjacent to the viable epidermis (Bouwstra et al., 2003a). While the mechanism excluding free water from the deeper cell layers of stratum corneum is not understood, it is speculated to play a role in preventing dehydration of the viable epidermis. In relatively dry conditions (18%-26% w/w), only bound water is present in the stratum corneum (Bulgin and Vinson, 1967; Hansen and Yellin, 1972; Bouwstra et al., 2003a).

Extracellular matrices and organelles
Certain extracellular matrices and organelles have been hypothesized to reduce water exchange across the integument, notably in amphibians. Calcium salts and a hydrophilous, amorphous `ground substance' are present in the stratum spongiosum of many amphibian species (Elkan, 1968; Moss, 1972). The so-called ground substance of the calcified dermal layer consists of a polysaccharide gel having glycosaminoglycans usually bonded covalently with proteins. The distribution of this layer among species exhibits little correlation with environment or susceptibility to dehydration, although the layer is generally more developed in dorsal than ventral skin. This layer was suggested to function in water conservation (Elkan, 1968), but the position of the layer and its mere hydrophilic property would appear to render it ineffective (Drewes et al., 1977). Other possible functions, such as a reservoir for mineral homeostasis (Moss, 1972), seem more plausible than a significant role related to water permeability.

Pigmented effector cells that impart color and capacity for physiological color change in vertebrates, have been suggested to influence R_s of amphibian skin. Chromatophore layers, mostly involving silvery iridophores, vary seasonally and appear to correlate with reduced rates of TEWL in some species of frogs exposed to dry conditions (Drewes et al., 1977; Withers et al., 1982; Kobelt and Linsenmair, 1986). However, these frogs remain exposed to sunlight during hot, dry conditions, and the iridophores likely function to increase reflectance of radiation (Kobelt and Linsenmair, 1986). Therefore, the role of iridophores as a causal mechanism for increasing resistance to TEWL is not conclusive. Moreover, the iridophore units usually have gaps between them, and they are overlain by living cells, so they cannot provide complete protection from dehydration of epidermis. Both pigments and structural colors in scales of reptiles, avian feathers and mammalian pelage potentially influence TEWL indirectly by modifying the reflectance and thermal properties of skin.

Secretions and secreted barriers
Fluid secretions can be important to the water relations of skin in a variety of vertebrates, particularly amphibians that lack a fibrous or mineralized covering of significant thickness. The skin of amphibians is glandular and produces three principal categories of secretions: mucus, various toxins, and lipids. A variety of toxic substances - largely alkaloids, peptides and amines - are usually secreted only during defensive interactions with other animals and are not considered further here (see Erspamer, 1994). Lipids are discussed in some detail in the next section. Mucous secretions are predominant and copious in many amphibian species, where they may form a virtually constant film overlying the outer skin layers. These secretions are largely water with varying amounts of proteoglycans and glycoproteins (glycoconjugates), various ions, and often lesser quantities of sugars, amino acids and lipids (Dapson, 1970).

Mucus plays multiple roles in the biology of integument and is especially effective in contexts related to lubrication and keeping the skin hydrated and moist (Lillywhite, 1971, 1975; Mittal and Bannerjee, 1980; Whitear, 1986; Lillywhite et al., 1998). While mucus has been conjectured to limit water movement where it is present in the extracellular spaces of the stratum corneum (Toledo and Jared, 1993), there is no demonstration that this is actually the case. Similarly, externally adhering mucus has been conjectured to reduce evaporative water loss from the skin surfaces (Wygoda, 1988) and to seal small gaps between the body and limbs of frogs (Geise and Linsenmair, 1986; Kobelt and Linsenmair, 1986). In these studies the composition of `mucus' was not determined, so the lipid content is not known. Although mucus is hygroscopic, biophysical studies have shown it is not particularly impermeable, even when air-dried (Machin, 1966, 1972). Further, it was shown by direct measurements in vivo that intact mucus covering over the skin of Litoria dahlia provided no extra resistance to TEWL (Young et al., 2005). While quantitative comparisons are not available, it seems strikingly clear that any resistance to transepidermal water loss attributable to mucus is miniscule compared with that for lipid secretions (see below).

In terrestrial amphibians, secretion of mucus transfers water to evaporating surfaces that are sculptured to retain the fluid (Lillywhite, 1971). In bullfrogs and several other species of anurans, the rate of mucus secretion is regulated to keep up with increasing evaporative demands related to heliothermy, and thus water evaporates from a regularly replenished mucous film rather than the underlying epidermis (Lillywhite, 1971; Lillywhite and Licht, 1975; Kaul and Shoemaker, 1989; Lillywhite et al., 1998). If frogs are deprived of the external mucus film, the skin dries and is unable to maintain normal levels of evaporative water loss (Lillywhite, 1975). In contrast, anurans without a mucus film (e.g. bufonids) either avoid dehydrating conditions or, in the case of some heliothermic toads, rely on water that is transferred from moist substrates to wet the skin via capillary forces that `wick' the liquid across a highly sculptured integument (Lillywhite and Licht, 1974). Whether the external film overlying the epidermis is mucus or water, the aqueous evaporating film must be replenished by water that is either stored within the animal or is absorbed from a moist substrate. Thus, a mucus film cannot be utilized as a strategy for maintaining a hydrated skin during exposure without water in xeric habitats or during long-term drought.

The importance of mucous secretions in protecting exposed epidermal surfaces from dehydration suggests a fundamental dichotomy of skin organization and water balance (Lillywhite and Maderson, 1988). With few exceptions, either the epidermis is protected from excessive water loss by a lipid and/or fibrous diffusion barrier (some amphibians, reptiles, birds, mammals) (Fig. 2), or the epidermis is covered with a wet film so that evaporation occurs from secreted fluids rather than the epidermis itself (many amphibians). If the epidermis or whole skin dries excessively, its viability diminishes as the dehydrating cell layers compress and stiffen (Lillywhite, 1975). Superficial water films associated with sculptured skin surfaces (channels that act like `blotting paper') appear to have an important role in protecting skin from dehydration in certain snakes (Lillywhite and SanMartino, 1993) and elephants (Lillywhite and Stein, 1987) as well as amphibians (Lillywhite and Licht, 1974).

	Lipids and the evolution of cutaneous permeability barriers

TOP Summary Introduction General features of vertebrate... Transepidermal water permeation Cellular junctions and the... Structural and secreted barriers Lipids and the evolution... Lipids and the evolution... Plasticity of the water... Conclusion References

 
The role of lipids in controlling transepidermal water loss is well established and has evolved numerous times during tetrapod evolution. Moreover, lipids are employed almost universally as a means of waterproofing the skin or body surfaces of terrestrial organisms, including plants, arthropods, some amphibians, reptiles, birds and mammals (Hadley, 1989, 1991). Thus, conferral of resistance to TEWL is fundamentally a matter of molecular rather than mechanical organization (biochemistry vs morphology), although these two attributes are intimately interconnected. Indeed, the efficacy of a lipid barrier depends in many cases on structural features that enhance or maintain its integrity and function (Table 1; Figs 1, 2). Understanding the significance and variation in permeability barriers requires first an appreciation for key features related to functional organization and structure of vertebrate integument.

The structural features of vertebrate integument are uniquely different from all other major phyla of animals. Clearly, mechanical strength is enhanced by a layered keratin structure, and the ß keratins provide superior strength and rigidity. Importantly, the evolution in basal amniotes of a stratified squamous stratum corneum produced a tough yet flexible epidermis across the body surfaces (Maderson and Alibardi, 2000). Such a stratified corneum conferred an additional important advantage, which is a convenient means to preserve the structural integrity of laminated lipids that might function to impede the transcutaneous efflux of essential body water (Figs 2, 3). The corneous layers provide a framework and sufficiently rigid support for stability of lipid structure without undue movement or mechanical disruption (see below).

View larger version (175K): [in this window] [in a new window]   Fig. 3. Electron micrographs showing details of stratum corneum and permeability barrier of terrestrial vertebrates. (A) Section through a portion of cocoon of a burrowing hylid frog, Pternohyla fodiens. The layers of squamous epidermal cells are separated by granular extracellular materials in the subcorneal spaces. Scale bar, 500 nm. Reproduced with permission (Ruibal and Hillman, 1981). (B) Section through mesos layer of snake epidermis (Natrix natrix), which is the recognized permeability barrier of squamates. Laminated lipids occur between the darker bands of keratin layers. Scale bar, 100 nm. Courtesy of Lukas Landmann. (C) Section through stratum corneum of human skin. Lipids (unstained) occur between the distinct layers of keratin. Scale bar, 200 nm. Courtesy of Gopi Menon. (D) Section through epidermis of a canary, showing nucleated layers as well as stratum corneum (top). Lipids occur between the distinct layers of keratin toward top of figure. Note the multigranular bodies (source of lipids; arrows). Scale bar, 200 nm. Courtesy of Gopi Menon.

Permeability barriers always contain a complex mixture of lipid molecules. Longer chain-length hydrocarbons tend to comprise a dominant category of lipids in most barriers examined. These tend to melt at higher temperatures and resist water permeation, whereas shorter chain-length molecules reduce the intensity of van der Waals interactions between hydrocarbon molecules and create a more fluid and permeable structure. Relative saturation of hydrocarbons also contributes to a tighter water barrier, whereas unsaturation and methyl branching tend to introduce kinks in molecules and disrupt packing. However, chain length alone is not necessarily a reliable indicator of water permeation because in some systems chain elongation and unsaturation offset each other (Gibbs et al., 1998). Hydrocarbons and wax esters are relatively non-polar, which assists in repelling water. Polar phospholipids and other classes of lipids having intermediate polarity, in addition to branching, might be important in structuring the geometry of a water barrier and providing a degree or specific orientation of fluidity important with respect to potential mechanical distortion or disruption of the barrier structure (Bouwstra et al., 2000, 2003b). These and other properties of lipids might also play roles that are important in barrier assembly, prevention of degradation by enzymes or microorganisms, thermal properties relevant to thermoregulation, and interactions with non-lipid molecules.

Normal stratum corneum, as studied in mice and humans, demonstrates a markedly acidic pH, ranging from 4.5 to 5.5 at the surface to physiologic pH (7.4) in hydrated, viable epidermis (Ohman and Vahlquist, 1994; Turner et al., 1998; Fluhr and Elias, 2002). The acidic pH is attributable to influence of key metabolites including urocanic acid, free fatty acids, and a non-energy dependent sodium-proton exchanger (Chuong et al., 2002). The acidic pH appears to regulate several key defensive functions of skin, including antimicrobial and permeability barrier properties, as well as integrity and cohesion of the stratum corneum. The stability of molecular structures is influenced importantly by pH, which also alters the water content of fibrous structures because bonding between chains are replaced by bonding between protein and water (Hackman, 1984). With respect to the permeability barrier, at least two key lipid processing enzymes affecting the barrier lipids within the interstices of stratum corneum are activated at low pH optima and are retarded by exposure to neutral buffers (Uchida et al., 2002; Schmuth et al., 2000). Moreover, the acidic pH also is important for direct influence of lipid-lipid interactions in the lamellar bilayers of the permeability barrier (Bouwstra et al., 1999). Hence, stratum corneum neutralization reduces competence of the permeability barrier lipids (Mauro et al., 1998; Hachem et al., 2003).

Lipid barriers of amphibians
The Amphibia present features, both in evolutionary history and specializations of extant forms, which are transitional between aquatic and terrestrial environments. Numerous species exhibit complex life histories with aquatic larval stages prior to acquisition of terrestrial adult characters, and the adults of extant taxa possess skin that is generally devoid of thick, rigid or heavily keratinized protective armor. Amphibians have retained integument that, in terrestrial as well as aquatic adults, is relatively thin and pliant - lacking extensive development of keratin and retaining permeability properties that allow significant gas exchange across the cutaneous surfaces. While only a small sample of some 4200 amphibian species have been examined in detail, it seems clear that many species of amphibians possess skin of characteristically high permeability and experience relatively high rates of TEWL.

Comparative investigations indicate that arboreal species of frogs tend to have generally higher R_s than do non-arboreal species (Table 2; see Withers et al., 1984; Wygoda, 1984; Young et al., 2005). Selection for increased R_s in arboreal habitats is no doubt related to exposure of animals to increased levels of radiation, temperature and convection relative to ground-dwelling, fossorial or amphibious relatives (e.g., McClanahan and Shoemaker, 1987). Various mechanisms have been suggested to play a role as determinants of R_s in amphibians, and these have been reviewed previously in attempt to evaluate the relative contributions of characters to the overall R_s (Toledo and Jared, 1993; Lillywhite and Mittal, 1999). As in other tetrapods, lipids appear to be of central importance to comparatively high R_s that has been reported for selected species (Table 2).

The role of cutaneous lipids in water economy is clear in some species, while problematic or elusive in others. Lipids confer exceptionally high resistance in certain tree frogs, which secrete lipids from cutaneous glands to form an external film that is subsequently wiped with complex and stereotyped movements involving all four limbs (Shoemaker et al., 1972). However, lipids that are located within the skin may or may not correlate with R_s (Withers et al., 1984; Toledo and Jared, 1993). Also, lipid mixtures that are produced by general extractions of whole skin undoubtedly include elements of membrane lipids not associated with a water barrier as well as precursor molecules that might be converted to other components if a barrier is present. Lipids that are structured within the dermis are purported to reduce TEWL (Amey and Grigg, 1995), but these cannot act to prevent dehydration of the overlying epidermis. Thus, the more effective lipid barriers among amphibians are those that create a barrier to TEWL at the skin surfaces (Table 1; Fig. 2).

Elaborate wiping of lipids on body surfaces was first described in phyllomedusine frogs, which exhibit very low rates of TEWL (Blaylock et al., 1976). The behavior is associated with a suite of behavioral and physiological characters, including selection of a permanent perch where frogs remain inactive during the day, secretion of lipids from cutaneous glands, wiping behavior, and the assumption of a condition resembling torpor. The secreted lipids are produced in specialized cutaneous glands and are a mixture comprising mostly wax esters, triglycerides, free fatty acids, hydrocarbons and cholesterol (McClanahan et al., 1978). Wax esters are dominant and average about 46 carbons in length. The externally wiped layer is estimated to be about 0.2 µm and 50-100 molecules thick, which is comparable to the epicuticular wax layers of various arthropods. This lipid barrier results in a R_s that is much greater than that demonstrated in typically amphibious anurans (Table 2) and enables frogs to remain exposed to sunlight in hot, dry weather where body temperatures approaching 40°C are tolerated (Shoemaker et al., 1987). The conservation of body water achieved by the high R_s of the waxy layer is complemented by excretion of uric acid, which also conserves water potentially involved in the excretion of nitrogenous wastes (Shoemaker et al., 1972; Shoemaker and Bickler, 1979).

Wiping behavior and secretion of lipids from cutaneous glands have been reported in several species of anurans having variable R_s (generally from about one to several 100 s cm^-1; Table 2). It seems likely that wiping behavior is more widespread among anurans than formerly supposed, and that components or precursors to the full behavior might have evolved in a number of different contexts (Blaylock et al., 1976; Lillywhite et al., 1997a; Barbeau and Lillywhite, 2005). Wiping behaviors observed in a rhacophorid tree frog, Polypedates maculatus, stimulate secretion of lipids from cutaneous mucous glands, which are activated by a tactile neurogenic reflex (Lillywhite et al., 1997a). The lipids are secreted with mucus, and these frogs have a relatively modest R_s (Lillywhite et al., 1997a,b). Both wiping complexity and R_s are variable among six species of hylid tree frogs in Florida (Barbeau and Lillywhite, 2005). The lipids appear to be produced in granular rather than mucous glands and, like Polypedates, these frogs are not very waterproof. In all the examples of anurans investigated, elaborate wiping of secreted lipids is associated with arboreal species living in arid, semiarid, or ephemerally arid environments where there is potential for dehydration stress.

The water barrier in amphibian skin is very different from that of amniotes for two fundamental reasons. First, lamellar granules have not been definitively identified in any amphibian, although structures bearing resemblance to these organelles ('small dense granules' and `tightly packed parallel lamellae') were reportedly seen in the stratum spinosum of Hyla arborea (Bani et al., 1985). These structures were possibly misinterpreted, as lamellar granules appear to be uniquely associated with keratinizing epithelia and are not generally recognized in the epidermis of amphibians or fish (Wertz, 1996, 2000; Alibardi, 2003). Secondly, the corneous layers of amphibian epidermis are too sparse to provide an effectively structured lipid-keratin complex, and lipid structures with complex lamellation have not been identified in association with interstices in the thin stratum corneum of any amphibian species. Hence, lipid layers comprising part of the tela subcutanea have been described in several species of arboreal frogs, but these lipids underlie blood vessels and the frogs are not particularly resistant to cutaneous water loss (Wygoda et al., 1987). Similarly, a lipid band has been demonstrated histochemically in the uppermost aspect of the stratum spongiosum of the arboreal frog Litoria fallax (Amey and Grigg, 1995). These lipids appear to be derived from congealed lipid droplets, but there is no reported evidence for structured lamination or mechanical support associated with adjacent cell layers or other epidermal structures. This lipid layer possibly contributes to reduction of evaporative water losses in this species, but the reported rates of TEWL are not exceptionally low.

The limited keratinization of the epidermis of modern amphibians imposes a critical constraint, due possibly to developmental canalization related to aquatic life stages (Lillywhite and Mittal, 1999). Although keratin was presumably present in basal amphibians (Findlay, 1968; Maderson, 1972), neither extensive keratinization nor synthesis of ß-type keratins characterizes the skin of modern amphibian lineages. The capacity for extensive synthesis of keratin is present in connection with a few specialized structures such as the cornified protrusions (spade) used in digging by fossorial anurans, so the generalized condition of the skin may be more related to a lack of genetic expression rather than gene deficiencies.

Amphibians thus differ from amniotes insofar as layered complexes of lipid and keratin are absent (Table 1; Figs 1,2). One possible exception might be the laminated structure characteristic of `cocoons' that occur in various species during dormancy of estivation (Fig. 3A). In the Australian frog Cyclorana auastralis, the composition of both skin secretions and cocoon material was shown to consist of 5-10% neutral lipids and 78-85% proteinaceous material (Christian and Parry, 1997). The lipid fraction of these materials was chemically similar to the secreted lipids that provide an exernal water barrier in phyllomedusine frogs (McClanahan et al., 1978), but it is not clear whether these were extracted from the cell layers of the cocoon or were derived from the interspersed `mucus.' Further investigations are required to examine the possibility that lipids are secreted in mucus (as in Polypedates maculatus: Lillywhite et al., 1997a,b) to provide a layered lipid-keratin complex in amphibian cocoons.

In the case of both secreted cocoons and the extraepidermal lipid layers that are secreted and wiped by arboreal frogs such as Phyllomedusa or Polypedates, subsequent function depends on immobility of the animal for otherwise the structural integrity of the lipid barrier is disturbed. Thus, amphibians produce cocoons when they are in soil and in a state of torpor, while wiping of lipids by tree frogs occurs characteristically prior to resting in a water-conserving posture while either in seclusion or on perches. In other systems, lipid water barriers occur either on external surfaces of rigid structures (as in plants, feathers and arthropod cuticle) or are contained in layered arrays within corneous tissues (as in reptiles, mammals and birds). With reference to the integument of amniotes, the corneous structure that contains barrier lipids is either comparatively rigid (scales) or somewhat supple (mammalian skin) while resilient to creasing. Importantly, the numerous layers of specialized corneocytes associated with the water barrier region of the stratum corneum of amniotes provide a tough and resilient framework for the intercellular lamellar lipids. On the other hand, the more delicate, pliant nature of amphibian integument and its limited keratinization appear to have constrained the possible evolutionary pathways for waterproofing mechanisms in amphibians (Lillywhite and Mittal, 1999). Due to the limitation of keratinization, in particular, external lipid barriers seem to provide the more effective and practical potential means of waterproofing in amphibians (Fig. 2).

Studies of `waterproof' frogs have demonstrated that reduction of skin permeability by means of lipids to prevent dehydration also reduces cutaneous gas exchange, which normally contributes importantly to respiration in amphibians (Feder and Burggren, 1985). Thus, under these circumstances of periodic waterproofing, frogs rely increasingly on pulmonary ventilation to maintain arterial blood pH and levels of respiratory gases (Stinner and Shoemaker, 1987). Increased use of the lung also is characteristic in circumstances such as increased temperature or activity when the metabolic demand for oxygen exceeds the passive uptake across the skin (Hutchison et al., 1968). A priori, there seems no compelling reason why amphibians could not have evolved more effective lungs and used them more dominantly in gas exchange, similar to reptiles. However, this has not been a directional trend in amphibian evolution, and some have argued that reliance on cutaneous gas exchange is the explanation for retention of a generally permeable integument with minimal keratinization in the stratum corneum. Thus, a permeable and pliant integument might be characteristic of modern amphibians either because these attributes are important for aquatic larval stages, and the integument of metamorphosed adults is genetically constrained, or the conditions are maintained by natural selection in the adult as well as larval stages of development. Either of these possibilities, of course, does not exclude the other (Lillywhite and Mittal, 1999).

	Lipids and the evolution of cutaneous water barriers in terrestrial amniotes