Living amphibians are the only group of Recent tet-rapods possessing so-called pedicellate teeth. There-fore, amphibian dentition attracts considerable atten-tion of morphologists and histologists. The studies onthe structure and development of individual pedicellateteeth of anurans and caudates have shown that the pedi-cellate teeth have a complex structure and consist oftwo calcified dentin elements, the pedicel and thecrown, connected to each other by a nonmineralizeddividing zone [1–4]. The study on the ontogeny of thedental system has revealed that each out of three extantamphibian orders are characterized by complexchanges of dentition until the stable definitive state isreached. Thus, in caudates, three morphological typesof teeth successively replace each other; anurans pos-sess two types distinguished mainly by the presence orabsence of the dividing zone [5–7]. In the order Gym-nophiona, the transformation consists mainly in thechanges of the crown shape of pedicellate teeth [6].The purpose of the present study was to analyze thedevelopment of teeth of different morphological typesin various groups and the formation of the dividingzone, since these aspects of tooth development remainlargely unknown.In addition to the interest in purely morphologicaland comparative evolutionary problems, this task isimportant for gaining an insight into such extensive andcomplex questions as the evolution of the entireamphibian class and the validity of the taxon Lissam-phibia.We examined age series of representatives of thethree extant amphibian orders (seven species of cau-dates, nine anuran and one apodan species). The prepa-rations were produced by staining the material fixed in10% formalin with alcohol solution of alizarin red S, sothat calcified tissue became red.The study on the development of the dental systemfrom the beginning of its formation (at the stages ofhatching in caudates and at the final stages of metamor-phosis or in postmetamorphosis in anurans) hasrevealed that, typically, members of both orders showsuccessive replacement of the nonpedicellate teethcharacteristic of early developmental stages by thepedicellate teeth of the late stages. These tooth genera-tions are distinguished not only by the morphologicalstructure (mainly by the presence or absence of thenonmineralized dividing zone between the crown andthe pedicel), but also by the calcification pattern.The calcification of a young developing nonpedicel-late tooth is initiated at the apical part and extends uni-directionally to the tooth base; subsequently, a toothfuses with the dentigerous bone and achieves the func-tional state. The calcification of pedicellate teeth alsobegins from the crown apex and proceeds proximally.However, this process abruptly stops approximately inthe middle of the height of the future mature tooth; sub-sequently, a second center of calcification is formed onthe external (labial) side of the nonmineralized pedicelproximal to the boundary of the calcified tissue. Inyoung teeth stained with alizarin, the second centerappears as a pink spot extending in parallel to the divid-ing zone formed in the tooth. Subsequently, the calcifi-cation extends from this center to the base and involvesfirst the labial part of the pedicel; then, the lateral part;and, finally, the lingual part. When the calcification ofthe pedicel is completed, the tooth becomes rigidlyattached to the bone and achieves the functional state;only the dividing zone remains nonmineralized.In some cases, in amphibians of either order, thedividing zone is also calcified to a greater or lesserextent. The generation of so-called subpedicellateteeth, distinctive of caudates and characteristic of thelate larval stages immediately before the metamorpho-sis, initially follows the same way of development astrue pedicellate teeth do, i.e., the calcification of thecrown and pedicel begins in two separate centers. How-ever, along with the tooth maturation, the dividing zonealso becomes completely calcified; thus, when thefunctional state is achieved, the zone becomes almostindistinguishable in stained preparations.Complete mineralization of the dividing zone anddevelopment of secondary nonpedicellate teeth werealso observed in anurans. For example, this is typical of Pyxicephalus adspersus, Conraua crassipes (Ranidae)[7], and old functional teeth of all adult anurans. On thecontrary, in some cases, the labial part of the pedicel is
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