Skull development in the Iberian newt, Pleurodeles waltl (Salamandridae: Caudata: Amphibia): timing, sequence, variations, and thyroid hormone mediation of bone appearance.

The cranial ossification sequence in Pleurodeles waltl is widely used in phylogenetic analyses of amphibian origin and evolution. However, the patterns published to date are far from completely resolved and contain certain discrepancies. Based on a large sample of P. waltl specimens ranging from early post-hatching larvae to post-metamorphic newts, we determined the most common cranial ossification sequence and revealed its intraspecific variations. Since thyroid hormones (THs) are involved in the mediation of skull development in salamanders, we studied the role of THs in the cranial development of P. waltl. The normal sequence and timing of bone appearance were compared with those in larvae reared under conditions of high (in 1 and 2 ng mL-1 triiodothyronine) and low [in 0.02% thiourea (TU), which inhibits thyroid gland activity] TH levels. Metamorphosis was greatly accelerated in the TH-treated larvae and was arrested in the TU-treated larvae, which retained the larval pattern of the palate and rudimentary external gills even after 2 years of the experiment. Early-appearing bones (the coronoid, vomer, palatine, dentary, squamosal, premaxilla, parasphenoid, pterygoid, prearticular, vomer, frontal, parietal, exoccipital, in this order) arise at the same stages and ages, and follow the same ossification sequence under different TH levels. The timing of the appearance of bones normally arising in the late larval and metamorphic periods (the quadratojugal, orbitosphenoid, prootic, maxilla, nasal, os thyroideum, prefrontal, quadrate, in this order) changes depending on the TH level. The maxilla and nasal display the most pronounced reaction to changes in the TH level: they appear precociously in TH-treated animals, while their appearance is postponed and they remain rudimentary in TU-treated animals. Because of different responses to THs, the order in which late-arising bones appear changes depending on the TH level. Although bones appearing early in larval ontogeny (e.g. the premaxilla, vomer, squamosal, palatine) display no TH-induced reaction when they start to develop, their further differentiation shows dependence on THs, and these bones become TH-inducible closer to metamorphosis. These findings indicate that TH involvement in the mediation of cranial development changes from minimal (if at all) in its early stages to maximal during metamorphosis. It is likely that the appearance of bones early in development is mediated by factors other than THs. Their further development is accompanied by changes in the mechanisms mediating their morphological differentiation. That is, likely non-hormonal mediation becomes replaced or/and complemented by hormonal mediation. The constituent parts of the same bone may exhibit differences in their reactions to changes in TH levels. Although in normal development, the overall cranial ossification sequence is constant, there was variation in the order in which late-appearing bones was recorded. These observations suggest that this variation results from individual variability in the internal TH level. Comparison with other salamanders suggests that (a) the pattern of TH mediation described in P. waltl is common for cranial development of metamorphosing urodeles and (b) the same bone may differ in its TH dependence in different salamanders, e.g. there are interspecific variations in the degree of TH dependence of individual cranial bones.

Allium pallasii and A. caricifolium-Surprisingly Diverse Old Steppe Species, Showing a Clear Geographical Barrier in the Area of Lake Zaysan.

Polymorph Allium pallasii s.l. from monotypic A. sect. Pallasia was studied using a wide spectrum of methods and divided into two clearly morphologically, geographically, cytologically and genetically isolated species: A. pallasii s. str.-North-East Kazakhstan, Western Siberia, and the Altai Mountains; A. caricifolium-Kyrgyzstan, Northwest China, South-East Kazakhstan until Zaysan Lake in the east. Despite serious genetic differences, both species are sisters and are related to species of the A. sect. Codonoprasum (Subg. Allium). Allium caricifolium differs from A. pallasii s. str. by taller stems, dense inflorescence, and with filaments longer than perianth. The possible phylogenetic reasons for the separation of these species are discussed. A nomenclature analysis of synonyms was carried out.

Frontoparietal Bone in Extinct Palaeobatrachidae (Anura): Its Variation and Taxonomic Value.

Palaeobatrachidae are extinct frogs from Europe closely related to the Gondwanan Pipidae, which includes Xenopus. Their frontoparietal is a distinctive skeletal element which has served as a basis for establishing the genus Albionbatrachus. Because little was known about developmental and individual variation of the frontoparietal, and its usefulness in delimiting genera and species has sometimes been doubted, we investigate its structure in Palaeobatrachus and Albionbatrachus by means of X-ray high resolution computer tomography (micro-CT). To infer the scope of variation present in the fossil specimens, we also examined developmental and interspecific variation in extant Xenopus. In adults of extinct taxa, the internal structure of the frontoparietal bone consists of a superficial and a basal layer of compact bone, with a middle layer of cancellous bone between them, much as in early amphibians. In Albionbatrachus, the layer of cancellous bone, consisting of small and large cavities, was connected with the dorsal, sculptured surface of the bone by a system of narrow canals; in Palaeobatrachus, the layer of cancellous bone and the canals connecting this layer with the dorsal surface of the frontoparietal were reduced. The situation in Palaeobatrachus robustus from the lower Miocene of France is intermediate-while external features support assignment to Palaeobatrachus, the inner structure is similar to that in Albionbatrachus. It may be hypothesized that sculptured frontoparietals with a well-developed layer of cancellous (i.e., vascularized) bone may indicate adaptation to a more terrestrial way of life, whereas a reduced cancellous layer might indicate a permanent water dweller.