The otic region of Doleserpeton (Temnospondyli) and its implications for the evolutionary origin of frogs

There is increasing evidence that the Palaeozoic temnospondyl amphibians had a frog‐like tympanic hearing system. For this reason, the otic region of Doleserpeton is described and compared with modern anurans. The otic capsules are expanded laterally and ventrally relative to other temnospondyls. The opisthotic has a bulbous ventral region resembling the ventrolateral ledge in modern frogs. Two lateral processes are located on the paroccipital process. Comparison with the condition in modern anurans with a tympanic hearing system shows that this may have been the attachment site for the tympanic annulus. Parts of the osseous labyrinth are also described. The inner ear shows numerous features resembling the condition found in frogs. These include strong evidence for the presence of a lissamphibian‐type perilymphatic duct most closely resembling that of anurans. This is the first time such a perilymphatic system has been described in any Palaezoic form. The posterior part of the braincase shows a jugular foramen closely associated with the perilymphatic foramen, as in anurans. Although the distribution of these traits among other temnospondyl groups remains little known, the sum of the evidence points to affinities between anurans and temnospondyls, and adds to the evidence for a close relationship between anurans and the Permian amphibamid Doleserpeton. © 2008 The Linnean Society of London, Zoological Journal of the Linnean Society, 2008, 154 , 738–751.     

Discrepancy in laboratory and field attraction of apple fruit moth Argyresthia conjugella to host plant volatiles

Abstract.  Apple fruit moth Argyresthia conjugella is a specialist seed predator of rowan Sorbus aucuparia . Large-scale synchronous fluctuation of seed production in rowan (i.e. named masting) drives the apple fruit moth to seek alternative host plants such as apple, during years when rowan berries are not available for oviposition. The role of plant volatile compounds in the attraction of gravid apple fruit moth females is studied in a laboratory wind tunnel. Volatiles from rowan branches with green berries stimulate female moths to fly upwind and to land at the odour source. By contrast, females are not attracted to rowan branches without green berries, and they are not attracted to apple, demonstrating that the chemical stimulus from rowan berries is required for attraction. Attraction to synthetic compounds identified from rowan, anethole and 2-phenyl ethanol confirms the role of plant volatiles in host finding. These two compounds, however, show a discrepant behavioural effect in wind tunnel and field tests. Field traps baited with 2-phenyl ethanol capture female moths but anethole does not produce significant captures. Wind tunnel tests produce the opposite results: moths fly upwind towards the anethole lure, whereas 2-phenyl ethanol is not attractive at all. Wind tunnel attraction to 2-phenyl ethanol is achieved by adding odour from a rowan branch without berries, which is not attractive on its own. This finding demonstrates that interaction with the background odour contributes to the behavioural effect of plant volatile stimuli in the field.     

Spontaneous All-or-Nothing Action Potentials in the Ciliate Bursaridium difficile

The electrical membrane properties and the swimming behaviour of the freshwater ciliate Bursaridium difficile were studied by current clamp recordings and video analysis. The resting membrane potential was –45 ± 6 mV (mean ± SD, n = 80), and the input resistance and membrane capacitance were 109 ± 42 megaohms (MΩ) (n = 63) and 457 ± 150 picofarads (pF) (n = 42), respectively. Based on an estimated surface area of 6.8 × 10^-4 cm², the corresponding specific membrane resistance and capacitance are 7.4 × 10⁴Ω× cm² and 0.7 μF/cm². Bursaridium difficile generates spontaneous, all-or-nothing action potentials with a well-defined threshold in normal medium. The spontaneous firing frequency was 0.22 ± 0.06 Hz (n = 80). The maximum rate of rise of the action potentials was less than 1 V/s, and they displayed a prolonged plateau phase (0.5–1 s). The action potentials were abolished in nominal Ca²⁺-free solution and are thus Ca²⁺-spikes. The swimming pattern of Bursaridium in homogeneous surroundings is composed of forward swimming periods interrupted by regular, short periods of backward swimming followed by a change in the forward swimming direction. The turning frequency corresponded to the spontaneous firing frequency, and only forward swimming was observed in nominal Ca²⁺-free solution. The periods of backward swimming activity are thus linked to the spontaneous action potentials.     

Multiphasic Uptake of Amino Acids by Barley Roots

Concentration-dependence and other characteristics of uptake of ³H-labeled l -lysine, l -methionine and l -proline by excised roots of barley (Hordeum vulgare L.) were studied. Use of relatively short uptake and wash periods and low solute concentrations ensured good estimates of influx across the plasmalemma. Uptake in the range of 10^?7M– 6.3 × 10^?3M can be precisely represented by four or five phases of single, multiphasic mechanisms. The mechanisms appear to be relatively specific as judged from the competition by unlabeled analogues. Structural requirements for interaction of a compound with the uptake site for methionine are given, as are the effects of analogues on the phase pattern for this amino acid. There is no indication of separate uptake and transition sites for methionine or lysine. i.e. phase transitions seem in this case to be caused by binding of molecule(s) to the uptake site. Uptake, but not phase patterns, was highly pH-dependent. The optima were pH 5 for lysine, pH 3–5 (a broad peak) for methionine and about pH 5.5 for proline. Uptake of the three amino acids was strongly inhibited by 2,4-dinitrophenol. sulfhydryl reagents and deoxycholate.     

The Structure and Mineralization of the Carapace of the Crab (Cancer pagurus L.) 3. The epicuticle

Decalcified and undecalcified preparations of the crab Cancer pagurus in the intermoult condition were studied to examine the mineralization and structure of the epicuticle, using light microscopic, electron microscopic, and microradiographic methods. The epicuticle was found to be composed of two layers, one superficial membrane, and one thicker layer, measuring 1-2 μm. From the base layer spines or microtrichia projected. These were approximately 18 μm long and built like the remainder of the epicuticle. The spines and the base layer of the epicuticle contained vertical canals which in undecalcified sections accomodated columns of crystals. These canals were the only location in which minerals occurred in the epicuticle. In decalcified preparations filamentous strands were observed in the canals. Elsewhere in the epicuticular tissue no fibrillar structure was observed. The canals and their contents seemed to extend across the junctional zone between the epicuticle and the exocuticle.     

Insulin and Amino-acid Regulation of Polysomes in Perfused,Diabetic Rat Liver

IN normal mammalian liver, protein synthesis and concomitant polyribosome assembly are controlled by amino-acids^1–4. A similar control may be exerted by insulin in liver⁵ and muscle⁶. Both the effect of amino-acids on liver and that of insulin on muscle can be demonstrated with isolated, perfused tissue^4,7, but the interrelationship between these agents has not been clarified either in liver or in muscle. We have used perfused livers from diabetic rats to establish whether amino-acids and insulin promote polysomal assembly independently or in concert.     

The Structure and Mineralization of the Carapace of the Crab (Cancer pagurus L.) 2. The exocuticle

The exocuticle of the dorsal carapace of the intermoult Cancer pagurus was studied by means of light microscopy, electron microscopy, and contact microradiography. In the exocuticle a 5-15 μm wide highly mineralized external zone was seen where prisms were not present. The cross-sectional shape and diameter of the prisms varied. The prisms were separated by interprismatic areas varying in width and in degree of mineralization. With increasing width of the interprismatic areas the diameter of the prisms decreased. The prism-less external zone may be the result of complete mineralization of the prisms. The pore canals of the exocuticle were circular in cross section and present both within the prisms and within the interprismatic areas. The lamellar system of the exocuticle was built up by layers of horizontal fibrils which were interconnected by vertical or oblique fibrils. The minerals of the external prism-less zone occurred as aggregates of crystalline matter or as large brick-like structures. Crystal edge lengths up to 300 nm were measured. In well mineralized interprismatic areas aggregates of crystals and relatively large crystals were observed. In poorly mineralized interprismatic areas small plate-like crystals occurred. Occasionally a prism-less zone was seen near the exocuticle/endocuticle junction.     

The origin of modern amphibians: a re‐evaluation

There are currently three competing hypotheses seeking to explain the evolutionary origins of modern amphibians. The lepospondyl hypothesis holds that the lysorophian lepospondyls constitute the sister taxon to all lissamphibians. The temnospondyl hypothesis suggests that modern amphibians are most closely related to the dissorophoid temnospondyls. Finally, the polyphyletic hypothesis posits that the modern amphibian orders have separate evolutionary origins from among different groups of Palaeozoic tetrapods. Here, we review the character matrices used in previous studies. These data sets differ significantly in choice of characters. Therefore, we built a matrix based on data from all three hypotheses and analysed key taxa phylogenetically using both Bayesian inference and parsimony. Uncorrected, the supermatrix yielded inconclusive results, demonstrating the presence of at least two phylogenetic optima. When the data were corrected according to new observations on Doleserpeton, Eocaecilia, and other fossil forms, the phylogeny supported the temnospondyl hypothesis of lissamphibian origins. This conclusion is also supported by a careful study of character changes in the individual lineages. © 2011 The Linnean Society of London, Zoological Journal of the Linnean Society, 2011, 162 , 457–469.