A review of the lower actinopterygian phylogeny

A review of lower actinopterygian phylogeny has led us to the conclusion that the Cladistia are the sister group of Recent actinopterygians (Actinopteri) and that the extinct Palaeonisciformes are a paraphyletic group, comprising stem-group actinopterygians (e.g. Cheirolepis ), stem-group actinopterans (e.g. Moythomasia ) and relatives of higher actinopterans such as Pteronisculus . Our analysis further concluded that the Acipenseriformes formed a clade together with Saurichthys and Birgeria , which was most parsimoniously resolved when the Acipenseriformes and Saurichthys were sister groups.  © 2005 The Linnean Society of London, Zoological Journal of the Linnean Society , 2005, 144 , 511−525.     

Ventral gill arch muscles and the interrelationships of gnathostomes, with a new classification of the Vertebrata

The ventral gill arch muscles of chondrichthyans, Latimeria , dipnoans, larval amphibians and actinopterygians are described and compared. Muscle patterns are characterized as primitive or derived and the derived patterns are used to test various hypotheses of the interrelationships of these griathostome groups. Gnathostomes differ from agnathans in having branchial muscles associated with the ventral gill arches. The monophyly of chondrichthyans is corroborated by the presence of coracobranchiales of hypobranchial origin. The monophyly of Recent teleostomes (Osteichthyes) is indicated by the presence of discrete transversi ventrales and interarcuales ventrales, and by the loss of the fifth superficial constrictor. A monophyletic Sarcopterygii which includes Latimeria is refuted by three paired branchial muscles found in dipnoans, Recent choanates and actinopterygians, but missing in Latimeria: pharyngoclaviculares, obliqui ventrales 1 and transversi ventrales 4. A new name, Euosteichthyes, is proposed for the group including dipnoans, choanates and actinopterygians. Sarcopterygii is restricted to include only dipnoans and choanates (among Recent organisms). Actinistia, including Latimeria , is proposed as the sister-group of all other Recent osteictithyans. Brachiopterygians (polypterids) are placed within Actinopterygii. A phylogenetic hypothesis supporting this classification is presented.     

The phylogenetic position of toadfishes (order Batrachoidiformes) in the higher ray-finned fish as inferred from partitioned Bayesian analysis of 102 whole mitochondrial genome sequences

In a previous study based on 100 whole mitochondrial genome (mitogenome) sequences, we sought to provide a new perspective on the ordinal relationships of higher ray-finned fish (Actinopterygii). The study left unexplored the phylogenetic position of toadfishes (order Batrachoidiformes), as data were unavailable owing to technical difficulties. In the present study, we successfully determined mitogenomic sequences for two toadfish species ( Batrachomoeus trispinosus and Porichthys myriaster ) and found that the difficulties resulted from unusual gene arrangements and associated repetitive non-coding sequences. Unambiguously aligned, concatenated mitogenomic sequences (13 461 bp) from 102 higher actinopterygians (excluding the ND6 gene and control region) were divided into five partitions (1st, 2nd and 3rd codon positions of the protein-coding genes, tRNA genes and rRNA genes) and partitioned Bayesian analyses were conducted. The resultant phylogenies strongly suggest that the toadfishes are not members of relatively primitive higher actinopterygians (Paracanthopterygii), but belong to a crown group of actinopterygians (Percomorpha), as was demonstrated for ophidiiform eels (Ophidiiformes) and anglerfishes (Lophiiformes) in the previous study. We propose revised limits of major unranked categories for higher actinopterygians and a new name (Berycomorpha) for a clade comprising two reciprocally paraphyletic orders (Beryciformes and Stephanoberyciformes) based on the present mitogenomic phylogenies.  © 2005 The Linnean Society of London, Biological Journal of the Linnean Society , 2005, 85 , 289–306.     

Symposium Summary: Evolutionary Patterns in Actinopterygian Fishes

SYNOPSIS. The actinopterygian fishes are an exemplary cladefor the study of structural and functional evolutionary patterns.With over half of all vertebrate species, ray-finned fisheshave diversified into a wide variety of habitats, and considerableprogress has been made over the last fifteen years in understandingthe genealogical relationships of actinopterygians. This symposiumhas contributed to our understanding of phylogenetic patternsin actinopterygians and to knowledge of the major structuraland functional patterns in locomotor, auditory, trophic, andneural systems. A number of key areas for future research havebeen identified. (1) The relationships of "palaeonisciform"fishes, (2) the study of trends in feeding and locomotor systemswithin a phylogenetic context, (3) the identification of primitivepatterns of pharyngeal jaw movement and steady and unsteadylocomotor patterns in actinopterygians, (4) the homologies,identification, and functional significance of neural pathwaysin the telencephalon, and (5) the comparative study of form-functionrelations in the auditory system. The study of teleost fishbiology has proceeded at the expense of data on primitive actinopterygians(e.g., Polypterus, Polyodon, Aapenser, Lepisosteus, Amia) whichare especially important in the analysis of structural and functionalpatterns in ray-finned fishes.     

Olfactory organ of acipenseriformes and comparison with other actinopterygians: Patterns of diversity

The position and structure of the olfactory organ and its openings vary among actinopterygians. The anterior nasal opening is a simple perforation in the skin in many extant actinopterygians (e.g., acipenseriforms, lepisosteids, and primitive Recent teleosts) and represents the primitive condition. Polypterids and Amia each exhibit a derived condition, in which the anterior nasal opening extends into a tube. The olfactory organ is relatively far away from the anterior end of the elongate rostrum in acipenseriforms, whereas the olfactory organs are closer to the anterior end of the snout in extant actinopterygians (e.g., polypterids, lepisosteids, and amiids). In adults, olfactory organs are cuplike structures in most actinopterygians, but these organs are tubelike in polypterids. Among extant actinopterygians, a nasal diverticulum is present only in polypterids. Teleosts have accessory nasal sacs, but chondrosteans, polypterids, lepisosteids, and amiids lack them. The olfactory rosette is formed by primary folds or lamellae that may be placed anterior, lateral, posterior, and/or medial to the axis of the organ. Large acipenserids have 20–32 lamellae, polyodontids have 13–18 lamellae, lepisosteids have 8–10 lamellae, and Amia may have over 100. In teleosts, the number of lamellae varies from none or a few to over 200. Secondary lamellae are present in acipenseriforms, lepisosteids, and some advanced teleosts; secondary lamellae are interpreted as independently acquired in these lineages. Secondary lamellae are absent in Amia and primitive teleosts such as Elops and Hiodon. Tertiary lamellae are present in Acipenser oxyrhynchus. The arrangement of the primary lamellae in relation to the axis of the organ results in at least 11 patterns of the olfactory rosette in actinopterygians. Lamellae that are enclosed in a tubelike sac and that have an anteromedial diverticulum are specializations of polypterids. Primary lamellae anterior, lateral, and posterior to an elongate axis are characteristic of lepisosteids. The presence of primary lamellae lateral, medial, and posterior to an elongate olfactory axis is a synapomorphy of Halecomorpha (Amia plus teleosts). The absence of secondary lamellae is a synapomorphy of Halecomorpha. © 1994 Wiley-Liss, Inc.     

Evolution of the facial musculature in basal ray-finned fishes

Background

The facial musculature is a remarkable anatomical complex involved in vital activities of fishes, such as food capture and gill ventilation. The evolution of the facial muscles is largely unknown in most major fish lineages, such as the Actinopterygii. This megadiverse group includes all ray-finned fishes and comprises approximately half of the living vertebrate species. The Polypteriformes, Acipenseriformes, Lepisosteiformes, Amiiformes, Elopiformes, and Hiodontiformes occupy basal positions in the actinopterygian phylogeny and a comparative study of their facial musculature is crucial for understanding the cranial evolution of bony fishes (Osteichthyes) as a whole.

Results

The facial musculature of basal actinopterygians is revised, redescribed, and analyzed under an evolutionary perspective. We identified twenty main muscle components ontogenetically and evolutionarily derived from three primordial muscles. Homologies of these components are clarified and serve as basis for the proposition of a standardized and unifying myological terminology for all ray-finned fishes. The evolutionary changes in the facial musculature are optimized on the osteichthyan tree and several new synapomorphies are identified for its largest clades, including the Actinopterygii, Neopterygii, and Teleostei. Myological data alone ambiguously support the monophyly of the Holostei. A newly identified specialization constitutes the first unequivocal morphological synapomorphy for the Elopiformes. The myological survey additionally allowed a reinterpretation of the homologies of ossifications in the upper jaw of acipenseriforms.

Conclusions

The facial musculature proved to be extremely informative for the higher-level phylogeny of bony fishes. These muscles have undergone remarkable changes during the early radiation of ray-finned fishes, with significant implications for the knowledge of the musculoskeletal evolution of both derived actinopterygians and lobe-finned fishes (Sarcopterygii).

     

Physiological epistasis, ontogenetic conflict and natural selection on physiology and life history

Ontogenetic conflict arises when optima for alleles governingfitness variation differ between juveniles and adults or betweenadult sexes. Loci that govern development of alternative phenotypesin the sexes, hereafter termed morph-determining loci, mediatedevelopment through the endocrine system. Morphotypic selectionis defined to be multivariate selection favoring discrete alternativemorphotypes (e.g., optima). When the optimal combinations ofalleles for alternative morphs differ between the sexes, itgenerates conflicting selection pressure and thus ontogeneticconflict. Selection on morph alleles promotes ontogenetic conflictbecause it perturbs physiological epistasis that governs theexpression of male versus female traits. Expression of physiologicaltraits arises from homeostasis that maintains trait expressionwithin a normal range. The genetic basis of homeostasis is likelyto arise from interactions among several genes (e.g., geneticepistasis) or protein products (e.g., physiological epistasis).For example, endocrine regulation arises from interactions betweengondatropins, which are protein hormones produced by the hypothalamic-pituitaryglands, and steroid hormones, which are produced by the gonads(e.g., HPG axis). The side-blotched lizard system is discussedwith respect to physiological bases of ontogenetic conflict.We also describe a novel molecular marker strategy for uncoveringgenome-wide physiological epistasis in nature. Finally, ontogeneticconflict exerts selection on females to evolve mate selectionor cryptic choice that is reflected in different sires beingchosen for son versus daughter production. We describe how side-blotchedlizard females ameliorate ontogenetic conflict by cryptic choiceof male genotypes to produce sons versus daughters.     

THE ECOLOGY OF THE HONG KONG LIMPETS CELLANA GRATA (GOULD 1859) AND PATELLOIDA PYGMAEA (DUNKER 1860): REPRODUCTIVE BIOLOGY

Cellana grata is large, relatively long lived (3 years), withone winter breeding season each year which can be correlatedwith major seasonal climatic and hydro-logical events, e.g.,winter reduction in temperature and higher seas. C. grata ischaracterised by a relatively low value of mean annual reproductiveeffort (males: 23%; females: 18%). Patelloida pygmaea is small,short lived (1 year), with one spring breeding season each yearand devotes a large proportion of metabolic energy for reproduction.P. pygmaea showed a higher value of mean annual reproductiveeffort (males: 46%; females: 31%) than C. grata. Mature gonads of Cellana grata first appeared in June and itreached a peak maturity (100%) in September, remaining so untilDecember, i.e., the maturation of the gonads coincided withincreasing water temperatures, with spawning associated witha decrease in water temperature. Gonadal development by Patelloidapygmaea began in either July or August and reached a peak inDecember, remaining so until a major peak in spawning took placebetween April and May, i.e., gonad maturation coincided witha decline in water temperature, with spawning following thesubsequent increase. Limpet gonadal cycles are likely gearedto temperature and food supply. Spawning occurred between Novemberand December, when wave heights are typically 1 m higher thanin summer. (Received 1 December 1992; accepted 25 June 1993)     

The dynamic ups and downs of genome size evolution in Brassicaceae

Crucifers (Brassicaceae, Cruciferae) are a large family comprisingsome 338 genera and c. 3,700 species. The family includes importantcrops as well as several model species in various fields ofplant research. This paper reports new genome size (GS) datafor more than 100 cruciferous species in addition to previouslypublished C-values (the DNA amount in the unreplicated gameticnuclei) to give a data set comprising 185 Brassicaceae taxa,including all but 1 of the 25 tribes currently recognized. Evolutionof GS was analyzed within a phylogenetic framework based ongene trees built from five data sets (matK, chs, adh, trnLF,and ITS). Despite the 16.2-fold variation across the family,most Brassicaceae species are characterized by very small genomeswith a mean 1C-value of 0.63 pg. The ancestral genome size (ancGS)for Brassicaceae was reconstructed as ^anc1C = 0.50 pg. Approximately50% of crucifer taxa analyzed showed a decrease in GS comparedwith the ancGS. The remaining species showed an increase inGS although this was generally moderate, with significant increasesin C-value found only in the tribes Anchonieae and Physarieae.Using statistical approaches to analyze GS, evolutionary gainsor losses in GS were seen to have accumulated disproportionatelyfaster within longer branches. However, we also found that GShas not changed substantially through time and most likely evolvespassively (i.e., a tempo that cannot be distinguished betweenneutral evolution and weak forms of selection). The data revealan apparent paradox between the narrow range of small GSs overlong evolutionary time periods despite evidence of dynamic genomicprocesses that have the potential to lead to genome obesity(e.g., transposable element amplification and polyploidy). Toresolve this, it is suggested that mechanisms to suppress amplificationand to eliminate amplified DNA must be active in Brassicaceaealthough their control and mode of operation are still poorlyunderstood.     

Making teeth to order: conserved genes reveal an ancient molecular pattern in paddlefish (Actinopterygii)

Ray-finned fishes (Actinopterygii) are the dominant vertebrate group today (+30 000 species, predominantly teleosts), with great morphological diversity, including their dentitions. How dental morphological variation evolved is best addressed by considering a range of taxa across actinopterygian phylogeny; here we examine the dentition of Polyodon spathula (American paddlefish), assigned to the basal group Acipenseriformes. Although teeth are present and functional in young individuals of Polyodon, they are completely absent in adults. Our current understanding of developmental genes operating in the dentition is primarily restricted to teleosts; we show that shh and bmp4, as highly conserved epithelial and mesenchymal genes for gnathostome tooth development, are similarly expressed at Polyodon tooth loci, thus extending this conserved developmental pattern within the Actinopterygii. These genes map spatio-temporal tooth initiation in Polyodon larvae and provide new data in both oral and pharyngeal tooth sites. Variation in cellular intensity of shh maps timing of tooth morphogenesis, revealing a second odontogenic wave as alternate sites within tooth rows, a dental pattern also present in more derived actinopterygians. Developmental timing for each tooth field in Polyodon follows a gradient, from rostral to caudal and ventral to dorsal, repeated during subsequent loss of teeth. The transitory Polyodon dentition is modified by cessation of tooth addition and loss. As such, Polyodon represents a basal actinopterygian model for the evolution of developmental novelty: initial conservation, followed by tooth loss, accommodating the adult trophic modification to filter-feeding.     

Hypoxic Reptiles: Blood Gases, Body Temperature and Control of Breathing

Our contribution to this symposium is a review of recent modelsand experimental cdata on oxygen homeostasis in vertebrateswith normal intracardiac shunts; i.e., amphibians and reptiles.We focus on the interactions among hemoglobin function, bodytemperature regulation, and cardiovascular shunts under normalconditions (i.e., breathing fresh air at or near sea level)and during external hypoxia (e.g., altitude, burrows) and internalhypoxia (e.g., anemia, hemorrhage). Mathematical models andexperimental data suggest that animals with venous admixturefrom cardiovascular shunts will show biphasic arterial and mixedvenous Po₂ responses to warming; i.e., first increasing andthen, as the dissociation curve shifts too far to the right,decreasing. This has implications for many physiological functionsincluding oxygen consumption by tissues, control of breathing,as well as preferred body temperature and its regulation. Wepresent some of the recent experiments that have explored theseimplications.     

On the homology of the posteriormost gill arch in polypterids (Cladistia,Actinopterygii)

Polypterids are unusual among ray‐finned fishes in possessing only four rather than five gill arches. We review the two current hypotheses regarding the homology of the last gill arch in polypterids: that it represents (1) the fifth or (2) the fourth arch of other actinopterygians. Arguments for the alternative hypotheses drawn from different anatomical systems are compiled and evaluated. We conclude that in polypterids the last arch represents the fourth arch of other Actinopterygii and the fifth arch is absent. © 2003 The Linnean Society of London, Zoological Journal of the Linnean Society, 2003, 138, 495–503.     

Short-term changes in the mesozooplanktonic community in theSeine ROFI (Region of Freshwater Influence)(eastern English Channel)

Discrete-depth, hourly mesozooplankton samples were collectedover a 92 h period in May 1992 at an anchor station within theSeine Region of Freshwater Influence (ROFI) (English Channel).The mesozooplankton community defined as a euryhaline marineassemblage was dominated by the calanoid copepods Acartia spp.,Temora longicornis and Centropages hamatus, the cladoceran Evadnenordmanni and the appendicularian Oikopleura dioica. The semi-diurnaltidal current was the dominant factor in determining the short-termtemporal changes in the community in terms of density and speciescomposition so that zooplankton patches displayed oscillatingmotion in relation to tidal advection. Although a few species(e.g. Pleurobrachia pileus) exhibited higher densities aroundlow tide, maximum densities were observed for most species (e.g.T.longicornis and E.nordmanni) around high tide, according tosalinity variations. Diurnal changes were only reported forcyclopoid copepods (i.e. Halicyclops sp. and Cyclopina sp.)which wer$$$ mainly endobenthic during the day and moved intothe water column at night. Besides temporal changes in depth-averageddensities, most species exhibited vertical migrations at dieland/or tidal periods. Tidal vertical migrations were reportedonly for a few taxa and could be the result of passive mechanisms(e.g. vertical mixing) rather than of active behaviour. Dielvertical migrations were observed in most of the abundant taxa.While this migration pattern did not appear to be an adaptationto predator avoidance within the Seine ROFI, it could regulatehorizontal transport of organisms and promote their retention.The consequences of the short-term mesozooplankton fluctuationsfor sampling designs are discussed.     

Endocranial preservation of a Carboniferous actinopterygian from Lancashire,UK, and the interrelationships of primitive actinopterygians

The gross brain structure of an Upper Carboniferous (ca. 310 Myr ago) ray-finned fish (Actinopterygii) is described from exceptionally well-preserved fossil material from the Burnley region of Lancashire, UK. Previously identified as ''Rhadinichthys'' planti, the species is reassigned to the genus Mesopoma. Morphological characters derived from these data are combined with reviews of cranial skeletal anatomy, enamel composition, oculomoter muscle insertion and paired fin morphology to test and reanalyse hypotheses of primitive actinopterygian interrelationships. Results indicate that ancestral chondrostean (sturgeon and paddlefish) and neopterygian (teleost, amiid and gar) lineages diverged earlier than current theories suggest. Palaeonisciformes, a taxonomic group widely used to include most Palaeozoic actinopterygians, include a significant number of primitive neopterygians, several of which may form a distinct monophyletic clade. Within this revised phylogenetic context, changes in gross brain morphology from primitive conditions, as revealed by fossil data, highlight likely specializations in extant non-teleostean actinopterygians.     

Model systems for environmental signaling

Studies of environmental signaling in animals have focused primarilyon organisms with relatively constrained responses, both temporallyand phenotypically. In this regard, existing model animals (e.g.,"worms and flies") are particularly extreme. Such animals haverelatively little capacity to alter their morphology in responseto environmental signals. Hence, they exhibit little phenotypicplasticity. On the other hand, basal metazoans exhibit relativelyunconstrained responses to environmental signals and may thusprovide more general insight, insofar as these constraints arelikely traits derived during animal evolution. Such enhancedphenotypic plasticity may result from greater sensitivity toenvironmental signals, or greater abundance of suitable targetcells, or both. Examination of what is known of the componentsof environmental signaling pathways in cnidarians reveals manysimilarities to well-studied model animals. In addition to theseelements, however, macroscopic basal metazoans (e.g., spongesand cnidarians) typically exhibit a system-level capabilityfor integrating environmental information. In cnidarians, thegastrovascular system acts in this fashion, generating localpatterns of signaling (e.g., pressure, shear, and reactive oxygenspecies) via its organism-wide functioning. Contractile regionsof tissue containing concentrations of mitochondrion-rich, epitheliomuscularcells may be particularly important in this regard, servingin both a functional and a signaling context. While the evolutionof animal circulatory systems is usually considered in termsof alleviating surface-to-volume constraints, such systems alsohave the advantage of enhancing the capacity of larger organismsto respond quickly and efficiently to environmental signals.More general features of animals that correlate with relativelyunconstrained responses to environmental signals (e.g., activestem cells at all stages of the life cycle) are also enumeratedand discussed.     

Density-dependent protogynous sex change in territorial-haremic fishes: models and evidence

Several hypotheses of the proximate control of protogynous (female-to-male)sex change propose that social group composition triggers sexchange, but they do not address how proximate cues are alteredby population density. I present three mutually exclusive encounter-ratethreshold hypotheses that assume that population density determinesrates of contact between social group members and that ratesof contact are cues for sex change. Different densities arepredicted to induce sex change, depending on the encountersassumed to be important in the sex change process (e.g., encounterswith smaller and larger individuals). Tests of the models usea pomacanthid angelfish(Centropyge potten) to show that continuedpresence of a smaller (female) conspecific is needed for sexchange, and that continued presence of a larger (male) conspecificcan either inhibit sex change or prevent its behavioral stimulation.Using constant social group composition, sex change is preventedat higher density but not at a lower density. The absolute encounter-ratethreshold hypothesis, which predicts sex change under intermediate-densityconditions, is the most probable model of the social controlof sex change in C.potteri     

‘Fish’ (Actinopterygii and Elasmobranchii) diversification patterns through deep time

Actinopterygii (ray‐finned fishes) and Elasmobranchii (sharks, skates and rays) represent more than half of today's vertebrate taxic diversity (approximately 33000 species) and form the largest component of vertebrate diversity in extant aquatic ecosystems. Yet, patterns of ‘fish’ evolutionary history remain insufficiently understood and previous studies generally treated each group independently mainly because of their contrasting fossil record composition and corresponding sampling strategies. Because direct reading of palaeodiversity curves is affected by several biases affecting the fossil record, analytical approaches are needed to correct for these biases. In this review, we propose a comprehensive analysis based on comparison of large data sets related to competing phylogenies (including all Recent and fossil taxa) and the fossil record for both groups during the Mesozoic–Cainozoic interval. This approach provides information on the ‘fish’ fossil record quality and on the corrected ‘fish’ deep‐time phylogenetic palaeodiversity signals, with special emphasis on diversification events. Because taxonomic information is preserved after analytical treatment, identified palaeodiversity events are considered both quantitatively and qualitatively and put within corresponding palaeoenvironmental and biological settings. Results indicate a better fossil record quality for elasmobranchs due to their microfossil‐like fossil distribution and their very low diversity in freshwater systems, whereas freshwater actinopterygians are diverse in this realm with lower preservation potential. Several important diversification events are identified at familial and generic levels for elasmobranchs, and marine and freshwater actinopterygians, namely in the Early–Middle Jurassic (elasmobranchs), Late Jurassic (actinopterygians), Early Cretaceous (elasmobranchs, freshwater actinopterygians), Cenomanian (all groups) and the Paleocene–Eocene interval (all groups), the latter two representing the two most exceptional radiations among vertebrates. For each of these events along with the Cretaceous‐Paleogene extinction, we provide an in‐depth review of the taxa involved and factors that may have influenced the diversity patterns observed. Among these, palaeotemperatures, sea‐levels, ocean circulation and productivity as well as continent fragmentation and environment heterogeneity (reef environments) are parameters that largely impacted on ‘fish’ evolutionary history, along with other biotic constraints.     

Nouvelles formulations des regles ecologiques connues sous le nom de reegle de Bergmann et loi de Jordan: Amendments of the ecological rules known as Bergmann's and Jordan's rules

Measurements of populations of planktonic and micronektonicspecies from the Atlanto-mediterranean region (about 10,000specimens) have lead to improvements in Bergmann's rule relatingto the increase in size with latitude. There are three cases : Mediterranean specimens may be smaller(e.g. the mysid Eucopia hansent), equal to (e.g. the decapodcrustacean Gennadas elegans) or larger than Atlantic ones (e.g.the thecosomatous genus Cymbulia). All the species in the last group have their principal distributionin warm ocean waters. In the Atlantic, tropical species (e.g.the euphausiid Euphausia gibboides) decrease in size in thenorthern parts of their range while temperate species (e.g.the decapod crustacean Sergesles corniculum) decrease in sizetowards both the pole and the equator. The comparison with the number of vertebrae of fish, which increasesas does the size according to Jordan's rule, is interesting:though correct for cold water species (e.g. Merlucdus merluccius),this rule cannot be applied to warm water species (e.g. Merlucciussenegalensis). Thus, these rules must be corrected like this:- "a species reachesits maximal size in high, intermediate or low latitudes of itsarea if it has a boreal, temperate or tropical distribution"; - "the number of vertebrae increases with latitude for borealfish and decreases for tropical ones".     

Properties of cytotoxic peptide-formed ion channels

Cytotoxic peptides are relatively small cationicmolecules such as those found 1) in venoms, e.g., melittin inbee, scorpion toxins in scorpion, pilosulin 1 in jumper ant, andlycotoxin I and II in wolf spider; 2) in skin secretions (e.g.,magainin I and II from Xenopus laevis, dermaseptin from frog,antimicrobials from carp) and cells of the immune system (e.g., insect,scorpion, and mammalian defensins and cryptdins); 3) asautocytotoxicity peptides, e.g., amylin cytotoxic to pancreatic-cells, prion peptide fragment 106-126[PrP-(106-126)], and amyloid -protein (AP)cytotoxic to neurons; and 4) as designed synthetic peptides based on the sequences and properties of naturally occurring cytotoxic peptides. The small cytotoxic peptides are composed of -sheets, e.g., mammalian defensins, AP, amylin, and PrP-(106-126),whereas the larger cytotoxic peptides have several domains composed of both -helices and -sheets stabilized by cysteine bonds, e.g., scorpion toxins, scorpion, and insect defensins. Electrophysiological and molecular biology techniques indicate that these structures modifycell membranes via 1) interaction with intrinsic ion transport proteins and/or 2) formation of ion channels. These twononexclusive mechanisms of action lead to changes in second messengersystems that further augment the abnormal electrical activity anddistortion of the signal transduction causing cell death.

     

The origin of metazoan complexity: porifera as integrated animals

Sponges [Porifera] are the phylogenetically oldest metazoanphylum still extant today; they share the closest relationshipwith the hypothetical common metazoan ancestor, the Urmetazoa.During the past 8 years cDNAs coding for proteins involved incell-cell- and cell-tissue interaction have been cloned fromsponges, primarily from Suberites domuncula and Geodia cydoniumand their functions have been studied in vivo as well as invitro. Also, characteristic elements of the extracellular matrixhave been identified and cloned. Those data confirmed that allmetazoan phyla originate from one ancestor, the Urmetazoa. Theexistence of cell adhesion molecules allowed the emergence ofa colonial organism. However, for the next higher stage in evolution,individuation, two further innovations had to be formed: theimmune- and the apoptotic system. Major defense pathways/moleculesto prevent adverse effects against microbes/parasites have beenidentified in sponges. Furthermore, key molecules of the apoptoticpathway(s), e.g., the pro-apoptotic molecule comprising twodeath domains, the executing enzyme caspases, as well as theanti-apoptotic/cell survival proteins belonging to the Bcl-2family have been identified and cloned from sponges. Based onthese results—primarily obtained through a molecular biologicalapproach—it is concluded that cell-cell- and cell-matrixadhesion systems were required for the transition to a colonialstage of organization, while the development of an immune systemas well as of apoptotic processes were prerequisites for reachingthe integrated stage. As the latter stage already exists insponges, it is therefore likely that the hypothetical ancestor,the Urmetazoa, was also an "integrated colony."