Phylogeography of Iurus dufoureius (Brullé, 1832) (Scorpiones, Iuridae)

Aim  This study uses molecular data in conjunction with palaeogeography to infer the most plausible biogeographical scenario accounting for the current distributional pattern of Iurus dufoureius .
Location  North-eastern Mediterranean region.
Methods  Sequencing of a 441-bp segment of the mitochondrial 16S rRNA gene in seven populations covering the whole distributional range of the species. Phylogenetic analyses performed included neighbour joining, maximum parsimony and Bayesian inference.
Results  The molecular phylogeny showed that two Iurus clades are strongly supported. These clades correspond to the two subspecies Iurus dufoureius dufoureius and Iurus dufoureius asiaticus , currently recognized within the genus. The assumption of a clock-like evolution could not be rejected, and this enabled us to estimate an approximation of the local rate of evolution for the I. dufoureius lineages. Based on the estimated evolutionary rate (0.79 ± 0.17 Myr⁻¹), the split between the two Iurus clades occurred c. 8 Ma.
Main conclusions  Contrary to what was believed in the past, the genus Iurus is an old north-eastern Mediterranean genus that has been differentiating in southern Greece and south-west Turkey at least from the middle Miocene. According to the phylogenetic trees obtained and the dating of the divergence times of lineages, the genus dispersed into the Aegean Archipelago when the Aegean was still a uniform land mass. Although the phylogenetic relationships of I. d. dufoureius populations have been shaped by the most recent vicariant events, the phylogenetic relationships of I. d. asiaticus populations are mostly attributable to older palaeoevents occurring in the area.     

Taxonomy of Electrogena antalyensis (Kazanci & Braasch, 1986) (Ephemeroptera,Heptageniidae)

Female imagines, subimagines, eggs and larvae of Electrogena antalyensis (Kazanci & Braasch) from Turkey are described for the first time. The results of a thorough analysis of larvae, based on the standard set of diagnostic characters for the identification of Electrogena species, are reported. The peculiarity of several characters places E. antalyensis in an isolated position within the genus Electrogena.     

The larva of Oecetis tripunctata (Fabricius, 1793) (Trichoptera,Leptoceridae)

Oecetis tripunctata is a widely distributed leptocerid in Europe, ranging from the Iberian and Apennine peninsulas and the Central and Western European highlands to the plains of Eastern Europe. The long, single-bladed mandibles are indicative for a predacious lifestyle. This paper describes the previously unknown larva of Oecetis tripunctata. Information on the morphology of the 5th larval instar is given, and the most important diagnostic features are illustrated. A synoptic key for the European species of Oecetis is also provided. In the context of existing identification keys the larva of Oecetis tripunctata keys together with Oecetis intima and Oecetis notata. Oecetis tripunctata is separated from the other two species by the fact that a double row of long setal fringes is lacking at the hind tibiae and that several long setae are present on the protrochantinus.     

Le « Mégalosaure » (Dinosauria,Sauropoda) de Saint-Agnant (Charente-Maritime,France) : description et origine stratigraphique

The “Megalosaur” remains from Saint-Agnant (Charente-Maritime, France), reported as early as 1881 by Boissellier, are here described and figured for the first time. These bones, as well as a few additional specimens from the nearby locality of Soubise, belong in fact to an indeterminate sauropod. The stratigraphical position of these remains unambiguously indicates an infra-Cenomanian age. However, the presence in this area of continental deposits with Purbeckian and Wealden facies does not allow to decide between an earliest or late Early Cretaceous age.     

Isotopes stables (C,N) du collagène des mammouths de Mezhyrich (Epigravettien,Ukraine) : implications paléoécologiques

The mammoth steppe ecosystem was characterized by a high diversity in large mammals species distributed on a vast geographical range. The isotopic analyses of the collagen of the faunal remains from this context testified the niche partitioning among large herbivores with a specialization in the types of consumed plants. In the case of the mammoth (Mammuthus primigenius), systematic higher abundances in ¹⁵N are found for this species compared to those of other grazers in Eurasia and Alaska during the Upper Palaeolithic. This distinct isotopic signature reflects a specific ecological niche. The analyses of mammoth remains at the Epigravettian site of Mezhyrich (15,000–14,300 conv BP) reveal low abundances in ¹⁵N that are equivalent to those of the associated horses. Thus, the mammoth of Mezhyrich experienced a significant change in their environment and diet that probably led to the loss of their ecological niche. A likely direct competition with other large herbivores and the possible predation by wolves and human populations should be considered for the mammoth of the Ukrainian plains, long before their extirpation from the region.     

Fossil frogs (Anura) from Shanwang (Middle Miocene; Shandong Province, China)

The early middle Miocene biota from the Shanwang locality in eastern China is one of the most diverse and well preserved in the world. This overall richness contrasts with its low diversity of anuran amphibians. The most abundant anurans are representatives of the family Ranidae, which remains the dominant group in the extant anuran fauna of China. Besides Rana basaltica Young, some other ranids can be recognised at the locality, and are clearly distinguishable from R. basaltica based on their larger size and different proportions. Ranids are also represented by a developmental series of tadpoles, ranging from approximately Nieuwkoop-Faber (NF) stage 43 to a metamorphosing tadpole of NF stage 57. This is the first known developmental series of fossil non-pipoid Anura outside the Pelobatidae. In addition to the ranids, Bufo shandongensis nov. sp. (replacement name for B. linquensis), represented by one of the earliest known articulated bufonid skeletons, is described and illustrated. Another large toad, Macropelobates linquensis (Yang) nov. comb., is re-described; it can be assigned to the Pelobatoidea, with a possible relationship to the Scaphiopodidae, and can be considered, based on the presence of a large spade, a tibiofibula shorter than the femur, and a short astragalus and calcaneus, to be the earliest known anuran burrower.     

Hymenopteran parasitoids of the ant-eating spider Zodarion styliferum (Simon) (Araneae,Zodariidae)

Calymmochilus dispar Bouček & Andriescu (Hymenoptera, Eupelmidae) and Gelis apterus (Pontoppidan) (Hymenoptera, Ichneumonidae) are newly recorded as parasitoids of the ant-eating spider Zodarion styliferum (Simon) (Araneae, Zodariidae). The larvae of both parasitoid species fed on juvenile spiders. The final instar larva and pupa of Calymmochilus dispar and the male of Gelis apterus are described for the first time. Both species represent new distribution records for Portugal. The biology and host associations of the parasitoids are discussed.     

Paroniceratinae (Ammonoidea, Hildoceratidae) del Toarciense en las Cordilleras Ibérica y Cantábrica (España)

The Paroniceratinae constitute a group widely recorded in the Tethys realm. However, they represent alone a small part, less than 1%, of the ammonoidea obtained in Toarcian sediments from the regions located at the east of the Iberian Plateau (Iberian Range). The values are yet smaller in the northern regions (Cantabrian Range) and in the west (Portugal), and show a sporadic presence in the Betics Ranges. In this study, the biostratigraphical distribution and the biochronostratigraphical position of the recorded species in the more representative expanded sections of Spain are checked and compared with those of other areas of the NW Europe bioprovinces and of the Tethys. The obtained specimens from Frechiella: F. subcarinata (Young and Bird), F. helenae Renz, F. venantii (Catullo), F. kammerkarensis (Stolley) and F. cf. octaviae Renz are described and figured, all of them proceeding from sediments of the Bifrons Zone in the Iberian Range, as well as those of Paroniceras: P.sternale (d’Orbigny) and P.helveticum Renz, and Oxyparoniceras: O. (O.) cf. telemachi (Renz), O. (O.) buckmani (Bonarelli), O. (N.) cf. undulosum (Monestier), O. (N.) cf. morbiense (Renz) and O. (N.) cf. brocardi Rulleau, Bécaud and Neige, proceeding from sediments of the interval between the Bifrons Zone (Semipolitum Subzone) and the Insigne Zone (Insigne Subzone), in the Iberian and Cantabrian Ranges. The Frechiella and Oxyparoniceras species are developed and recorded in the Iberian Plateau margins during the Bifrons Zone and the Insigne Zone, respectively, during the same intervals than the transgressive maxima of the LJ3 and LJ4 second order cycles recognized in all the studied area, while Paroniceras species make it during the Variabilis Zone, that concur with the final regressive stage of the LJ3 cycle.     

Synthesis, crystal structure, spectral properties and catalytic activity of hexakis(imidazole)manganese(II) bisindole-2-carboxylato bisneocuproine bisdimethyl sulfoxide solvates {[Mn(Im)6] · 2(2-IC) · 2(NC) · 2(DMSO)}

Synthesis, X-ray crystal structure and IR spectrum of {[Mn^II(Im)₆] · 2(2-IC) · 2(NC) · 2(DMSO)} (Im = imidazole, 2-HIC = indole-2-carboxylic acid, NC = 2,9-dimethyl-1,10-phenanthroline, DMSO = dimethyl sulfoxide) are reported. The manganese(II) ion has octahedral geometry with a MnN₆ core. The crystal structure is completed by two NC, two 2-IC⁻ and two DMSO solvate molecules. The individual cations are linked into chains running parallel to the a axis by four intermolecular hydrogen bonding involving two 2-IC⁻solvate. Moreover, these chains are connected by π-π stacking interactions which occur between neocuproine molecules related through inversion center. In IR spectroscopy, the compound spectrum is roughly similar to the imidazole one: (i) above 1800 cm⁻¹, the bands are broad, but when focussing on some of them a doublet structure can be found; (ii) below 1800 cm⁻¹, the bands are sharp and it is then possible to point out the modification of S-O band when this later is involved in bifurcated hydrogen bonding to a second solvate 2-IC⁻. The compound catalyses the disproportionation of H₂O₂; moreover an additional quantity of imidazole increases the reaction rate.     

Phylogenetic position of two Patagonian Cibicididae (Rotaliida, Foraminifera): Cibicidoides dispars (d’Orbigny, 1839) and Cibicidoides variabilis (d’Orbigny, 1826)

Cibicidoides dispars and Cibicidoides variabilis are two neritic cibicidids commonly found on the Patagonian coasts. Phylogenetic analyses of partial SSU rDNA sequences show that they both belong to the genus Cibicidoides. Cibicidoides dispars branches close to Cibicidoides wuellerstorfi, whereas C. variabilis clusters with Cibicidoides pachyderma. In both cases, species clustering together are well separated morphologically and ecologically but close genetically. Molecular data indicate clearly that C. dispars and C. variabilis are well separated genetically from Cibicidoides lobatulus, another shallow water cibicidid sharing a similar ecology and morphology. Moreover, our molecular results show that neritic and bathyal or abyssal species are found together in different clades, suggesting multiple colonization events from shallow to deep water or vice versa. The analysis of more variable ITS rDNA region, on the other hand, reveals small differences between individuals of C. variabilis sampled in the south and north of Chilean Patagonia, which could indicate a cryptic speciation undergoing in this species.     

Taxonomie du grand canidé de la grotte du Vallonnet (Roquebrune-Cap-Martin, Alpes-Maritimes, France)

The large canid of Vallonnet cave belongs to Xenocyon lycaonoides. Its remains are similar to the Xenocyon from Untermassfeld in Germany. X. Lycaonoides, and evoluated form of the Xenocyon genus, is characteristic of the second half of the Lower Pleistocene. The genus Xenocyon may be the ancestor of both Cuon and Lycaon.     

Ultrastructural observations on spermiogenesis in the peanut worm,Themiste pyroides (Chamberlin, 1920) (Sipuncula; Sipunculidea)

Summary

The process of spermiogenesis and the ultrastructure of the spermatozoa in the peanut worm, Themiste pyroides, from the Sea of Japan were observed with electron microscopy (SEM and TEM). The testes are composed of groups of spermatogonia and are covered by peritoneal cells. Clusters of spermatocytes are released from the testes into the coelomic fluid. Connected by intercellular bridges, the spermatocytes within a given cluster develop asynchronously. Proacrosomal vesicles and a flagellum appear in spermatocytes. Spermatids in the clusters retain the intercellular connections. During spermiogenesis, the acrosomal vesicle, formed by coalescence of small proacrosomal vesicles in the basal part of the spermatid, migrates to the apical part of the cell to form a conical-shaped acrosome. The basal concavity lying above the nucleus is filled with subacrosomal substance. The midpiece contains four mitochondria, two centrioles, and some residual cytoplasm with dark glycogen-like granules. A peculiar annulus structure develops around the base of the flagellum. The distal centriole has a pericentriolar complex consisting of radially oriented elements. Before the spawning process, the spermatozoa are filtered throughout the ciliary nephrostomal funnel into the excretory sac of paired nephridia where they are stored for a short time. The sperm are released into the sea water via nephridiopores. Spermatozoa remaining in the coelomic fluid after spawning are resorbed by amoebocytes. This species from Vostok Bay is characterized by a prolonged spawning period from June to early October. The reproductive strategy of T. pyroides is discussed in comparison with that of Thysanocardia nigra, the latter having a unique pattern of packaging of the spermatozoa, resulting in the formation of spermatozeugmata, as a reproductive adaptation to the very short spawning period.     

Symbiotic microorganisms in <Emphasis Type="Italic">Puto superbus</Emphasis> (Leonardi, 1907) (Insecta,Hemiptera, Coccomorpha: Putoidae)

The scale insect Puto superbus (Putoidae) lives in mutualistic symbiotic association with bacteria. Molecular phylogenetic analyses have revealed that symbionts of P. superbus belong to the gammaproteobacterial genus Sodalis. In the adult females, symbionts occur both in the bacteriocytes constituting compact bacteriomes and in individual bacteriocytes, which are dispersed among ovarioles. The bacteriocytes also house a few small, rod-shaped Wolbachia bacteria in addition to the numerous large, elongated Sodalis-allied bacteria. The symbiotic microorganisms are transovarially transmitted from generation to generation. In adult females which have choriogenic oocytes in the ovarioles, the bacteriocytes gather around the basal part of the tropharium. Next, the entire bacteriocytes pass through the follicular epithelium surrounding the neck region of the ovariole and enter the space between oocyte and follicular epithelium (perivitelline space). In the perivitelline space, the bacteriocytes assemble extracellularly in the deep depression of the oolemma at the anterior pole of the oocyte, forming a “symbiont ball”.     

Euxinocythere (Ostracoda, Cytheridae, Leptocytherinae) du Miocène supérieur du Bassin de Turiec (Slovaquie) : taxonomie et paléoécologie

Eight new species of the family Cytheridae have been identified in the Upper Miocene deposits of the Turiec Basin (Slovakia), a small isolated intermountain depression. Six species are new - Euxinocythere aphroditae, E. delicata, E. lactea, E. minuscula, E. quadricostata, E. satyrica - and two are kept in open nomenclature. Their attribution to the genus Euxinocythere is based on arrangement of the hinge elements and of anterior marginal zone. This genus is known from brackish ostracod assemblages of the Paratethys and the Eastern Mediterranean while the species from the Turiec Basin are associated to fresh-water assemblages. The Euxinocythere have been found in littoral as well in deep limnic environment.     

Les Oppeliidae (Ammonitina) de l'horizon à Collotiformis (Callovien supérieur, zone à Athleta) de la région dijonnaise (Côte-d'Or, France)

In the Dijon area, the top of the Athleta zone contains rich ammonite fauna dominated quantitatively by two families: Perisphinctidae and Oppeliidae. The Oppeliidae are diversified and make up a numerically larger proportion of the ammonite fauna than in the underlying strata (up to 57 %). The exceptional state of preservation of the ammonites has permitted a precise study to be made of ontogenesis and intraspecific variability. Four sub-families are found (Oppeliinae, Hecticoceratinae, Distichoceratinae and Taramelliceratinae), within which sexual dimorphs have been recognised. One small form, characterized by lappets and a body chamber with ellipticoidal-trending coiling, is interpreted as the microconch dimorph of the Paralcidia genus which was unknown until now. One specimen of Creniceras, the oldest collected in Côte-d'Or, can be interpreted as the microconch dimorph of Taramelliceras.

Résumé

Dans la région dijonnaise, le sommet de la zone à Athleta renferme une riche faune ammonitique, quantitativement dominée par deux familles : Perisphinctidae et Oppeliidae. Par rapport aux niveaux sous-jacents, la famille des Oppeliidae est diversifiée et représente une part numériquement plus importante de la faune ammonitique (jusqu'à 57 %). L'excellente conservation des ammonites a autorisé une étude précise de l'ontogenèse et de la variabilité intraspécifique au sein de la famille. Quatre sous-familles sont représentées (Oppeliinae, Hecticoceratinae, Distichoceratinae et Taramelliceratinae), au sein desquelles les dimorphes sexuels ont été reconnus. Une petite forme, caractérisée par des apophyses jugales et une chambre d'habitation à enroulement à tendance ellipticoïde, est interprétée comme le dimorphe microconque, inconnu jusqu'à présent, du genre Paralcidia. Un spécimen de Creniceras, le plus ancien récolté en Côte-d'Or, pourrait correspondre au dimorphe microconque des Taramelliceras.