New grylloblattid insects (Insecta: Grylloblattida) from the Grès à Voltzia of the Vosges (Middle Triassic of France)

New grylloblattid insects (Grylloblattida) are described from the Grès à Voltzia of the Vosges (Anisian of Alsace and Lorraine, France): Chauliodites anisicus, sp. nov. (Chaulioditidae), Palaeomesorthopteron pullus gen. et sp. nov. (Mesorthopteridae), Megakhosarodes vosgesicus sp. nov. (Megakhosaridae), Dorniella elcanoides sp. nov., D. apectinata sp. nov., D. diluta sp. nov., D. ovalis sp. nov., Baharellinus umbrosus sp. nov. Embigryllus shcherbakovi gen. et sp. nov., and Vosgesopterum arzvillerensis gen. et sp. nov. (Blattogryllidae).     

Aethophyllum BRONGNIART 1828, Conifère (non Équisétale)du Grès à Voltzia (Buntsandstein supérieur) des Vosges (France): Note préliminaire

AethophyllumBRONGNIART 1828 is a plant genus from the Voltzia Sandstones (Upper Bunter) of the Vosges which has been classified first into the Monocotyledons and than into the Equisetales. A careful study of new material shows that it actually is a Gymnosperm and more exactly a Conifer. Male cones found separately have already been described under the name Masculostrobus acuminatusGRAUVOGEL-STAMM and GRAUVOGEL, 1973. This Triassic plant presents simultaneously affinities with some Cordaites (Poacordaites) and with some Podozamites (P. schenki-agardhianus group of Harris 1935 + Swedenborgia).     

New Middle Permian insects from Salagou Formation of the Lodève Basin in southern France (Insecta: Pterygota)

Summary

New insects are described from the Middle Permian (Guadalupian) of Salagou Formation in the Lodève Basin (Languedoc region, France). Palaeopterans are represented by new odonatopterans viz. Huangiopterum lodevense n. gen., n. sp. and Huangiopterum species B, attributed to clade Panodonata (Huangiopteridae n. fam.), already recorded through the family Saxonagrionidae in the same formation, and a diaphanopterodean Martynovia cf. halli Beckemeyer 2004 (Martynoviidae) known from the Lower Permian of Oklahoma. Archaeorthopterans are supplemented by Bethouxia ariegensis n. gen., n. sp., Paralongzhua elongata n. gen., n. sp., Lodevolongzhua incompleta n. gen., n. sp., the caloneurodean Jarmiloptera mouralensis n. gen., n. sp., and a cnemidolestodean cf. Tococladus sp. (Tococladidae). Permophyllum rotundatum n. sp. (?Tettigoniidae) demonstrates the first presence of Orthoptera with wings probably mimicking Peltaspermales reproductive organs in Late Palaeozoic possibly analogous to the known crypsis of roachoid tegmina with pteridosperm pinnules. Frequent occurrence of hardly identifiable grylloblattid wing fragments support their significant role in term of abundance and diversity of the Permian faunas. New taxa based on wing venation pattern as Genera and species undetermined A, B (Liomopteridae), Permobaharellus salagousensis n. gen., n. sp. (family uncertain), Lodevophlebia reticulata n. gen., n. sp. (Sylvaphlebiidae), Oborella lodevensis n. sp. (Euryptilonidae), and Genus and species undetermined C, were described. Paoliida is represented by a paoliid gen. et sp. indet. and three anthracoptilids Strephocladus gandi n. sp., Strephocladus mouralensis n. sp., Lodevocladus subtilis n. gen., n. sp. The first record of miomopteran Palaeomantis sp. (Paleomanteidae) from Salagou Formation is presented. Acercarian insects are represented by the first record of Thripida and diverse new hemipterans, namely Euroscytina lutevanorum n. gen., n. sp. (Cicadomorpha: Scytinopteridae), Prosbole dio n. sp., Prosbole garrici n. sp., Pervestigia cf. veteris Becker-Migdisova 1961 (Prosbolidae), Archescytina species A (Paleorrhyncha: Archescytinidae) and Permopsyllidium lesclansis n. sp. (Sternorrhyncha: Psylloidea: Protopsyllidiidae). Entomofauna from the Salagou Formation demonstrate highly diverse insect communities with some taxa linked to early and late Permian ones known from assemblages in Euramerica and Russia, such as Obora (Czech Republic), Wellington Formation (Kansas and Oklahoma, USA), and Tshekarda (Ural, Russia).     

A traversodont cynodont from the Middle Triassic (Ladinian) of Baden-Württemberg (Germany)

Nanogomphodon wildi n. gen., n. sp. is based on a tiny lower postcanine tooth from the lower Lettenkeuper (Lower Keuper or Erfurt Formation; Ladinian) of Michelbach an der Bilz (Baden-Württemberg). It represents the first record of a traversodont cynodont from the Middle Triassic of Europe and exhibits a distinctive combination of dental features. Along with recent discoveries of other traversodont taxa from the Upper Triassic of eastern North America,Nanogomphodon indicates the existence of a distinct lineage of these cynodonts in the Northern Hemisphere.      

The nassariids from the Gulf of Gabès revisited (Neogastropoda,Nassariidae)

Since the latter half of the nineteenth century, marine biologists have recognized that many molluscs living in the Gulf of Gabès, on the southern coast of Tunisia, exhibit a number of morphological characters that set them apart from the ‘typical form or variety’ that occurs in the rest of their Mediterranean distribution area. In the family Nassariidae, local forms (varieties or subspecies) were recognized as early as 1882, but none of these is currently recognized as having taxonomical significance. We have revisited the species-level systematics of the family using an integrative approach, based on morphological, geographic and molecular evidence (COI and 28S). Besides Tritia gibbosula (not sampled by us), we delimitated seven species, three with a broad range: Tritia neritea (probably introduced), T. mutabilis (but with considerable genetic structure between localities), and T. corniculum; and four not previously recognized as valid, and which may be considered Gulf of Gabès endemics: T. lanceolata, T. tenuicosta, T. pallaryana sp. nov. and T. djerbaensis sp. nov. Also, Tritia elongata is recognized as a valid species in the T. corniculum complex, with a distribution outside the Gulf of Gabès. It is remarkable that all have paucispiral protoconchs indicating non-planktotrophic larval development.

http://zoobank.org/urn:lsid:zoobank.org:pub:069F3B3B-66E8-4C07-A974-3023924426EB     

The late Miocene mammals from the Konservat-Lagerstätte of Saint-Bauzile (Ardèche,France)

Diatomite deposits of Saint-Bauzile near Privas (Ardèche) in southern France have been known since more than two centuries for abundant and extremely well-preserved fossils of plants and animals. The radiometric dating brackets fossil-bearing horizons between 7.2 and 7.6 Ma, which is consistent with the biochronologic age given by fossil mammals, which are characteristics of the late MN11 zone, i.e. the second part of the late Miocene. The main interest of this site for mammals is that they are preserved almost “in the flesh”, as entire skeletons with bones in their anatomical connection, and often with skin and fur charred and forming a halo around the body. In this work, we studied the remains of a lagomorph, two rodents, an equid, a suid, a bovid and a rhino. The mode of preservation of mammals as entire bodies suggests sudden death and rapid burial of individuals.     

The Miocene mammal record of the Vallès-Penedès Basin (Catalonia)

The land mammal record of the Vallès-Penedès Basin (Catalonia, NE Spain) ranges from the early Miocene (Ramblian) to the late Miocene (Turolian), that is from about 20 to 7 Ma. Here we present an updated review of the mammal succession focusing on biochronology as well as on environmental and faunal changes. Based on faunal similarities with central Europe, we interpret this basin as a transitional zone between the forested environments of northern regions and the more arid landscapes of the inner Iberian Peninsula. The quality of the Vallès-Penedès record and its chronostratigraphic control is clearly better for the late Aragonian and the Vallesian (between 12.6–9.0 Ma), especially for small mammals. Therefore, we analyze small mammal diversity dynamics during this interval. Contrary to previous analyses, which found an abrupt extinction event coinciding with the early/late Vallesian boundary (the Vallesian Crisis), our results show that this pattern is due to uneven sampling. Instead, taxonomic richness slowly decreased since the late Vallesian as a result of a series of extinctions that mostly affected forest-dwelling taxa.     

The scimitar-toothed cat Machairodus aphanistus (Carnivora: Felidae) in the Vallès-Penedès Basin (NE Iberian Peninsula)

Here, we revise all the published and unpublished scimitar-toothed cat remains from the Vallès-Penedès Basin (NE Iberian Peninsula), in order to confirm their taxonomic attribution to Machairodus aphanistus as well as to provide more precise information about its chronological distribution in this basin. The studied material (including dentognathic as well as postcranial remains) comes from the following localities: Can Mata indeterminate (late MN7+8 or MN9), Creu Conill 22 (MN9), Can Poncic 1 (MN9), Can Llobateres 1 (MN9), Santiga (MN9), La Tarumba 1 (MN10), Viladecavalls (MN10), Ronda Oest Sabadell ROS-D3 (MN10), and Torrent de Febulines (MN10). Most of the studied material fits well with the morphologic and metrical features characteristic of the Vallesian species M. aphanistus, with the exception of the remains from Creu Conill 22 (an undescribed partial P4 formerly attributed to this taxon), which belongs in fact to a medium-sized hyaenid. From a biostratigraphic viewpoint, the removal of the Creu Conill material from the hypodigm of M. aphanistus has important implications, because this locality (11.1 Ma) was considered to record the first appearance datum of this taxon in the Vallès-Penedès Basin. However, the report of a previously unpublished talus from Can Mata (late MN7+8 or MN9) indicates that this taxon was present in this basin at least by the earliest Vallesian. Therefore, our results indicate that the first appearance datum of Machairodus in the Vallès-Penedès Basin might be somewhat younger than previously assumed, although dating uncertainties for the Can Mata remains preclude a more precise assessment. In contrast, the new mandibular remains from ROS-D3 (MN10) are likely coeval with those from La Tarumba 1, with the last appearance datum of M. aphanistus in the Vallès-Penedès Basin corresponding to Torrent de Febulines (ca. 9.1 Ma). The postcranial material described from various Vallès-Penedès localities further indicates that M. aphanistus displayed less cursorial adaptations than its purported descendant Homotherium.     

New Pseudaelurus and Styriofelis remains (Carnivora: Felidae) from the Middle Miocene of Abocador de Can Mata (Vallès-Penedès Basin)

New remains of felid jaws and teeth are described from several localities of the local stratigraphic series of Abocador de Can Mata (ca. 11.9 to 11.6 Ma, Middle Miocene; Vallès-Penedès Basin, Catalonia, Spain). Three different taxa are identified: Styriofelis turnauensis, Pseudaelurus romieviensis and Pseudaelurus quadridentatus. The described remains of P. romieviensis enable extending considerably the chronological range of this species in the Iberian Peninsula, in agreement with its record in the rest of Europe. Moreover, it is shown for the first time that P. romieviensis may possess a p2. The presence of this tooth therefore does not constitue a valid diagnostic feature to distinguish P. romieviensis from P. quadridentatus.     

New dental remains of Hispanopithecus laietanus (Primates: Hominidae) from Can Llobateres 1 and the taxonomy of Late Miocene hominoids from the Vallès-Penedès Basin (NE Iberian Peninsula)

Here we report 12 teeth of the fossil great ape Hispanopithecus (Hominidae: Dryopithecinae: Hispanopithecini), recovered in 2011 from the locality of Can Llobateres 1 (MN9, early Vallesian, Late Miocene, ca. 9.7 Ma [millions of years ago]) in the Vallès-Penedès Basin (Catalonia, Spain). Besides an isolated dP³ from layer CLL1.1b in the eastern (classical) sector of the site, all of the remaining teeth come from facies CLL1.0 (roughly equivalent to CLL1.2 and CLL1.1b), located in the newly excavated western sector, and representing at least two different individuals. Based on facet congruence and degree of wear, all of the upper cheek teeth, a central incisor and a lateral incisor most likely correspond to a single young adult individual of unknown sex, whereas a very worn I² and a female C¹ represent one or two additional individual(s). Morphological and metrical comparisons allow us to attribute these remains to Hispanopithecus laietanus, which is the single hominoid species recognized at CLL1. The newly described teeth represent a significant addition to the hypodigm of this taxon, enabling us to more completely assess the degree of variation displayed by several teeth. In light of the new specimens, the previous tooth position assignment of several upper molars from Can Llobateres and Can Poncic is revised, and the criteria employed to distinguish Hispanopithecus crusafonti from H. laietanus are critically evaluated. On the basis of the available upper cheek teeth from these localities, a distinction at the species level between both samples is tentatively favored, mainly on the basis of P³, M¹ and M² proportions as well as I¹ lingual morphology and proportions. The results of the 2011 field season unambiguously confirm that hominoid-bearing fossiliferous layers from CLL1 are not exhausted. Additional excavations at this site are promising for the discovery of additional remains of H. laietanus in the near future.     

Middle Pleistocene Human Remains from Tourville-la-Rivière (Normandy,France) and Their Archaeological Context

Despite numerous sites of great antiquity having been excavated since the end of the 19th century, Middle Pleistocene human fossils are still extremely rare in northwestern Europe. Apart from the two partial crania from Biache-Saint-Vaast in northern France, all known human fossils from this period have been found from ten sites in either Germany or England. Here we report the discovery of three long bones from the same left upper limb discovered at the open-air site of Tourville-la-Rivière in the Seine Valley of northern France. New U-series and combined US-ESR dating on animal teeth produced an age range for the site of 183 to 236 ka. In combination with paleoecological indicators, they indicate an age toward the end of MIS 7. The human remains from Tourville-la-Rivière are attributable to the Neandertal lineage based on morphological and metric analyses. An abnormal crest on the left humerus represents a deltoid muscle enthesis. Micro- and or macro-traumas connected to repetitive movements similar to those documented for professional throwing athletes could be origin of abnormality.     

Histology of the reproductive tissue of the clam Ruditapes decussatus from the gulf of Gabès (Tunisia)

Summary

The gametogenic cycle of the clam Ruditapes decussatus was investigated during one year. Samples were collected each month in two different sites located at the gulf of Gabès area. Gametogenic activity was characterized on the basis of histological analysis of the gonads. A classification and a scoring system were then proposed. According to our study, Ruditapes decussatus gametogenesis can be divided in four major steps: (1) a sexual rest (December- February), (2) starting of gametogenesis (February-March), (3) development (March-May), (4) ripe (from April onwards). This study revealed that the gonad of the clam Ruditapes decussatus was surrounded by muscular tissue which could represent the principal storage tissue. Two kinds of hermaphroditism appeared since maturity of gonads: simultaneous one showing gonadal tubules of both males and females in regionally distinct and separate zones and a “superposed” one showing a gonad consisting essentially of mature male gametes and few residual oocytes.     

Dinosaur footprints from the Early Jurassic of Le Mazel (Lozère,Southern France)

During the 20^th century, the first dinosaur tracks of the Causses Basin were identified at Saint-Laurent-de-Trèves, in the Parc National des Cévennes (southern France). A recent excavation reveals a new theropod tracksite in the Hettangian deposits from Le Mazel, 2 km from the historical tracksite at Saint-Laurent-de-Trèves. The tracks are here described combining a biometric approach and 3D imaging photogrammetry. The main track-bearing surface bears 64 in situ tridactyl footprints preserved as concave epireliefs. Two morphotypes were identified, a “Grallatorid” morphotype and a “Kayentapus” morphotype. Footprints belonging to the first morphotype are closely similar to Grallator lescurei, Grallator minusculus, and Grallator sauclierensis. This study shows the difficulty to distinguish quite similar tridactyl tracks from an ichnotaxonomic point of view and highlights the importance of detailed biometric comparisons. Tracks are preserved in a brown to yellowish dolomudstone showing abundant cryptalgal laminites and mud cracks. These deposits were accrued in shallow environments such as intertidal and supratidal zones of a tidal flat.     

The status of the sauropterygian reptilePartanosaurus zitteli Skuphos from the Middle Triassic of the Austrian Alps,with comments onMicroleptosaurus schlössen Skuphos

Partanosaurus zitteli Skuphos 1893 from the Ladinian (Partnachschichten) of the northern Alps (Vorarlberg, Austria) is identified as a junior synonym ofSimosaurus gaillardoti Meyer 1832. Its occurrence in the Germanic Basin (Upper Muschelkalk) predates its appearance in the Alpine Triassic, and suggests faunal interchange between these two faunal provinces during Middle and Upper Ladinian times.Microleptosaurus schlossen Skuphos 1893 is represented by very incomplete material only and must be treated as a nomen dubium.     

Taxonomy of a platy coral association from the Late Cenomanian of the southern Corbières (Aude,France)

The Upper Cenomanian cover of the Palaeozoic Mouthoumet Massif (southern Corbières, Aude, France), on the southern flank of the Bézu anticline, shows accumulations of large platy corals. However, while being already presented in stratigraphic, palaeoecological and sedimentological contexts, these organisms have not been the subject of a palaeontological study. The coral fauna encompasses 16 species of the families Leptophylliidae, Microsolenidae, and Siderastraeidae and is here presented in detail.     

Variation of metallothioneins in gills of the clam Ruditapes decussatus from the Gulf of Gabès (Tunisia)

Cadmium (Cd) and metallothionein (MT) concentrations were determined in the subcellular fractions of the gills of the clam Ruditapes decussatus. Clams were collected monthly during the period of sexual development (from June to August 2001) from two different sites situated in the Gulf of Gabès (Tunisia). These sites differ by their degree of metal contamination. Differences in condition index (CI) were observed in June and August between clams from both sites. In clams from both sites, cadmium was approximately equally distributed between the soluble (S1) and insoluble (C1) fractions. MT levels varied according to month but not sex. Site and body mass of clams seem to be important factors to explain the variation of MT levels compared to cadmium.