Wildungenichthys grossi n. gen., n. sp. — a new selenosteid arthrodire (Placodermi, Arthrodira) from the Kellwasserkalk (late Frasnian, Upper Devonian) of Bad Wildungen (Hessen, W-Germany)

A new arthrodire genus and species,Wildungenichthys grossi, is described from the Frasnian Kellwasserkalk of Bad Wildungen (W-Germany) from an incomplete skull with parts of the mandible and shoulder girdle. The new taxon is unique in a number of features, including the loss or probable fusion of the postmarginal, strong reduction of infraorbital sensory line canal on suborbital, firm connection of the cheek and skull roof and an unusual configuration of the cheek bones. It is an advanced pachyosteomorph eubrachythoracan and is referred to the Selenosteidae, showing close resemblances toEnseosteus.     

New teleostean fishes from the Jurassic of southern Germany and the systematic problems concerning the ‘pholidophoriforms’

A new genus,Siemensichthys, from the Upper Jurassic of southern Germany is described. The new genus includes two species,S. macrocephalus (Agassiz) which was formerly in the genusPholidophorus, andS. siemensi n. sp. The two species share synapomorphies such as only one supramaxillary bone covering the dorsal margin of the maxilla. Both species are described, and their phylogenetic position is analyzed. The phylogenetic analyses, based on 27 taxa and 141 characters, show thatAnkylophorus from the Kimmeridgian of Cerin,Siemensichthys andEurycormus from the Solnhofen Lithographic Limestone of Bavaria, form a monophyletic group. The new extinct clade (preliminarily identified as theSiemensichthys- group) is proposed as the sister-group ofPholidophorus s. str. plus more advanced teleosts. This sister-group relationship is supported by eight characters (e.g., supraoccipital bone extending forward in the roof of the otic region; articular bone fused with both the angular and retroarticular; presence of an elongated posteroventral process of quadrate; presence of dorsal processes at the base of the innermost caudal rays of upper lobe; mobile premaxillary bone). Comparisons with species ofPholidophorus s. str. provide a new understanding of the genusPholidophorus. At least four synapomorphies are proposed to support the monophyly ofPholidophorus. As a consequence of this new interpretation, the European Late Jurassic species previously assigned to the Pholidophoridae and to the genusPholidophorus (e.g., ‘Ph.’armatus, ‘Ph.’ falcifer, ‘Ph.’ micronyx, ‘Ph.’ microps) should be reexamined because they do not belong to the family nor to the genus. The order PholidophoriformesBerg is not a monophyletic group as currently constructed. Therefore, all so-called pholidophoriforms are in need of revision.     

Description of two new species of Santelmoa (Teleostei, Zoarcidae) from the Southern Ocean

Detailed examination of eelpouts in collected material from the Gerlache Strait and the Bellingshausen Sea, during the Spanish Antarctic Expeditions Bentart 03 and Bentart 06, and from the Bransfield Strait, during the Danish Galathea 3 Expedition, at depths between 1,056 and 1,837?m, revealed two undescribed species of Santelmoa Matallanas 2010. Herein, Santelmoa fusca sp. nov. and Santelmoa antarctica sp. nov. are described on the basis of twelve specimens. Santelmoa fusca can be separated from all other Santelmoa species by the following characters: mouth terminal; two posterior nasal pores; lateral line double; two irregular rows of palatine teeth; dorsal fin rays 109–113; anal fin rays 88–94; vertebrae 27–29?+?87–91?=?114–118; two pyloric caeca well developed; scales reduced to tail; pelvic fins and vomerine teeth present. Santelmoa antarctica can be separated from all other Santelmoa species by the following characters: mouth subterminal; two posterior nasal pores; suborbital pores seven (6?+?1); lateral line double; single row of palatine teeth; supraoccipital dividing the posterior end of frontals; central radials notched; dorsal fin rays 109–112; anal fin rays 89–93; vertebrae 27?+?89–92?=?116–119; two pyloric caeca well developed; scales, ventral fins and vomerine teeth present. Santelmoa fusca and S. antarctica can readily be separated from each other by squamation (reduced to tail vs. on the tail and on the posterior part of body); suborbital pore pattern (6?+?0 vs. 6?+?1), as well as several morphometric characters. The relationships of the two new species with congeners are discussed.     

Comparative morphology and development of bony elements in the head region in three species of Japanese catfishes (Silurus: Siluridae; Siluriformes)

The shape and development of bony elements of the neurocranium and suspensorium were studied in three species of Japanese catfish (Silurus) from the viewpoint of comparative morphology. InS. asotus andS. biwaensis the order of appearance of the bony elements was similar, but the ossification of most elements was delayed inS. lithophilus. The neurocranium and Suspensorium of adultS. lithophilus retain juvenile features compared with the other two species. On the other hand, in the skull ofS. biwaensis the sagittal crest of the supraoccipital, the ridge of the pterotic, and the hyomandibular process are more developed than in the other two species.     

Ultrastructure of the spermatozoon of Lepidogalaxias salamandroides and its phylogenetic significance

The spermatozoon of Lepidogalaxias salamandroides possesses an acrosome (putative), one or two perforatoria (putative) but no nine-triplet centrioles. Two elongated mitochondria (12 μm long) are situated in parallel between the nucleus (20 μm long) and the axoneme (53 μm long). The above features are unique among other teleosts with internal fertilization. The presence of an “acrosome” in this primitive teleost supports the hypothesis that this structure has been secondarily lost in teleosts during evolution. The uncertainty of phylogenetic placement of this fish is reflected by its unique sperm ultrastructure.     

An Additional Baurusuchid from the Cretaceous of Brazil with Evidence of Interspecific Predation among Crocodyliformes

A new Baurusuchidae (Crocodyliformes, Mesoeucrocodylia), Aplestosuchus sordidus, is described based on a nearly complete skeleton collected in deposits of the Adamantina Formation (Bauru Group, Late Cretaceous) of Brazil. The nesting of the new taxon within Baurusuchidae can be ensured based on several exclusive skull features of this clade, such as the quadrate depression, medial approximation of the prefrontals, rostral extension of palatines (not reaching the level of the rostral margin of suborbital fenestrae), cylindrical dorsal portion of palatine bar, ridge on the ectopterygoid-jugal articulation, and supraoccipital with restricted thin transversal exposure in the caudalmost part of the skull roof. A newly proposed phylogeny of Baurusuchidae encompasses A. sordidus and recently described forms, suggesting its sixter-taxon relationship to Baurusuchus albertoi, within Baurusuchinae. Additionally, the remains of a sphagesaurid crocodyliform were preserved in the abdominal cavity of the new baurusuchid. Direct fossil evidence of behavioral interaction among fossil crocodyliforms is rare and mostly restricted to bite marks resulting from predation, as well as possible conspecific male-to-male aggression. This is the first time that a direct and unmistaken evidence of predation between different taxa of this group is recorded as fossils. This discovery confirms that baurusuchids were top predators of their time, with sphagesaurids occupying a lower trophic position, possibly with a more generalist diet.     

Morphological studies on the genusClematis Linn

While the axes of branched axillary inflorescences seen in most species ofClematis show fundamentally the same features in nodal vasculature as the vegetative stems, those of simple axillary inflorescences, having only a pair of opposite sterile bracts at specific positions, exhibit an exclusive feature in nodal vasculature because they have entirely lost lateral branches or buds in the bract axils. Noticeably, at the nodal level of the axis of the simple inflorescence ofC. japonica andC. Williamsii, trace bundles to the missing lateral branches are formed and extend unaltered beyond the node. Thus, in these two species stelar bundles in the inflorescence axis generally increase in number upwardly from six to eight or more through the node with sterile bracts. On the basis of both anatomical and morphological data, a probable evolutionary trend in floral shoots with simple axillary inflorescences is proposed. The type of floral shoot ofC. tosaensis bearing simple, scale-subtended and basally fascicled inflorescences is the most primitive and constitutes an initial phase of evolution, and progressive changes in a kind of inflorescence-subtending leaves as well as in the shape and position of the sterile bracts resulting in the type of floral shoot ofC. japonica and further in that ofC. obvallata. A floral shoot ofC. Williamsii follows another line of evolution from an ancestral type similar to that ofC. tosaensis.     

Innervation of the lateral line system in Rhyacichthys aspro: the origin of superficial neuromast rows in gobioids (Perciformes: Rhyacichthyidae)

The lateral line system and its innervation were examined in the most primitive gobioid taxon, Rhyacichthys aspro (Rhyacichthyidae). The infraorbital canal was present, whereas superficial neuromast rows a and c, typically present on the cheek of gobioids, were absent. Because the infraorbital canal (absent in other gobioids) and the two rows were commonly innervated by the buccal ramus, the latter were categorized as replaced rows from canal neuromasts. On an innervation basis, rows b and d on the cheek were considered to comprise superficial neuromasts only in all gobioids. The trunk lateral line system comprised canal and superficial neuromasts, the former being included in the lateral line scales (each bearing 1–7 neuromasts arranged longitudinally along the direction of a groove). Absence of bony roofs in the lateral line system was proposed as a synapomorphy of Gobioidei, and a progressive neotenic shift in the lateral line system of the suborder discussed.     

Ausgangsform und Entwicklung der rhombischen Schuppen der Osteichthyes (Pisces)

Ganoid and cosmoid scales, the two types of rhombic scales within the osteichthyans, can be traced back to a primitive scale similar to the scales ofLophosteus. The primitive rhombic scale did not have a peg-and-socket articulation, it is composed of lamellar bone superposed by many layers of spongy bone + dentine. That kind of superposition of layers of spongy bone + dentine (+ enamel) has been retained in the cosmoid scale; in contrast in the ganoid scale the growth of the dentine has become restricted to the lateral surface, the growth of ganoin to the outer surface and the growth of bone to the inner surface of the scale. The scales ofAndreolepis have a position between the primitive rhombic scale and the ganoid scale. — Scales from the Gedinnian (Lower Devonian) of New Sibirian Islands, USSR, are described asDialipina markae n. sp. The morphological features are very typical for the genus, but the histology is different from the type speciesD. salgueiroensis. Within the two Devonian palaeoniscoid generaDialipina andOrvikuina acellular bone with irregular non-vascular canals of Williamson has developed twice from cellular bone.     

Bibarba bibarba: A new genus and species of Cobitinae (Pisces: Cypriniformes: Cobitidae) from Guangxi Province (China)

A new genus of Cobitinae, Bibarba gen. n., and a new species, B. bibarba sp. n., were discovered and are described for the Chengjiang River, a tributary of the Hongshuihe River in Guangxi Province of southern China. This river region is characterized by a Karst landscape, and the river that is inhabited by the new genus is a slowly moving stream with arenaceous and cobblestone beds. The new genus resembles Cobitis Linnaeus, 1758 (subfamily Cobitinae) in the shape and pigmentation pattern of their body, the absence of scales on their head, and the presence of a suborbital spine, but differs from it by a single Lamina circularis on the third pectoral fin ray instead of on the base of the second pectoral fin ray; two pairs of barbels (one rostral pair and one maxillo-mandibular pair) instead of three pairs of barbels (one rostral pair, one maxillary pair, and one maxillo-mandibular pair); a relatively thick and short suborbital spine with a strong medio-lateral process instead of a suborbital spine without or with a weakly formed medio-lateral process as in Cobitis; and the lack of a black stripe extending from the occiput through the eye to the insertion of the rostral barbel. The first two characters have not been reported in any other genus of the subfamily Cobitinae. A morphometric character analysis based on PCA reveals differences between B. bibarba and C. sinensis in body size, barbel length, interorbital width, pectoral fin length in males, and the position of the dorsal and ventral fins. Type specimens of the new species are kept in the Freshwater Fishes Museum of the Institute of Hydrobiology at the Chinese Academy of Sciences in Wuhan, Hubei Province.     

Midribs of cycad pinnae

Comparisons of midribs of three cycad genera,Chigua, Cycas, andStangeria, the only three genera characterized by midribs in the pinnae, show that those ofChigua andStangeria are very similar to each other and quite unlike those ofCycas. Midribs ofCycas include a single, median vein, and the pinnae of these species lack lateral veins. Pinnae midribs ofChigua andStangeria include several (2–5 and 2–8, respectively) longitudinal parallel veins, and dichotomizing lateral veins arising from the midrib. Pinnae of other cycads, includingZamia, with whichChigua appears to be most closely allied, exhibit evenly spaced, longitudinally parallel, dichotomizing veins, a character considered to be primitive. All veins in cycad leaves have a single mesarch protoxylem pole. The midrib condition inChigua andStangeria represents an advanced state in comparison to that in the leaf of the Marattiales, for example, where there is a single veined midrib but with numerous mesarch protoxylem poles. It would appear that the midrib has been derived independently at least three times within the cycads, once in each major group.     

Reevaluation of the caudal skeleton of some actinopterygian fishes: II. Hiodon,Elops, and Albula

The vertebral centra of Hiodon, Elops, and Albula are direct perichordal ossifications (autocentra) which enclose the arcocentra as in Amia. An inner ring of ovoid cells forms in late ontogeny from the intervertebral space inside the autocentrum. The chordacentrum is reduced or completely absent in centra of adult Elops, whereas it forms an important portion of the centra in adult Hiodon. The posterior portion of the compound ural centrum 3+4+5 is partially (Hiodon) or fully formed by the chordacentrum (Elops, Albula). The haemal arches and hypurals are fused medially by cartilage or bone trabecles of the arcocentrum with the centra, even though they appear autogenous in lateral view in Elops and Albula. The composition of the caudal skeleton of fossil teleosts and the ontogeny of that of Hiodon, Elops, and Albula corroborate a one-to-one relationship of ural centra with these dorsal and ventral elements. The first epural (epural 1) of Elops relates to ural centrum 1, whereas the first epural (epural 2) of Hiodon and Albula relates to ural centrum 2. In Albula, the first ural centrum is formed by ural centrum 2 only. With 4 uroneurals Hiodon has the highest number within recent teleosts. Juvenile specimens of Hiodon have eight, the highest number of hypurals within recent teleosts; this is the primitive condition by comparison with other teleosts and pholidophorids. Reduction of elements in the caudal skeleton is an advanced feature as seen within elopomorphs from Elops to Albula. Such reductions and fusions occur in osteoglossomorphs also, but the lack of epurals and uroneurals separates most osteoglossomorphs (except Hiodon) from all other teleosts.     

Electron microscopic studies of the corpuscles of Stannius of an airbreathing teleost (Heteropneustes fossilis)

The ultrastructure of the corpuscles of Stannius (CS) ofHeteropneustes fossilis reveals a homogenous cellular composition characterized by only one cell type, with large secretory granules and abundant ribosomal endoplasmic reticulum. These cells are comparable to the type 1 cell described in the CS of other teleosts; type 2 cells, whose presence is ubiquitous in the CS of freshwater species are absent inH. fossilis. Our data on the CS ofH. fossilis demonstrate that not all freshwater species possess type 2 cells in their CS and these are not essential for life in freshwater.     

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.     

What isIvanantonia efremovi (Rodentia, Mammalia)?

Ivanantonia efremovi Shevyreva 1989, known from the Tsagan Khushu locality (Early Eocene of Mongolia), erroneously has been described asOrogomys obscurus Dashzeveg 1990. This form shows an interesting association of primitive and derived characters: the enamel of the incisors is two-layered and has pauciserial Hunter-Schreger bands in portio interna; the lower tooth row has only three jugal teeth; the tooth pattern of lower molars is primitive and looks very similar to that ofAlagomys, but the trigonid is less reduced with regards to the talonid. It also differs from other primitive rodents in the distribution of wear facets, suggesting that mandibular propalineal movement was pre-eminent during chewing. Comparisons ofIvanantonia with several Eocene-Oligocene rodents indicate possible relationships to the Early Oligocene North American genusNonomys.     

Sexual dimorphism in a Lower Miocene moronid?

A series of questionable elements in certain specimens ofMorone cf.aequalis (Koken 1891) from Lower Miocene deposits near the village of Berkersheim, N of Frankfurt a. M. (Hessen, Germany) is described, which has not been known from any other percoid before. These elements are fully ossified and cover the cheek and the preopercular region. Even within well-preserved material, they are only present in some specimens. Therefore, they may be specialized structures that are indicative for sexual dimorphism. Nevertheless, they clearly differ from all other respective structures that have been described from teleosts: Multicellular epidermal horny tubercles (“breeding tubercles”) mainly consist of keratine and not of calciumphosphate. By contrast, contact organs consist of bone and are located mainly at the surface of the fin rays and scales, respectively. At present, “breeding tubercles” are the favorite interpretation and the original substance may have been replaced via post-mortem phosphatization.     

Halichoeres bleekeri (steindachner & döderlein), a valid japanese species of labrid fish, distinct fromH. tenuispinis (günther) from china

Halichoeres bleekeri (Steindachner &; Döderlein, 1887), previously regarded as a junior synonym ofH. tenuispinis (Günther), is a valid species. It is distinct fromH. tenuispinis in nearly always having 13 instead of 14 pectoral rays. 11–15 instead of 7–11 suborbital pores, longer dorsal soft rays (1.95–2.3 in head length vs 2.25–2.4 fortenuispinis). and some features of color such as the absence of a dark spot at the upper base of the caudal fin of the female.H. tremebundus Jordan and Snyder, 1902 is a synonym ofH. bleekeri based on the female form, andArtisia festiva de Beaufort is a synonym ofH. tenuispinis, also described from the female phase,H. bleekeri is known from Korea and in Japan from Tokyo to the Izu Islands.H. tenuispinis is recorded from Hong Kong and Xiamen. China, and Taiwan. Records ofH. tenuispinis from the Philippines by Fowler and Bean (1928) represent misidentifications ofH. papilionaceus (Valenciennes).     

Ostéologie et position systématiquedu genre Thrissops Agassiz, 1833 (sensu stricto) (Jurassique supérieur de l'Europe occidentale) au sein des Téléostéens primitifs

The osteological study of the genus ThrissopsAgassiz, 1833 (sensu stricto) from the Upper Jurassic of Germany and France allows to define the systematic position of that fossil fish within the primitive Teleosts. The general shape of the skull, the jaws, the ethmoidal area, the circumorbital bones, the fronto-parieto-supra occipital area, the parasphenoid and the opercular bones are all characters which prove that Thrissops belongs to the family Ichthyodectidae (order Ichthyodectiformes, super-order Osteoglossomorpha). However Thrissops is more primitive than the other Ichthyodectidae which are all of Cretaceous age. It possesses indeed two parietals bearing pit-lines, a premaxillary and a maxillary normally developed, a palatine and a metapterygoid without any contact, a denticulated entopterygoid, three free epurals and six uroneurals, while, in the Cretaceous Ichthyodectidae, the parietals are fused in one bone without any pit-line, the premaxillary and the maxillary are hypertrophic, the palatine touchs the metapterygoid, the entopterygoid is toothless, the epural disappear or fuse with the terminal neural arches to form supplementary neural spines, and the uroneural are only five.