The erectile cheek-spine apparatus in the bristlenose catfish Ancistrus (Loricariidae, Siluriformes), and its relation to the formation of a secondary skull roof

In the South American catfish family Loricariidae, the opercle has been decoupled from the lower jaw, and has also lost its function in expiration. While many loricariid species have a small and slightly mobile opercle with reduced opercular musculature, within the hypostomine subfamily a novel opercular mechanism has developed that erects a tuft of enlarged odontodes anterior to the opercle. This defensive mechanism is examined in Ancistrus cf. triradiatus. The opercle has a prominent anterior process and the orientation of the reinforced articulation hinge to the hyomandibular bone has shifted. The opercular musculature is well developed, with a hypertrophied dilatator operculi that extends deep inside the skull roof bones and toward the midline, over the brain, but below the superficial skull roof. Hence the frontal, sphenotic, parieto-supraoccipital and compound pterotic bones consist of a dorsal, superficial part and a deeper part separating the brain from the muscle: two functional skull roofs are thus formed. The impact on the path of the cranial sensory canals is substantial, moving canals away from the skull surface. Hypertrophy of cranial muscles is known from many teleosts, but the invasion of such large muscles into the skull, which is drastically modified and literally hollowed out, has never been described before. These cranial modifications are greater in males than in females, related to the territorial behavior of the former, in which the erectile spines are usually used.     

A partial skull roof of an embolomere from Linton,Ohio (Middle Pennsylvanian) and its phylogenetic affinities

Among the famous Middle Pennsylvanian tetrapod fauna from Linton, Ohio, embolomeres are extremely rare and known only from three snout fragments which are referred to as the eogyrinid Leptophractus obsoletus. We describe herein a skull roof fragment from Linton that consists of the left orbital and cheek region and parts of the palate preserved in dorsal view, which belonged to a skull of approximately 100 mm length. Although diagnostic parts such as the tabular horn and the otic region are not preserved, it can be assigned to embolomeres by its attenuated, irregular dermal bone sculpture. The specimen can be interpreted most plausibly as an eogyrinid because of (1) the distinct, mostly continuous lateral lines that appear like a string of beads due to the subdued ridges on their bottom, and (2) the kinetic line between skull table and cheek in combination with the firm suture between the postorbital and intertemporal. The participation of the lacrimal in the anterior orbital margin is unusual for eogyrinids but might represent a juvenile character. Because the eogyrinid skull roof is derived from the same locality and strata as the eogyrinid L. obsoletus, we tentatively assign it to that genus and species.     

Mechanisms of mesendoderm internalization in the Xenopus gastrula: lessons from the ventral side.

Two main processes are involved in driving ventral mesendoderm internalization in the Xenopus gastrula. First, vegetal rotation, an active movement of the vegetal cell mass, initiates gastrulation by rolling the peripheral blastocoel floor against the blastocoel roof. In this way, the leading edge of the internalized mesendoderm is established, that remains separated from the blastocoel roof by Brachet's cleft. Second, in a process of active involution, blastopore lip cells translocate on arc-like trails around the tip of Brachet's cleft. Hereby the lower, Xbra-negative part of the lip moves toward the interior, to contribute mainly to endoderm. In contrast, the upper, Xbra-expressing part moves toward the blastocoel roof-apposed surface of the involuted mesoderm, and eventually becomes inserted into this surface. Vegetal rotation and active mesoderm surface insertion persist over much of gastrulation ventrally. Both processes are also active dorsally. In fact, internalization processes generally spread from dorsal to ventral, though at different rates, which suggests that they are independently controlled. Ventrally and laterally, mesoderm occurs not only in the marginal zone, but also in the adjacent blastocoel roof. Such blastocoel roof mesoderm shares properties with the remaining, ectodermal roof, that are related to its function as substratum for mesendoderm migration. It repels involuted mesoderm, thus contributing to separation of cell layers, and it assembles a fibronectin matrix. These properties change as the blastocoel roof mesoderm moves into the blastopore lip during gastrulation.     

Patterns and processes in the early evolution of the tetrapod ear

This article reviews some of the latest information on the evolution of the tetrapod ear region as seen in the fossil record. It looks at the changes that can be documented across the fish-tetrapod transition, the patterns that they show and what can be inferred of the processes that brought some of them about. These processes include an increased role for neural crest, and heterochronic processes such as pedomorphosis. The earliest tetrapods show a common pattern of a short stout stapes with a large stapedial foramen, that primitively contacted the palatal bones and probably supported the braincase. Modifications to this pattern can be seen in tandem with changes to the occiput and are bound up with changes to jaw and breathing mechanisms. By the Late Carboniferous, tetrapods had diversified into a range of groups showing a wide variety of otic morphologies, some of which were probably tympanic, while others were not, and some which are very different from those found in extant tetrapods. In amniotes, the evolution of a tympanic ear appears to correlate with consolidation and integration of the occiput to the skull roof. Competing phylogenies suggest different numbers of iterations for the origin of a tympanic ear, but a minimum of four separate occasions is implied.     

云南武定节甲类的新材料

文中描述了采自云南武定中泥盆统一新的属种Yinostius maior gen.et sp.nov.属于短胸节甲类Heterosteidae科,这类化石在我国系初次发现。     

Evolution of petal epidermal micromorphology in Leguminosae and its use as a marker of petal identity

Background and Aims

The legume flower is highly variable in symmetry and differentiation of petal types. Most papilionoid flowers are zygomorphic with three types of petals: one dorsal, two lateral and two ventral petals. Mimosoids have radial flowers with reduced petals while caesalpinioids display a range from strongly zygomorphic to nearly radial symmetry. The aims are to characterize the petal micromorphology relative to flower morphology and evolution within the family and assess its use as a marker of petal identity (whether dorsal, lateral or ventral) as determined by the expression of developmental genes.

Methods

Petals were analysed using the scanning electron microscope and light microscope. A total of 175 species were studied representing 26 tribes and 89 genera in all three subfamilies of the Leguminosae.

Key Results

The papilionoids have the highest degree of variation of epidermal types along the dorsiventral axis within the flower. In Loteae and genistoids, in particular, it is common for each petal type to have a different major epidermal micromorphology. Papillose conical cells are mainly found on dorsal and lateral petals. Tabular rugose cells are mainly found on lateral petals and tabular flat cells are found only in ventral petals. Caesalpinioids lack strong micromorphological variation along this axis and usually have only a single major epidermal type within a flower, although the type maybe either tabular rugose cells, papillose conical cells or papillose knobby rugose cells, depending on the species.

Conclusions

Strong micromorphological variation between different petals in the flower is exclusive to the subfamily Papilionoideae. Both major and minor epidermal types can be used as micromorphological markers of petal identity, at least in papilionoids, and they are important characters of flower evolution in the whole family. The molecular developmental pathway between specific epidermal micromorphology and the expression of petal identity genes has yet to be established.Key words: Epidermis, Fabaceae, Papilionoideae, Caesalpinioideae, Mimosoideae, petal surface, scanning electron microscopy, papillose conical cells, tabular rugose cells, tabular flat cells, organ identity     

A NEW PARASEMIONOTID-LIKE FISH FROM THE LOWER TRIASSIC OF JURONG, JIANGSU PROVINCE, SOUTH CHINA

Abstract:  Based on a well-preserved specimen from the Early Triassic Lower Qinglong Formation exposed at Qingshan Quarry, Jurong, Jiangsu Province of China, the new taxon Peia jurongensis gen. et sp. nov. is named and described with anatomical details of its dermal skull, neurocranium and postcranial skeleton. The new taxon is characterized by the following set of characters: shallow V-shaped, tuber-like rostral; anterior part of frontal widened to roughly same width as its posterior part; roughly squared parietal; supraorbital absent; wide and slightly posteriorly inclined preopercle; five small ossifications present in dorsal half of preopercle; preopercular canal shifting anteriorly in ventral half of the preopercle, and reaching the anteroventral corner of this bone; dermosphenotic joining the skull roof and with a descending lamina; numerous branchiostegal rays. Comparisons are made between the new taxon and several parasemionotids from the same locality; a discussion is carried out on the distribution and evolution of several characters in halecomorphs and other closely related neopterygians.     

A NEW DIPNOAN FISH FROM THE MIDDLE DEVONIAN (EIFELIAN) OF SCOTLAND

Abstract:  A new dipnoan fish, Pinnalongus saxoni gen. et sp. nov., is described from a suite of recently discovered specimens from Caithness and East Sutherland, northern Scotland. The stratum where Pinnalongus occurs is within the middle Eifelian of the Middle Devonian. Pinnalongus has a skull roof consisting of a mosaic of small bones at the anterior end, a feature more typically found in Early Devonian dipnoans. The posterior part of the skull roof is more typical of later advanced Middle Devonian dipnoans with the B-bone separating the I-bones. The postcranial body is now considered not to be so important with respect to the classification of dipnoans as originally proposed by Dollo in 1895, who thought there was an evolutionary transformation series. Nevertheless, the postcranial body of Pinnalongus has more in common with later Middle and Late Devonian dipnoans such as Scaumenacia , with a very long second dorsal fin. Based on the skull morphology, Pinnalongus is most closely related to Tarachomylax from the Lower Devonian of Severnaya Zemlya, Russia. Pinnalongus represents the earliest known complete articulated dipnoan with tooth plates.     

黑犀(奇蹄目,犀科)化石在中国的首次发现

黑犀(Diceros属)的惟一现生代表D.bicornis生活在非洲。该属在新近纪时期曾广泛分布于希腊、土耳其和伊朗等地区,但从未在东亚地区发现过。新种甘肃黑犀(Diceros gan- suensis sp.nov.)是该属在中国和东亚的首次发现。化石采自甘肃临夏盆地晚中新世柳树组中部。新种以尺寸较小、头型短、枕顶高耸、枕面窄而高、枕嵴无中沟、副枕突短小、下颌上升支距m3较近、前臼齿较小、DP1无后脊、P2原脊孤立、P2和P3后脊细窄而区别于东地中海地区的Diceros neumayri。D.neumayri的分类位置一直是一个争论的焦点,曾在黑犀(Diceros属)和白犀(Ceratotherium属)之间反复变更。研究显示,甘肃黑犀和D.neumayri的一系列共同的原始特征表明它们与更进步的白犀有明显的区别,应该归入黑犀属。     

Skull size and shape variation versus molecular phylogeny: a case study of alpine newts (<Emphasis Type="Italic">Mesotriton alpestris</Emphasis>, Salamandridae) from the Balkan Peninsula

We explored the phylogenetic signal of skull size and shape in alpine newts from the Balkans, a group of European newts that, in spite of their considerable phylogeographic substructuring (as inferred from previous DNA analyses), maintain a conserved phenotype. In terms of skull shape disparity, geometric morphometrics show that the dorsal cranium carries a significant phylogenetic signal, the most notable evidence in this present study. On the contrary, no phylogenetic signal in the shape of the ventral cranium was found. This result indicates that the variation in the shape of the ventral cranium is more prone to other factors and processes, such as adaptations to local environments rather than phylogenetic constraints. Variation in skull size within alpine newts seems to be independent from phylogenetic constraints.     

The subdivisions and fusions of the exoskeletal skull bones ofDiscosauriscus austriacus (Makowsky 1876) and their possible homologues in rhipidistians

Two localities in the Boskovice Furrow region of Moravia (Czecho-Slovakia) have produced new, well preserved material of the Lower Permian tetrapodDiscosauriscus austriacus (Makowsky 1876). A relatively large number of specimens have been found with some dermal skull roof bones partly or fully subdivided, and/or fused. These are the first records of such subdivisions and fusions in this tetrapod and the following bones are discussed: frontal, postfrontal, parietal, intertemporal, supratemporal, tabular and postparietal. The subdivided bones within the skull roof ofDiscosauriscus (and some dissorophoids) are situated at the same places as those found in Devonian rhipidistians, and may relate to the homology of the bones of the cranial exoskeletal roof inDiscosauriscus and in osteolepiforms. It shows that the “orthodox” terminology of the skull roof bones used in osteolepiforms is correct.     

The Fine Structure of Some Blood Vessels of the Earthworm, Eisenia foetida

The fine structure of the main dorsal and ventral circulatory trunks and of the subneural vessels and capillaries of the ventral nerve cord of the earthworm, Eisenia foetida, has been studied with the electron microscope. All of these vessels are lined internally by a continuous extracellular basement membrane varying in thickness (0.03 to 1 µ) with the vessel involved. The dorsal, ventral, and subneural vessels display inside this membrane scattered flattened macrophagic or leucocytic cells called amebocytes. These lie against the inner lining of the basement membrane, covering only a small fraction of its surface. They have long, attenuated branching cell processes. All of these vessels are lined with a continuous layer of unfenestrated endothelial cells displaying myofilaments and hence qualifying for the designation of "myoendothelial cells." The degree of muscular specialization varies over a spectrum, however, ranging from a delicate endowment of thin myofilaments in the capillary myoendothelial cells to highly specialized myoendothelial cells in the main pulsating dorsal blood trunk, which serves as the worm's "heart" or propulsive "aorta." The myoendothelial cells most specialized for contraction display well organized sarcoplasmic reticulum and myofibrils with thick and thin myofilaments resembling those of the earthworm body wall musculature. In the ventral circulatory trunk, circular and longitudinal myofilaments are found in each myoendothelial cell. In the dorsal trunk, the lining myoendothelial cells contain longitudinal myofilaments. Outside these cells are circular muscle cells. The lateral parts of the dorsal vessels have an additional outer longitudinal muscle layer. The blood plasma inside all of the vessels shows scattered particles representing the circulating earthworm blood pigment, erythrocruorin.     

纤细滇美龙(Dianmeisaurus gracilis Shang & Li,2015)新材料

根据一件产自云南罗平中三叠世关岭组Ⅱ段的新标本并结合产自相同地点和地层中的模式标本对纤细滇美龙(Dianmeisaurus gracilis Shang & Li,2015)进行了详细研究.原模式标本暴露其腹而,而新标本暴露其背面,两者互相补充提供了更完整、精确的纤细滇美龙解剖学信息.新材料揭示该种具有非常短小的吻部,眶前区的长度不仅短于眶后区长度,甚至短于眼眶的长度;外鼻孔小且位置靠前,即鼻孔前区的长度短于鼻孔后缘与眼眶前缘之间的距离;由两额骨构成的眼眶间隔非常狭窄,宽度小于顶骨平台宽度的1/3;额骨前后两端均具渐尖的突起;顶骨后部不收缩,顶骨平台后缘呈深V型.补充了新信息和包含更多属种(如Dawazisaurus)后的系统发育学分析支持了之前滇美龙和滇东龙互为姊妹群的结论,同时它们和马家山龙、滇肿龙、贵州龙和大洼子龙一起构成了一个仅由中国的属种组成的单系类群.与欧洲肿肋龙类群(Dactylosaurus,Anarosaurus,Serpianosaurus和Neusticosaurus)相比,这一单系类群与幻龙类有更近的亲缘关系.     

Tegumental ultrastructure of adult Gynaecotyla squatarolae (Digenea: Microphallidae)

Gynaecotyla squatarolae (Digenea: Microphallidae) adult flukes were recovered from experimental chicks at day 4-6 post-infection and their tegumental ultrastructure was observed with a scanning electron microscopy. They were pyriform in shape, and their anterior halves were concaved ventrally. The whole body surface was covered with tegumental spines, which were wide and 16-17 digitated between oral and ventral suckers. The density of spines and number of digits decreased posteriorly. The oral sucker was subterminal and the excretory pore was at the posterior end of the worm. Two ventral suckers were similar in appearance and protruded near midline of the worm. The genital atrium was dextral to the small ventral sucker. The dorsal surface was covered with tegumental spines, but the spines were sparser than on the ventral surface. On the middle portion of the dorsal surface, a small opening presumed to be the Laurer's canal was seen. From these findings, it has been confirmed that the adult G. squatarolae has unique characteristics in the surface ultrastructure.     

滇东中泥盆统的节甲鱼类化石

本文记述了节甲鱼类中称为北极鱼类的三个新属种:Exutaspis megista,Kunmingolepislucaowanensis,Yangaspis jinningensis,化石分别采自武定海口组(广义),海口和晋宁的海口组。代表我国中泥盆世该类化石鱼类的首次记述。     

A rhinesuchid-like temnospondyl from the Permo-Triassic of Uruguay

A new temnospondyl species, Arachana nigra, from the Permo-Triassic Buena Vista Formation of Uruguay is described. The holotypic and only known specimen consists of an almost complete skull lacking most of the snout, the tabular horns and the posterolateral corners of the skull table. As with other specimens from the same unit, Arachana shows a transitional morphology. It shares several characters with rhinesuchids, such as the large size and the general shape of the skull, orbits positioned slightly posterior to the skull roof mid-length, a coarsely pitted dermal ornamentation lacking pustules, and a smoothly convex cheek contour. The palatal ramus of the pterygoid suturing with the vomer, and excluding the palatine and ectopterygoid from the margin of the interpterygoid vacuity, and the presence of a small basioccipital, visible in both occipital and ventral view, also resemble the conditions found in rhinesuchids and other basal temnospondyls. Other characters present in Arachana, however, are commonly found in lydekkerinids, but are absent in almost all rhinesuchids: supratemporal excluded from otic notch; supraorbital and infraorbital sensory sulci encroaching the lacrimal, although lacking a step-like lacrimal flexure; otic notch not deeply incised; post-temporal fenestra large and rounded; occipital condyles well-separated from each other; palatine tooth row behind the palatine tusk reduced; pterygoid corpus slightly ornamented; and presence of an interorbital depression. This combination of primitive and derived characters is consistently present in most components of the Buena Vista fauna, which could thus be transitional between typical Permian and Triassic tetrapod communities found elsewhere. The location of the PTB in the Uruguayan sequence is controversial, mainly due to the lack of clear faunal correlations with other well-known sequences, such as those of southern Africa and Russia. Moreover, the mosaic-like character combinations in most of the recorded tetrapods ally them to both Triassic and Paleozoic groups, and this has complicated even more the possibility of age assignment. Transitional faunas associated with the PTB, such as the Russian Uppermost Permian faunas, could be equivalent to the unique Colonia Orozco fauna. If true, this scenario will substantially change estimates about survivorship rates, suggesting a speciation rate increase in temnospondyls after the Permian-Triassic event. Based on taxonomic, phylogenetic, and geochronologic data, the Buena Vista fauna allows us to quantify faunal turnover across the PTB and in the aftermath of the end Permian extinction event.     

基于Cyt b基因和形态学的鼠兔属系统发育研究及鼠兔属1新亚属5新种描述

本研究扩增了169号鼠兔属样本的cyt b序列,代表13个种11亚种及5个未分类单元,下载了66条分类地位确定而完整的Cyt b序列,包括25种及9个亚种。构建了Bayesian系统发育树,计算了遗传距离,开展了物种界定分析;对13个种4亚种及5个未分类单元174号完整头骨和外形的20个形态学量度数据开展了主成分分析、判别分析和T检验;对头骨和身体外部特征进行了比较研究。结果显示：鼠兔属包含5个亚属,分别是Ochotona, Conothoa, Pika, Lagotona 和一新亚属;5个亚属间的遗传距离在12.8%-16.0%之间;高黎贡鼠兔（Ochotona gaoligongensis）是灰颈鼠兔（O. forresti）的亚种;喜马拉雅鼠兔(O. himalayana)是灰鼠兔(O. roylei)的亚种;木里鼠兔(O. muliensis)是川西鼠兔(O. gloveri)的亚种;宁夏鼠兔(O. argentata)应为蒙古鼠兔(O. pallasi)的亚种;西伯利亚鼠兔（O. turuchanensis） 为高山鼠兔(O. alpina)的同物异名。藏鼠兔循化亚种（O. thibetana xunhuaensis）应提升为种：循化鼠兔(O. xunhuaensis);东北鼠兔长白山亚种(O. hyperborea coreana)应该提升为种：长白山鼠兔(O. coreana);藏鼠兔峨眉亚种（O. thibetana sacraria）应提升为种：峨眉鼠兔（O. sacraria）; 藏鼠兔锡金亚种（O. thibetana sikimaria）应提升为种：锡金鼠兔（O. sikimaria）。通过分子系统学和形态学研究,发现了鼠兔属1 新亚属和5个新种。新亚属命名为异耳鼠兔亚属(Alienauroa subgen. n.),属模为黄龙鼠兔（O. huanglongensis sp. n.）,成员包括黄龙鼠兔新种、峨眉鼠兔、循化鼠兔,以及在龙门山和大巴山发现的2个新种,共计5个种。新亚属的鉴定特征是：耳上前缘内侧有一个密被短毛的异耳屏（Congenial tragus）;头骨扁平,颅面平直;眼小,眼眶长和眼眶宽均小于其他亚属;被毛粗长而无光泽;腹毛多为灰白色。5个新种分别发现于四川黄龙自然保护区、四川北部龙门山、四川北部大巴山、四川西部邛崃山、西藏雅鲁藏布江中游的朗县。我们分别将其命名为黄龙鼠兔（Ochotona huanglongensis sp. n.）,扁颅鼠兔（Ochotona flatcalvariam sp.n.）,大巴山鼠兔（Ochotona dabashanensis sp. n.）,雅鲁藏布鼠兔（Ochotona yarlungensis sp. n.）和邛崃鼠兔（Ochotona qionglaiensis sp. n.）。黄龙鼠兔的鉴定特征是：门齿孔前段平行;脑颅扁平,颅高为颅全长的33.5%;耳大,平均20mm以上（不含耳基部的管）,异耳屏三角形,但顶端圆形;毛长而粗糙,无光泽,背部毛长约20mm;腹面毛色以灰白为主;前后足背面灰白色,腹面黑灰色,指（趾）垫大,橘黄色,露出毛外,爪黄白色半透明。扁颅鼠兔的鉴定特征是：脑颅异常扁平,颅高约11mm,颅高仅为颅全长的31%;眼眶很小,平均6.7mm×5.6mm;个体小,体长140mm以下;体毛长而粗糙无光泽,背部毛长22mm;耳小,平均17mm左右,异耳屏阔圆型,相对较小;背毛沙黄色,腹毛黄白。大巴山鼠兔的鉴定特征是：异耳屏镰刀状;耳相对较小,均在17mm以下,和峨眉鼠兔、扁颅鼠兔差不多,比该亚属循化鼠兔和黄龙鼠兔小。颅高相对较大,颅面更隆突,颅高平均12.45mm, 眼眶相对较大,平均8.52mm×7.13mm。雅鲁藏布鼠兔的鉴定特征是：与黑唇鼠兔（O. curzoniae）和努布拉克鼠兔拉萨亚种（O. nubrica lhasaensis）有很近的亲缘关系;唇缘有很窄的深灰色圈,深灰色圈外侧为灰白色;前后足底部毛浓密,趾端毛多而长,趾垫和爪隐于毛中;个体中等,体长150mm左右,比黑唇鼠兔和努布拉克鼠兔拉萨亚种小得多;颅面较隆突,但与黑唇鼠兔相比,颅面相对平直;被毛黑褐色。邛崃鼠兔的鉴定特征是：大小及头骨和藏鼠兔很相似,但该种和藏鼠兔的显著不同是眶间宽狭窄,平均4.05mm（3.64-4.19mm）,而藏鼠兔眶间宽一般超过4.2mm,平均为4.45mm;该种毛色为沙色带黄色调,毛粗长;藏鼠兔为黑褐色调,毛相对较短;邛崃鼠兔前后足背面为显著的草黄色,而藏鼠兔前后足背面黄白色。     

A new species of Haborophocoena, an Early Pliocene phocoenid cetacean from Hokkaido, Japan

A new species of phocoenid cetacean Haborophocoena , collected from the Early Pliocene Embetsu Formation, in the close vicinity to the site where the holotype of the type species of the genus Haborophocoena was retrieved, improves our knowledge of the anatomy of this cetacean. The new species, represented by a skull, lacking distal half of the rostrum, ear bones, and teeth, is significantly smaller than, but morphologically similar to, the type species Haborophocoena toyoshimai Ichishima and Kimura 2005 . This new record of Haborophocoena confirms the veracity of the genus Haborophocoena as a biological entity, contributes to understanding the interspecific variation, and suggests that the genus diversified in the northwestern Pacific of early Pliocene time. The adult-like degree of ossification in this small skull precludes it from being a juvenile of Haborophocoena toyoshimai . Autapomorphies of Haborophocoena minutus include narrow premaxilla on the dorsal surface of the rostrum, the anterior position of the premaxillary foramen, and a distinct ridge dividing a fossa on the lateral face of the base of the zygomatic process into the dorsal and the ventral halves, the zygomatic process rectangular in lateral profile, and its small size, which is the most compelling feature, making it a distinct species.     

Micro-mechanical properties of different sites on woodpecker’s skull

The uneven distributed microstructure featured with plate-like spongy bone in woodpecker’s skull has been found to further help reduce the impact during woodpecker’s pecking behavior. Therefore, this work was to investigate the micro-mechanical properties and composition on different sites of Great Spotted woodpecker’s (GSW) skull. Different sites were selected on forehead, tempus and occiput, which were also compared with those of Eurasian Hoopoe (EH) and Lark birds (LB). Micro structural parameters assessed from micro computed tomography (μCT) occurred significantly difference between GSW, EH and LB. The micro finite element (micro-FE) models were developed and the simulation was performed as a compression process. The maximal stresses of GSW’s micro-FE models were all lower than those of EH and LB respectively and few concentrated stresses were noticed on GSW’s trabecular bone. Fourier transform infrared mapping suggesting a greater organic content in the occiput of GSW’s cranial bone compared with others. The nano-hardness of the GSW’s occiput was decreasing from forehead to occiput. The mechanical properties, site-dependent hardness distribution and special material composition of GSW’s skull bone are newly found in this study. These factors may lead to a new design of bulk material mimicking these characteristics.     

2 new species of catfish of the Trichomycterus genus (Siluriformes: Trichomycteridae) of the Gran Sabana,Escudo de las Guayanas,Venezuela

Trichomycterus celsae n. sp. and Trichomycterus lewi n. sp. are described from the river Kukenán a tributary of the river Caroní, Orinoco basin, Guyana Shield, Venezuela. The new species are diagnosed within the Guyana Shield Trichomycterus species by a distinctive color pattern. Trichomycterus celsae has a uniform light brown color on dorsum and sides of the body; the ventral surface is yellowish or creamy. Trichomycterus lewi has an irregular pattern of black spots of different sizes on dorsum and sides of the body, the larger spots are located at the posterior part of the body, and, the ventral surface is whitish. The osteology of the new species showed that they belong to the genus Trichomycterus. Osteological features support the external diagnosis of both species, some of them are: in T. celsae, the skull has the fontanels well separated, T. lewi has the fontanels closer and joined by a narrow canal. In T. celsae, the dorsal border of the hyomandibula has a conspicuous notch. In T. lewi, the metapterygoid has a projection on the posteroventral angle. Neural spine of the first preural centra is more elongated in T. lewi.