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1.
    
The origin of the Brachiopoda has long been a hotly debated topic, and various models have been proposed following the latest finds of exceptionally preserved material. The lower Cambrian (Stage 3) Heliomedusa orienta from the Chengjiang Konservat-Lagerstätte, eastern Yunnan of South China, is an important example of exceptional preservation. A wide variety of affinities have been proposed for Heliomedusa, but recently it has been suggested to reside within the mickwitziids, which may form a stem group to the Brachiopoda. Detailed studies of exceptionally preserved Heliomedusa have increased our knowledge of the soft-part anatomy of this important early brachiopod, but unfortunately, almost nothing is known about its shell structure. Here, we describe new exceptionally preserved specimens from the Chengjiang biota to better reveal both shell structure and ornamentation. Its reticulate–pustulose ornament and tubular structure are reminiscent of traits seen in other mickwitziid brachiopods. In addition, two types of setae can be observed. Apart from the pyritized marginal mantle setae, some tubules are filled with iron oxides, potentially representing thinner and shorter penetrative setae. Both valves of H. orienta appear to have been less mineralized as compared to Mickwitzia monilifera, and the two species differ in diameter and density of tubules and pustules, and in terms of slightly less projected profile of ventral valve with lower umbo posteromedially placed. Although Heliomedusa clearly is closely related to Mickwitzia, their different preservational modes (compacted poorly mineralized/noncompacted mineralized) make detailed comparison difficult; they are provisionally kept as separate genera pending further studies of better-preserved Chinese material.  相似文献   

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Scanning electron micrographs of the tarsal adhesive setae of 84 species of beetle are described. These show a vast range of setal structure and distribution.  相似文献   

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Abstract

The intra-specific variations of the setae arrangements was evaluated in three populations of Eisenia fetida (Savigny, 1826), e.g., to apply and test of the usefulness of setal formula at the intra-specific (population) level. The results confirm the role of the expected geographic isolation on the inter-population variability, and the results showed that variability in the setal formula (variability in paired setae groups aa, ab, and dd) could be used in the study of the intra-specific variations.  相似文献   

4.
Two main types of micro-ornament can be observed in the family Delthyrididae (Brachiopoda, Spiriferidina): capillae (with continuity of the structures from one growth lamella to the next one) and spines (with the appearance of discontinuity). SEM studies of the spines show that, contrary to previous assumption, the cross section is not circular but subquadrangular with a longitudinal groove on top. Each spine is connected in front to the next one so that they give rise to a continuous radial structure. Thus the spine is a local external differentiation of the underlying microfila. Furthermore, the spinose ornament is derived from the capillate ornament. During growth, new fila and spines appear in the grooves and diverge towards the top of adjacent costae, running across several lamellae. When there are few spines, they have a uniform size, but when there are many spines, small spines (issued from newer fila) are juxtaposed with large spines (issued from older fila). The use of micro-ornament in systematics has often been based on misinterpretations; attention is drawn to the fact that the shape of the spine base is not representative of the original shape of the spine but generally resulted from the erosion of the shell. Nevertheless, more detailed studies on spine shape and arrangement offer interesting prospects for classification.  相似文献   

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Abstract: Since the brachiopod Order Lingulida has been greatly revised in recent years, with particular emphasis on Cambrian and Ordovician genera, many well‐established Silurian linguloid species from the British Isles have been left without an appropriate genus in which to place them. This is rectified here by allocating the various species, mostly erected in the nineteenth or early twentieth centuries, to a variety of genera which have been mainly erected within the last forty years. Two new genera are erected, Mergliella, with type species Lingula bechei Davidson, 1866 , and Striatilingula, with type species Lingula? striata J. de C. Sowerby, 1839 .  相似文献   

7.
The central fold of the Late Devonian brachiopods Cyrtospirifer monticola, Cleiothyridina devonica, Rugaltorostrum madisonense, Sinotectirostrum banffense and Trifiodorostellum dunbarense (Three Forks Formation, Central Idaho) varies intraspecifically from nearly rectimarginate or weakly developed to chevron-shaped. Frequency of central fold morphotypes through succesSjve size classes indicates selective survival in favor of variants with a strongly developed central fold, although morphotypes with the most extremely developed central fold never numerically dominate the larger size classes of any species. Differential mortality among the morphotypes can be attributed to: (1) less resistance to shell fracture by morphotypes with weakly developed uniplicae which were preferentially culled out of the population by durophagous predators, (2) less efficiency of weakly uniplicate morphotypes in the generation of nutrient-bearing eddies against the downcurrent inhalant margins. Failure of the morphotypes with the most strongly developed uniplicae to numerically dominate adult (largest) size classes is attributed to the hydrodynamic instability of such shell geometries on current-scoured substrates.  相似文献   

8.
川东南兴文地区长兴期腕足动物及其群落结构   总被引:2,自引:0,他引:2  
通过川东南兴文地区长兴期腕足动物地层的研究,总结了腕足动物群的性质,指出了本区长兴期腕足动物群不同于灰岩相类群,也不同于硅质岩相类群,而属于灰岩、砂页岩混合相类群。文章重点研究了本区腕足动物群落结构,并提出了生态类群这一新观点,指出生态类群是以生态学而不是以纯分类学标准进行分类的,这有助于群落生态研究中简化群落内物种间的复杂关系。  相似文献   

9.
《Palaeoworld》2016,25(4):600-615
Conodont biostratigraphical work was done at four sections recently found with occurrence of the rhynchonellide brachiopod genus, Dzieduszyckia Siemiradzki, in southern Guangxi and in the border area between Dushan County of Guizhou and Nandan County of Guangxi, South China. These sections represent two different types of facies, i.e., carbonate platform and intraplatform basin. The conodont analysis reveals that this genus occurs in the Upper triangularis Zone and the Middle crepida Zone at the Dazhai Section, through the Lower to Upper crepida zones at Dalong, and is restricted within the Upper rhomboidea Zone at the two intraplatform basin sections (Changtang and Duli). This result demonstrates that the occurrence of these peculiar rhynchonellide brachiopods in South China, regardless of the depositional environments, is within the Lower Famennian instead of the previously suggested Upper Famennian. Furthermore, this brachiopod genus in South China began to inhabit on the carbonate platform almost since the beginning of the Famennian and did not extend to the intraplatform basin facies until the late Early Famennian.Available biostratigraphic data indicate that during the Early and Middle Famennian, Dzieduszyckia is widely distributed not only in South China, but also throughout the world, such as Morocco and southern Ural.Observation on the new collections from the four studied sections reveals that the peculiar rhynchonellide brachiopods have a great morphological variation within each section. Significant differences existed among the collections from different sedimentary settings and localities, probably reflecting the environmental and geographic constraint on the morphology of Dzieduszyckia. Samples from different layers in the same section have nearly identical morphological variation, suggesting the temporal inheritance in morphology of the rhynchonellide brachiopod.  相似文献   

10.
Summary Queens inMegaponera foetens are permanently wingless. In a colony from Kenya we observed that the ergatoid queen was often surrounded by a large number of workers, all conspicuously facing her. To investigate the nature of this attraction, we divided the colony in half. When the queen was transferred from one group to the other, a large court of workers formed immediately. When marked workers were transferred from the queenright group to the other, they attracted much attention and were licked repeatedly. These data suggest that the queen produces a chemical signal which attracts workers, and this signal is transferred onto the workers. In a histological investigation of queen and workers, we found many intersegmental glands in both castes. However, only the queen had a thick glandular epithelium lining her entire body, and this may be the source of her signal. The numerous erect setae covering the queen (but not the workers) may help to dispense the secretions. Our results confirm that ergatoid queens in the Ponerinae are morphologically specialized, despite their external similarity with workers.  相似文献   

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洪泽湖鱼类寄生甲壳动物区系调查及一新种的记述   总被引:2,自引:0,他引:2       下载免费PDF全文
1979年秋对江苏省洪泽湖鱼类寄生甲壳动物的调查研究结果,共得18种寄生甲壳动物,其中包括一个新种。分析了该湖寄生甲壳动物的区系组成、繁殖季节及种类分布的情况,同时还根据虫体感染率和感染强度,提出了对鱼类危害性较大的中华鳋和多态锚头鳋,在洪泽湖中不可能出现严重感染的见解。  相似文献   

13.
    
Abstract. Setae of the first segment of the marine annelid Sthenelais berkeleyi (family Sigalionidae) are arranged in the shape of an antero-dorsally directed tube. When the worm is in resting position buried in sediment, this setal tube projects slightly from the sediment surface. A current of water is drawn into it by cilia on the parapodia of the first segment. The water is then diverted to a pair of lateral spaces between the body wall and elytra, moved posteriorly in these spaces along the length of the body by segmental cilia, and eventually exits posteriorly or ventrally. This flow permits the worm to respire while remaining buried and immobile for long periods of time, waiting for prey to move over the sediment near it. Setae of the first segment are probably used as snorkels in some other infaunal sigalionids as well.  相似文献   

14.
    
《Palaeoworld》2016,25(4):569-580
The glaciomarine sediments related to the Late Paleozoic Ice Age (LPIA) have an excellent stratigraphic record in Argentina, particularly those associated to the Late Carboniferous glacial episode identified along the southwestern margin of South America: Bolivia (Tarija Basin), west central Argentina (Calingasta-Uspallata Basin) and Patagonia (Tepuel-Genoa basins). The aim of this contribution is mainly a biostratigraphy update of the carboniferous brachiopod faunas that occur in the earliest postglacial interval (late Serpukhovian–Bashkirian) in the west central Argentina (i.e., Levipustula and Aseptella-Tuberculatella/Rhipidomella-Micraphelia faunas) and its regional correlation with those equivalents in the nearby basins. Components of these faunas are recognized from the Bolivia to Argentine Patagonia and their compositional variations appear to be controlled principally by a paleolatitudinal factor. The affinities showed by the postglacial faunas of the Calingasta-Uspallata Basin and the faunal assemblages that integrate the Lanipustula and Tuberculatella biozones in Patagonia differ from the significant contrast proposed by other authors, based on the paleogeographical position of Patagonia in the Late Paleozoic. Paleoecological studies focused on the paleoenvironmental controls related with the glacial dynamic are suggested to understand the complex relationship between these postglacial faunas.  相似文献   

15.
    
Compilation of the marine, benthic megafossils from approximately the mid-Ashgill of the Mediterranean region, including much of Central and Southern Europe plus North Africa, and elsewhere indicates a warm interval featuring bioclastic limestone and a warm climate marine fauna. These mid-Ashgill faunas immediately precede the latest Ashgillian, Hirnantian, cool interval that featured widespread glaciation, and are underlain by typical, cold water, Mediterranean Realm, older Ordovician rocks and faunas. The cause or causes responsible for the brief warm interval are uncertain, but may have involved a warm water gateway that is geographically still not located. There is a possibility that South Africa was similarly affected by this roughly mid-Ashgillian marine situation. Early Paleozoic bauxite minerals and kaolins in northwestern Sudan and kaolins elsewhere in North Africa may represent the same time interval, which would suggest that there was a non-marine amelioration of the local climate as well as the marine effects.  相似文献   

16.
  总被引:1,自引:0,他引:1  
The stratiform laminae of Micrina sclerites originally consisted of rheomorphic successions of monolayers of micrometric–sized, apatitic tablets, presumably interleaved with chitin and glycosaminoglycans (GAGs). Paired laminae enclose slot–like chambers swelling into lobes distally that originally contained GAGs and deposits of spherulitic and prismatic apatite. The laminae are pervaded by apatitic tubes, apparently secreted by microvillous setoblasts and containing, at the surface, chitinous setae. Internal markings suggest that the triangular (sellate) sclerite supported a pair of muscles and the planospiral (mitral) sclerite, a medial muscle and gonadal sacs flanked by a pair of crescentic muscle bases. Both sclerites were secreted by a mantle with a circumferential fold. The sellate and mitral sclerites are homologized with the anterior and posterior shells of Halkieria and could have become the dorsal and ventral valves of the ancestral brachiopod by a sequence of transformations. These include: the folding of the halkieriid body axis; accelerated mixoperipheral growth of the anterior (dorsal) shell to enclose, with the posterior (ventral) shell, a mantle cavity lined with modified ciliated epithelium of the foot; reduction of sclerite–secreting epithelium to the locus of the brachiopod pedicle epithelium; and the anterior (dorsal) spread of gonadal lamellae.  相似文献   

17.
    
Abstract:  Brachiopods from the late Ordovician (late Caradoc) Dulankara Formation of the Chu-Ili Range, Kazakhstan, are reviewed. Those from the upper two members of the formation, the Degeres and Akkol members, are systematically described. New genera from the Dulankara Formation are Nikitinamena (Plectambonitoidea: Leptellinidae), with type species Nikitinamena bicostata sp. nov., and Weberorthis (Orthoidea: Plectorthidae), with type species Mimella brevis Rukavishnikova. Another new genus is Glyptomenoides (Strophomenoidea: Glyptomenidae), with type species Rafinesquina girvanensis Salmon from the Caradoc of Girvan, Scotland. Other new species from the Dulankara Formation are Holtedahlina orientalis , Platymena tersa , Christiania proclivis , Leangella ( Leangella ) paletsae , Metambonites subcarinatus , Ogmoplecia nesca and Plectorthis licta . The ecology and assemblages of all three members of the Dulankara Formation are identified or reviewed, and their palaeogeographical significance assessed: the Chu-Ili Terrane (on which the Dulankara Formation was situated during the Ordovician) formed part of the relatively low-latitude peri-Gondwanan complex of terranes, and was probably not far from North and South China. The faunal links suggested between the Dulankara brachiopods and contemporary faunas from Australia are now perceived to be weaker than previously thought.  相似文献   

18.
Ultraviolet reflectance is a widely distributed phenomenon among certain families of Coleoptera. It is so far found to occur in Carabidae, Scarabaeidae, Buprestidae, Elateridae, Tenebrionidae, Cerambycidae, Anthribidae and Curculionidae. Of more than 100 species examined, 70 were found to possess UV reflectant structures. Reflection is almost always from pigments contained within microtrichia or other setae. In some Tenebrionidae and Buprestidae, dried secretions forming patches or stripes on the pronota and elytra are reflective and, in a few desert-living Tenebrionidae, reflectance is from subcuticular pigment in the elytra.  相似文献   

19.
    
We examined the morphology of setae and microtrichia in Aquarius paludum during larval development using a scanning electron microscope. We then conducted immersion experiments with larvae and adults in oxygenated and deoxygenated water. The adult water strider body is covered by a pilose double layer consisting of upper long setae (30-80 microm) and lower filiform microtrichia (5-9 microm). Only setae are present on the legs. Microtrichia on the larval body are very short: 0.5-0.6 microm in first and second instars, and 0.8-1.7 microm in third to fifth instars. Larval body setae are approximately as long as those of adults (25-50 microm), but are much less dense at 1,800-5,750 setae per mm(2) versus 15,000-20,000 setae per mm(2) in adults. The density of setae on the legs remains relatively constant throughout development (larvae: 15,000-20,000 setae per mm(2); adults: 20,000-26,000 setae per mm(2)). Immersion experiments demonstrated that young instars may use cuticular respiration. First- and second-instar larvae survived underwater for several hours without a visible air supply, although they did not survive in deoxygenated water. We posit that the short body microtrichia have a waterproofing function in larvae, whereas they create a compressible air bubble in adults. In adults, waterproofing is accomplished by the setae. The density and length of setae on the legs of larvae was nearly the same as that on the body and legs of adults and is presumably optimized for waterproofing. Thus, a change in morphometrical parameters can result in a large functional change in the same structure. We discuss this interpretation in both ecological and physiological contexts.  相似文献   

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