广西泥盆纪早埃姆斯期郁江组Heterophaulactis Yu,1974的再研究(英文)

Heterophaulactis Yu是作者建立并发表于1974年的一四射珊瑚属,产自广西郁江沿岸、南宁至六景一带的泥盆纪郁江组,其时代属早埃姆斯期牙形刺kitabacus带(前dehiscens带)。对此珊瑚属再行研究,是出于:1)发表在"中国南方泥盆系的新进展"一文,是与其它门类化石共同作为划分和对比地层的化石依据,只限于中文简短描述,对化石图影的展示也有严格的数量限制。尽管此属己被收录在Hill(1981)主编的古生物专论的珊瑚分册中,也只是简短的英文描述和有限的图影,未能充分展示其骨骼演变特征;2)此属的分类位置、科的归属及与相关属的属征比较与讨论,当初均未交待,应予阐明;3)Heterophaulactis属的地理分布广,遍及滇桂两省,通过再研究,其产地已扩展至中国西北地区;其地层分布又有一定的时限性,在广西仅限于郁江组下部的石州段,时代为kitaba-cus带,其它地区也仅见于下泥盆统。文中对Heterophaulactis属的模式种,Heterophaulactis semicrassa的骨骼特征及个体发育过程中的演变均作详细的英文描述和图影展示;与相关属比较之后,认为与本属关系最为密切的是产于西秦岭山区下泥盆统、发表在西北区化石图册上的有些属种,其中的有些属种可以归于本属。文中还记述一新建种Heterophaulactis yujiangense sp.nov.。文章对Heterophaulactis的分类位置和科的归属也有详细比较讨论,认为它是源出自志留纪Pycnactis—Phaulactis的演化序列,应归属于Lykophyllidae Wedekind,1927科。对Miroelasmatinae Cao,1983亚科的原始定义作全面修订后,把它归为Lykophyllidae Wedekind,1927科下的一个亚科;在对化石图册及相关文献上记述的产自西秦岭区下泥盆统四射珊瑚属种的全面修订之前,暂把以下各属置于此亚科:Heterophaulactis Yu,Miroelasma Cao,Qinlingophyllum Cao,Wenxianophyllum Cao,Protaulacophy-llum Cao,Bethanyphyllum sensu Cao,Aulacophyllum sensu Cao和Aulacophyllum sensu Zhang。     

Air-breathing adaptation in a marine Devonian lungfish

Recent discoveries of tetrapod trackways in 395 Myr old tidal zone deposits of Poland (Niedźwiedzki et al. 2010 Nature 463, 43–48 (doi:10.1038/nature.08623)) indicate that vertebrates had already ventured out of the water and might already have developed some air-breathing capacity by the Middle Devonian. Air-breathing in lungfishes is not considered to be a shared specialization with tetrapods, but evolved independently. Air-breathing in lungfishes has been postulated as starting in Middle Devonian times (ca 385 Ma) in freshwater habitats, based on a set of skeletal characters involved in air-breathing in extant lungfishes. New discoveries described herein of the lungfish Rhinodipterus from marine limestones of Australia identifies the node in dipnoan phylogeny where air-breathing begins, and confirms that lungfishes living in marine habitats had also developed specializations to breathe air by the start of the Late Devonian (ca 375 Ma). While invasion of freshwater habitats from the marine realm was previously suggested to be the prime cause of aerial respiration developing in lungfishes, we believe that global decline in oxygen levels during the Middle Devonian combined with higher metabolic costs is a more likely driver of air-breathing ability, which developed in both marine and freshwater lungfishes and tetrapodomorph fishes such as Gogonasus.     

Two new species of Dunkleosteus Lehman, 1956, from the Ohio Shale Formation (USA,Famennian) and the Kettle Point Formation (Canada,Upper Devonian), and a cladistic analysis of the Eubrachythoraci (Placodermi,Arthrodira)

Two pachyosteomorph arthrodires are described from the Upper Devonian of North America, Dunkleosteus raveri sp. nov. and Dunkleosteus amblyodoratus sp. nov. (from the Appalachian and the Michigan basins, respectively). Dunkleosteus raveri sp. nov. is found stratigraphically below the only other species within the Ohio Shale Formation (Famennian), and is characterized by the retention of a primitive dermal ornamentation, and shares with Dunkleosteus terrelli ( Newberry, 1873 ) the possession of articular facets on the parasphenoid. Dunkleosteus amblyodoratus sp. nov. (Kettle Point Formation, Upper Devonian), known only from incomplete nuchal, paranuchal, and parasphenoid plates, also retains dermal tuberculation, and is characterized by tapering articular facets on the parasphenoid. The current study reviews three North American species of Dunkleosteus (Du. terrelli, Du. raveri sp. nov. , and Du. amblyodoratus sp. nov. ). Formerly, two subgroups were recognized within the Dinichthyidae, the terrelli and herzeri groups, which are shown here to be members of distinct clades. Dinichthys herzeri Newberry, 1868 (the namesake member of the herzeri group) is now the sole member of the family Dinichthyidae comb. nov. , and is assigned to the Aspinothoracidi sensu Miles & Dennis, 1979 . Heintzichthys Whitley, 1933 and Gorgonichthys Claypole, 1892 (additional members of the herzeri group) were previously placed among the aspinothoracid arthrodires. Likewise, Holdenius holdeni Dunkle & Bungart, 1942 (the final member of the herzeri group) and Hadrosteus rapax Gross, 1932 are now placed within the Aspinothoracidi. The remaining taxa, formerly assigned to the Dinichthyidae (i.e. Dunkleosteus Lehman, 1956 ; Eastmanosteus Obruchev, 1964 ; Golshanichthys Lelièvre, Janvier, & Goujet, 1981 ; and Westralichthys Long, 1987 ), are united within the Dunkleosteidae Stensiö, 1963 . © 2010 The Linnean Society of London, Zoological Journal of the Linnean Society, 2010, 159 , 195–222.     

Level-bottom brachiopod communities in the Middle Devonian of New York

Depositional environments of the Onondaga Limestone from central to southeastern New York are found to be normal, subtidal marine, due to the absence of characteristic supratidal or intertidal sedimentary features and the presence of a typical, diverse, marine level-bottom community framework. Post-mortem transport has not been extensive, as evidenced by low articulation ratios, lack of abraded valves, and complete ontogenetic gradations within species, which precludes large scale winnowing. Sedimentation rates appear to have been greatest in eastern New York where the Onondaga Limestone reaches a thickness almost three times that of the strata in central New York. Shaly beds in the central area represent periods of cessation of carbonate deposition rather than an influx of clastic material. Deposition terminated with the onset of deeper water characterized by a westerly advance of terrigenous sedimentation (the Marceilus Shale of the Hamilton Group). Nine brachiopod communities can be recognized in the Onondaga Limestone. There is a strong correlation between sediment-substrate and community type, reflecting the sedimentologic control of brachiopod community distribution. Sandy facies, cherty limestones and coral biostromes and bioherms are associated with inner-neritic deposition in Edgecliff time; argillaceous lime muds and lime sands are characteristic of mid-neritic deposition in Nedrow to Moorehouse time; and highly argillaceous lime muds are associated with outer-nerittc deposition in Seneca time.     

Siluro-devonian Conodonts from the Camelford Limestone, Wellington, New South Wales, Australia

Conodont data have been utilized to identify the Silurian/Devonian boundary within the Camelford Limestone near Wellington, NSW. Conodont faunas are documented from the eosteinhornensis Zone to early delta Zone with one new species of Walliserodus ( W. multistriatus ) and two new species of Ozarkodina ( O. brocki and O. camelfordensis ) described. An apparatus reconstruction of Belodella anomalis is also presented.     

Aspects of control of the cardiovascular-respiratory system during orthostatic stress induced by lower body negative pressure

This paper considers a model developed to study the cardiovascular control system response to orthostatic stress as induced by two variations of lower body negative pressure (LBNP) experiments. This modeling approach has been previously applied to study control responses to transition from rest to aerobic exercise, to transition to non-REM sleep and to orthostatic stress as produced by the head up tilt (HUT) experiment. LBNP induces a blood volume shift because negative pressure changes the volume loading characteristics of the compartment which is subject to the negative pressure. This volume shift induces a fall in blood pressure which must be counteracted by a complicated control response involving a variety of mechanisms of the cardiovascular control system. There are a number of medical issues connected to these questions such as orthostatic intolerance in the elderly resulting in dizziness or fainting during the transition from sitting to standing. The model presented here is used to study the interaction of changes in systemic resistance, unstressed venous volume, venous compliance, heart rate, and contractility in the control of orthostatic stress. The overall short term response depends on a combination of these physiological reactions which may vary from individual to individual. There remain open questions about which factors have greater importance. The model simulations are compared to experimental data collected for LBNP exerted from the hips to feet and from ribs to feet.     

Fungal endophytes in a 400-million-yr-old land plant: infection pathways, spatial distribution, and host responses

The Early Devonian Rhynie chert has been critical in documenting early land plant-fungal interactions. However, complex associations involving several fungi that enter into qualitatively different relationships with a single host plant and even interact with one another have not yet been detailed. Here, we studied petrographic thin sections of the Rhynie chert plant Nothia aphylla. Three fungal endophytes (co)occur in prostrate axes of this plant: narrow hyphae producing clusters of small spores; large spherical spores/zoosporangia; and wide aseptate hyphae that form intercellular vesicles in the cortex. Host responses on attack include bulging of infected rhizoids, formation of encasement layers around intracellular hyphae, and separation of infected from uninfected tissues by secondarily thickened cell walls. A complex simultaneous interaction of N. aphylla with three endophytic fungi was discovered. The host responses indicate that some of the mechanisms causing host responses in extant plants were in place 400 million yr ago. Anatomical and life history features of N. aphylla suggest that this plant may have been particularly susceptible to colonization by fungi.     

A new pachyosteomorph arthrodire (Pisces: Placodermi) from the Upper Frasnian of the Central Devonian Field,Russia

A new genus and species of pachyosteomorph arthrodire, Omalosteus krutoensis gen. et sp. nov. from shallow-water marine deposits of the Evlanovo Regional Stage (Upper Frasnian, Upper Devonian) of the Central Devonian Field is described. It is tentatively referred to the family Trematosteidae Gross, 1932, which was earlier believed to be endemic to central Europe. The new genus is characterized by a rounded, dorsoventrally compressed cross section of the pectoral region and smooth head shield and postcranial membrane bones. The centrale is elongated, forming a narrow lateral lobe. The praeorbitale, postorbitale, and centrale come in contact in the center of the orbital region. The mediodorsale is wide, its carinal process projects considerably posteriorly. The anterior margin of the anterior ventrolaterale lacks articular facets for the interlaterale.     

New radiolarian species from the Upper Cretaceous-Lower Paleogene of the eastern slope of the northern Ural Mountains

Five new radiolarian species, Dictyophimus? orbiculiporosus sp. nov., Spongomelissa imperceptusa sp. nov., Theocoronium puncticulatum sp. nov., Pterocyrtidium porrectum sp. nov., and Tripodiscinus corona sp. nov., from the Campanian-Danian diatomites of the Leplinskaya Formation of the northern Ural Mountains are described. They are useful for stratification and correlation of the Upper Cretaceous and Lower Paleogene beds of the Ural Region of Western Siberia.