甘肃天水武山县南峪村的维曼嵌齿象及其生物地层学意义(英文)

报道了甘肃天水地区武山县四门镇南峪村地点发现的一件残破的未成年维曼嵌齿象(Gomphotherium wimani)下颌,标本保存有完整的p3,dp4,m1齿列。颊齿齿冠显示出嵌齿象属(Gomphotherium)的一些进步特征,例如齿脊前后压缩,齿谷宽阔,副齿柱后中心小尖凸显,中附锥和中心小尖趋于分裂,有弱的白垩质发育,符合维曼嵌齿象的鉴定特征。维曼嵌齿象此前发现于甘肃的中中新统,而南峪村地点的含化石地层可与周围其他地点的中中新统对比,因此,南峪村地点维曼嵌齿象层位的地质时代为中中新世。同时,结合孢粉学研究的结果,可能说明中中新世时期,天水地区气候温暖湿润,适宜低齿冠的哺乳类如嵌齿象等动物生存。     

Limb posture and gait in Numidotherium koholense, a primitive proboscidean from the Eocene of Algeria

The tapir-sized late Early Eocene proboscidean, Numidotherium koholense , is the oldest known member of the mammalian order to which the living elephants belong. Morphology of the limb skeleton is reviewed and newly discovered elements are described, with emphasis placed on features considered to have a bearing on limb posture and locomotion. Structure of the shoulder joint and the fact that the antebrachium is fused in a supinated position, indicates that forelimb posture would have been of the abducted or semi-sprawling type. The carpus, while exhibiting the typically proboscidean serial arrangement of carpals (no contact between unciform and lunar), also possesses a free os centrale. The presence of an os centrale and entepicondylar foramen in the humerus are unexpected eutherian plesiomorphies. The structure of the hip joint indicates an abducted hindlimb posture. In both the fore- and hindlimb, mechanisms exist at the major joints to cope with the complicated flexion-extension paths typical of a semi-sprawling gait. Both the carpus and tarsus are indicative of a plantigrade stance. This, in concert with an abducted limb posture, indicates that the gait in numidotheres contrasts markedly with the sub-unguligrade, parasagittal gait of elephantiform proboscideans. The recent suggestion that Proboscidea have their origins in a cursorially adapted phenacodontid-like stock receives no support from this analysis.     

A new scaphognathid pterosaur from western Liaoning,China

A partial skeleton of a new pterosaur, Jianchangnathus robustus gen. et sp. nov. from western Liaoning, China, is described. The specimen (IVPP V16866) was collected near Linglongta, Jianchang County, whose deposits have a disputed age that range from Middle Jurassic to Early Cretaceous. The new species shares several features with the non-pterodactyloid Scaphognathus from the Late Jurassic deposits of southern Germany, such as a deep anterior end of the lower jaw, a piriform lower temporal fenestra with the ventral margin broader than the dorsal one and the interalveolar spacing of the maxillary teeth about three alveolar spaces, allowing its allocation to the Scaphognathidae. The main diagnostic features of J. robustus include the large maxillary process of the jugal, the convex alveolar margin of the lower jaw and the procumbent disposition of the first three pairs of dentary teeth. The new Chinese taxon also differs from Fenghuangopterus lii, which comes from the same deposit and is here regarded as Scaphognathidae incertae sedis, mainly by the lower number of teeth and several proportions of the wing elements. The discovery of J. robustus demonstrates a larger diversity in the pterosaur fauna of the Linglongta region so far dominated by the non-pterodactyloid clade Wukongopteridae.     

Paleobiological implications of shell repair in recent marine gastropods from the northern Gulf of California

Shell repair frequencies in eleven species of Recent gastropods from the northern Gulf of California vary with habitat, shell morphology and intensity of durophagous predation. Squat shells with large apertures tend to have high repair frequencies (0.25–0.50). Shell thickness at the aperture and shell size are not correlated with frequency of repair. Significant intraspecific variation in repair frequency exists between habitats. Samples from rocky habitats have statistically higher repair frequencies than samples of the same species from sandy habitats. However, habitat‐related variation between species is not apparent.

Trends in co‐evolution of gastropods and their durophagous predators are based on the indirect evidence of shell repair frequencies through time. Variation in repair frequency due to environmental and morphological factors may obscure predator‐related temporal trends in repair frequency.     

Seasonal succession,standing crop and determinants of primary productivity of the phytoplankton of Ministik Lake,Alberta, Canada

Ministik Lake (longitude 113°01; latitude 53°21), a well-mixed, shallow (mean depth 1.83 m), eutrophic lake is characterized by eutrophic chlorococcalean and cyanophycean phytoplankton associations, and little change in standing crop size with increasing depth. Standing crops and primary productivity are low during the winter but pronounced spring and late summer/early autumn maxima occur. Mean yearly areal standing crop (B) and primary productivity (A) were 199.2 mg m^–2 chlorophyll a and 319.5 mg C hr^–1 m^–2 respectively. Annual productivity was estimated at 1399,6 g C m^–2yr^–1. The mean increase in the extinction coefficient () per unit increase in standing crop (B) was 0.03 In units m^–1. High non-algal light attenuation (q) occurred averaging 46% which prevented the ratio B from attaining more than 74.2% of the theoretical maximum except once when selfshading occurred. Insignificant relationships existed between B (mg m^–3 chlorophyll a) and A_max (mg C hr^–1 m^–3), A and B and A and B. Close correlations existed between A and A_max/ and A and I₀ (W m^–2). The depth of the euphotic zone (Z_eu) varied between 0.6 and 2.0 m; the average relationship between z_eu and was z_eu = 3.78/_te, and the mean standing crop in the euphotic zone represented 58.3% of the theoritical maximum. The high _q values made the model of Talling (1957) inapplicable to this lake. The Q₁₀ value for the lake was 1.20. _max (mg C chlorophyll a ^–1 hr^–1) was closely related to both temperature and irradiance, and depressed by high pH values.Growth of the cyanophycean algae was correlated with temperature, chlorophycean algae with phosphate-phosphorus and temperature and the diatoms with dissolved silica and phosphate-phosphorus, but only in the case of Chaetoceros elmorii did any nutrient appear limiting. Indirect evidence that free CO₂ limited photosynthetic rates is provided by the _max:pH relationship.     

Oreocharis xieyongii,an unusual new species of Gesneriaceae from western Hunan,ChinaOA

A new species,Oreocharis xieyongii T.Deng,D.G.Zhang & H.Sun,from Hunan Province,central China,is described.The combination of purple zygomorphic corolla with longer adaxial lobes and exserted stamens defines the species and discriminates it from all other current Oreocharis species.Morphological traits of the new species were compared to those of two similar species,Oreocharis xiangguiensis and 0.rubrostriata.Phylogenetic analysis indicates that the new species is nested within the Oreochari...     

Revegetation and its Effect on the Ground-Dwelling Beetle Fauna of Matiu-Somes Island, New Zealand

A study of beetle (Coleoptera) communities was conducted in three revegetated sites of different ages (5, 17, and 100 years) and in a remnant coastal habitat dominated by Muehlenbeckia complexa (a liane) on Matiu‐Somes Island, Wellington Harbor, New Zealand. The 25‐ha island has had a 110‐year history as a pastoral agricultural quarantine station. Beetles were surveyed from May 1997 to April 1998 using pitfall traps. We collected a total of 3,430 adult beetles from 78 beetle species belonging to 22 families. Various environmental factors influencing the distribution of beetles in revegetated habitats were investigated. The most important factors were canopy height and canopy density (functions of vegetation age). Overall, results suggest that as habitat/vegetational heterogeneity increases at a site, beetle diversity and abundance also increase. Thus, older replanted sites contained a greater species richness and abundance of beetles than newly replanted sites. Revegetation is, thus, successfully facilitating the establishment and recolonization of the beetle fauna on Matiu‐Somes Island.     

A new spalacolestine mammal from the Early Cretaceous Jehol Biota and implications for the morphology,phylogeny, and palaeobiology of Laurasian ‘symmetrodontans’

‘Symmetrodontans’ are extinct mammals characterized by having a reversed‐triangle molar pattern in which three main cusps define a triangular molar crown. This dental morpholgy has been regarded as being intermediate between the ‘triconodont’ tooth and the tribosphenic pattern characterizing therians; it is a key feature in taxonomy of Mesozoic mammals and one to understand mammalian evolution and palaeobiology. Here we report a new genus and species of ‘symmetrodontan’ mammal, Lactodens sheni, from the Early Cretaceous Jehol Biota, represented by a partial skeleton with dentary and upper and lower teeth with dental morphologies well‐preserved. The new species has a dental formula of three upper incisors, one canine, three premolars, and six molars/three lower incisors, one canine, five premolars and six lower molars, double‐rooted canines, extremely low‐crowned and transversely thin premolars, and acute angled molars. The dental morphologies of molars and peculiar deciduous premolars are similar to those of Spalacolestes from North America. The associated upper and lower dentitions from one individual animal helped to clarify tooth identification of some spalacotheriids represented only by fragmentary material. Phylogenetic analyses indicate a close relationship of the new species to North American spalacolestines and faunal interchanges between Eurasia and North America, thus supporting the notion that small‐bodied spalacotheriids were diverse and had a pan‐Laurasian distribution during the Early Cretaceous. Absence of the Meckelian groove suggests acquisition of the definitive mammalian middle ear in spalacolestines, and deciduous canines and premolars in the slim and extremely long dentary imply a faunivorous diet.     

A new species of Hydrocotyle (Umbelliferae) from western Yunnan, China

Hydrocotyle peltiformis R.Li & H.Li,sp.nov. 盾叶天胡荽 (S1-2.Fig.1,S1-3.Fig.2) Type:China.Yunnan:Baoshan Prefecture,Longyang,Mangkuang township,Baihualing village,spring pool,east side of Gaoligong Shan,second evergreen broad-leaved forest,growing along trail,25°18′20.9″(N,98°47′59.7″ E,alt.1600 m,2007-10-12,H.Li R.Li & X.C.Shi 1337 (holotype,KUN).     

A low-diversity,silicified Hirnantia Fauna from Butuo,southwestern Sichuan,on the western margin of Yangtze Platform

The latest Ordovician Hirnantia Fauna is distributed worldwide including South China, but with very few records from the western margin of the Yangtze Platform. A silicified Hirnantia Fauna from the uppermost Tiezufeike Formation in the Laoga section, Butuo County, southwestern Sichuan, enriches the fauna’s record and warrants the recognition of the upper part of the Tiezufeike Formation as the Kuanyinchiao Bed. Etching bulk limestone samples from this level with acetic acid yielded 275 specimens of Dalmanella testudinaria, Plectothyrella crassicosta, and Hindella crassa. The population dynamics are analyzed for three successive populations in the section. Size-frequency histograms and survivorship curves indicate gradual improvement of the palaeoenvironments during the end of the Late Ordovician glaciation. The low-diversity brachiopod assemblages recognized in our study are assigned to the Dalmanella-Plectothyrella Community (DP Community) according to their dominant species. It is comparable with two other examples of DP communities, one from the neighboring Guizhou Province of Southwest China, and the other from the Baltica Region.     

Biostratigraphic and palaeoecological implications of new fossil felid material from the Plio-Pleistocene site of Tegelen, the Netherlands

The Plio-Pleistocene site of Tegelen in the Netherlands contains some of the oldest evidence for the presence of the medium-sized pantherine felid of the European Pleistocene, Panthera gombaszoegensis , based on published fragmentary dental specimens. Measurements of these specimens, together with those from other localities, suggest that earlier representatives of the species are small, but one of a small number of previously unstudied specimens from the site now indicates the presence of a larger pantherine individual. Such a size difference could point to the presence of a second species, or suggest that the Tegelen deposits encompass a longer time span than has been supposed. Either of these would have serious implications; the first would increase the complexity of the early Pleistocene carnivore guild, and the second would threaten the status of Tegelen as a type site in the European Pleistocene biostratigraphic scheme. However, consideration of the size range in sexed samples of extant pantherines in conjunction with a re-examination of the size distributions in the hypodigm of P. gombaszoegensis suggests that sexual dimorphism offers a more plausible interpretation.     

The tarsus of erythrosuchid archosaurs, and implications for early diapsid phylogeny

The morphology of the erythrosuchid ankle joint is reassessed. Two specimens, recently thought to have been incorrectly referred to Erythrosuchus africanus , are shown without doubt to belong to this taxon. Furthermore, the morphology is essentially similar to that of other early archosaurs. The tarsus of Erythrosuchus is poorly ossified and consists of a calcaneum, astragalus, and two distal tarsals. The calcanea of Erythrosuchus, Vjushkovia triplicostata , and Shansisuchus shansisuchus are all similar in being dorsoventrally compressed, possessing a lateral tuber, and lacking a perforating foramen. The astragalus of V. triplicostata is currently unknown. The astragalus of Shansisuchus is apparently unique in form. The erythrosuchid pes is therefore more derived than has been recently proposed. The tarsal morphology of several other archosauromorph taxa is reviewed and many details are found to be at variance with the literature. The plesiomorphic condition for the Archosauromorpha consists of four distal tarsals and a proximal row of three elements; two of which articulate with the tibia. These proximal elements are interpreted as the astragalus, calcaneum, and a centrale, and the same pattern is retained in the earliest archosaurs. This reassessed tarsal morphology has implications for the homology of the centrale and reconstruction of early diapsid phylogeny.     

浙江天童常绿阔叶林演替过程的凋落物现存量

凋落物现存量是土壤表层的死有机物质,由尚未分解、半分解和已分解的凋落物组成,它是森林生态系统腐屑食物链的起点,有机碳和营养元素的储库,为生态系统的运转过程提供物质和能量［３,９］;同时,它也能创造幼苗定居环境的异质性［８］。因此,研究演替过程凋落物现...     

Middle–Late Ordovician chitinozoans from Songliang of Qiaojia,western South China,and their biostratigraphic implications

Ordovician chitinozoans are as yet inadequately documented from the western Yangtze Platform, South China. Here we present a systematic study on chitinozoans from a Middle–Upper Ordovician succession at Songliang of Qiaojia, northestern Yunnan, southwestern China. Altogether 34 species of 12 genera are identified from the upper Hungshihyen and the Huadan formations. The top of the Hungshihyen Formation yields typical Early and Middle Ordovician forms, for instance, Lagenochitina obeligis and Belonechitina chenjiawuensis, with the latter only known from the lower Darriwilian in South China, thus suggesting an early Darriwilian age for this interval. The chitinozoans recovered from the Huadan Formation include Lagenochitina prussica and Spinachitina fossensis, both are mainly confined in Katian and sometimes ranging into younger strata. This indicates an age younger than the middle to late Darriwilian previously determined for the Huadan Formation. However, conflicts exist in age assignment of the Huadan Formation based on chitinozoan and other evidence, and further work is required.     

The relationships of Gasteroclupea branisai Signeux, 1964, a freshwater double-armored herring (Clupeomorpha,Ellimmichthyiformes) from the Late Cretaceous-Paleocene of South America

The clupeomorph fish Gasteroclupea branisai Signeux, 1964 from the Late Cretaceous-Paleocene of El Molino Formation, Cayara locality, Bolivia is redescribed in detail. This South American double-armored herring is the sole member of the family Gasteroclupeidae and exhibits a unique combination of features (skull roof ornamented with fine tubercles, beryciform foramen, endopterygoid teeth, about 16–18 supraneurals, a series of 35–38 predorsal and 40 ventral scutes, median fins small and containing 12–14 rays) that clearly supports its assignment to the extinct clupeomorph order Ellimmichthyiformes. G. branisai shares a number of synapomorphies with Sorbinichthys elusivo and S. africanus (five hypurals, second hypural autogenous, distal end of the second uroneural not reaching the distal end of the first uroneural) with which it forms a monophyletic assemblage recognized herein for the first time as the new suborder Sorbinichthyoidei. The peculiar morphology of Gasteroclupea that is characterized by having an extremely deep abdominal profile, hypertrophied coracoid, and elongated pectoral fins, resembles in many aspects the body plan of extant freshwater hatchetfishes of the characiform family Gasteropelecidae, suggesting that the morphological adaptations of G. branisai can be related, at least in part, to a similar lifestyle.     

中国四川西部阳蝇属4新种(双翅目:蝇科)

记述蝇科(Muscidae)棘蝇亚科(Phaoniinae)棘蝇族(Phaoniini)中的阳蝇属(HelinaRobineau-Desvoidy,1830)4新种:四方阳蝇(Helina quadratasp.nov.),团宝山阳蝇(Helina tuanbaoshanicasp.nov.),短叶阳蝇(Helina pedanasp.nov.),二郎山阳蝇(Helina erlangshannasp.nov.)。模式标本存于军事医学科学院微生物流行病研究所医学昆虫标本馆。     

内蒙古上白垩统窃蛋龙科一新属种及其地层学意义(英文)

记述了一件发现于内蒙古临河巴彦满达呼上白垩统乌兰苏海组的窃蛋龙科新材料并建立了一新属新种——戈壁乌拉特龙(Wulatelong gobiensis gen. et sp. nov.)。新属种具有以下不同于其他窃蛋龙科成员的独特特征:外鼻孔大而细长,腹端低于前上颌骨中部;上颌骨的颧骨支呈带状,并向后延伸至眶前隔之后,叠覆于颧骨外侧面;外侧视,上隅骨的前背突基部收缩。戈壁乌拉特龙具有一些其他窃蛋龙科成员不具有的近祖特征,而与更原始的窃蛋龙类接近,说明戈壁乌拉特龙代表了窃蛋龙科中一个相对原始的属种。这些近祖特征包括:下颞颥孔的背缘较窄,泪骨的前突和后突相对较长,外翼骨和外下颌孔的位置都相对靠后,肩胛骨短而纤细,肠骨的耻骨茎较坐骨茎向腹侧延伸更长并前后向更宽,坐骨较短,以及第三跖骨近端侧扁等。因此戈壁乌拉特龙的系统发育位置可能居于原始窃蛋龙类和其他窃蛋龙科成员之间。对巴彦满达呼恐龙动物群的初步分析支持巴彦满达呼红层代表了蒙古高原戈壁地区上白垩统红层中的最早沉积层位的结论。     

Apogon selas,a new cardinalfish from the western Pacific

A new species of cardinalfish,Apogon selas, is described from 27 specimens from New Guinea, Ryukyu Islands, and Philippines; also known from photographs taken in the Solomon Islands and Indonesia. It is a species of the subgenusOstorhinchus Lacepède, distinctive in having a first dorsal fin of VII spines, 13 pectoral rays, 14–19 gill rakers, smooth preopercular ridge, body depth 2.9–3.6 in SL, and a color pattern of a black spot as large as the eye centered on the caudalfin base and two dusky stripes (mainly red or golden in life), one midlateral and the other from tip of lower jaw across cheek to thorax.A. selas appears to be most closely related toA. endekataenia Bleeker which differs in having 14 pectoral rays, 18–21 gillrakers, and six dark stripes on the body.