四川省岷山地区花蝇科泉种蝇属四新种（双翅目;花蝇科）

本文记述四川省松潘县和茂汶县地区花蝇科泉种蝇属４新种,即蝶肛泉肿蝇Ｐｅｇｏｈｙｌｅｍｉａ ｐａｐｉｌｉｏｃｅｒｃａ ｓｐ．ｎｏｖ。巨板泉种蝇Ｐｅｇｏｈｙｌｅｍｙｉａ ａｌｃａｅｃｅｒｃａ ｓｐ．ｎｏｖ。角泉种蝇Ｐｅｇｏｈｙｌｅｍｙｉａ ｃｏｒｎｕｔａ ｓｐ．ｎｏｖ．四尖泉种蝇Ｐｅｇｏｈｙｌｅｍｙｉａ ｔｅｔｒａｃｒｕｌａ ｓｐ．ｎｏｖ。     

青第省花蝇科二新种（双翅目）

记述青海省花蝇科Ａｎｔｈｏｍｙｉｉｄａｅ２新种,即周氏泉种蝇Ｐｅｇｏｈｙｌｅｍｙｉａ ｃｈｏｕｉ,ｓｐ．ｎｏｖ．及多曲草种蝇ｈｏｒｂｉａ ｐｏｌｙｓｔｒｅｐｓｉｓ,ｓｐ．ｖｎｏ．。模式标本均存中国科学院上海昆虫研究所。     

四川西部泉种蝇属三新种记述(双翅目：花蝇科)

四川西部泉种蝇属三新种记述（双翅目：花蝇科）邓安孝（华西医科大学寄生虫学教研室成都６１００４４）李岭,刘阳（华西医科大学临床医学系成都６１００４４）本文报道花蝇科泉种蝇属ＰｔｈｅｌｍｐｉａＳｃｈｎａｂｌ三新种均产于纸山山系,模式标本存于华西医科大学寄...     

中国蝇总科六新纪录

整理1980年以来在河北省集采的花蝇科和蝇科标本中,共发现6种系国内新纪录。名录如下: 1.波斯地种蝇Delia persica Hennig,1974河北(都山,1♂,80.8.24.) 2.棒叶泉种蝇Peegohylemyia clavata Hennig,1970河北(小五台山,5♂,80.7.9.2♂,81.7.10.) 3.摩纳泉种蝇Pegohylemyia monacensis Hennig,1970     

重庆市蝇类记录

据范滋德1963年的总结,本市已经记录了23种蝇类。本文再记录75种。标本采自重庆市市区及近郊、綦江、四面山、缙云山、金佛山等地。1.黄粪蝇Scatophaga stercoraria 2.灰地种蝇Delia plaura 3.海南粪泉蝇Emmesomyia kempi4.乡隰蝇Hydrophria ruralis 5.山隰蝇H.montans 6.粪种蝇Adia cinerlla 7.四条泉蝇Pegomya guadrivttata 8.夏厕蝇Fannia canicularis 9.白纹厕蝇F.leucosticta 10.宜宾厕蝇F.ipinensis 11.     

泉种蝇属一新种(双翅目:花蝇科)

本文记述泉种蝇属Pegohylemyia一新种。新种模式标本采自位于黔北高原的宽阔水自然保护区,保存于作者所在单位。 诹访泉种蝇Pegohylemyia suwai新种 雄 体长7.0mm。眼具稀疏微毛。额约为头宽的1/19或触角第三节宽的2/3。间额前方橘红,向后渐黑;粉波银灰;间额交叉鬃发达,其前下方尚具一个小鬃。侧额狭,至     

青海省花蝇科二新种 (双翅目)

记述青海省花蝇科 Anthomyiidae 2新种 ,即周氏泉种蝇 Pegohylemyia choui,sp.nov.及多曲草种蝇 Phorbia polystrepsis,sp.nov.。模式标本均存中国科学院上海昆虫研究所。     

中国花蝇科和厕蝇科新纪录

整理作者在山西省雁北地区采集的蝇总科标本中,发现五种系国内新纪录,名录如下:拟瘦端地种蝇Delia dovreensis Ringdahl,1954 采集地:山西广灵(上白羊2,1980.8.9)细叶叉泉蝇Eutrichota praeclara(Stein,1914) 采集地:山西平鲁(只泥泉1,1980.9.3)直角泉种蝇Pegohylemyia rectangularis Ringdahl,1952 采集地:山西广灵(上白羊1,1980.8.9)     

山西省地种蝇属一新种：双翅目：花蝇科

本文记述地种蝇属Ｄｅｌｉａ Ｒ．－Ｄ鞭阳地种蝇新种Ｄｅｌｉａ ｍａｓｔｉｇｏｐｈａｌｌａ ｓｐ．ｎｏｖ．的形态特征,并与近缘种作了比较。     

神农架林区花蝇的初步调查

我国花蝇种类繁多,但鄂西北神农架林区的花蝇尚缺乏研究。为此,我们于1985年4、5月间,以网捕法对该区花蝇进行了调查,隔日一次,全天采集。经鉴定,包括以往发现的虫种在内,共有8属10种,其中鞍板球果花蝇为湖北省新纪录,标本保存于镇江医学院寄生虫学教研室。一、种类名录1.粪种蝇Adia cinerella(Fallen);2.横带花蝇Anthomyia illocata Walker;3.陈氏拟花蝇Calythea cheni Fan;4.白斑拟花蝇C.nigricans(R.-D.);5.三条地种蝇Delia flabellifera(Pandelle);6.灰地种蝇D.platura(Mg.);7.长板粪泉蝇Emmesomyia hasegawai Suwa;8.乡隰蝇Hydr…     

Importance of biological and abiotic factors for geochemical cycling in a freshwater eutrophic lake

Here we report the results of a comprehensive biogeochemical monitoring of Rostherne Mere in 1998, including changes in dissolved oxygen, organic carbon and nitrogen, nitrate/nitrite, ammonia, Al, Na, S, K, Mg, Ca, Si, Fe, Mn, orthophosphate, particulate N & P, suspended solids, temperature, pH, chlorophyll-a and zooplankton. The results demonstrated the major influence of primary producers on the overall geochemical cycling of N, P and Si, and suggested that the significance of zooplankton might have been previously underestimated. For major anions and cations, however, the influence of biota on lake water concentrations appeared to be negligible, reflecting the fact that these chemicals were present far in excess of plankton requirements. Thus changes in concentrations of Ca, K, Na, Mg and S were rather limited and must have reflected changes in hydrological and meteorological parameters. K, however, demonstrated a transitional pattern, reflecting some influence of biological uptake. During the stratification period, the slow processes of bacterial decomposition in the hypolimnion gradually released chemicals contained in the materials accumulated in the bottom layer, remarkably increasing the concentrations of dissolved compounds of those elements present in amounts comparable with the pool stored in the sedimenting detritus (e.g. orthophosphate P, ammonia N, Si and DOC). The decomposition also resulted in a drop in the redox potential, followed by partial denitrification and chemical release from the sediments. The hypolimnion of the Mere was confirmed to remain at the stage of Mn release, characterised by accumulation of DOC, orthophosphates, ammonia and initial stages of denitrification. High levels of P released from the sediments during the stratification period suggest that the lake’s recovery after sewage diversion might be further delayed.     

Early Cretaceous Palynofloras from Tarim Basin,Xinjiang

One hundred and eight species of fossil spores and pollen referred to 55 genera found from the Lower Cretaceous Kapushaliang (Kizilsu) Group in the Tarim Basin of Xinjiang have been studied in this paper. The Kapushaliang Group may be divided into the Yageliemu Formation, the Shushanhe Formation and Baxigai Formation in ascending order. The Yageliemu palynoflora is characterized by the predominance of gymnospermous pollen, the relative abundance of pteridophytic spores and the absence of angiospermous pollen. Coniferae is dominant, while Lygodiaceae and Schizaeaceae are important in the flora. The most common species of palynomorphs are Todisporites minor, Cicatricosisporites dorogensis, C. australiensis, Lygodiumsporites subsimplex, Schizaeoisporites cretacius, S. zizyphinus, S. certus. Cibotiumspora paradoxa, Cyathidites australis, C. minor, Biretisporites potoniael, Cycadopites minimus, Pseudowalchia hiangulina, Parvisaccites radiatus, Podocarpidites multesimus, P. canadensis, Alisporites bilateralis, Cedripites cretaceus, C. canadenris, Abietineaepollenites microalatus, Clarsopollis classoides, C annulatus, C. xinjiangensis (sp. nov.), Ephedripites multicostatus, E. tarimensis (sp. nov.), etc . The palynoflora is comparable with those of the lower part of the Lower Xinminbu Formation in northwestern China and the lower part of the Lower Mannville Formation in western Canada, which is considered corresponding from Berriasian to Valanginian in age. The Shushanhe palynoflora is also characterized by dominance of gymnosperms and subdominance of pteridophyta. Some primitive angiospermons pollen grains are found in the upper part of the formation. In addition to the most common species of the above mentioned palynoflora, the important species in the present palynoflora comprise Cicatricosisporites potomacensis, C. orbiculatus, C. subrotundus, Concavissimisporites punctatus, C. verrucosus, C. globosus, lmpardecispora apiverrucata, Trilobosporites crassus, T. trioreticulosus, Pilosisporites verus, P. trichopapillosus, Klukisporites pseudoreticulatus, Verrucosisporites obscurilaesuratur, Converrucosisporites saskatchewanensis, Foraminisporis wonthaggiensis, Cingulatisporites valdensis, C. ruginosus, Jiaohepollis verus, Pityosporites constrictus, etc. More than 40 in dicative species of Early Cretaceous occur in the assemblage. The palynoflora compares clcsely with those of the middle part of the Lower Xinminbu Formation and the Quartz Sand Member of the Lower Mannville Formatton. It is suggested that the Shushanhe Formation should belong to Hauterivian of Barremian in age. The Baxigai palynoflora is basically similar to the Shushanhe palynoflora. But the palynoflora shows an obvious increase in abundance of lygodiaceous spores and angiospermous pollen accompanied by a great reduction of Classopollis and Ephedripltes. Most of the Early Cretaceous species occurring in the above mentioned palynofloras are present. In addition, some Cretaceous species recorded from Aptian and Albian Stages in Europe, North America and Australia, such as Trilobosporites tribotrys, T. trioreticulosus, Coptospora paradoxa, Camarozonosporites insignis, Crybelosporites punctatus, etc., appear in the assemblage. In comparison with the microfloras of the upper part of the Lower Xinminbu Formation, the Upper Mannville Formation and the lower part of the Lower Colorado Group, the Baxigai Forma- tion should be referred to Aptian to Albian in age. Judging from the palynofloras, the early Cretaceous palaeoclimate in the basin should belong to the arid or semi-arid type of the subtropic zone. However, from Barremtan through Albian the climatic conditions might appear relatively wet.     

Embryology of Swertia (Gentianaceae) relative to taxonomy

The embryological features of three species of Swertia ( s.l.) – S. erythrosticta , S. franchetiana , and S. tetraptera – were characterized, and the observations were used, together with previously gathered data on other species, to evaluate a recently proposed polyphyly, based on molecular data, of Swertia s.l. Comparisons of species within the genus showed that they have diversified embryologically, and there are significant between-species differences. Notable features that vary between species include the number of cell layers that form the anther locule wall, the construction of the wall of the mature anther, tapetum origin, the cell number in mature pollen grains, the structure of the fused margins of the two carpels, the ovule numbers in placental cross-sections, the shape of the mature embryo sac, the degree of ovule curvature, antipodal variation and the presence of a hypostase, and seed appendages. They share characters that are widely distributed in the tribe Gentianeae, such as a dicotyledonous type of anther wall formation, a glandular tapetum with uninucleate cells, simultaneous cytokinesis following the meiosis of the microsporocytes, tetrahedral microspore tetrads, superior, bicarpellary and unilocular ovaries, unitegmic and tenuinucellar ovules, Polygonum -type megagametophytes, progamous fertilization, nuclear endosperm, and Solanad-type embryogeny. The presence of variation in embryological characters amongst the species of Swertia s.l. strongly supports the view that Swertia s.l. is not a monophyletic group. Frasera is better separated from Swertia s.l. as an independent genus, and is only distantly related to Swertia s.s. judging from the numerous differences in embryology. Swertia tetraptera is very closely related to Halenia , as they show identical embryology.  © 2007 The Linnean Society of London, Botanical Journal of the Linnean Society , 2007, 155 , 383–400.     

Origin,Differentiation, and Geographic Distribution of the Chenopodiaceae

Numbers of species and genera,endemic genera,extant primitive genera,relationship and distribution patterns of presently living Chenopodiaceae(two subfamilies,12 tribes,and 118 genera)are analyzed and compared for eight distributional areas,namely central Asia,Europe,the Mediterranean region,Africa,North America,South America, Australia and East Asia． The Central Asia,where the number of genera and diversity of taxa are greater than in other areas,appears to be the center of distribution of extant Chenopodiaceae．North America and Australia are two secondary centers of distribution． Eurasia has 11 tribes out of the 12,a total of 70 genera of extant chenopodiaceous plants,and it contains the most primitive genera of every tribe． Archiatriplex of Atripliceae,Hablitzia of Hablitzeae,Corispermum of Corispermeae,Camphorosma of Camphorosmaea,Kalidium of Salicornieae,Polecnemum of Polycnemeae,Alexandra of Suaedeae,and Nanophyton of Salsoleae,are all found in Eurasia,The Beteae is an Eurasian endemic tribe,demonstrating the antiquity of the Chenopodiaceae flora of Eurasia．Hence,Eurasia is likely the place of origin of chenopodiaceous plants． The presence of chenopodiaceous plants is correlated with an arid climate．During the Cretaceous Period,most places of the continent of Eurasia were occupied by the ancient precursor to the Mediterranean,the Tethys Sea．At that time the area of the Tethys Sea had a dry and warm climate．Therefore,primitive Chenopodiaceae were likely present on the beaches of this ancient land．This arid climatic condition resulted in differentiation of the tribes Chenopodieae,Atripliceae,Comphorosmeae,Salicornieae,etc．,the main primitive tribes of the subfamily Cyclolobeae. Then following continental drift and the Laurasian and Gondwanan disintegration, the Chenopodiaceae were brought to every continent to propagate and develop, and experience the vicissitudes of climates, forming the main characteristics and distribution patterns of recent continental floras. The tribes Atripliceae, Chenopodieae, Camphorosmeae, and Salicornieae of recent Chenopodiaceae in Eurasia, North America, South America, southern Africa, and Australia all became strongly differentiated. However, Australia and South America, have no genera of Spirolobeae except for a few maritime Suaeda species. The Salsoleae and Suaedeae have not arrived in Australia and South America, which indicates that the subfamily Spirolobeae developed in Eurasia after Australia separated from the ancient South America-Africa continent, and South America had left Africa. The endemic tribe of North America, the tribe Sarcobateae, has a origin different from the tribes Salsoleae and Suaedeae of the subfamily Spirolobeae. Sarcobateae flowers diverged into unisexuality and absence of bractlets. Clearly they originated in North America after North America had left the Eurasian continent. North America and southern Africa have a few species of Salsola, but none of them have become very much differentiated or developed, so they must have arrived through overland migration across ancient continental connections. India has no southern African Chenopodiaceae floristic components except for a few maritime taxa, which shows that when the Indian subcontinent left Africa in the Triassic period, the Chenopodiaceae had not yet developed in Africa. Therefore, the early Cretaceous Period about 120 million years ago, when the ancient Gondwanan and Laurasian continents disintegrated, could have been the time of origin of Chenopodiaceae plants.The Chinese flora of Chenopodiaceae is a part of Chenopodiaceae flora of central Asia. Cornulaca alaschnica was discovered from Gansu, China, showing that the Chinese Chenopodiaceae flora certainly has contact with the Mediterranean Chenopodiaceae flora. The contact of southeastern China with the Australia Chenopodiaceae flora, however, is very weak.     

草鱼鳃上寄生毛管虫一新种——变异毛管虫的研究

吸管亚纲(Subclass suctoria)中,多数种类具有或长或短的炳,附着它物上营固着生活。寄生在鱼类体表、鳃丝内的毛管虫(Trichophrya)和簇管虫(Erastophrya)的种类中,至今未见报道有固着柄的代表。       

Cuban Calisto (Lepidoptera, Nymphalidae, Satyrinae), a review based on morphological and DNA data

The Cuban species of Calisto are reviewed based on the morphology of adult and immature stages, as well as DNA sequences of six genes (COI, EF1α, wingless, GAPDH, RpS5, CAD). A new species, Calisto occultasp. n., is described from the northeastern Cuban mountains. Calisto smintheus Bates, 1935 and Calisto bruneri, Michener 1949 are revised and revalidated. A new status, the species level, is proposed for Calisto brochei, Torre 1973, Calisto muripetens, Bates 1939 and Calisto bradleyi, Munroe 1950. The immature stages of Calisto smintheus, Calisto brochei,and Calisto occulta are described for the first time, and those of Calisto herophile, Hübner 1823 are redescribed. Useful morphological characters for adults are the shape and conspicuousness of androconial patch, the number and relative size of white dots on underside of hindwing, the shape of aedeagus, the shape of digitiform projection of genitalia valve, the shape and relative size of tegumen and uncus, the relative size of female genitalia, the height of sterigmal ring dorsal crown of the latter, and the relative size of corpus bursae and ductus bursae. For the immature stages, the most important characters are the color pattern of head capsule, the number and width of longitudinal lines of body, in the larvae; and the color pattern and the absence or presence of dorsal ridges on the abdomen of pupae. The phylogenetic relationships between the Cuban Calisto species are quite robust and well-supported; however, conflict between mitochondrial and nuclear datasets was detected in Calisto brochei, Calisto muripetens and to a lesser degree in Calisto bradleyi.     

小鼠基因组中的微卫星重复序列的数量、分布和密度

作者分析了老鼠基因组中各染色体及其内含子、外显子和基因间区上各种类型的微卫星(1-6个碱基的重复序列)的数量及其密度。SSR约占老鼠基因组的2.85%,其中46.2%存在于基因间区,4.75%存在于外显子,49.05%在内含子区域,即非编码区富含微卫星。微卫星的数量与染色体或基因区域的大小有关,但密度与染色体或基因区域的大小的关系并不十分密切。第4染色体的外显子区域中6种类型的SSR含量都比其它区域少。A,T,AC,AG,AT,AAC,AAG,AGG,AAAC,AAAG,AAAT,AACC,AAAAC,AAAAG,AAAAT,AAACC,AAAGG,AAGAG,AAAAAC,AAAAAG,AAAAAT,AAAGAG,ACACAT,ACAGAG,ACAGGC,ACATAT是老鼠基因组中主要的SSR类型,而一些5碱基重复单元的SSR在老鼠基因组的某一条甚至某几条染色体都不存在     

From the creation of the Veterinary Schools to the evolution of the notion of contagion in the 19th and 20th centuries

The creation of the Veterinary Schools in the 18th century would reveal a plethora of scientists, some of whom would be the precursors of Pasteur, some rivals, others followers collaborators or friends of the Master. Among the precursors let us name Chabbert, Huzard, Girard, Delafond, Renault, Toussaint, Galtier ; among the rivals: Chauveau, Arloing, Cornevin and Thomas; among the followers, collaborators or friends of Pasteur: Bouley, at first a resolute spontaneist, then the most fervent in defense of Pasteur (President of the Academy of Medicine and of the Academy of Sciences) and Nocard, Director of the School in Alfort, an important collaborator of Pasteur. Later, there was Leclainche, who created the International Office of Epizootics, and who was President of the Academy of Sciences; Guérin, who with Calmette developed the BCG vaccination; Ramon, the father of anatoxins (vaccines against diphtheria, and tetanus, combined vaccines, adjuvants to immunity). Thus, the creation of the Veterinary Schools contributed not only to the evolution of the notion of contagion, to the amelioration of animal health and the economics of agricultural production, but also to serious advances in human care, and to the protection of public health.     

Comparative morphology of male reproductive systems in Mediterranean blennies (Blenniidae)

The male reproductive organs of 16 species of Mediterranean Blenniidae ( Aidablennius sphynx, Blennius ocellaris, Coryphoblennius galerita, Lipophrys adriaticus, L. canevae, L. dalmatinus, L. nigriceps, Parablennius gattorugine, P. incognitus, P. sanguinolentus, P. rouxi, P. tentacularis, P. zvonimiri, Paralipophrys trigloides, Salaria pavo and Scartella cristata ) consist of pairs of testes, testicular glands, spermatic ducts, and blind pouches. Three main types of accessory sex organs were found by comparing the external morphology of the male gonads. Differences between species were observed in the volume of the testicular gland in relation to the volume of the testis and in the size and length of the spermatic ducts, and blind pouches. The anatomy of the testicular glands of all species investigated do not differ. Each gland consists of ducts that appear to be tubules which terminate at the testis periphery on one side and at the spermatic duct on the other side. Contrary to previous claims, A. sphynx has no fat body in place of the testicular gland; the gland of this species was not distinguishable from that of the other species investigated. In the Lipophrys species, in P. trigloides , and in B. ocellaris , a transition zone between testis and testicular gland is present. The testicular blind pouches empty into the spermatic ducts, into the ureter, or separately on the genital papilla. In most species, the epithelium has no or low folds, while in S. pavo it possesses high folds that nearly fill the lumen of the blind pouches. The morphological results are discussed in connection with taxonomy, ecology, and behaviour of the fishes.     

Phylogeny and evolutionary history of the Aplodontoidea (Mammalia: Rodentia)

Athough over a hundred species of fossil aplodontoids have been described since the extant species, Aplodontia rufa (the mountain beaver), was first described by Rafinesque in 1817, a thorough survey of the relationships among all the species in this clade has not been undertaken since McGrew's study in 1941. Here, a complete phylogenetic analysis of all published species of aplodontoids is used to reconstruct the evolutionary relationships within the clade, and to present an updated classification of the Aplodontoidea. Several of the traditionally recognized subfamilies are found to be paraphyletic, namely the Prosciurinae, the Allomyinae, and the Meniscomyinae. Others, however, including the Aplodontinae and the Mylagaulidae, appear to be monophyletic. These latter two taxa, which include all of the hypsodont members of the aplodontoid clade, seem to be sister taxa. The history of the aplodontoid clade shows several episodes of rapid diversification in the Early Oligocene, the Late Oligocene, and the Early to Middle Miocene. The Ansomyinae and Aplodontinae show comparatively low speciation rates. The patterns of change in morphology and evolutionary rates suggest a need for a more detailed study of the causes of diversification, extinction, and ecological change in this lineage.  © 2008 The Linnean Society of London, Zoological Journal of the Linnean Society, 2008, 153 , 769–838.