多形小克银汉霉、暗孢小克银汉霉和褐孢小克银汉霉应否被接受为独立的种?

多形小克银汉霉(Cunninghamella polymorpha Pisnek)、暗孢小克银汉霉(Cunninghamella phaeospora Boedijn)和褐孢小克银汉霉(Cunninghamella brunnea J.N. Rai,S.C. Agarwal & J.P. Tewari)自分别在1929, 1958, 1968年发表以来,一直存在着不同意见上的争论,或承认或不承认,或合并到这个种或合并到那个种等等.我们在研究中国的小克银汉霉属的过程中,分离得到了九株多形小克银汉霉的菌株。为了确定这个种的分类地位以及澄清它与其他一些相关种的关系,我们将这些菌株与从国外交换获得的一些相关种的模式后代作了比较研究,所得结果表明多形小克银汉霉、暗孢小克银汉霉及褐孢小克银汉霉三种既不能相互合并亦不能合并到其他任何一种中去,而应作为独立的种被人们所接受。在我们的工作之前,这三个种的有性型均未有报道。我们在国内尚未发现暗孢小克银汉霉和褐孢小克银汉霉,只找到了多形小克银汉霉,但同时也找到了它的有性型.因此,多形小克银汉霉为我国的新记录种,其有性型的发现则为全世界的首次报道。多形小克银汉霉的主要区别性特征为孢囊梗主枝形成顶生泡囊或不形成而在顶部叉分为二至数个分枝,同一孢囊梗上的分枝长短不齐,接合孢子囊不正球形,配囊柄细长可达80微米等等.暗孢小克银汉霉的主要区别性特征为孢囊梗分枝很少或不分枝,在同一孢囊梗上分枝相距很远且都很短,泡囊形状多不规则且略呈多角形。褐孢小克银汉霉更易与其他种相区别,它的孢囊梗分枝很多,分枝成堆且指向不同的方向,泡囊典型地呈多角形,内外璧不重合。这三个种首次发表时以及后来经过不同作者重新研究后发表的描述及绘图均过于简单而未能充分显示出它们的区别性特征,因此我们在本文中再次作了描述并再次提供了详尽的线条图和显微照相。     

刺孢小克银汉霉原变种和轮生刺孢小克银汉霉变种(新组合)

刺孢小克银汉霉[Cunninghamella echinulata(Thaxt.) Thaxt. ex Blakeslce]是小克银汉霉属的模式种,多年来因不同作者是否将贝尼尔小克银汉霉(C. bainieri Naum.)包含在内而对此种持广义(sensu lato)或狭义(scnsu stricto)的不同理解。我们在国内分离到51株刺孢小克银汉霉(广义)菌种,经与获自css的7株菌(包括刺孢小克银汉霉的模式菌种在内)和IMI的1株菌(原定名称均为刺孢小克银汉霉)一起研究后,根据它们的无性型形态特征有明显不同但在配合试验中又可互相配合形成可育的接合孢子的结果,认为将它们处理为同一个种的两个不同变种较为合理.其中,13株中国的菌和3株CBS及IMI的菌被鉴定为刺孢小克银汉霉原变种(C. echinulata var. echinulata);其余的38株中国的菌和5株CBS的菌被鉴定为轮生刺孢小克银汉霉变种(新组合)[C. echinulata var. verticillata (F. S. Paine.) comb. nov.j.以‘轮生(verticillata)’作为新组合变种的加词是根据与贝尼尔小克银汉霉同物异名的‘轮生布拉小克银汉霉(C. blakesleeana var. verticillata (F. S. Paine) Baijal & B. S. Mchrotra)’而来的.在前人的工作中,对刺孢小克银汉霉持狭义理解的作者往往根据孢子枝的分枝方式、巨型暗色孢子的有无、以及40℃能否生长来区分这两个分类群.对刺孢小克银汉霉持广义理解的作者则认为这些特性毫无意义.我们同意后面两个特性意义不大,因为二者的许多菌系都能形成巨型暗色袍子并在40℃生长,但认为孢子枝分枝方式确实是区别这两个分类群的重要依据.此外,根据产孢构造的种类、孢子枝主枝的直径、孢子枝第一次分枝的数目、分枝长度、孢子枝主枝的顶生泡囊形状以及其直径等性状综合考虑,这两个分类群是不难明确区分的,对12株刺孢小克银汉霉原变种和13株轮生刺孢小克银汉霉相互之间所进行的配合试验结果表明,在具一定性亲和力的(+)、(一)菌系同时存在时,两个变种内和变种之间均可形成可育的接合孢子。对上述三种配合的各六对菌所形成的有性型形态的研究结果则表明,除轮生刺孢小克银汉霉变种内形成的接合孢子的壁往往较厚外,各种配合形成的有性型形态基本上是一致的.我们研究组的其他成员最近曾对小克银汉霉的22株菌进行了rDNA的ITS区的PCR产物长度测定,其中包括了刺孢小克银汉霉原变种和轮生刺孢小克银汉霉变种的各3株菌,它们的平均长度(bp)分别为890±7.5和915±7.6.这个结果也支持了我们在这两个分类群可以互相配合的情况下仍将它们作为两个不同变种的处理.这两个分类群虽然已被发表多次,但它们的描述和绘图均过于简单而未能充分显示出它们的区别性特征,因此我们在本文中再次作了描述并再次提供了详尽的线条图和显微照相.     

克氏鱼(Clarkeosteus)的新发现

文中记述了采自云南盘溪地区一真节甲鱼类化石,根据材料特征认为属于克氏鱼属—新种,即一打得克氏鱼(Clarkeosteus yidadeinsis sp. nov.).     

克柔念珠菌对抗真菌药物耐药机制的研究进展

近年来,克柔念珠菌感染明显增加,对抗真菌药物尤其是唑类药物的耐药现象越来越严重,深入研究其耐药机制已引起高度关注.克柔念珠菌耐药机制可能与以下因素有关:唑类药物作用靶酶结构的改变、真菌细胞膜上外排泵过度表达、真菌细胞内药物蓄积减少等.克柔念珠菌对唑类的耐药可能是多种耐药机制共同作用的结果.     

陆谟克堂

陆谟克,即拉马克(Lamarck Jean Baptiste,1744—1829),是最先提出生物进化学说的法国生物学家。陆谟克堂则是按他的名字命名的一所建筑,在现在的北京动物园内。     

他克莫司对HaCaT细胞NF-kB表达的影响

目的:探讨他克莫司对HaCaT细胞中NF-kB分子表达的影响.方法:培养人HaCaT细胞,分别与10 μ mol.l-1和50 μ mol.l-1他克莫司溶液共孵育后,通过RT-PCR和Western-blot方法,分别从基因和蛋白水平,观察NF-kB分子表达的变化.结果:经10 μ mol.l-1和50 μ mol.l-1的他克莫司(FK506)溶液孵育后,HaCaT细胞中NF-kB分子表达明显低于对照组,同时体现一定的剂量效应,50 μ mol.l-1组的表达水平更低.结论:他克莫司可以剂量依赖性地抑制HaCaT细胞中NF-kB的分子表达.     

克蚱属一新种记述(直翅目,蚱科)

报道采自长白山地区克蚱属Clinotettix Bei-Bienko昆虫1新种,即长白山克蚱C. changbaishanensis sp.nov.,该种隶属于直翅目蚱总科,并与本属的其他种类进行比较.模式标本保存于东北师范大学生命科学学院动物标本室.     

克木毒蛋白三种酶活性与色氨酸残基的关系

对一种新的核糖体失活蛋白──克木毒蛋白的研究表明,该分子中仅含一个色氨酸.此色氨酸与克木毒蛋白具有的三种酶活性有明显不同的关系.     

肺炎克氏杆菌(K.pneumoniae)中的固氮基因区

来源于肺炎克氏杆菌(K.pneumoniae)中的固氮基因位于质体pRDI。它是由寄主范围很广的质体pRDI及肺炎克氏杆菌染色体上一个60 md的片段所组成。     

霉克舒对致病性浅部真菌的体外抑菌作用研究

从湛江地区 15 4例癣病患者分离真菌 ,评价一种新的抗真菌药—霉克舒对上述真菌菌株的体外抑菌活性。应用琼脂稀释法测定霉克舒对浅部真菌的最小抑菌浓度 (MIC) ,同时以兰美抒作为对照药物。从 15 4例癣病患者中分离出 14 1株真菌 ,其中以红色毛癣菌和须癣毛癣菌为主 ,分别占 6 6 .7%和 14 .2 %。霉克舒的抑菌作用与兰美抒相比略强或相当 ;对霉克舒各单一成分的初步抑菌效果进行比较 ,复合物的抑菌作用明显强于水杨酸或特比萘芬等单一成分。上述结果显示 ,霉克舒在体外对常见致病性浅部真菌具有较强的抗菌活性。     

内蒙古阿左旗乌兰塔塔尔地区渐新世地层剖面及动物群初步观察

内蒙古阿左旗乌兰塔塔尔地区的渐新世地层中,哺乳动物化石丰富,种类繁多。本文是这个动物群研究的初步报道,除对动物群中各成员和地层概况做了简单介绍外,还对化石层的时代作了初步探讨。     

内蒙阿左旗乌兰塔塔尔中渐新世的梳趾鼠类

本文描述和比较了发现在我国内蒙古阿左旗乌兰塔塔尔地区中渐新统的三属七种啮齿类梳趾鼠科化石,其中包括三个新种.并对某些种类的归属和性质做了初步的讨论.     

Lithostratigraphic context of Oligocene mammalian faunas from Ulantatal,Nei Mongol,China

The Ulantatal area is well-known for its extraordinarily rich Oligocene mammalian fossils. The Ulantatal fauna was originally considered to be the representative fauna for the Chinese Land mammalian Age, Ulantatalian. However, the abundant fossils collected in the 1980s lack coordinates and/or detailed stratigraphic levels, and have been lumped together as either single, coeval fauna or grouped into three units. This lack of stratigraphic information hampers more precise biostratigraphic division and correlation of the faunas. Here we present a complete lithostratigraphic profile of the Ulantatal Formation with new fossil localities calibrated into the profile. Lithologically, the sequence shows a rather uniform pattern characterized by interbedded reddish to yellowish brown claystones and siltstones, with minor fine-grained sandstones. Preliminary biostratigraphic analysis shows that the Ulantatal Formation covers most of the Oligocene, and offers a long sequence and successive fossil records for understanding the evolution of mammal faunas after the critical Eocene/Oligocene transition.     

Early Ordovician bivalves from Dali, West Yunnan, China

A bivalve fauna of Early Ordovician (late Arenig) age is described from the Hsiangyang Formation of the eastern part of West Yunnan, China. The fauna contains elements in common with Early Ordovician faunas of southern Gondwanan areas such as the Montagne Noire and Morocco and with those of Avalonia, together with several previously undescribed taxa. The following taxa are new: Biseriodonta simplex gen. et sp. nov.; Glyptarca sinensis sp. nov.; Trigonoglyptarca magna gen. et sp. nov.; Erhaiconcha xiangyangensis gen. et sp. nov.; Fasciculodonta impressa gen. et sp. nov.; Yunnanoredonia laevis gen. et sp. nov.; Daliella gen. nov.; Goniophorina ( Goniophorina ) contracta sp. nov.; Haidongoconcha radialis gen. et sp. nov.; Eopterinea aequiconcha gen. et sp. nov. The bivalve fauna includes the most diverse glyptarcid fauna and the earliest nuculanid and paracyclid known hitherto.   Eastern West Yunnan belonged to the Indochina terrane and it is concluded that the bivalve fauna represents a high-latitude assemblage and that the Indochina terrane should be considered a component part of the Peri-Gondwanan continent in the Ordovician; its bivalve faunas contrast with those of neighbouring terranes which have affinities with those of lower latitudes.     

Early Silurian(Telychian)rugose coral fauna of Daguan area, northeast Yunnan Province,China

Study on rugose coral fauna of the Sifengya Formation(early Telyehian)and Daluzhai Formation (mid-late Telychian)in Daguan area,northeast Yunnan Province,China was carded out.Rugose coral fauna of the Sifengya Formation included 18 genera and 34 species,while Daluzhai Formation with nine genera,ten species.We described rugose coral fauna(12 genera,19 species)including one new genus and five new species,i.e.Protoketophyllum daguanense gen.et sp.nov..Crassilasma huanggexiense sp.nov.,Pseudophaulactis heae sp.nov.,P.convolutus sp.nov.,and Shensiphyllum minor sp.nov..The characteristics and geological significance of rugose coral fauna of Sifengya Formation and Daluzhai Formation were analyzed.Particularly,mgose coral fauna of the Sifengya Formation represent early Telychian rugosan fauna in the Upper Yangtze region and improve the sequences of early Silurian(Llandovery)mgose coral assemblages in Yangtze region.It is therefore very meaningful to further analyze radiation period of rugose coral fauna in such epoch.     

A new ammonoid fauna from the Carnian (Upper Triassic) Kasimlar Formation of the Taurus Mountains (Anatolia,Turkey)

We describe a new ammonoid fauna from the Taurus Mountains of southern Turkey. The Carnian ammonoid fauna from A?a?iyaylabel is presented for the first time. Ammonoids were obtained from limestone to marl beds of an approximately 35‐m‐thick section, which presents the rare opportunity to investigate ammonoid faunas across the Lower–Upper Carnian boundary. Intense sampling near the village of A?a?iyaylabel led to the recognition of a new Lower Carnian (Julian 2) to Upper Carnian (Tuvalian 1) ammonoid fauna from the Kasimlar Formation. The genus Kasimlarceltites gen. nov. is reported for the first time from the Taurus Mountains, which represents the main faunal element and occurs as huge mass occurrence (n ? 1 million). Kasimlarceltites krystyni gen. et sp. nov., Klipsteinia disciformis sp. nov. and Anasirenites crassicrenulatus sp. nov. occur within the Lower Carnian Carbonate member (Units A–B) of the Kasimlar Formation from the Taurus Platform Units. Ammonoids described from the marls of the Tuvalian Marlstone member were deposited during a major, Tethyan‐wide climate crisis – the so‐called Carnian crisis – characterized by a demise of carbonate platforms. Based on the biostratigraphic relevance of certain ammonoid taxa described herein, the age of the analysed parts of the Kasimlar Formation is Julian 2 to Tuvalian 1. The discovery of the new ammonoid assemblages from A?a?iyaylabel substantiates the significance of Upper Triassic faunas within the Taurus Mountains and facilitates the correlation with faunal assemblages from other regions in the Tethyan Realm. The ammonoid fauna and facies indicate a general deepening from open‐platform margins, over deeper shelf settings down to an open marine‐influenced basinal environment. The tentative habitat for Kasimlarceltites gen. nov. is a shallow platform environment to upper mid‐ramp.     

New dipodid rodents from the Late Eocene of Erden Obo (Nei Mongol,China)

New dipodid occurrences (Heosminthus nomogenesis sp. nov., Sinosminthus sp., Allosminthus cf. A. majusculus, Allosminthus ernos and Allosminthus cf. A. diconjugatus) are reported from the ‘Upper Red’ beds of the Erden Obo section in Nei Mongol, China. Heosminthus nomogenesis is similar to Heosminthus primiveris from the Caijiachong Formation, and it is more primitive than Heosminthus chimidae of the Mongolian biozone A. Allosminthus cf. A. majusculus has a more variable mesolophid and metalophid in m1-2. Based on the dipodid assemblage, the age of the ‘Upper Red’ of the Erden Obo section is late Eocene and correlative to the Ergilian. Based on the comparison of their morphological characters, we recognize some differences between the stem dipodoids and muroids.     

江苏泗洪早中新世下草湾组仓鼠科化石(英文)

描述了20世纪80年代在江苏泗洪早中新世下草湾组采集的5属5种仓鼠类动物化石,其中包括1新属和4新种,即Eumyarioninae亚科的Alloeumyarion sihongensis gen.et sp.nov.,Cricetodontinae亚科的Cricetodon wanhei sp.nov.,Copemyinae亚科的Primus pusillus sp.nov.和Democricetodon suensis sp.nov.,以及Megacricetodontinae亚科的Megacricetodon sinensis Qiu et al.,1981。Cricetodon,Democricetodon和Megacricetodon属常见于早、中新世地层,并有较广泛的地理分布;Primus属仅发现于印度次大陆下中新统;新属Alloeumyarion可能与Eumyarion属有较接近的亲缘关系。泗洪发现的仓鼠是该哺乳动物群中种类最多、材料最丰富的一类啮齿动物。泗洪地点位于现代东洋界与古北界的过渡地带,这一化石组合的出现为我国中新世哺乳动物地理及其演变的研究提供了有用的证据。根据仓鼠类化石的研究,下草湾组的时代很可能属于早中新世晚期,或者是中国陆相哺乳动物时代的山旺期,大体相当于欧洲陆相哺乳动物时代的奥尔良期或MN4带的时代。这些新属和新种的特征如下:异美鼠(新属)(Alloeumyarion gen.nov):美鼠亚科中个体中等者。牙齿低冠;齿尖中度鼓胀、趋于脊形。上臼齿三根,内谷前指向,原脊和后脊近横向平行排列,无前尖后刺;M1前叶前后向伸长,前边尖简单,有宽大的后边谷,但无前脊刺;M2的原脊稍前指向,舌侧与原尖前边连接;M3的后部明显退化。下臼齿双根,下外谷横向、近对称;m1下前边尖简单,下前脊单一,下原尖和下次尖的后臂不很发育;m2无下次尖后臂。万合古仓鼠(新种)(Cricetodon wanhei sp.nov.):个体中等大小。M1和M2四齿根,在早期磨蚀的牙齿中有清楚的后边谷,但外脊发育弱;M1的前边尖简单或略微分开;M2前边脊舌侧支模糊;M3冠面近圆形,多数牙齿的内谷为连接原尖和次尖的脊封闭,时见原脊后刺;m1具双下后脊和短的下中脊;m3与m2等长或比m2稍大,具短的下前边脊舌侧支。细先鼠(新种)(Primus pusillus sp.nov.):个体小。M1的前叶前后向较短,前边尖和前边脊弱,原脊略后指与原尖后臂连接,后脊稍前指与次尖前臂相连;m1具较宽且呈刀形的前边尖,下次脊前指向。苏众古仓鼠(新种)(Democricetodon suensis sp.nov.):个体中等大小,颊齿低冠,齿尖和齿脊较弱,臼齿中脊的长度一般在中长至长之间,上臼齿的双原脊不甚发育。M1的前边尖简单而窄,原尖前臂和原脊II间常有一脊相连;M2的后脊横向或稍前向;M2和M3多具"轴脊"("axi-oloph");m1的下前边尖单一而窄小;多数m1和m2有下外中脊;m3的下中脊通常显著。     

新疆布尔津地区晚始新世哺乳动物化石的发现及其意义(英文)

1995年以来作者等人在新疆准噶尔盆地北缘乌伦古河地区开展了第三纪哺乳动物地层研究工作。在调查研究该区乌伦古河组地层同时 (叶捷等 ,2 0 0 1a ,b) ,为搞清乌伦古河组的区域分布 ,我们在 1 999年和 2 0 0 1年先后两次前往布尔津地区考察了那里的“乌伦古河组”。在布尔津县城西北 1 4km处额尔齐斯河北岸的一片新生代露头 ,长期被视为乌伦古河组 ,因而时代也被定为始新世至渐新世 ,但一直没有确凿的化石依据。 1 999年我们首次在该套地层中采集到哺乳动物化石 ( 990 2 7地点 ) ,2 0 0 1年再次在同一地点、同一层位采集到化石并实测了地层剖面。布尔津的该乌伦古河组地层可大致分为两段 ,下段为富含铁质的砂岩与泥岩互层 ,上段为浅灰绿色砂岩与杂色泥岩互层 ,整套地层的风化表面呈黄棕色。在乌伦古河组建组的乌伦古河流域 ,乌伦古河组则由一套浅灰绿色砂岩与棕灰色含砂泥岩构成 ,整套地层风化表面呈灰白色 (叶捷等 ,2 0 0 1a)。两个地区的乌伦古河组的岩性显然是不同的。野外追索证明 ,这两个地区的两套不同岩性的地层是两个不同沉积盆地的堆积物 ,这两个盆地在乌伦古湖附近 (E87°1 2′)被一由古生代地层构成的山岭隔开。作为地质体 ,这两套地层间没有联系 ,不应当归为同一岩石地层单位。因此 ,布尔津     

Early Silurian (Telychian) rugose coral fauna of Daguan area, northeast Yunnan province, China

Study on rugose coral fauna of the Sifengya Formation (early Telychian) and Daluzhai Formation (mid-late Telychian) in Daguan area, northeast Yunnan Province, China was carried out. Rugose coral fauna of the Sifengya Formation included 18 genera and 34 species, while Daluzhai Formation with nine genera, ten species. We described rugose coral fauna (12 genera, 19 species) including one new genus and five new species, i.e. Protoketophyllum daguanense gen. et sp. nov., Crassilasma huanggexiense sp. nov., Pseudophaulactis heae sp. nov., P. convolutus sp. nov., and Shensiphyllum minor sp. nov. The characteristics and geological significance of rugose coral fauna of Sifengya Formation and Daluzhai Formation were analyzed. Particularly, rugose coral fauna of the Sifengya Formation represent early Telychian rugosan fauna in the Upper Yangtze region and improve the sequences of early Silurian (Llandovery) rugose coral assemblages in Yangtze region. It is therefore very meaningful to further analyze radiation period of rugose coral fauna in such epoch. __________ Translated from Acta Palaeontologica Sinica, 2005, 44(2): 229–246 [译自: 古生物学报, 2005, 44(2): 229–246]