白柄菌属一新种

本文报告粘菌一新种,团孢白柄菌 Diachea synsPora sp.nov.文中对该新种的形态特征作了汉文和拉丁文的描述,附有照片和绘图,并讨论了新种与本属其它种的区别。模式标本保存在中国科学院微生物研究所真菌标本室。     

DISCOVERY OF THE UPPER CHEEK TEETH OF GOBIOLAGUS TOLMACHOVI (LAGOMORPHA, MAMMALIA)

<正> The upper cheek teeth of a Late Eocene laporid, Gobiolagus tolmachovi, are described here for the first time.Of 9 genera of Palaeolaginae of Leporidae, it is only the genus Gobiolagus, whose upper cheek teeth have never been reported before.The specimen was collected by the Sino-Soviet Palaeontological Expedition team in Shara Murun area, Nei Mongol in 1960. Its geological age is considered to be of Late oEcene (Shara Murun Formation).     

THE PLIOCENE MICROMAMMALIAN FAUNA FROM JINGLE, SHANXI——A DISCUSSION OF THE AGE OF JINGLE RED CLAY

<正> The Cenozoic deposits of Jingle area was first explored by Teilhard de Chardin & Young in 1929, and six species of mammals: Hipparion houfenense, Gazella blacki Antilospira licenti, Elephas sp., Cervus sp., and Rhinocerotidae gen. indet, were found from the Red Clay in Loc. 1 (Hefeng). Based on the Jingle Fauna, Teilhard de Chardin & Young concluded that the fossil-bearing layer was situated between the typical Hipparion richthofeni Red Clay (Pontian) and the Sanmenian deposits (Polycene) (Teilhard de Chardin & Young, 1930, 1931) and called it "Upper Pontian". Since then, Jingle Formation (or Jingle Red Clay) has been widely used in the stratigraphic generalization of North China (Pei et al., 1963) although its definition and age assignment have never been cleared up. "Jinglean" was put into use for the first time as a stage name by Li et al. (1984, in Chinese) to represent Early Pliocene tentatively: "It may be equivalent to Early Pliocene, more plausibly, it is later ...... Jinglean was temporarily used here to represent Early Pliocene by tradition." In order to make clear the age of Jingle Red Clay and enrich the Hefeng Fauna, a field survey was made in the Summer of 1986 by Chen Xiaofeng and the author. An assemblage of fossil micromammals was unearthed by means of wet-sieving techniques. About 1 ton of sediments from Hefeng (Loc. 86007, or Loc. 1) and Xiagaoai (Loc. 86008, or Loc. 2) in Jingle county (see fig. 1), yielded over 1000 specimens of small mammals. The specimens are from four layers (see table 1), and the present paper only deals with the micromammals from the sand layer and the Red Clay at Hefeng (fig. 2).     

中国境内大角鹿属的下颌骨厚度问题

中国境内的大角鹿属是第四纪期间与人类化石相伴生的重要动物化石,过去常根据下颌骨厚度指数来鉴定大角鹿属各个种,现在看来,其角的形态变化,才是最重要依据.在中国大角鹿主要分布于北方地区,早期类型生存于温暖地带,晚期生存于稍寒冷一些地带.     

REMARKS ON THE OIOCEROS SPECIES (BOVIDAE, ARTIODACTYLA, MAMMALIA) FROM THE NEOGENE OF CHINA

<正> The genus Oioceros was created by C. Gaillard (1902) based on the species Antilope rothii Wagner, 1857 from the Turolian of Pikermi, Greece. Its diagnosis is that 'Bovidae of small size with long slender muzzle; face bent down on basicranial axis either slightly or to a moderate extent; orbits with expanded orbital roof; horn-cores twisted counter-clockwise in a fairly close spiral of one or two revolutions, widely separate, tilted backward or fairly upright, divergent, with a cross-section almost circular or elliptical, keeled either anteriorly or posteriorly or both; dentition moderately hypsodont, premolar series rather long and slender, molars broad with ribs of medium strength.' (after Pilgrim and Hopwood, 1924, p. 24). Up to now, it has included approximately seventeen species from the Neogene of the Old World (twelve species in Asia, four in Europe and one in Africa).     

猫丘脑束旁核神经元对电刺激外周神经与动脉注射缓激肽的放电反应

为了确定丘脑束旁核神经元对外周神经伤害性刺激的各类反应是否都属于痛敏反应,在氯醛糖麻醉的36只猫上观察了束旁核神经元对强电流刺激外周神经与动脉注射缓激肽的放电反应。根据放电的潜伏期和持续时间,可将观察到的162个单位对强电流刺激外周神经的反应分成四种类型。1.短潜伏期反应,69个单位。2.长潜伏期反应,15个单位。3.短-长潜伏期反应,37个单位。4.自发放电抑制,41个单位。静脉注射芬太尼不能抑制短潜伏期反应,动脉注射缓激肽不能诱发这类神经元放电,说明这类反应不是痛敏反应。其它三种反应,都可为静脉注射芬太尼所抑制或减弱,又可为动脉注射缓激肽所诱发,说明这三类反应都属于痛敏反应。     

A NEW GENUS OF HIODONTIDAE FROM LUOZIGOU BASIN, EAST JILIN

<正> Manchurichthys (Saito, 1936) has been, for a long time, the only representative of fossil vertebrate known from the Oil-bearing member of Dalazi Formation, Luozigou Basin, East Jilin. Since 1978, some new materials have been collected there by the Regional Geological Brigade of Jilin Province and the present author. Two more forms of fossil fishes are not known to occur in the rocks of this section. One is Sinarnia luozigouensis (Li, 1984) which is referred to Amiiformes; the other, Yanbiania (gen. nov.), is described in this paper and included in the osteoglossomorphan family Hiodontidae.     

MAMMALIAN REMAINS FROM THE PLIOCENE OF THE HANSHUI RIVER BASIN, SHAANXI

<正> A lot of mammalian remains from Yangjiawan village, the Hanshui River basin, Mianxian, Shaanxi, were collected by a field team of IVPP and the Geological Museum of Shaanxi Province in the autumn of 1984. Fossil mammals found in Yangjiawan Formation include 13 species (including three new species) belonging to 12 genera. This paper will give a preliminary study of the mammalian remains and observation of stratigraphic sections of several localities.     

内蒙古阿左旗乌兰塔塔尔中渐新世的鼠兔科化石及有关问题的讨论

本文记述了发现在内蒙古阿左旗乌兰塔塔尔中渐新世地层中的鼠兔科化石,计两属四种.着重对微型链兔的形态特征做了较多的补充和订正,并对链兔属中种的性质作了初步探讨,取消了步林兔属名,将亚洲的链兔归并成五个种.还对链兔和中华兔的地史分布、某些进化趋势及其他有关问题提出了初步看法.     

THE ARAGONIAN VERTEBRATE FAUNA OF XIACAOWAN, JIANGSU——7. APLODONTIDAE (RODENTIA, MAMMALIA)

<正> The fossils which form the subject of the present study were collected in the recent years from the middle Miocene Xiacaowan Formation at three sites, Songlinzhuang, Shuanggou and Zhengji of Sihong, Jiangsu. Most of the material from the first two sites have been reported previously as Prosciurus sp. (Li et al., 1983). Further study indicates that all the specimens mentioned and the M_1/2 previously assigned to Prosciurus? shantungensis Rensberger et Li (1986) are quite different from those of Prosciurus, but represent a new genus, Ansomys. In some features, the new form resembles Plesispermorphilus? descedens of Europe. For the two taxa a new subfamily Ansomyinae is created. It is morphologically intermediate between Meniscomyinae and Allomyinae, and may be the sister taxon of the higher aplodontids Allomyinae and Aplodontinae.