湖北五峰三棱齿象化石

一、前言湖北省文物管理委员会于1960年时,曾由湖北五峰县征集到一枚古乳齿象类牙齿的化石。据当时的记录,它出产的确切地点虽不详,但发现于五峰县境内出产“龙骨”化石的山洞中,是没有疑问的。因当时著者正在研究柳城巨猿洞及广西其他山洞的长鼻类化石,其中包括有由柳城巨猿洞和封门山洞发现的古乳齿象类化石,故湖北省文物管理委员会委讬著者代为鉴订并作比较研究。     

扬子区五峰组胞石

本文首次详细描记了扬子区五峰组中已发现的胞石，计有7属12种。文中提出了二个胞石带，并与国外其它地区作了对比。根据本文所研究的胞石，认为苏北地区五峰早期为陆架深水环境．因此推断东台以北应面对或毗邻大陆域而不是华北古陆。扬子板块与华北板块的碰撞对接，不可能发生在晚奥陶世。     

湖北五峰后河国家级自然保护区鸟类多样性

为了解湖北五峰后河国家级自然保护区(以下简称后河保护区)鸟类物种多样性及其区系组成的变化, 我们通过样线、红外相机调查和检索文献资料相结合的方法获得了后河保护区鸟类名录, 并将其与后河保护区1999年科学考察结果进行对比分析。本研究于2017-2019年共在后河保护区内设置了82 km的鸟类调查样线, 共在309个位点上放置了红外相机, 累计99,586个相机日。我们用“后河” “鸟类” “湖北省”等关键词搜索相关出版物, 并查阅中国观鸟记录中心经审核后发布的鸟类信息, 结合样线和红外相机调查结果形成后河保护区鸟类名录。共整理得到后河保护区鸟类255种, 隶属于16目55科。其中, 国家I级重点保护野生鸟类2种, 包括中华秋沙鸭(Mergus squamatus)和金雕(Aquila chrysaetos); 国家II级重点保护野生鸟类46种, 包括红腹角雉(Tragopan temminckii)、棉凫(Nettapus coromandelianus)、松雀鹰(Accipiter virgatus)、灰林鸮(Strix aluco)、蓝鹀(Emberiza siemsseni)等。此外, 后河保护区有11种中国特有鸟类, 占我国特有鸟类种数(n = 93)的11.83%。在区系成分上, 后河保护区鸟类以东洋种为主(151种, 占59.22%), 其次为广布种(55种, 占21.57%)。与1999年科学考察结果相比, 鸟类增加了116种, 其中有15种国家重点保护野生鸟类。在区系组成上, 后河保护区内东洋种占比增加, 包括分布区向北扩散的物种成分。此外, 本次调查未记录到20世纪在保护区内有分布的白冠长尾雉(Syrmaticus reevesii)和海南鳽(Gorsachius magnificus)。本研究表明, 后河保护区鸟类物种多样性高、特有种及珍稀濒危物种丰富, 具有极高的保护价值和意义。通过对比分析后河保护区内野生鸟类动态变化, 可为保护区生物多样性监测方案设计和保护对策的制定提供科学依据。     

江西武宁晚奥陶世五峰期的叉笔石

首次系统描述了江西修水流域五峰期叉笔石９种和亚种。在对性状极性和性状状态分析的基础之上,运用最小进化单质法对该区五峰期叉笔石的分支图进行重建,揭示了叉笔石的亲近关系和进化水平;主要依据地层分布将分支图转化为系统树,探讨了叉笔石的演化关系。     

五峰尖贝原植物形态及有效成分研究

通过对湖北民间常用中药——五峰尖贝的产地调查,系统地对其原植物及药用器官(鳞茎)的形态及有效成分进行了研究。确定五峰尖贝为百合科(Liliaceae)植物太白贝母(Fritilliaria taipaiensis P.V.Li)。     

安徽泾县上奥陶统五峰组鹦鹉螺化石

一、前言本文所描述之鹦鹉螺化石标本为我所李积金、钱义元、张俊明以及南京地质矿产研究所应中锷等同志于1982年夏季采集,化石产于安徽泾县北贡公社南面三华里山冲附近走路岗和鸡笼坑上奥陶统五峰组。上奥陶统五峰组的鹦鹉螺化石曾在我国四川城口、西藏申扎、云南保山以及安徽贵池等地发现,但因多数保存在泥岩和页岩中,一般都成压扁状态,内部构造没有保存。由于壳形细长而直,往往被误认为是小型     

华南五峰期笔石动物群的分异及缺氧环境

前言晚奥陶世五峰期,即Ashgill期的笔石动物群在我国南部特别发育,其分布范围包括从扬子流域至珠江流域的广大地区。这些地区在五峰期都属于同一个大地构造单元,即华南古板块。扬子地台五峰期的笔石最早由穆恩之教授(1945,1954)研究,近年来穆恩之等正在系统总结这一地区的五峰期笔石动物群,多年来他还提出了笔石动物群生态分异的概念(穆恩之,1974,1980,1983;Mu,1984)。从六十年代以来,笔者曾先后观察了不少华南晚奥陶世地层剖面,采集了笔石。这些丰富的笔石动物群和岩石地层的资料,使笔者感到深入认识和探讨这一动物群的分异以及黑色笔石页岩的特殊形成环境是很有必要的。本文涉及的材料中,仅对桂北兴安、临桂、赣南崇义古亭和浙西江山     

江西武宁宁国组上部牙形刺兼论黑色页岩的形成环境和牙形刺的生态

本文研究了江西武宁奥陶系宁国组上部黑色页岩中的牙形刺。共发现牙形刺11属15种,其中Eoplacognathus suecicus Bergstrom,Eoplacognathus foliaceus(Fahraeus)为世界性分布的牙形刺带化石,为宁国组上部黑色页岩的划分与对比提供了可靠的依据。根据牙形刺的保存状态,笔者推论当时本区水底层为偏酸性还原环境,并认为牙形刺动物是浮游生活在不同深度的水层中。     

江苏仑山地区上奥陶统五峰组放射虫动物群及其地质意义

五峰组以盛产笔石动物群著称,时代为凯迪晚期(相当于英国的阿什极尔期),其中也发现了放射虫.该时期的放射虫在全球并不多见.本文首次描述江苏句容仑山地区五峰组的放射虫动物群,该动物群以不具刺的球形放射虫最为发育,并出现少量Inaniguttidae科的分子,化石保存较差,属种单调,分异度很低,这些特点与大西洋沿岸地区陆表海...     

SOME LOWER PERMIAN OSTRACODS FROM WESTERN HUPEH

IntroductionThe material described in the present paper was collected from the LowerPermian Chihsia limestone by Messrs.K.C.Yang and A.T.Mu in 1951 dur-ing their excursion in Western Hupeh.The Chihsia limestone is underlain by theMaan Coal series containing Lepidodendron ituense and is succeeded by the Mao-kou limestone bearing Verbeekina verbeeki.The most characteristic fossils collect-ed from the Chihsia limestone are:Hayasakaia elegantula Yabe et Hayasaka,Fistulipora chinensis Yoh,Stylidophyllum of intermidicum Huang,Polythecalisof.yangtzeensis Huang,Corwenia of.chihsiaensis Yoh.The Ostracods came     

SOME LOWER ORDOVICIAN OSTRACODS FROM WESTERN HUPEH

The specimens of Ostracoda dealt herewith were collected by Messrs.K.C.Yangand A.T.Mu from the Ichang formation of Lower Ordovician during their field tripin western Hupei in the Spring of 1951.Six new species in three different genera ofwhich one is new,are described in the present paper.All of them are found inassociation with graptolites and triobites.The Ichang formation has been divided     

NEW DEVONIAN OSTRACODS FROM HUPEH

The materials which form the subject of the present paper was collected fromthe Upper Devonian Hsiehkingssu formation of Changyang district,W.Hupeh.The majority of the ostracods are more or less ironized,and are usually wellpreserved.The specimens illustrated and described in this paper comprise 15 species in11 genera,of them 4 genera and 11 species are new.The Hsiehkingsuu formation of Changyang district of Hupeh is estimatedabout 30 meters in thickness.The ostracods obtained from the thin-bedded and     

ON SOME NEW OSTRACODS FROM KWANGSI

IntroductionThe materials which form the subject of the present paper were collectedfrom the following formations and localities:(1)The Middle Devonian Yukiangformation of Yungchun district and(2)The Devonian lenticular limestone ofLingchuan district of Kwangsi.The ostracods of the second locality are preservedas internal moulds and therefore are far from being complete.     

PERMIAN OSTRACODS FROM THE CHIHSIA LIMESTONE OF LUNGTAN, NANKING

The specimens described in this paper were collected in the spring of 1955 by the writer andher friends from the Lower Permian Chihsia limestone at Kwanshan, Lungtan, about 20 kmsoutheast of Nanking. The ostracods described and illustrated here comprise 37 species in 11genera, of which 29 species are new. The majority of the specimens were found in the middlepart (ca. 138 m. in thickness) of the Chihsia formation. The specimens are more or less     

SOME TREMADOCIAN OSTRACODS FROM TAITZEHO VALLEY,LIAOTUNG

IntroductionThe ostracods dealt with in the present paper were found in the Taitzehovalley in 1950 by Messrs.Y.Wang,Y.H.Lu,K.C.Yang,A.T.Mu,andJ.C.Sheng of the Institute of Palaeontology,Academia Sinica,and Messrs.S.W.Tang,C.C.Chiang and C.L.Chow of the Geological Survey ofN.E.China.The specimens were derived from the beds consisting of theyellowish green shales and thin bedded limestones at the following localitiesof Penchi district:1.Wee-Ning-Ying,east of Chien-Tun,2.Tou-Fang-Kou,west of Ying-Tze-Tun,3.Ho-Tee-Kou,4.Tien-Shih-Fu.between Sin-Ta-Pu     

TAXONOMY OF QUATERNARY DEEP-SEA OSTRACODS FROM THE WESTERN NORTH ATLANTIC OCEAN

Abstract:  Late Quaternary sediments from Ocean Drilling Program (ODP) Hole 1055B, Carolina Slope, western North Atlantic (32°47.041' N, 76°17.179' W; 1798 m water depth) were examined for deep-sea ostracod taxonomy. A total of 13 933 specimens were picked from 207 samples and c . 120 species were identified. Among them, 87 species were included and illustrated in this paper. Twenty-eight new species are described. The new species are: Ambocythere sturgio , Argilloecia abba , Argilloecia caju , Argilloecia keigwini , Argilloecia robinwhatleyi , Aversovalva carolinensis , Bythoceratina willemvandenboldi , Bythocythere eugeneschornikovi , Chejudocythere tenuis , Cytheropteron aielloi , Cytheropteron demenocali , Cytheropteron didieae , Cytheropteron richarddinglei , Cytheropteron fugu , Cytheropteron guerneti , Cytheropteron richardbensoni , Eucytherura hazeli , Eucytherura mayressi , Eucytherura namericana , Eucytherura spinicorona , Posacythere hunti , Paracytherois bondi , Pedicythere atroposopetasi , Pedicythere kennettopetasi , Pedicythere klothopetasi , Pedicythere lachesisopetasi , Ruggieriella mcmanusi and Xestoleberis oppoae . Taxonomic revisions of several common species were made to reduce taxonomic uncertainty in the literature. This study provides a robust taxonomic baseline for application to palaeoceanographical reconstruction and biodiversity analyses in the deep and intermediate-depth environments of the North Atlantic Ocean.     

广西西部二叠纪生物礁中的海绵、水螅动物化石

广西西部田林,凌云、凤山地区二叠纪生物礁的造礁生物－海绵、水螅化石保存完美。文中描述串管海绵7属：Stylothalamia,Lichuanospongia,Tebagathalamia,Imbricatocoelia,Intrasporeocoelia,Rhabdactinia,Lingyunocoelis;纤维海绵3属：Peronidella,Intratubospongia,Cavusonella;水螅1属Radiotrabeculopora以及海托盘类Calathium,其中Lingyunocoelia spherica为新属新种,Lichuanospongia guangxiensis为新种,其它均为中国南方二叠纪生物礁内常见分子。Senowbari-Daryan(1990)提出以Discosiphonella来代替Cystauletes,Ascosymplegma,Lichunospongia3属,但Lichuanospongia的房室形状和中央腔缺失横板（泡沫板）显著不同于Discosiphonella,因此文中仍把Lichuanospongia视作独立属,Lingyuncoelia gen.nov。与Sollasia,Girtyocoelia相似,但房室外壁缺乏任何种类的穿孔,因此明显不同于后两属,作者仍把Radiotrabeculopora视为螅纲内的一属,而没有归于纤维海绵目,因为它最明显的特征是发育分布较规则的放射状支柱（不能视为骨纤构造）,且那些纵向分布的出水管实际上应视为支柱之间的沟道。     

黔桂皖二叠纪末期硅泥质岩相地层中的介形类

对广西柳桥剖面、贵州晒瓦剖面和安徽平顶山西剖面晚二叠世末期硅泥质岩相地层中产出的介形类化石进行了系统分类学研究,共鉴定介形类化石30属86种,其中包括1个新属Denticupachydomella Yuan gen.nov.和2个新种Pseudobythocypris guiqianensis Yuan sp.nov.和Denticupachydomella spinosa Yuan sp.nov..该动物群主要由薄壳和个体较小的介形类组成,呈现出以古生代分子为主,同时含有少量典型中生代先驱分子(如:Abrobairdia,Lobobairdia)的混合动物群面貌.通过这些剖面之间的对比以及与前人研究资料对比,发现各剖面产出的介形类动物群具有强烈的地方性,三个剖面之间无相同分子,亦仅有20种曾报道于欧洲和东南亚等地区晚石炭世-晚二叠世地层.