内蒙古西乌珠穆沁旗早二叠世阿木山组的一个牙形刺新种

在内蒙古西乌珠穆沁旗哈尔努尔山西南阿木山组剖面的一个层位中发现早二叠世牙形刺新种Neostreptognathodus costatus sp.nov.。根据牙形刺地层分布分析判断,该剖面地层是倒转的,但由于现有资料有限,地层是否连续或有缺失存疑;此剖面是否适合全部归入阿木山组,也有待进一步论证。期待能对此剖面重新详细的考察和大量采样,以便解决上述问题。     

Conodonts from the Permian Jisu Honguer (Zhesi) Formation of Inner Mongolia, China

The Jisu Honguer Formation (“Zhesi Formation”) is a North China marine carbonate unit of Permian age containing a mixed fauna of Tethyan, Boreal and endemic elements. The age of the Jisu Honguer Formation has been thought to range from Artinskian to Kazanian based on previous studies using mostly benthic macrofossils. A typical Mesogondolella aserrata conodont fauna is reported from the lower part of the upper member of the Jisu Honguer Formation in the Ulanqub District, Zhesi area, of northern China. The fauna indicates a Middle Permian (Guadalupian) age, most likely late Wordian to early Capitanian, for the strata yielding conodonts. The whole Jisu Honguer Formation could be assigned to the Wordian to early Capitanian age. The overlying Yihewusu Formation is probably of Capitanian age. There are no Wuchiapingian marine deposits in the Zhesi area. As characteristic of the open sea Guadalupian conodont faunas of the Tethys, smooth Mesogondolella dominate the fauna. The view that all Tethyan Guadalupian conodont faunas consist exclusively of serrated Mesogondolella cannot be confirmed. Three new species are described: Mesogondolella neoprolongata C. - y. Wang, Mesogondolella mandulaensis C. - y. Wang and Wardlawella jisuensis C. - y. Wang.     

New Phoenicopsis leaves (Czekanowskiales) from the Middle Jurassic Daohugou Biota,China and their roles in phytogeographic and paleoclimatic reconstruction

The Middle Jurassic Jiulongshan Formation, distributed in the Daohugou area, Ningcheng County, Inner Mongolia, China, is famous for yielding abundant, well-preserved fossil vertebrates and invertebrates. However, only a few fossil plants have been reported to date. In this paper, one new species of Czekanowskiales, Phoenicopsis (Windwardia) daohugouensis n. sp. is described based upon leaf morphology and epidermal characters. The new species represents the first record of Czekanowskiales from the Daohugou Biota. The discovery of the new species reveals the significance of the Daohugou flora as one of the deciduous forests in the temperate-warm temperate zone of Eurasia during the Middle Jurassic.     

内蒙古二叠系哲斯组的牙形刺及其时代

哲斯组是我国北方最有代表性的海相二叠纪地层,但其时代尚未得到解决。以往的研究多偏重于底栖大化石,难以解决洲际间的对比。作者对哲斯组的牙形刺进行了研究,在哲斯组上段下部发现了Mesogondolellaaserrata动物群,从其同层的其它牙形刺化石分析,产这一牙形刺化石的层位的时代应为Wordian期晚期至Capitanian期早期,而整个哲斯组的时代可能为中二叠世Wordian期至Capitanian期早期,推测义和乌苏组的时代可能为Capitanian期。哲斯地区可能不存在吴家坪阶的海相沉积。对MesogondolellaneoprolongataWang,2004,M.mandulaensisWang,2004,WardlawellajisuensisWang,2004作了重新描述,这3个种可能为地方性分子或北方区(Borealrealm)分子。     

A new ground beetle (Carabidae, Protorabinae) from the Lower Cretaceous of Inner Mongolia, China

Cretorabus rasnitsynisp. n., belonging to the extinct subfamily Protorabinae of Carabidae, was described based on a well-preserved specimen from the Lower Cretaceous Yixian Formation of Yangshuwanzi, Inner Mongolia. The diagnostic characters forCretorabus are revised, and the key to species of the genus was presented. The fossil record of Protorabinae was summarized. Sinocarabus Hong, 1982 and Obesofemoria Hong, 1982 cannot be attributed to Protorabinae.     

乌兰坝紫萼藓(紫萼藓科)成熟孢子体的发现

最近在中国内蒙古发现了乌兰坝紫萼藓(Grimmia ulaandamana J. Mu?oz, C. Feng, X.L. Bai&J. Kou)的可育植株,介绍了乌兰坝紫萼藓成熟孢子体、雌株和雄株的特征。孢子体的孢蒴长于蒴柄,蒴柄弯曲,蒴壶表面具纵褶,蒴壁中部表皮细胞厚壁,环带细胞方形或短长方形,蒴盖有喙;蒴齿具疣并在上部分叉,蒴齿在基部分开,蒴齿基部低于蒴壶口,蒴壁表皮细胞和蒴齿之间存在一层小型细胞,蒴齿骨小梁在基部1/3处强烈凸出;蒴帽基部完整。最内侧雌苞叶较茎叶大。乌兰坝紫萼藓具有重要的形态特征变异,可育植株与相似种直叶紫萼藓(G. elatior)易于区分。对乌兰坝紫萼藓进行了全面的描述并配显微图,探讨了孢子体对确定其系统发育位置的重要性。     

内蒙古沼泽蝗属一新种记述(直翅目:斑翅蝗科)

记述采自内蒙古地区斑翅蝗科昆虫1新种,即红股沼泽蝗Mecostethus rufifemoralis, sp. nov.,模式标本保存于陕西师范大学动物研究所昆虫标本室及河北大学博物馆.     

内蒙古牧草上一新害虫——沙打旺小食心虫(鳞翅目: 卷蛾科: 小卷蛾亚科)

记述内蒙古牧草沙打旺上的 1种新害虫——沙打旺小食心虫 Grapholitashadawana,sp.nov.,模式标本保存在中国科学院动物研究所标本馆。     

内蒙古哈素海发现池鹭繁殖群

正池鹭(Ardeola bacchus)在内蒙古夏季见于呼伦贝尔市、赤峰市克什克腾旗和敖汉旗、呼和浩特市哈素海、包头和鄂尔多斯市黄河沿岸、巴彦淖尔市乌梁素海,但未见繁殖记录的报道。哈素海(E 110°56'~111°01',N 40°34'~40°38')位于大青山南部土默川平原北端,在呼和浩特市区向西70km处的土默特左旗境内,是黄河改道而遗留的椭圆形牛轭湖,属于大黑河水系的外流性淡水湖泊,主要水源来自     

内蒙古乌海大石门奥陶系牙形刺和Histiodella动物群发现的意义

本文描述了内蒙古乌海大石门剖面奥陶系的牙形刺动物群:下克里摩里组主要有Histiodella kristinae,H.holodentata,H.wuhaiensis sp.nov.,Polonodus newfoundlandensis和Paroistodus horridus等,应归属于中奥陶统达瑞威尔阶(Darriwilian)之Histiodella kristinae带,并在同一剖面上与笔石Pterograptus elegans带和Didymograptus murchisoni带下部相当;下克里摩里组顶部产Histiodella kristinae,Baltoplacognathus cf.reclinatus,Periodon aculeatus和Protopanderodus rectus等,所以大石门剖面的Histiodella kristinae带顶部可能已与北欧Pygodus serra带之底部相当;乌拉力克组底部的砾状灰岩透镜体产有牙形刺Pygodus anserinus?,Protopanderodus liripipus,Yangtzeplacognathus protoramosus和Dapsilodus viruensis等,其中Pygodus anserinus?Pa分子(器官种的一组成分子)的口面瘤齿列的瘤齿比较粗糙,与典型的Pygodus anserinus稍有不同,且在牙形刺十分丰富的样品中仅有一枚此种之Pa分子,所以本文尚有疑问地把这层砾状灰岩归入Pygodus anserinus带,同时不能排除把它归入Pygodus serra带顶部Yangtzeplacognathus protoramosus亚带的可能。由于此剖面牙形刺化石与丰富的笔石共生,为牙形刺带与笔石带的精确对比提供了直接证据。Histiodella动物群在此剖面的发现,不仅具有十分重要的地层意义,而且具有明显的岩相古地理意义。本文详细描述了新种Histiodella wuhaiensis并讨论了Histiodella属5个种之区别。     

内蒙古根瘤菌的数值分类

对63株新分离的内蒙古根瘤菌与6株来自Rhizobiumleguminosarum及Sinorhizobiummililoti的参比菌株一起进行了数值分类。结果表明：所有测试菌株在67％的相似性水平上分为三个表观群,群Ⅰ包括3株Sinorhizobiummeliloti的参比菌和9株新分离的内蒙古根瘤菌;群Ⅱ包括3株RhizobiumLoguminosarum参比菌和37株新分离的内蒙古根瘤菌;群Ⅲ全部由20株新分离的内蒙古根瘤菌组成。在78％的相似     

中国灰石藓属研究新资料

中国灰石藓属长期缺乏系统的形态特征描述和种间区分特征研究,分类鉴定较为困难。该研究采用经典分类学方法,通过查阅灰石藓属内相关物种的原始文献,借阅该属在中国有记载的3个物种的相关模式标本,同时搜集和观察来自美国、加拿大、俄罗斯、瑞典、瑞士、挪威、尼泊尔的标本以及中国内蒙古、四川、新疆等地的地方标本,确认了该属物种在中国的分布,增加了直叶灰石藓在内蒙古和新疆以及灰石藓在四川的新分布记录,并提供了详细的形态描述和图版,编制了中国灰石藓属植物的分种检索表。这3个物种在植物大小、叶是否具褶皱、茎叶和枝叶是否同形等特征上具有区别。该文增补的分布信息及种间区分特征可为中国灰石藓属及棉藓科相关类群的鉴定工作提供依据。     

褪黑素对内蒙阿白山羊在非生绒季节促绒生长及绒产量的影响

用简易的外科手术在阿白山羊梳绒后的非长绒季节,给羊体颈部皮下埋植一种含褪黑素的胶囊试验,经５周后受试羊群长出了新绒,对照群则未见新绒生长。在８月下旬天然生绒季节快下到时,试验组羊绒已长至近３公分;而对照群才开始生绒,但绒长不足１分分。表明含上述激素胶囊促绒生长首次成功。翌年对上述羊群跟踪检测结果：受试羊群个体产绒量的特级（≥４５０克／头）率。提高为５０－６８．４％,与对照群（３５％）相比,提高１５     

褪黑素对中国绒山羊在非生绒期促绒生长与绒产量的影响

用简易的外科手术对阿白羊,盖县红山羊及二者杂交改良型绒山羊在梳绒后于其颈部皮下埋植一种含褪黑素的胶囊,经５周后受试羊群开始长绒,而对照群羊则未见绒生长。在９月中旬天然生绒开始时,受试群羊绒已分别长至３－５ｃｍ,,而对照群则刚开始生长至２ｃｍ。表明上述各受试群当年被成功地诱发二次生绒。     

A new middle Miocene pliopithecid from Inner Mongolia, China

In addition to the new fragments of the Omo I skeleton, renewed fieldwork in the Kibish Formation along the lower reaches of the Omo River in southwestern Ethiopia has yielded new hominin finds from the Kibish Formation. The new finds include four heavily mineralized specimens: a partial left tibia and a fragment of a distal fibular diaphysis from Awoke's Hominid Site (AHS), a parietal fragment, and a portion of a juvenile occipital bone. The AHS tibia and fibula derive from Member I and are contemporaneous with Omo I and II. The other specimens derive from Chad's Hominid Site (CHS), and derive from either Member III or IV, which constrains their age between approximately 8.6 and approximately 104ka.