苏皖南部孤峰组放射虫动物群

南京天宝山、安徽巢湖平顶山、泾县晏公堂和南陵丫山孤峰组中含有较丰富的放射虫化石,包括７属１６种（未定种）,分属于６个科,可以分成三个化石组合带,即下部的Ｐｓｅｕｄｏａｌｂａｉｌｌｅｌｌａｆｕｓｉｆｏｒｍｉｓ－Ｐｓ．ｌｏｎｇｔａｎｅｎｓｉｓ带,中部的Ｆｏｌｌｉｃｕｃｕｌｌｕｓｍｏｎａｃａｎｔｈｕｓ带和上部的Ｒｕｚｈｅｎｃｅｖｉｓｐｏｎｇｕｓｕｒａｌｉｃｕｓ－Ｆｏ．ｓｃｈｏｌａｓｔｉｃｕｓ带。这三个带分别可以同广西钦州地区的Ｐｓ．ｇｌｏｂｏｓａ带,Ｆｏ．ｍｏｎａｃａｎｔｈｕｓ带和Ｆｏ．ｓｃｈｏｌａｓｔｉｃｕｓ－Ｆｏ．ｖｅｎｔｒｉｃｏｓｕｓ带对比。根据孤峰组下伏地层栖霞组灰岩中所含类Ｐａｒａｆｕｓｕｌｉｎａｍｕｌｔｉｓｅｐｔａｔａ带和上覆地层堰桥组或武穴组灰岩中所含类Ｍｅｔａｄｏｌｉｏｌｉｎａ动物群证实,孤峰组与华南地区茅口组下部类Ｎｅｏｓｃｈｗａｇｅｒｉｎａ带大体相当。最近的古地磁和古生物资料证明,在华北板块与扬子板块之间,二叠纪时存在一个宽阔的海洋,孤峰组硅质岩中的这些放射虫动物群就是由这个洋中发育的上升洋流带入扬子板块断陷盆地中沉积的。     

云南叉科五新种(目:亚目)

本文描述云南省叉科（Ｐｓｅｕｄｏｃａｅｃｉｌｉｉｄａｅ）五新种：其中劳属ＬｏｂｏｃａｅｃｉｌｉｕｓＬｅｅｅｔＴｈｏｒｎｔｏｎ１种;四裂劳Ｌ．ｑｕａｄｒｉｐａｒｔｉｔｕｓｓｐ．ｎｏｖ,蛇属Ｏｐｈｉｄｏｄｐｅｏｍａ　Ｅｎｄｅｒｌｅｉｎ１种;波纹蛇Ｏ．Ｆｌｕｃｔｏｓａ　ｓｐ．ｎｏｖ,异属ＨｅｔｅｒｏｃａｅｃｉｌｉｕｓＬｅｅａｎｄＴｈｏｒｎｔｏｎ３种;八斑异Ｈ．ｏｃｔｏｍａｃｕｌａｔｕｓｓｐ．ｎｏｖ,景洪异Ｈ．Ｊｉｎｇｈｏｎｇｉｃｕｓ　ｓｐ．ｎｏｖ,乳突异Ｈ．ｐａｐｉｌｌａｔｕｓｓｐ．ｎｏｖ．。     

中国粉蚧科一新属一新种（同翅目：蚧亚目）

记述我国粉蚧科１新属：结粉蚧属Ｓｉｎｏｃｏｃｃｕｓ,ｇｅｎ．ｎｏｖ．及其模式种：采自天津南开大学校园榆树Ｕｌｍｕｓ ｐｕｍｉｌａ Ｌ．枝干树皮裂缝内的榆华粉蚧Ｓｉｎｏｃｏｃｃｕｓ ｕｌｍｉ,ｓｐ．ｎｏｖ．。模式标本保存在南开大学生物系。     

五加属学名考证及其一些新组合

本文考证了五加属学名,支持废弃不合法名称ＡｃａｎｔｈｏｐａｎａｘＭｉｑ．,强调应用合法名称ＥｌｅｕｔｈｅｒｏｃｏｃｃｕｓＭａｘｉｍ,在此基础上,将Ａｃａｎｔｌｈｏｐａｎａｘ属名下２种及１变种并入Ｅｌｅｕｔｈｅｒｏｃｏｃｃｕｓ属名,并对Ｅｌｅｕｔｈｅｒｏｃｏｃｃｕｓ属的４个异名作了订正。     

东濮地区奥陶纪牙形石

本文记叙了东濮地区井下奥陶纪牙形石１６属３２种（１新种、３未定种、４未定属种）,识别出５个牙形石带,１个未建带,自下而上为１．Ｓｃｏｌｏｐｏｄｕｓｆｌｅｘｉｌｉｓ带;２．Ｔａｎｇｓｈａｎｏｄｕｓｔａｎｇｓｈａｎｅｎｓｉｓ带;３．未建带;４．Ｐｌｅｃｔｏｄｉｎａｏｎｙｃｈｏｄｏｎｔａ带;５．Ａｕｒｉｌｏｂｏｄｕｓｓｅｒｒａｔｕｓ带;６．Ｍｉｃｒｏｃｏｅｌｏｄｕｓａｓｙｍｍｅｔｒｉｃｕｓ－Ｂｅｌｏｄｉｎａｃｏｍｐｒｅｓｓａ带。     

中国茸卷象属研究（鞘翅目：卷象科）

本文共记述中国茸卷象属Ｅｕｓｃｅｌｏｐｈｉｌｕｓ Ｖｏｓｓ７种,其中包括２新种：皱胸茸卷象Ｅｕｓｃｅｌｏｐｈｉｌｕｓ ｒｕｇｕｌｏｓｕｓ ｓｐ．ｎｏｖ．、齿腿茸卷象Ｅｕｓｃｅｌｏｐｈｉｌｕｓ ｄｅｎｔｉｃｕｌａｔｕｓ ｓｐ．ｎｏｖ．、１个中国新纪录种：缅甸茸卷象Ｅｕｓｃｅｌｏｐｈｉｌｕｓ ｂｕｒｍａｎｕｓ Ｍａｒｓｈａｌｌ,并将亚种Ｅｕｓｃｅｌｏｐｈｉｌｕｓ ｇｉｂｂｉｃｏｌｌｉｓ ｄｉｍｉｄａｔ     

地涌金莲化学成分的研究

从地涌金莲（Ｍｕｓｅｌｌａ ｌａｓｉｏｃａｒｐａ（Ｆｒａｎｃｈ．）Ｃ．Ｙ．Ｗｕ．）新鲜植物中分离得到了５种化合物,经理化常数和ＩＲ,ＥＩ－ＭＷ、＾１Ｈ ＮＭＲ,＾１５ＣＮＭＲ波谱数据分析,分别鉴定为,正二十四烷（ｔｅｔｒａｃｏｓａｎｅ,１）,β－谷甾醇（β－ｓｉｔｏｓｔｅｒｏｌ,２）,硬脂酸（ｓｔｅｒａｒｉｅ ａｃｉｄ,３）２,４－二羟基苯甲酸（２,４－ｄｉｔｈｙｄｒｏｘｙ ｂｅｎｚｏｌｅ ａｃｉ     

塔里木西部与东北部奥陶系的牙形刺及其意义

采自塔里木西部和东北部４个主要剖面的牙形刺共有５８属１０８种。在塔里木西部,奥陶系的牙形刺由下而上可分为Ｍｏｎｏｃｏｓｔａｄｕｓ ｓｅｖｉｅｒｅｎｓｉｓ,Ｃｈｏｓｏｎｏｄｉｎａ ｈｅｒｆｕｒｔｈｉ,Ｇｌｙｐｔｏｃｏｎｕｓ ｑｕａｄｒａｐｌｉｃａｔｕｓ,Ｐａｒｏｉｓｔｏｄｕｓ ｐｒｏｔｅｕｓ,Ｓｃｏｌｏｐｏｄｕｓ？ｔａｒｉｍｅｎｓｉｓ,Ｅｏｐｌａｃｏｇｎａｔｈｕｓ ｃｒａｓｓｕｓ,Ｅ．ｓｕｅｉｃｕｓ     

中国黑粉蚧属及其近似属种类记述(半翅目:蚧总科:粉蚧科)

研究和整理了我国黑粉蚧属Ａｔｒｏｃｏｃｃｕｓ及其近似属的种类,计有５属１２种,其中包括２新种;鹤虱奥粉蚧Ａｌｌｏｃｏｃｃｕｓ ｌｅｐｐｕｌｕｓ Ｗｕ,ｓｐ．ｎｏｖ和山西配粉蚧Ａｌｌｏｔｒｉｏｎｙｍｕｓ ｓｈａｎｘｉｅｎｓｉｓ Ｗｕ,ｓｐ．ｎｏｖ．,和个中国新纪录种,细长黑粉蚧Ａｔｒｏｃｏｃｃｕｓ ｃｒａｃｅｎｓ Ｗｉｌｌｉａｍｓ。模式标本保存在山西农业大学蚧虫研究中心。     

二叠纪放射虫Follicucullus bipartitus－F．charveti组合带的发现及其地质意义

二叠纪丑中虫科放射虫中有一类顶锥部分向腹边弯曲的放射虫,Ｉｓｈｉｇａ称为Ｆｏｌｌｉｃｕｃｕｌｌｕｓｂｉｐａｒｔｉｔｕｓ－Ｆ．ｃｈａｒｖｅｔｉ组合带,由于其形状奇特,层位稳定,已成为二叠纪较好的标准带化石,并与类Ｌｅｐｉｄｏｌｉｎａｋｕｍａｅｎｓｉｓ带对比。目前这类化石仅在东南亚地区的西南日本、菲律宾巴拉望地区和中国广西钦州地区发现表明,这些地区的放射虫当时很可能是在同一个洋盆中沉积的,只是由于它们各自的沉积历史不一样,以及后来的板块活动,造成了原始块体的离散、飘移,形成目前这种分布格局。这个放射虫动物群包括６科１１属２１种（比较种、未定种）,其中有新种１个。这个动物群的时代要早于晚二叠世。     

Mesozoic Radiolaria of Bosnia and Serbia: New data

Jurassic and Cretaceous radiolarian faunas were discovered in bedded chert of the Dinaric and Vardar tectonic zones of Bosnia and Herzegovina. Only Triassic radiolarians have previously been described in Bosnia and Herzegovina, while the finds of Bajocian, Bathonian-Callovian, Oxfordian-Kimmeridgian, Tithonian-Berriasian, and Campanian are new. Additional localities of Triassic and Jurassic radiolarians were investigated in Serbia. By correlation with radiolarians from the previous studies within Serbia, the Late Aalenian-Bajocian and Bathonian-Callovian Serbian radiolarian beds are newly dated. The first find of Cretaceous radiolarians in Serbia is reported. The oldest Mesozoic Radiolaria-bearing formations outcropping in the Western Belt of the Vardar Zone are dated Mid-Upper Triassic. The youngest radiolarians come from the Upper Cretaceous (Campanian) of the northern part of this belt of the Vardar Zone, where they co-occur with planktonic foraminifers. The distribution of 70 radiolarian samples within sections is shown. The taxonomic composition of 39 samples is analyzed. Radiolarian species extracted from 13 samples are described and figured. The list of 72 taxa and 3 plates of Jurassic radiolarians of Bosnia and Herzegovina, 3 plates of Triassic, 1 plate of Middle Jurassic, and 1 plate of Upper Cretaceous radiolarians of Serbia are presented.     

青藏高原白垩纪双壳类生物地理

青藏高原白垩纪沉积见于６条东西向延伸的条带内。双壳类主要发育于这些条带的Ｂｅｒｒｉａｓｉａｎ,Ａｐｔｉａｎ－Ａｌｂｉａｎ,Ｃｅｎｏｍａｎｉａｎ－Ｔｕｒｏｎｉａｎ,Ｃｏｎｉａｃｉａｎ－Ｓａｎｔｏｎｉａｎ和Ｃａｍｐａｎｉａｎ－Ｍａａｓｔｒｉｃｈｔｉａｎ５个时期的地层。雅鲁藏布江缝合线为白垩纪双壳类地理分布的主要控制界线。早白垩世期间,雅鲁藏布江缝合带以南的喜马拉雅地区的双壳类Ｐｅｔｒｏｃｅｒａｍｕｓ,     

Distribution,community characteristics and classification of Thymus mongolicus steppe in China北大核心CSCD

Thymus mongolicus steppe was a vegetation formation dominated by typical dwarf semi-shrub of Lamiaceae. Based on the previous literatures and primary plot data sampled during the growing seasons from 2015 to 2017, the distribution, ecological features, community characteristics and classification of Thymus mongolicus steppe were summarized. (1) Thymus mongolicus steppe is mainly distributed on the loess hills of Xar Moron River Watershed, Bashang region in the northwest of Hebei Province, the hills surrounding the Yinshan Mountains, the east part of Erdos Plateau and the northern Loess Plateau. This formation occurrs mainly on the stony slopes or loess hills with severe soil erosion. (2) In total, 167 seed plant species belonging to 101 genera of 34 families were recorded in the 91 sample sites, and families of Compositae, Leguminosae and Gramineae played crucial roles in the species composition. Eight of these families were semi-shrub and dwarf semi-shrub species, and 112 were perennial forb species. Typical xerophytes (58 species) and Meso-xerophytes (45 species) account for more than half part of all species. Eight geographic elements were involved. East Palaearctic (70 species) and East Asia (46 species) were the two major floristic elements. (3) Based on life form and dominance of species in the community, the formation was classified into 6 association groups (Thymus mongolicus, dwarf shrubs/dwarf semi-shurbs association group; Thymus mongolicus association group; Thymus mongolicus, bunchgrasses association group; Thymus mongolicus, rhizomatous grasses association group; Thymus mongolicus, Carex association group; Thymus mongolicus, forbs association group), consisting of 28 associations. © Chinese Journal of Plant Ecology.     

朝鲜南部的Pseudogl yptagnostus(三叶虫)并论朝鲜寒武纪斜坡相的意义

朝鲜南部Ｍａｃｈａｒｉ组Ｏｌｅｎｏｉｄｅｓ带的Ａｇｎｏｓｔｕｓ（Ｐｔｙｃｈａｇｎｏｓｔｕｓ？）ｏｒｉｅｎｔａｌｉｓ Ｋｏｂａｙａｓｂｈｉ一种应归于Ａｇｎｏｓ－ｔｏｔｅｓ（Ｐｓｅｕｄｏｇｌｙｐｔａｇｎｏｓｔｕｓ）Ｌｕ,１９６４一属,时代是晚寒武世长山期,不是早期中寒琥世,小林贞一的Ｏｌｅｎｏｉｄｅｓ带是中及晚寒武三叶虫混杂在一起的一个化石带。他建立的该组５个化石带也有问题。Ｃｏｒｅｏｌｅｎｕｓ,Ｃｈ     

Phylogeography of the fiscal shrike (Lanius collaris): a novel pattern of genetic structure across the arid zones and savannas of Africa

Aim Savanna occupies a substantial part of Africa, being distributed around the two major tropical rain forest blocks in what is referred to as the Savanna Belt. Our current understanding of the genetic structure within species distributed across the Savanna Belt is primarily derived from mammalian taxa, studies of which have revealed a suture zone or transition between northern and east/southern Africa clades in south‐western Kenya and north‐western Tanzania. We conduct a phylogeographic study of the fiscal shrike (Lanius collaris), a polytypic species distributed across the Savanna Belt of Africa and for which morphological and vocal data are in agreement with the suture zone recovered for mammalian taxa, to test the hypothesis of a spatially congruent genetic break across several taxa, including birds. Location Africa, south of the Sahara. Methods We analysed DNA sequences recovered from four loci (one mitochondrial, two autosomal and one Z‐linked) in 66 individuals, representing all recognized subspecies, as well as putatively closely related species. We make use of a combination of tree‐building and population genetic methods to investigate the phylogeographic structure of the fiscal shrike across Africa. Results The fiscal shrike consists of two primary lineages with a strong geographic component: a northern group distributed from southern Tanzania to Senegal, and a southern group distributed from Botswana/Zambia to South Africa with isolated populations in Tanzania and northern Malawi. Unexpectedly, Souza’s shrike (L. souzae) was nested within L. collaris, as the sister group of the southern group. The positions of Mackinnon’s shrike (L. mackinnoni) and that of the São Tomé shrike (L. newtoni) were variable, being either nested within the fiscal shrike or sister to the L. collaris–L. souzae clade. Our divergence time analyses suggest that the Lanius collaris species complex started to diversify around 2.2 Ma. Main conclusions Our study reveals a distinct biogeographic pattern for a savanna distributed species in Africa, with the transition between the two primary genetic lineages occurring at a latitude of c. 15–16° S, 10° S further south than shown elsewhere for several mammalian species.     

A biogeographically mixed, Middle Permian brachiopod fauna from the Baoshan Block, western Yunnan, China

A small brachiopod fauna is described from the carbonate rocks of the basal Shazipo Formation of the Baoshan Block, western Yunnan, south-west China, including significant new ventral and dorsal internal morphological features of Cryptospirifer omeishanensis Huang. This fauna is regarded as Wordian (Middle Guadalupian, Middle Permian) because of the presence of Cryptospirifer omeishanensis Huang and associated fusulinids ( Neoschwagerina craticulifera Zone). Palaeobiogeographically, the brachiopod fauna is of considerable interest because of its admixed nature characterized by typical warm-water Cathaysian elements intermingled with temperate Peri-Gondwanan taxa. This in turn is interpreted to indicate that the Baoshan Block may have been situated in an intermediate palaeogeographical position between Gondwanaland to the south and Cathaysia to the north during the Mid Permian and, as such, it probably furnished an important 'stepping stone' for the dispersal of Mid Permian eastern Tethyan marine invertebrate taxa (e.g. Cryptospirifer ) to the western Tethys.     

Resolving Terreneuvian stratigraphy in subtidal–intertidal carbonates: palaeontological and chemostratigraphical evidence from the Turukhansk Uplift,Siberian Platform

Both diverse assemblages of small skeletal fossils and a representative chemostratigraphical record make the Siberian Platform widely regarded as one of the key regions for the reconstruction of global biotic and abiotic events in the late Ediacaran and early Cambrian. However, the wide distribution of intertidal–subtidal facies in the Ediacaran–Cambrian transitional strata of the central and southwestern Siberian Platform (Turukhansk–Irkutsk–Olekma facies region) produces a dramatic depletion of the palaeontological record and considerably limits their age‐calibration and long‐distance correlation. We report new lithological, palaeontological and carbonate carbon‐isotope data for the Ediacaran–Cambrian sections of the Turukhansk Uplift (northwestern Siberian Platform, western facies region). These data provide a robust framework for the chemostratigraphical correlation of the western facies region with sections of the transitional and eastern regions of the Siberian Platform and further confirms a depositional hiatus at the base of the Tommotian Stage in the stratotype section (Aldan River, SE Siberia). The carbon‐isotope curve from the Turukhansk Uplift sections correlates positively with the most chemostratigraphically representative Ediacaran–Cambrian sections (Siberia, Morocco, South China). It records major carbon‐isotope oscillations globally recognized in the lower Cambrian, enabling localization of the Fortunian and Cambrian Stage 2 boundaries in the Platonovskaya Formation. Although there is extreme paucity and poor preservation of the small skeletal fossils in the western facies region, we report individual Barskovia, Blastulospongia and chancelloriid sclerites from the Platonovskaya Formation. A combination of palaeontological and chemostratigraphical data suggests the base of P. antiqua Assemblage Zone is located in the middle Platonovskaya Formation. The earliest spiral gastropods probably occurred at ~541 Ma, as demonstrated by the discovery of a specimen of Barskovia near the base of the large negative excursion in the lower Platonovskaya Formation, correlated with the BACE negative carbon‐isotope peak in the sections of the Yangtze Platform.     

Distribution,community characteristics and classification of Thymus mongolicus steppe in China

百里香(Thymus mongolicus)草原是以唇形科小半灌木百里香为建群种的草原类型。该文以编写《中国植被志》为契机, 结合2015-2017年生长季野外调查数据和文献资料, 对中国百里香草原的分布、生态特征、群落特征和分类等进行了总结。结果表明: (1)百里香草原主要分布于辽河上游西拉木伦河流域的黄土丘陵、河北西北部坝上高原、阴山山脉两翼低山丘陵、鄂尔多斯高原东部和黄土高原北部, 常分布在水蚀风蚀强烈的黄土丘陵和砾石质化基质的坡地。(2)根据91个样地记录统计, 百里香草原组成物种较丰富, 有种子植物167种, 隶属于34科101属, 以菊科、豆科和禾本科为主; 其中有8种半灌木和小半灌木, 112种多年生杂类草; 水分生态类型以典型旱生植物(58种)和中旱生植物(45种)为主; 区系地理成分以东古北极成分(70种)和东亚成分(46种)为主。(3)根据生活型和优势度, 百里香草原可以划分为百里香、半灌木/小半灌木群丛组, 百里香群丛组, 百里香、丛生禾草群丛组, 百里香、根茎禾草群丛组, 百里香、薹草群丛组, 百里香、杂类草群丛组, 共计6个群丛组28个群丛。     

A new threespine stickleback,Gasterosteus nipponicus sp. nov. (Teleostei: Gasterosteidae), from the Japan Sea region

Gasterosteus nipponicus sp. nov. is described from the holotype, 35 paratypes, and 60 additional specimens. The species differs from congeners in the following combination of characters: lateral plates complete, abruptly reducing in size above the anus, depth of lateral plate above the anus < 60 % that of the deepest plate; caudal keels thin, membranous. The new species is distributed in coastal Japan facing the Sea of Japan from Kyushu to Hokkaido Islands, along the Pacific coast of northern Japan from the Chiba Prefecture to Hokkaido, along the Sea of Okhotsk of Hokkaido, west to the southern and eastern coasts of Korean Peninsula, the Maritime Territory and north to Sakhalin Island, Russia.