中国二叠纪煤核中具解剖构造的鳞木类植物:似封印叶属(英文)

报道了产于中国二叠纪煤核中的 3种具解剖构造的鳞木类叶 ,它们都具双木质部束 ,与似封印叶属 (Sigil lariopsisScott)特征一致。与该属已有种进行了对比 ,确认它们为 3个新种 :产于山西太原西山煤田太原组上部 7号煤层 (早二叠世早期 )煤核中的山西似封印叶 (Sigillariopsisshanxiensissp .nov .)和太原似封印叶 (S .taiyuanensissp .nov .)以及产于贵州水城矿区汪家寨组 1号煤层 (晚二叠世晚期 )煤核中的贵州似封印叶 (Sigillariopsisguizhouensissp .nov .)。根据煤核中共生的鳞木类植物其他器官以及欧美植物区鳞木类植物的研究资料推断 ,它们可能属于封印木属 (SigillariaBrongniart)的叶。在国外 (主要是欧美植物区 ) ,封印木属植物主要分布于石炭纪 ,见于二叠纪的封印木很少。华夏植物区的封印木属过去很少发现 ,其叶和生殖器官均未报道过。本文是首次报道华夏植物区具解剖构造的封印木属的叶 ,它们的发现不仅丰富了华夏植物区封印木属植物的内容 ,而且对于研究封印木属的演化以及华夏植物区与欧美植物区鳞木类植物之间的关系也具有重要的意义。     

中国二叠纪煤核中具解剖构造的鳞木类植物:似封印叶属

报道了产于中国二叠纪煤核中的3种具解剖构造的鳞木类叶,它们都具双木质部束,与似封印叶属(Sigillariopsis Scott)特征一致.与该属已有种进行了对比,确认它们为3个新种:产于山西太原西山煤田太原组上部7号煤层(早二叠世早期)煤核中的山西似封印叶(Sigillariopsis shanxiensis sp. nov.)和太原似封印叶(S. taiyuanensis sp.nov.)以及产于贵州水城矿区汪家寨组1号煤层(晚二叠世晚期)煤核中的贵州似封印叶(Sigillariopsis guizhouensis sp.nov.).根据煤核中共生的鳞木类植物其他器官以及欧美植物区鳞木类植物的研究资料推断,它们可能属于封印木属(Sigillaria Brongniart)的叶.在国外(主要是欧美植物区),封印木属植物主要分布于石炭纪,见于二叠纪的封印木很少.华夏植物区的封印木属过去很少发现,其叶和生殖器官均未报道过.本文是首次报道华夏植物区具解剖构造的封印木属的叶,它们的发现不仅丰富了华夏植物区封印木属植物的内容,而且对于研究封印木属的演化以及华夏植物区与欧美植物区鳞木类植物之间的关系也具有重要的意义.     

吐鲁番-哈密盆地早二叠世晚期植物群

首次记述了吐鲁番－哈密盆地的早二叠世晚期植物１１属１３种（包括４新种和４未定种），这是一个以科达类及其相关属为主的安加拉植物群。典型的安加拉植物Ｖｏｊｎｏｖｓｋｙａ属的发现，不但在时代的判定上，而且在植物地理区划上都具重要意义。文中还对这一植物群的特征和时代问题作了简要讨论。     

中国华夏植物区二叠纪几种科达植物分散角质层及其意义

中国华夏植物区科达植物的研究历史虽然最早可上溯至1883年,但直到1991年才首次报道其角质层构造.到目前为止,中国华夏植物区总共描述了4种科达植物原位角质层和3种分散角质层.但与欧美植物区相比,有关中国华夏植物区科达植物角质层的研究工作还较薄弱.本文较详细地描述了3种产自中国华夏植物区二叠纪煤系地层中的科达植物分散角质层.其中2种采自华北亚区南缘的安徽淮南新庄孜矿山西组A1煤顶板,地质时代为早二叠世;另一种采自华南亚区的贵州水城矿区大河边矿龙潭组顶部的11号煤层,地质时代为晚二叠世早期.将这3种科达植物分散角质层与已知的欧美植物区和中国华夏植物区的种类进行了对比,认为它们都是新的类型.讨论了这3种新的科达植物分散角质层所具有的古植物学意义.     

New radiolarian genera and species from the Lower Permian of the Southern Urals and Northern Mugodzhary

Two new genera and five new species of Lower Permian radiolarians, Arcoclathrata alekseevi gen. et sp. nov., Entactinia pinrasensis sp. nov., Microporosa rozhnovi gen. et sp. nov., M. aktastensis sp. nov., and Somphoentactinia saecularis sp. nov., from the Southern Urals and Northern Mugodzhary are described. The new spherical radiolarian taxa belong to three orders: Entactiniata, Cancelliata, and Spongiata of two classes, Sphaerellaria and Spumellaria.     

中国华夏植物区二叠纪几种科达植物分散角质层及其意义

中国华夏植物区科达植物的研究历史虽然最早可上溯至1883年,但直到1991年才首次报道其角质层构造。到目前为止,中国华夏植物区总共描述了4种科达植物原位角质层和3种分散角质层。但与欧美植物区相比,有关中国华夏植物区科达植物角质层的研究工作还较薄弱。本文较详细地描述了3种产自中国华夏植物区二叠纪煤系地层中的科达植物分散角质层。其中2种采自华北亚区南缘的安徽淮南新庄孜矿山西组A1煤顶板,地质时代为早二叠世;另一种采自华南亚区的贵州水城矿区大河边矿龙潭组顶部的11号煤层,地质时代为晚二叠世早期。将这3种科达植物分散角质层与已知的欧美植物区和中国华夏植物区的种类进行了对比,认为它们都是新的类型。讨论了这3种新的科达植物分散角质层所具有的古植物学意义。     

New fossil insects (Diaphanopterodea: Martynoviidae) from the Lower Permian of the Boskovice Basin, southern Moravia

Two new genera and new species assigned to the family Martynoviidae (Diaphanopterodea), Boskovicia celtai nov. gen., nov. sp. and Moravoptera hladilovae nov. gen., nov. sp. are described and illustrated from the Lower Permian (Artinskian/Sakmarian) locality of Obora, southern Moravia (Czech Republic). Discovery of the species Martynovia insignis Tillyard, originally described from the Lower Permian of Kansas (USA), supports close relationship of both faunas across Euramerica.     

New Genera and Species of Psychodoid Flies from the Lower Cretaceous Amber Lebanon

Until now, only two Psychodoidea were known from Lebanese amber. We describe two new genera and species of Phlebotomidae ( Mesophlebotomites hennigi gen. et sp. nov., Libanophlebotomus lutfallahi gen. et sp. nov.) and four new genera with six new species of Psychodidae ( Paleopsychoda solignaci gen. et sp. nov., Paleopsychoda jacquelinae sp. nov., Protopsychoda nadiae gen. et sp. nov., Protopsychoda hammanaensis sp. nov., Libanopsychoda abillamai gen. et sp. nov., Cretapsychoda inexpectata gen. et sp. nov.) from the Lower Cretaceous amber of Hammana/Mdeirij, Lebanon. These fossils are included in a phylogenetic analysis of the subfamilies of Psychodoidea. This superfamily was probably as diverse in the Early Cretaceous as now.     

Trend of changes in species diversity of Permian radiolarians of the genus <Emphasis Type="Italic">Entactinia</Emphasis> Foreman

The trend of species diversity and spatiotemporal distribution of spherical radiolarians of the genus Entactinia Foreman, 1963 in the Permian Period is analyzed. The center of origin of Permian entactinians in the Cis-Ural Paleobasin is established in the area of the modern interfluve of the Ural River and latitudinal current of the Belaya River on the Southern Urals. It is shown that the species composition of this genus almost completely changed in certain Permian epochs. Two forefather species of each new pleiad of Early, Middle, and Late Permian are revealed: Entactinia parapycnoclada and E. tyrrelli. Two new species of the Lower Permian radiolarians from the Southern Urals and Northern Mugodzhary, E. chernykhi sp. nov. and E. subquadrata sp. nov., are described.     

New species of <Emphasis Type="Italic">Inoceramus</Emphasis>-like bivalves of the genus <Emphasis Type="Italic">Aphanaia</Emphasis> Koninck from the Lower Permian of northeast Asia

Historical development of Permian Inoceramus-like bivalves of the genus Aphanaia Koninck in northeastern Asia is briefly considered. Five new species from the Lower Permian of the western Verkhoyansk Region and Omolon Massif are described: Aphanaia waterhousei sp. nov., A. budnikovi sp. nov., A. kutygini sp. nov., A. dulgalakhensis sp. nov., and A. korkodonica sp. nov.     

河南固始早石炭世杨山组植物群

系统描述了扬山组植物18属25种,其中以石松类及种子蕨和真蕨纲为主,仅少数属楔叶纲;石松类中发现不少叶座较小,叶痕相对较大的鳞木类植物,颇似华夏植物群中的鳞木类;首次报道了我国发现的古芦木孢囊穗.据对植物群综合分析,杨山组的时代为早石炭世中晚期.     

内蒙古乌达地区早二叠世晋囊蕨属一新种

通过扫描电镜研究,建立了内蒙古中部乌达地区下二叠统山西组晋囊蕨诉一个新种Ｃｈａｎｓｉｔｈｅｃａ ｗｕｄａｅｎｓｉｓ ｓｐ ．ｏｎｖ．。新种的小心片Ｓｐｈｅｎｏｐｔｅｒｉｓ型,囊群椭圆形,由４～１０个孢子囊组成,着生一示羽片背面,位于中脉的两侧。环带横列于孢子囊的上部,完全,单排细胞,细胞数目约为１８个,这些特征表明新种属于里白科。     

A new tribe of dictyoclostid brachiopods from the Lower Permian of the Tarim Basin,north-west China

Several finely capillated brachiopod genera are re-examined based on new material obtained from the Lower Permian of the Tarim Basin, north-western China and previously published information. A new genus, Tarimoplecta, is proposed. Comparison with other related genera reveals that Liraplecta Jin and Sun and Tarimoplecta gen. nov. represent a new tribe, Liraplectini, of the Dictyoclostidinae Stehli. The stratigraphical and geographical distributions of both LiraplectaTarimoplecta indicate that they are restricted to the Sakmarian to Kungurian (Lower Permian) of the Tethyan Realm. Four species are described herein: Liraplectapaojianggouensis sp. nov., L. richthofeni (Chao), L. apsera (Wang), and Tarimoplecta tarimensis gen. et sp. nov.     

内蒙古乌达地区早二叠世晋囊蕨属一新种

Chansitheca (Sphenopteris) wudaensis sp. nov. is described based on the materials collected from the Lower Permian Shansi Formation of Wuda, Nei Mongol, China. The frond is small and at least two times pinnate. The pinnule is sphenopteroid. The sori are borne on the abaxial surface of the pinnule, arranged in two rows parallel to the midvein, elliptic,and composed of 4-10 round sporangia. The indusium is absent. The annulus is transverse and complete, and consists of about 18 thickened cells. The features of the fertile parts, sori, sporangia and annulus and the absence of indusium indicate that the new species belongs to the Gleicheniaceae.     

New Martynoviidae from the Permian of Southern France (Lodève basin) (Insecta: Palaeoptera: Diaphanopterodea)

A new genus and two new species, Salagouneura chimaira nov. gen. and nov. sp. and Phaneroneura minuta nov. sp., together with several other specimens of uncertain affinities, are herein assigned to the family Martynoviidae. This family was previously only known from the Lower Permian of Oklahoma and Kansas (USA). The new specimens have been discovered in the Salagou Formation (Permian; Hérault, France). Stratigraphical and palaeoecological implications of the occurrence of this family in the Salagou Formation are discussed. These discoveries seem correlated with similar palaeoenvironmental conditions between the Salagou Formation and the Midco Salt Lake Formation (Oklahoma).     

CHILBINIA GEN. NOV., AN ARCHAIC SEED FERN IN THE LATE TRIASSIC CHINLE FORMATION OF ARIZONA, USA

Abstract:  A seed-bearing pinnate leaf found in the Chinle Formation of Late Triassic age in Arizona appears to be an archaic seed fern that more closely resembles typical Carboniferous–Permian seed fern leaves than any younger form. The fossil, which is described here as Chilbinia lichii gen. et sp. nov., incorporates characters of several Palaeozoic taxa. These characters include pinnules that have reticulate venation resembling that in some species of Lonchopteris , cordate bases similar to those found in many species of Sphenopteris , and, except for a significant difference in size, linear ovate seeds that resemble the radially symmetrical seeds found attached to a species of Alethopteris in the Permian of China. The presence of this fossil in strata of Late Triassic age is further evidence that plant extinctions after the Permian–Triassic ecological crisis followed a stepwise pattern and apparently continued for at least 20–25 myr after the end of the Permian in western parts of the Triassic paratropical belt.     

New species of the Inoceramus-like bivalve genus Maitaia Marwick from the Permian of northeastern Asia

Historical development of Permian Inoceramus-like bivalves of the bipolar genus Maitaia Marwick in northeastern Asia is briefly considered. Five new species (Maitaia vedernikovi sp. nov., M. kusnezovi sp. nov., M. orulganica sp. nov., M. regularicostatum sp. nov., and M. tobonnoensis sp. nov.) from the Middle and Upper Permian of the Omolon Massif, northern, western, and southern Verkhoyansk Region are described.     

A new representative of <Emphasis Type="Italic">Neocalamites</Emphasis> Halle from the Upper Permian of northeastern China (Jiefangcun Formation)

A new species, Neocalamites hunchunensis sp. nov. from the Upper Permian Jiefangcun Formation of northeastern China is described. The Jiefangcun Upper Permian Flora is briefly characterized. Its taxonomic composition, age, and significance for paleophytogeographical reconstructions are discussed. The Late Permian phase in equisetophyte evolution is considered.     

A new species of Discinites (Noeggerathiales) from the Upper Permian of Weibei Coalfield, North China

A new species of Discinites is described from the Late Permian Upper Shihhotse Formation of the Weibei Coalfield, Shaanxi Province, China. D. hanchengensis sp. nov. has decurrent and disk-like sporophylls with deep-toothed apices, elliptical sporangia and rectangular epidermal cells. The spores are generally of the Calamospora type. The megaspores and microspores are 300–380 and 45–90 μm in diameter, respectively. The microspores are similar in size to those of all other species of Discinites that contain Calamospora, but the megaspores are remarkably smaller. The new species represents the first record of Discinites with Calamospora from China and from the Cathaysian flora. Finally, we summarize the associated foliages of Discinites in the Cathaysian flora and find that they are all markedly different from those found in the Euramerican flora.     

海南岛东方早二叠世双壳类动物群及其古生物地理学研究──兼评南龙杂砾岩的冰川成因说

在海南岛东方县江边地区下二叠统南龙组中发现双壳类９属１０种，其中２新种。除新种外，这些双壳类常见于华南和日本的茅口期晚期地层，其它动、植物化石的研究也得出了相同结论，本区无疑是华夏生物区系的组成部分。海南岛的琼中地体不大可能在石炭一二叠纪仍位于冈瓦纳大陆北缘或其附近，南龙杂砾岩应属裂谷成因，与冰川无关。