2008040137辽 西 北 票 中 侏 罗 世 髫 髻 山 组 发 现 雌 球 果 新 种Araucaria beipoiaoensis sp.nov. 及 其 演 化 意 义= A New Female Cone,Araucaria beipoiaoensissp.nov.from the Middle Jurassic TiaojishanFormation,Beipiao,Western Liaoning,China andIts Evolutionary Significance. ( 英 文 ). ZhengShaolin; Zhang Lidong; Zhang Wu; Ynag Yajun.Acta Geologica Sinica, 2008, 82(2): 266-282A new species of Araucaria,Araucaria beipiaoensissp.nov.,collected from the Middle JurassicTiaojishan Formation,southern hill of Shebudaivillage,near Beipiao city,western Liaoning isbased on a permineralized female cone,which isovate to elliptical in shape,about 11 cm×7cm×4.5 cm in size.The cone bears rhomboidbracts that are spirally attached,texturethicker,with wings on both sides,with a detachedlamina-like apex at the tip.In inner structure theovuliferous scales are thicker and fused withbracts...被 子 植 物2008040138气 候 和 玄 参 科 Nemesia 属 一 年 生 / 多 年 生 生 活史 的 演 化 = Climate and the evolution of annual/perenniallife-histories in Nemesia (Scrophulariaceae).( 英 文 ). Datson P M; Murray B G;Steiner K E. Plant Systematics and Evolution,2008, 270(1-2): 39-57The Cape Floristic Region and the SucculentKaroo in southwestern Africa are both noted fortheir plant species richness and high levels ofendemism. The southwestern tip of Africa is oneof the world's five Mediterranean-type climateregions. The biodiversity in the Cape FloristicRegion and Succulent Karoo is thought to be atleast partly due to changes to the climate of theseregions that have occurred since the middleMiocene. Annual species are usually a significantproportion of local flora in Mediterraneantypeclimate regions. Previous studies of speciesradiations in the Cape Floristic Region haveconcentrated on genera that predominantly containperennial species. Nemesia (Scrophulariaceae)comprises c. 65 species of annual andperennial herbs and sub-shrubs that are native tosouthern and tropical Africa. Annuals make up asignificant proportion (~75%) of Nemesia species.We have reconstructed a phylogeny of 23Nemesia species using nucleotide sequences ofthe ITS, ETS and trnL-spacer regions. Specieswere grouped into five clades, two composed ofannual species, one that contained two annualand one perennial species, one that containedone annual and two perennial species, and onethat was predominantly composed of perennialspecies. Phylogenetic dating of the ITS + ETSbased phylogenetic tree using penalised likelihoodsuggested the genus evolved during theMiocene, and that the majority of extant Nemesiaspecies studied radiated during the Pliocene.Ancestral state reconstruction supports at leastthree separate origins of the annual habit fromplants with a perennial life history. One origincan be traced to the late Miocene while the othertwo transitions occurred more recently duringthe Pliocene. The transition from perennial toannual life-histories in Nemesia may have been aresponse to climate change.2008040139波 兰 经 选 择 的 更 新 世 化 石 材 料 证 明Oenanthe(subgenus Phellandrium) 花 粉 和 分果 爿 的 微 演 化 趋 势 = Microevolutionary trendsin fossil Oenanthe pollen and mericarps (subgenusPhellandrium) evidenced by material fromselected Pleistocene sites in Poland. ( 英 文 ).Bińka K; Stachowicz-Rybka R; Winter H;Nitychoruk J. Review of Palaeobotany and Palynology,2007, 145(1-2): 25-34Mericarps and pollen grains collected in thePleistocene lacustrine deposits in Poland wereanalyzed. Well-developed mericarps, resemblingrecent fruits of water dropwort Oenanthe (Phellandriumsubgenus), are found since the Eemian.Mericarps found in the Pliocene and in the AugustovianInterglacial (= Bavelian Complex orCromerian I), in the Mazovian Interglacial(= Holsteinian interglacial) and in one of theinterstadials after this interglacial are a distinctmorphological type. They differ from recentmericarps of Oenanthe aquatica in shape andsize. As late as the Vistulian, pollen grains aredecidedly smaller and in parts with different microsculpturethan recent reference material ofpollen of O. aquatica. Probably, changes ofvegetation in the late Pleistocene and in theHolocene could have induced changes in thecomposition of the pollinator assemblages, andas a consequence increase in size of pollen.Compared to mericarp evolution, the evolutionof pollen of O. aquatica is somewhat delayed.2008040140墨 西 哥 Coahuila 晚 坎 潘 期 至 早 马 斯 特 里 赫 特期 Olmos 组 出 产 的 木 化 石 = Fossil woodsfrom the late Campanian–early MaastrichtianOlmos Formation, Coahuila, Mexico. ( 英 文 ).Estrada-Ruiz E; Martínez-Cabrera H I; Cevallos-Ferriz S R S. Review of Palaeobotany and Palynology,2007, 145(1-2): 123-133Three fossil wood types are described fromthe Olmos Formation, Coahuila, Mexico. Theanatomical characters of two of them enableidentification to Malvaceae and Fagaceae, whilethe affiliation of the third type is uncertain (Fa-42
gaceae?). The wood of the Malvaceae fossilplant is characterised by the presence of vesselrayand vessel-parenchyma pits with reducedborders, larger than the intervascular pits, scantyparatracheal parenchyma, septate fibres and storiedstructure. This wood type, Javelinoxylon,has been also found in the Maastrichtian JavelinaFormation, Texas. Aggregate and uniseriate homocellularrays, apotracheal diffuse and diffusein aggregates parenchyma, simple perforationplates, vessel-ray pits variable with reduced bordersand vasicentric tracheids relate the wood ofa second plant to Quercinium. The third woodtype, Sabinoxylon pasac Estrada-Ruiz, Martínez-Cabrera et Cevallos-Ferriz, is very similar tosome species of Quercinium; however, the presenceof heterocellular rays and the almost exclusivepresence of scalariform perforation platesmake unlikely its relationship with this genus.Since observation of vessel parenchyma andvessel ray pits was not possible, its inclusion inFagaceae cannot be confirmed. Nevertheless, S.pasac and Quercinium centenoae Estrada-Ruiz,Martínez-Cabrera et Cevallos-Ferriz representthe earliest record of fagaceous plants in Mexico,while the presence of Javelinoxylon weberiEstrada-Ruiz, Martínez-Cabrera et Cevallos-Ferriz extends the geographic distribution of thegenus in North America.2008040141马 斯 特 里 赫 特 型 地 区 ( 马 斯 特 里 赫 特 阶 , 丹宁 阶 , 比 利 时 东 北 部 , 荷 兰 东 南 部 ) 的 海 草叶 化 石 = Seagrass foliage from the Maastrichtiantype area (Maastrichtian, Danian, NEBelgium, SE Netherlands). ( 英 文 ). van der HamR W J M; van Konijnenburg-van Cittert J H A;Indeherberge L. Review of Palaeobotany andPalynology, 2007, 144(3-4): 301-321Seagrasses are the only angiosperms that haveinvaded the marine environment. Fossil seagrassesare rare and received only little attentionto date. However, among the scarce plant fossilsin the marine deposits of the Maastrichtian typearea, remains of seagrasses are relatively common.The present paper provides a detailed descriptionof the morphology and anatomy of theleaves. Maastrichtian and Danian material isconsidered here as a single species: Thalassotaeniadebeyi gen. nov., sp. nov. Campanian materialis assigned to Zosterites, but this is notnecessarily a seagrass.Thalassotaenia includesthe oldest anatomically preserved material ofseagrass leaves. Comparison with extant seagrassesshows that there is not an easy matchwith any of the extant genera or families. Amphibolisand Thalassodendron (Cymodoceaceae)and Posidonia (Posidoniaceae) show the greatestresemblance. Possibly, Thalassotaenia representsthe leaves of an ancestor of the Cymodoceaceae–Posidoniaceae(–Ruppiaceae) cladefound in several phylogenetic analyses. BecauseThalassotaenia also shows some features notfound in extant seagrasses, it might also representan extinct clade of seagrasses.2008040142阿 根 廷 卡 塔 玛 卡 省 下 上 新 统 Andalhuala 组 古植 物 群 ( 豆 科 和 漆 树 科 ) = Paleoflora (Fabaceaeand Anacardiaceae) from the AndalhualaFormation (Lower Pliocene), Catamarca Province,Argentina. ( 法 文 ). Anzotegui L M; Horn Y;Herbst R. Ameghiniana, 2007, 44(3): 525-535A leaf impression flora from the Pie delMedano locality, (on national route 40, km 914-915) in Catamarca Province, is described. Itcomes from the Andalhuala Formation, which atthat locality was dated as 5.22 +/- 0.9 W, indicatinga Lower Pliocene age. The flora is composedof Fabaceae (Prosopis sp. a, Eriosemapliocenica Anzotegui and Horn sp. nov. andMacroptilium sp.) and Anacardiaceae (Lithrea sp.and Schinus aff. terebinthifolia Raddi). The associationindicates a warm climate, xerophytevegetation and riparian vegetation along riverbanks.2008040143北 美 洲 西 部 晚 古 新 世 茶 茱 萸 科 Iodeae 族 果 实化 石 = Fruits of Icacinaceae (Tribe Iodeae) fromthe Late Paleocene of western North America.( 英 文 ). Pigg K B; Manchester S R; DeVore M L.American Journal of Botany, 2008, 95(7): 824-832 4 图 版 .The Icacinaceae occur pantropically today,but are well represented by fossil fruits of thewarm Early Middle Eocene, when tropical plantsthat currently occupy low latitudes were morewidely distributed in higher latitudes. Membersof this family are first known in the Late Cretaceous;however, fossil fruits of tribe Iodeae arequite rare before the Eocene. In this paper wedescribe the first formally recognized Late Paleoceneicacinaceous taxa from western NorthAmerica. We name two new species of Icacinicaryabased on anatomically preserved fruitsand establish a new genus, Icacinicaryites, forimpressions with a strong similarity to Icacinicaryathat lack anatomical preservation.These new records from the Almont/BeicegelCreek flora in North Dakota and several localitiesin Wyoming, Colorado, and Montana complementrecords known from the Early Eoceneof England and document an increased diversityof Iodeae and related forms in the Paleogene ofwestern North America.古 无 脊 椎 动 物 学43
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corded in the Colli Berici (type lo
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most complete OAE 2 sections. While
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oceanic plate stratigraphy from gra
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A series of layers rich in organic
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lowermost Danian planktonic foramin
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characters shows that only one geno
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able for regional palaco-environmen
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margin of the southwest Caribbean.
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Brachyelasma, Amplexobrachyelasma,
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litic biozones lower than their FAD
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The middle Permian Cryptospirifer f
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石 科 = Ammonoid faunas from the
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Buchiid bivalves are geographically
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velopment of both the sedimentary a
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China. ( 英 文 ). Huang Diying; N
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德 国 南 部 上 侏 罗 统 (Ox
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shelf basin off the northern coast
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like base referred to Primocandelab
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鱼 类2008040413大 西 洋 鳕
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long as the humerus plus radius, ve
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members in both size and abundance
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ple's Republic of China. ( 英 文
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K-P transition in Brazil. ( 英 文
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wide tooth crowns, a sub-rectangula
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2008040459罗 马 尼 亚 特 兰
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logical descriptions of all availab
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东 副 特 提 斯 晚 萨 马 期
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S; Vaiani S C. Rivista Italiana di
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adiocarbon dating the arrival of th
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able problems, particularly differe
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done with glyphs on paper. In this
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obtained through extensive field-ba
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noli G; Maletz J; Stouge S. Canadia
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法 国 蒙 塔 格 尼 努 尔 中
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presence of well-rounded, coarse-sa
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缅 甸 北 部 Hukawng 峡 谷 琥
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graphy and Geological Correlation,
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plex,northwestern Iran. ( 英 文 )
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松 辽 盆 地 晚 白 垩 世 青
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ous nannoplankton) points of view.O
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the"Yanshan Movement".During the Mi
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geochemical approach discussed in t
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sediments from the northern shelf o
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意 大 利 北 亚 平 宁 Lamone
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nano record further into the early
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lankovitch-scale frequency. Analyse