scabrate–verrucate, and rugulate micromorphology.The first two types of sculpturing aremostly limited to the evergreen oaks and can beused to identify fossil evergreen oak pollen,while the last two types can also be seen in manydeciduous oaks. On the other hand, deciduousoak pollen grains have relatively uniform sculpturing,with only two types encountered:scabrate–verrucate and rugulate sculpturing.This sculpturing is mainly present in deciduousoaks, despite its occurrence in some evergreenoaks. An absolute discrimination between evergreenand deciduous oak pollen is thus impossibleand would require additional evidence in theform of macrofossils. The diagnostic criteria areapplied to a Miocene pollen assemblage fromZhejiang Province, eastern China and demonstratethe high diversity of fossil oaks in thevegetation. The fossil pollen includes three morphotaxaof deciduous origin, two morphotaxa ofevergreen habit, and three oaks whose habit isuncertain.2008040054中 国 云 南 蛛 网 花 粉 分 析 = Pollen analysis ofspider webs from Yunnan, China. ( 英 文 ). SongXiao-Yan; Blackmore S; Bera S; Li Cheng-Sen.Review of Palaeobotany and Palynology, 2007,145(3-4): 325-333This study concerns the palynological analysisof 19 spider webs, which were collected fromthe northwestern, central and southern parts ofYunnan, China. Pollen grains and spores of 20taxa belonging to 16 families were recordedfrom northwestern Yunnan and 28 taxa from 23families from central Yunnan. Spider webs fromsouthern Yunnan yielded 28 taxa belonging to25 families from Mengla County, 38 taxa in 34families from Wangtianshu Garden and 11 taxarepresenting 10 families from XishuangbannaBotanical Garden. The pollen grains and sporesextracted from spider webs reflect the distinctcharacteristics of the regional vegetation whichchanges from north to south Yunnan. This demonstratesthe potential of spider webs as a naturaltrap for the study of modern pollen rain.2008040055Pseudolarix amabilis 花 粉 的 描 述 与 区 分 : 古生 态 推 断 和 新 鲜 双 气 囊 花 粉 新 的 鉴 定 标 准 =Description and differentiation of Pseudolarixamabilis pollen Palaeoecological implicationsand new identification key to fresh bisaccatepollen. ( 英 文 ). Zanni M; Ravazzi C. Review ofPalaeobotany and Palynology, 2007, 145(1-2):35-75The differentiation of Pseudolarix from otherbisaccate pollen is considered as a tool to investigatethe fossil history of this genus. UsingLight Microscope (LM) and Scanning ElectronMicroscopy (SEM) we performed a descriptiveand morphometric analysis of Pseudolarixamabilis (Pinaceae) bisaccate fresh pollen grains.Descriptive differentiation characters from Pinusand from other bisaccates have been established.A morphometric differentiation from pine pollenbelonging to Pinus sylvestris type was obtainedthrough a study of twelve living species of Pinus.A new identification key for bisaccate pollengrains of living conifers has been elaborated.Although it is addressed to identification of freshpollen, the proposed descriptive criteria may alsobe applicable to well-preserved fossil material. APliocene site from N-Italy, rich in Pseudolarixcone scales and needles, was used to test the reliabilityof the proposed criteria on fossil pollen.We also identified Pseudolarix pollen from thelacustrine sediments from Massif Central(France), about 3 My.We carried out a complementary evaluation ofthe ecological and climate ranges both of theliving species and of the fossil assemblages thatincluded Pseudolarix. This tree was a componentof the warm-temperate mixed conifers rainforestsof the Cenozoic, a biome yielding, afterconsiderable reduction of floristic diversity,overall conifer decimation, to the modern“mixed mesophytic” and “mixed hardwood”forest types. Although its fossil record reveals awide distribution in the Northern Hemisphereduring the Cenozoic, macrofossils are only scattered.On the other hand, information about thepollen production, aerodynamics and taphonomyof Pseudolarix pollen suggests that this tree isamong the properly or moderately overrepresentedgenera in pollen images from itsnatural habitat. Therefore, its pollen record mayadd clarifications to palaeoclimate reconstructionsof Cenozoic environments.2008040056非 洲 树 木 和 灌 木 花 粉 类 型 数 据 库 = Africanpollen database inventory of tree and shrub pollentypes. ( 英 文 ). Vincens A; Lézine A-M;Buchet G; Lewden D; Thomas A L; Contributors.Review of Palaeobotany and Palynology, 2007,145(1-2): 135-141African pollen data have been used in manyempirical or quantitative palaeoenvironmentalreconstructions. However, the pollen types usedin these studies were not controlled and standardised,preventing the precise understandingof pollen–plant and pollen–climate relation thatis necessary for the accurate quantification ofcontinental scale climate change or ecologicalprocesses in the past. This paper presents asummary of the progress made with the AfricanPollen Database (APD) inventory of plant diversityfrom pollen data extracted from 276 fossilsites and more than 1500 modern samples, with18
a focus on tropical tree pollen types. This inventory(1145 taxa) gives, for each pollen taxonwhose nomenclature is discussed, informationon the habit, habitat and phytogeographical distributionof the plants they come from. Specialattention has been paid to pollen types with similarmorphology, which include several plant speciesor genera, whose biological or environmentalparameters can differ considerably.2008040057哥 伦 比 亚 杜 伊 塔 马 内 安 第 斯 盆 地 Pantano deVargas 全 新 世 花 粉 记 录 所 反 映 的 植 被 变 化 和人 类 影 响 = A Holocene pollen record of vegetationchange and human impact from Pantanode Vargas, an intra-Andean basin of Duitama,Colombia. ( 英 文 ). Gómez A; Berrío J C;Hooghiemstra H; Becerra M; Marchant R. Reviewof Palaeobotany and Palynology, 2007,145(1-2): 143-157Holocene environments in the intra-Andeanbasin of Duitama (Eastern Cordillera of Colombia,2510 m altitude) are presented based on the620 cm long Vargas pollen and sediment record.Seven AMS radiocarbon dates show these lakeand swamp sediments represent the period from8800 to 2610 14 C yr BP. We identified sevendistinct periods of environmental conditions inthe basin.From ca. 8800 to 7700 14 C yr BP (9450–8300 cal yr BP) Alnus and Myrica swamp forestgrew on wet soils. On the surrounding slopesAndean forest was present with Hedyosmum,Melastomataceae and Quercus. Between 7700and 6090 14 C yr BP (8300–6750 cal yr BP) openwater with aquatics alternated with peat-formingPlantago meadows reflecting repeated lake levelschanges. From 6090 to 5220 14 C yr BP(6750–5680 cal yr BP) open water and grassyvegetation around the lake was replaced by Alnus-dominatedswamp forest, suggesting lowerlake levels and drier climatic conditions. Between5220 and 4500 14 C yr BP (5680–4810 calyr BP) an alternation between Alnus-dominatedswamp forest and open grassy vegetation continued,reflecting fluctuating water levels. Atthat time Hedyosmum, Miconia, Quercus, Solanaceae,Relbunium and Rubiaceae were commonelements in the Andean forest. From about4500 to 3680 14 C yr BP (4810–3800 cal yr BP)Alnus-dominated swamp forest alternated withMyrica shrub and much organic material accumulatedin the basin. Evidence of deforestation(reduction of Quercus in particular), lowering ofwater tables and increasing disturbance, probablyby erosion (presence of Amaranthaceae/Chenopodiaceae,Borreria and Dodonaea)point to the settlement of pre-Hispanic populations.Between 3680 and 2610 14 C yr BP (3800–2470 cal yr BP) there is clear evidence of cropcultivation (presence of Zea mays) and frequentfires (high amounts of charcoal in the sediments).Erosion all over the basin led to significantsediment supply and the lake gradually changedinto a swamp. By this time pre-Hispanic populationshad used nearly all alder wood in thecatchment area. The uppermost sediments areoxidised and the last 2610 radiocarbon years ofthe Holocene are not represented, possibly dueto agricultural activities.2008040058南 极 维 多 利 亚 地 南 部 Carapace Nunatak 早 侏罗 世 费 拉 群 的 孢 粉 = Early Jurassic miosporesfrom Ferrar Group of Carapace Nunatak, SouthVictoria Land, Antarctica. ( 英 文 ). Ribecai C.Review of Palaeobotany and Palynology, 2007,144(1-2): 3-12Along the Transantarctic Mountains, thesiliciclastic foreland basin deposits of the BeaconSupergroup and the effusive rocks of theFerrar Group overlay the pre-Devonian metamorphicbasement. The Ferrar Group at CarapaceNunatak is composed of fluvial volcanicsandstones of the Carapace Sandstone Formation,which is overlain by the volcanic flows andbreccias of the Kirkpatrick Basalt Formation.Fossiliferous horizons are present in both formations.Palynological analyses have been carriedout on fifteen samples collected in marly–siltyhorizons within the Carapace Sandstone andKirkpatrick Basalt formations. Samples from theCarapace Sandstone Formation contain a scarcebut quite well preserved palynoflora, which isorange to light brown in colour. The spore–pollen assemblages lack dominant species andare very similar in composition. The stratigraphicallysignificant taxa Corollina torosa andPodosporites variabilis are present. The twosamples from the Kirkpatrick Basalt Formationcontain a very rich microflora dominated byCorollina species (mainly C. torosa) and Exesipollenitestumulus. Some representatives of thegenus Callialasporites are also present. Comparisonswith previous Carapace Nunatak andAntarctic palynological studies are discussed.2008040059日 本 宫 古 群 和 手 取 群 的 早 白 垩 世 陆 地 孢 粉 组合 及 其 古 植 物 地 理 区 系 意 义 = Early Cretaceousterrestrial palynomorph assemblages fromthe Miyako and Tetori Groups, Japan, and theirimplication to paleophytogeographic provinces.( 英 文 ). Umetsu Keita; Sato Yoko. Review ofPalaeobotany and Palynology, 2007, 144(1-2):13-24Terrestrial palynomorph assemblages werefound from the Lower Cretaceous MiyakoGroup in the Tanohata area, northeast Japan, and19
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was pulsed, with major declines usu
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mycelium, was observed where reticu
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suggest that reticulopodia are self
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to OIS 3, compared to the more stab
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Patterson R T. Journal of Foraminif
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known xenophyophore species grouped
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aminiferal Research, 2001, 31(4): 2
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arctic environment over this critic
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Semeniuk T A. Journal of Foraminife
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sible to make production calculatio
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arcellacean strains from within the
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annual flux rates is calculated and
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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