Semeniuk T A. Journal of Foraminiferal Research,2000, 30(2): 99-109 1 图 版 .Density of epiphytic foraminifera varies spatiallyfrom sub-leaf to regional scales withinPosidonia australis meadows of south WesternAustralia. Foraminiferal populations on individualseagrass leaves show compositional zoningand aggregation around algae and serpulid wormtubes. Such microscale spatial heterogeneitycould reflect microhabitat, leaf growth history,food source and recruitment patterns. Most foraminiferahave homogeneous densities on individualplants, and are distributed evenlythroughout seagrass samples from meadows at agiven geographic site. Only species associatedwith patchy epiphytic algae within the meadowsshow spatial heterogeneity at the local scale.Spatial homogeneity within the seagrassmeadow reflects repetition of seagrass leaf substrateand microhabitats, and the uniformity ofambient environmental variables at scales largerthan the seagrass leaves. Spatial homogeneity inthis environment permits characterization of agiven geographic site based on three samples. Atregional scales, foraminifera may have homogeneousand heterogeneous distributions. Abundanceof individual species is uniform, sporadic,or shows a gradient pattern along the coast. Patternsof variation in foraminiferal populationsregionally, partly reflect the climate gradient, butalso factors operating at micro- and local scales.Regionally distinct assemblages could be definedfor different climatic regions along thecoast. Thus, populations of the various foraminiferalspecies are regulated by environmentalor biotic variables at different scales.This study shows how sample composition ateach site reflects spatial variation of species atmicro-, local and regional scales and how thesedifferences can be used to define assemblageswhich characterize microhabitats, localities andregions.2008040261意 大 利 北 部 特 兰 托 地 台 Calcari Grigi 地 区 威尼 斯 早 三 叠 世 有 孔 虫 EverticyclamminaRedmond 1964( 新 种 E. praevirguliana) 的首 次 记 录 = First record of EverticyclamminaRedmond 1964(E.praevirguliana n. sp., foraminifera)from the early jurassic of the venetianprealps (Calcari Grigi,Trento platform,northern Italy). ( 英 文 ). Fugagnoli A. Journal ofForaminiferal Research, 2000, 30(2): 126-134 3图 版 .The rich fossil content of the Lower Jurassiccarbonate successions of the Trento Platform(northeastern Italy) have been studied since thebeginning of the nineteenth century. This detailedstudy on several stratigraphic sectionscropping out in this area, all spanning the LiassicRotzo Member (Calcari Grigi formation, VenetianPrealps), provides us new biostratigraphicdata about the genus Everticyclammina Redmond1964. A new species of Everticyclammina,E. praevirguliana n. sp., is formally describedfrom the Calcari Grigi, where it occurs in levelsattributed to the late Sinemurian to Domerianage. Everticyclammina praevirguliana n. sp.thus becomes the first representative of the genusin the Early Jurassic; this record consequentlyenables the stratigraphic distribution ofthe genus to be lowered to the Liassic. Hence theplexus of Everticyclammina evolving communitiesnow bridges the Liassic (late Sinemurian) toEarly Cretaceous (Aptian) interval.2008040262变 形 虫 Arcellaceans 作 为 印 度 尼 西 亚 IrianJaya 岛 Sentani 热 带 湖 中 的 湖 泊 指 示 物 的 初步 调 查 = Preliminary survey of Arcellaceans(Thecamoebians)as limnological indicators intropical lake Sentani, Irian Jaya, Indonesia. ( 英文 ). Dalby A P; Kumar A. Journal of ForaminiferalResearch, 2000, 30(2): 135-142 1 图版 .Arcellacean (thecamoebian) assemblages recoveredfrom Lake Sentani, a large tropical lakesouthwest of Jayapura, Irian Jaya, Indonesia, arecharacterized by low diversity and low abundances.Dominated by Centropyxis aculeata andArcella vulgaris, this fauna is similar to thoseindicative of stressed environments (brackishconditions, high levels of industrial contaminants)in temperate regions. However, neithercondition exists in Lake Sentani. Previous workhas determined that the lake is oligomictic, characterizedby weak circulation with turnover occurringonly every few years. Prolonged isolationof the lake bottom produces progressivelyreduced oxygen levels and results in reducedproductivity among benthic organisms. The feeblestratification that exists here creates reducedoxygen levels at depth providing a likely explanationof the stressed arcellacean fauna. The oligomicticconditions observed here and the resultantfauna are widespread and are characteristicof a large proportion of tropical lakes around theworld. As the low bottom water oxygen conditionswill have a serious impact on most benthicorganisms in these lakes, other limnological signalsincluding anthropogenic contamination willbe masked. This is a disappointing result as theutility that has been developed for the group as alimnological indicator in temperate lakes doesnot appear to apply in a significant proportion oflow latitude lakes.200804026384
维 吉 尼 亚 Philips Creek 地 区 维 吉 尼 亚 盐 沼 中的 有 孔 虫 组 合 = Foraminiferal assemblagesfrom a virginia salt marsh, Phillips Creek, Virginia.( 英 文 ). Spencer R S. Journal of ForaminiferalResearch, 2000, 30(2): 143-155Phillips Creek is a salt marsh located on theseaward side of the southern Delmarva Peninsulaof Virginia, is part of the World BiosphereReserve designated by the United Nations, and issituated within the Virginia Coast Reserve/LongTerm Ecological Research area (VCR/LTER).This marsh does not exhibit well-defined vegetationalzones but rather tends to be a patchy mixof vegetation. Cluster analysis indicates that thearea can be divided into low, middle or transitionaland high marsh. The low marsh zone doesnot exhibit any unique assemblages of agglutinatedforaminifera that would allow further subdivisionof this area. The fact that no calcareousspecies were found may be due to the season(May) when sampling was done. The low marshis dominated by M. fusca and T. inflata. The occurrenceof a transitional or middle marsh zoneappears to be dependent upon gradient. Traverse1 with a gradient of 3 percent has a poorly definedmiddle marsh zone while Traverse 2 with agradient of 0.6 percent has a broad, well definedtransitional zone. Tiphotrocha comprimata and T.inflata are the dominant species in this zone. Thehigh marsh can be subdivided into two subzones.The lower part of the high marsh is dominatedby T. inflata, T. comprimata and J. macrescenswhile the upper part has a relief ranging between5 and 8 cm, has a reduced population and containsJ. macrescens and T. salsa almost to theexclusion of all other foraminiferal species. Thissubzone, marking the occurrence of highest highwater, is topographically very narrow, requiringclosely spaced sampling to detect its presence.The highest high water zone can be extendedsouthward into Virginia.2008040264拉 普 帖 夫 外 海 和 Fram 海 峡 中 的 浮 游 有 孔 虫的 现 代 分 布 和 生 态 特 征 = Planktic foraminifersin the outer Laptev sea and the Fram straitmoderndistribution and ecology. ( 英 文 ). VolkmannR. Journal of Foraminiferal Research,2000, 30(3): 157-176Planktic foraminifers were studied in the ArcticOcean in the outer Laptev Sea (76–80°N,100–150°E) in 1995, in the Fram Strait (81–82°N, 10°W–15°E) and in the western BarentsSea (76°N, 33°E) in 1997. Five depth intervalswere sampled vertically between 500 m waterdepth and the sea surface. In the 125–250 µmsize class, highest abundances of living individualswere present in the western Fram Strait(17 ind/m3) and the Barents Sea (14 ind/m3),decreasing to 4 ind/m3 near Severnaya Zemlyaand less than 2 ind/m3 at the eastern Laptev Seacontinental margin. The most common speciesNeogloboquadrina pachyderma (sinistral coiling)occured in cold Polar water masses between 50and 100m water depth, where they accounted for>70% of all shells. A synodic lunar reproductivecycle is demonstrated in all sampled areas,where reproduction takes place around full moon.In warmer Atlantic water masses of the WestSpitzbergen Current and the Barents Sea, Turborotalitaauinqueloba contributes >85% to thetotal assemblage. Most individuals were obtainedbetween 50 and 200 m water depth. In thewestern Fram Strait affected by the EastGreenland Current and at the outer Laptev Searelative abundances decrease to 2–10%. Allother species combined make up only 5% of thetotal fauna. In general, empty tests are mostabundant in water depths deeper than 200m as aresult of gametogenesis and due to high juvenilemortality. The strong gradient in absolute abundancesseems to be determined by the availabilityof food, low salinity due to freshwater dischargefrom the Siberian rivers and the ice coverageof the Arctic Ocean. The relative abundances,however, reflect the complex hydrographicinteraction between relatively warm Atlanticwater inflow and cold polar water exportin the Arctic Ocean.2008040265潮 间 带 有 孔 虫 月 变 化 的 主 要 特 征 ( 现 存 量 和生 物 量 ) 研 究 = Major aspects of foraminiferalvariability (standing crop and biomass) on amonthly scale in an intertidal zone. ( 英 文 ).Murray J W; Alve E. Journal of ForaminiferalResearch, 2000, 30(3): 177-191Temporal and spatial variability of intertidalbenthic foraminiferal assemblages in the surface(0–1 cm) sediments have been determined by atime series survey (27 months) of the Hambleestuary, southern England. One pair of replicateswas collected each month from two stations atdifferent elevations in the intertidal zone. Theassemblages were dominated by three species,Haynesina germanica, Ammonia beccarii (formatepida), and Elphidium excavatum. Patchinessoccurred on a scale of a few centimeters and hada major impact on tracking temporal changes inthe standing crop. The study clearly shows theneed for replicate sampling in order to obtainreliable information especially on absoluteabundance data. The absence of juveniles is dueto loss through drying the samples prior to picking.The results show that it is not possible todetermine the lifespan of continuously reproducingspecies (i.e., young individuals always present)where it is impossible to follow the growthof cohorts, and for the same reason it is not pos-85
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第 4 卷 第 4 期古 生 物 学
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Fossils, i.e. remains of living org
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nus, a new ichnospecies of Fuersich
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以 松 柏 类 和 盾 籽 类 为
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Island, Papua New Guinea. ( 英 文
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A C. Canadian Journal of Earth Scie
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mated depositional interval of 10 t
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北 海 古 近 纪 一 种 新 型
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scabrate-verrucate, and rugulate mi
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the Tetori Group in the Kuzuryu are
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during the Late Pleistocene are rec
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ane have been previously reported f
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Albian-early Paleocene in the Anady
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Poaceae and Plantago lancelata. shr
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the eastern segment of its southern
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member of the La Despedida Formatio
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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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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