arctic environment over this critical interval andfor which such sections are few.2008040255西 太 平 洋 有 孔 虫 Nummulitidae 的 评 述 = Remarkson west Pacific Nummulitidae (foraminifera).( 英 文 ). Hohenegger J; Yordanova E. Journalof Foraminiferal Research, 2000, 30(1): 3-28 5 图 版 .Living Nummulitidae achieve their highestdiversity in the subtropical and tropical WestPacific. Although all house symbiotic microalgae,they avoid highly illuminated areas near thewater surface, since their flat tests could be easilydamaged by the hydrodynamic regime. Thepreference for calm water conditions extendstheir depth distribution down to the base of thephotic zone. West Pacific Nummulitidae can bedifferentiated into ten species belonging to sixgenera according to an ecological species concept.The genus Operculina d’Orbigny is representedby three species. While O. discoidalis(d’Orbigny) prefers a fine-grained bottom undermedium light conditions (10% surface intensity),O. ammonoides (Gronovius) prefers a coarsersubstrate and sometimes can be found on hardbottoms. Light dependence ranges from 1.5% to68% surface intensity. Less illuminated coarsesands are inhabited by Operculina cf. O. complanata(Defrance), which is the dominant symbiont-bearingforaminifer between light intensitiesof 0.2% to 12% surface illumination. Thegenus Planostegina Banner and Hodgkinsondemonstrates transitions to the genus Operculinain test form and surface, while the division intochamberlets is similar to Heterostegina.Planostegina operculinoides (Hofker) is distinguishedby flat tests and delicate chamberlets. Itlives on sandy bottoms restricted to light intensitiesbetween 0.45% and 26% surface illumination.The more robust Planstegina aff. P. operculinoides(Hofker) prefers light intensities between0.4% and 2.7% surface illumination.Planoperculina heterosteginoides (Hofker)shows morphological transition to Operculina cf.O. complanata in developing incomplete septula.This species lives in low illuminated areas (0.3%to 2.5% surface intensity) and prefers medium tofine-grained sands. Heterostegina depressad’Orbigny spans a broad range in light intensities(2% to 70% surface illumination), and isprotected against irradiation by thick tests and acryptic life mode near the surface. Test constructionenables life under strong hydrodynamic regimes.This species lives firmly attached to hardsubstrates, thus counteracting transportation bywater movement. Nummulites venosus (Fichteland Moll) differs from H. depressa in havingundivided chambers. It lives exclusively oncoarse sand and avoids high sediment movement,thus starting its distribution beneath the fairweather wave base. According to light intensities,the upper limit may be similar to O. ammonoides(80%), while the lower limit is 2.5% surface illumination.Operculinella cumingii (Carpenter)inhabits coarse to medium sand in deeper regionsbetween 1.2% and 25% surface illumination.Tests of the cyclic, large-sized speciesCycloclypeus carpenteri Brady are easily transporteddue to the thin, plate-like form. The upperdistribution limit correlates with the storm wavebase, restricting C. carpenteri to depths below50 m. The lower distribution limit depends onlight intensity and is located near the base of thephotic zone (0.4% surface illumination).2008040256红 海 亚 喀 巴 湾 埃 拉 特 市 北 部 海 湾 网 笼 养 鱼 场对 底 栖 有 孔 虫 分 布 的 影 响 = Impact of a netcage fish farm on the distribution of benthic foraminiferain the northern Gulf of Eilat (Aqaba,Red Sea). ( 英 文 ). Angel D L; Verghese S. Journalof Foraminiferal Research, 2000, 30(1): 54-65Two sediment transects, at 23m depth, weresampled below a commercial fish farm at thenorthern end of the Gulf of Eilat in order to describethe benthic foraminiferal communityalong an organic enrichment gradient. Sedimentorganic matter, porewater ammonia and phosphateconcentrations reflected the input from theoverlying fish cages and there was generally adecrease in these variables with distance fromthe point source. Rose-bengal stained foraminiferawere found at all of the stations sampled belowthe fish farm, i.e. there were no azoic sediments.Fifty-one species of foraminifera (>45µm) were found in the sediments around the fishfarm but most were rare species. The most abundant(generally > 83% of the foraminifer abundance)species (stained + unstained) found wereAmphisorus hemprichii, Amphistegina lessonii,Assilina ammonoides, Borelis schlumbergeri,Challengerella bradyi, Hauerina diversa, andPeneroplis planatus. Five of these foraminiferaare algal symbiont bearing forms. The diatombearingspecies, A. lessonii and A. ammonoides,constituted 40 to 50% of the total number oftests. The most abundant stained species were A.ammonoides, B. schlumbergeri, H. diversa and P.planatus. Abundances of foraminifera werehighest in the "hypertrophic" zone, adjacent tothe fish cages. The most abundant speciesshowed negative correlations between totalabundance of tests and organic matter in the uppercentimeter of the sediment. Negative correlationswere also found between abundances ofboth total and stained tests of the most abundantspecies and integrated ammonia concentrations.No clear indicator species of the organically-82
enriched benthos were identified. Deformed tests(mainly P. planatus) were observed in the samplesand it is not clear whether they formed as aresult of adverse conditions related to the fishfarm because such variants also occurred at unenrichedsites.2008040257识 别 现 生 有 孔 虫 的 死 亡 率 、 原 生 质 腐 烂 率 和染 色 技 术 稳 定 性 的 综 述 = Mortality, protoplasmdecay rate, and reliability of stainingtechniques to recognize ‘living’ foraminifera: areview. ( 英 文 ). Murray J W; Bowser S S. Journalof Foraminiferal Research, 2000, 30(1): 66-70Non-vital staining, especially with rose Bengal,has been widely used in ecological studies todifferentiate between the tests of dead (unstained)foraminifera from those presumed to be living atthe time of collection (stained). Doubts havebeen expressed about staining methods becauseof the possibility that dead individuals may retainundecayed protoplasm for weeks or monthsafter death; when stained, such individualswould be recorded as living. To assess the importanceof such false positives, it is necessary toexamine rates of mortality, and the modes ofgeneration of empty tests, i.e., whether due toreproduction, growth stages (leaving empty testsduring growth) or death. It can be argued thatreproduction, ontogeny, and death through predationlead to tests devoid of protoplasm.Whereas reproduction may affect only a smallproportion of the population of each species (dueto high pre-reproductive mortality), predation inoxygenated environments may be responsible forthe major part of that pre-reproductive mortality.In oxygenated environments, disease or adverseenvironmental conditions are most likely to leadto dead individuals having tests containing protoplasm.In dysaerobic/anoxic environments,predation by macrofauna may be excluded, soforaminifera die through other causes and thusmore tests with dead protoplasm may be potentiallyavailable for staining. Therefore, for mostother environments, the problem of staining deadindividuals is almost certainly overstated. Furthermore,from comparative studies, it seemsthat the most commonly used technique (stainingwith rose Bengal) is as reliable as others. Nowthat new vital staining techniques, especially theuse of fluorescent probes, are being introduced,it is timely for further objective comparativestudies of all techniques to be made in order toevaluate data already gathered and to developthe best strategies for future ecological studiesaccording to whether they are field-based or experimental.2008040258远 东 地 区 渐 新 世 晚 期 到 中 新 世 的Lepidocyclina (L.) isolepidinoides 、 L.(Nephrolepidina) nephrolepidinoides sp.nov.、L. (N.) brouweri 和 L. (N.) ferreroi 的演 化 = The evolution of Lepidocyclina (L.)isolepidinoides, L. (Nephrolepidina) nephrolepidinoidessp. nov., l. (n.) brouweri and L. (N.)ferreroi in the Late Oligocene- Miocene of theFar East. ( 英 文 ). Boudagher-fade M K; Lord AR. Journal of Foraminiferal Research, 2000,30(1): 71-76 2 图 版 .Material from Borneo and Sumatra show thatthere is a morphological evolution from Lepidocyclina(Lepidocyclina) isolepidinoides van derVlerk, 1929, to L. (Nephrolepidina) nephrolepidinoidessp. nov., L. (N.) brouweri Rutten,1924 and L. (N.) ferreroi Provale, 1909. Thelineage demonstrates one of the evolutionaryprogressions from Lepidocyclina (Lepidocyclina)to Lepidocyclina (Nephrolepidina) for the FarEast region.2008040259底 栖 有 孔 虫 和 介 形 类 对 不 同 污 染 源 的 反 应 —来 自 埃 及 两 个 泻 湖 的 研 究 = The response ofbenthic foraminifera and ostracods to variouspollution sources: a study from two lagoons inEgypt. ( 英 文 ). Samir A M. Journal of ForaminiferalResearch, 2000, 30(2): 83-98 3 图 版 .A study of foraminiferal assemblages was carriedout at two Egyptian Nile Delta lagoons.Analysis of surficial sediment samples fromManzalah Lagoon shows enrichment in heavymetals (Pb, Zn, Cu, Cr and Cd). The environmenthas become so lethal to foraminifera thatno species can currently survive. Among ostracods,only one species (Cyprideis torosa) wasfound living and able to invade the polluted lagoonregion. Samples from Edku Lagoon, whichreceives only agricultural drainage water, showheavy metal concentrations close to natural baselinelevels, and yield living foraminifera. Thefrequent occurrence of deformed specimens inManzalah Lagoon, comparable to Edku Lagoon,reveals that: (1) benthic foraminifera are moresensitive to industrial wastes containing heavymetals; (2) agricultural wastes do not significantlyharm benthic foraminifera; (3) Ammoniabeccarii forma parkinsoniana is less resistant topollution than forma tepida; (4) morphologicalabnormalities of the foraminiferal tests dependupon the nature of the pollutant; and (5) benthicforaminifera are less tolerant to pollution thanostracods and molluscs.2008040260从 微 观 到 区 域 尺 度 下 附 生 有 孔 虫 的 空 间 分 布特 征 = Spatial variability in epiphytic foraminiferafrom micro-to regional scale. ( 英 文 ).83
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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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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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sediments from the northern shelf o
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nano record further into the early
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lankovitch-scale frequency. Analyse