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lowermost Danian planktonic foraminifera: Palaeoglobigerinan. gen.. ( 其 他 ). Arenillas I; ArzJ A; Nanez C. Revista Espanola de paleontologia,2007, 22(1): 21-62The lowermost Danian contains oligotaxicplanktic foraminiferal assemblages with speciesof small size and very simple morphology, derivedfrom an evolutionary radiation occurredafter the Cretaceous/Paleogene mass extinctionevent. The taxonomic classification of this foraminiferalgroup has been revised, after performingbiometric and morphological analysis inorder to delimit the species. Palaeoglobigerina n.gen. is proposed to include the small trochospiralglobigerinid species, with smooth wall-texture,3-4 chambers in the last spire whorl, occurring inthe guembelitria cretacea and Parvularugoglobigerinaeugubina Zones. Twenty two speciesare recognized, described and illustrated.2008040309安 徽 巢 湖 二 叠 系 最 晚 期 晚 长 兴 期 放 射 虫 动 物群 及 其 与 华 南 同 期 动 物 群 对 比 = A lateChanghsingian (latest Permian) radiolarian faunafrom Chaohu, Anhui and a comparison with itscontemporary faunas of South China. ( 英 文 ). HeWeihong; Zhang Yang; Zheng Yinger; ZhangKexin; Gui Biwen; Feng Qinglai. Alcheringa,2008, 32(2): 199-222A well-preserved late Changhsingian radiolarianfauna (15 species attributed to 12 genera) isrecorded from the upper part of the Talung Formation,Chaohu, Anhui Province, South China.This radiolarian fauna includes Entactinia itsukaichiensis,Entactinia sashidai, Triaenosphaeraminutus, Hegleria mammilla, ?Wuyia dongpanica,Tetraspongodiscus stauracanthus,Tetrapaurinella discoidalis, Klaengspongusformosus, Klaengspongus spinosus, Paroertlispongusfontainei, Ormistonella elegans, Quadricaulisinflata, Ishigaum trifustis, Ishigaum obesum,and Foremanhelena robusta. This fauna ismore diverse than the fauna from the Meishansection in Zhejiang Province but is less diversethan the fauna of the Dongpan section inGuangxi Province, South China. The new faunaincorporates a higher percentage of Latentifistulariaforms than the fauna from the Meishan section,but incorporates a lower percentage of Latentifistulariaand Albaillellaria forms than thatfrom the Dongpan section. These differencescould be due to deposition of the Chaohu sedimentsin deeper waters than at Meishan, but inshallower waters than at Dongpan.2008040310藏 南 萨 迦 县 混 杂 岩 晚 白 垩 世 有 孔 虫 动 物 群 =Late Cretaceous Foraminiferal Faunas from theSaiqu“mélange”in Southern Tibet. ( 英 文 ). LiGuobiao; Wan Xiaoqiao; Jiang Ganqing; HuXiumian; Goudemand N; Han Hongdou; ChenXi. Acta Geologica Sinica, 2007, 81(6): 917-921+924+922-923As one of the mélanges in the southern side ofthe Yarlung-Zangbo suture zone,the Saiqu mélangein southern Tibet is important for understandingthe evolution of the Neo-Tethysocean.The age of the Saiqu mélange,however,hasbeen debated due to the lackof reliable fossil evidence in matrix strata.Basedon lithological similarities with platform strata insouthern Tibet and limited fossils from exoticblocks,previous studies variously ascribed theSaiqu mélange to be Triassic in general,LateTriassic,or Late...2008040311西 印 度 群 岛 尼 维 斯 岛 附 生 有 孔 虫 的 居 群 结 构= Population structures among epiphytal foraminiferalcommunities, Nevis, West Indies.( 英 文 ). Wilson B. Journal of Micropalaeontology,2008, 27(part 1): 63-73The taxocene of live epiphytal foraminiferawas for one year monitored monthly on six phytalsubstrates in shallow water (