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corded in the Colli Berici (type locality CavaZengele) within the Bartonian part of the CalcariNummulitici formation, and possibly in the Priabonianof Italy and Slovenia. This taxon isherein described from Mossano, and the associatedlarger foraminifera (Nummulites biedai)confidently establish the age of these beds asLate Bartonian (SBZ 18), enabling the stratigraphicdistribution of B. vonderschmitti to beextended to the base of SBZ 18. A new speciesof Glomalveolina Hottinger 1960, G. ungaroi n.sp. is formally described herein; this taxon differsfrom the other Middle Eocene representativesof this genus by having a lower elongationindex and a larger proloculus. It is so far knownonly from the Late Bartonian of the Colli Berici,and represents one of the smallest alveolinidsfollowing the peak diversity of the Lutetian.Both species occur in shallow water calcarenites,and are the only representatives of the Alveolinidaein Upper Bartonian carbonate units of theColli Berici2008040283土 耳 其 Malatya 西 北 Hekimhan 地 区Campanian 晚 期 到 Maastrichtian 早 期 的 新种 Pseudedomia hekimhanensis = Pseudedomiahekimhanensis n. sp. from the late Campanian(?)to Maastrichtian of Hekimhan, NWMalatya, Turkey. ( 英 文 ). Gormus M. Journal ofForaminiferal Research, 1999, 29(3): 236-242 3图 版 .Pseudedomia hekimhanensis, a new species ofPseudedomia Henson 1948 from the Late Campanian(?)to Maastrichtian of Hekimhan, NWMalatya, Turkey, is described. It differs from theother Pseudedomia species by its smaller testsize, having fewer chambers, and the presence ofsecondary septa that are more or less parallel tocoiling.2008040284堪 萨 斯 州 Hooster 附 近 下 二 叠 统 CouncilGrove 群 中 的 钙 质 小 有 孔 虫 = Calcareoussmaller foraminifers from the Lower PermianCouncil Grove Group near Hooster, Kansas. ( 英文 ). Groves J R; Boardman D R. Journal of ForaminiferalResearch, 1999, 29(3): 243-262 4 图版 .The classic work of Erich Spandel (1901) onEarly Permian foraminifers from Hooser, Kansasis revised here on the basis of new collections.The stratigraphic interval exposed at Hooser isassigned to a portion of the Council GroveGroup that spans the Asselian-Sakmarian stadialboundary within the Cisuralian Series. Preliminaryanalysis of the Hooser fauna demonstrateslittle congruence between foraminiferal biofaciesand fourth-order depositional sequences independentlydefined on both sedimentologic andconodont abundance criteria. The lack of congruenceis probably attributable to coarse andlithologically biased sampling for foraminifers.Nevertheless, diverse foraminiferal faunas correspondgenerally to shallow, normal marine depositionalphases and impoverished faunas to restrictedmarine phases. Among the taxa first describedfrom Hooser, only Geinitzina postcarbonicaSpandel retains its original nomenclaturaldesignation. The taxonomic status of MonogenerinaSpandel has been unclear historically,and it remains so because we are unable to relatethe type illustrations to anything recovered fromthe new samples. Specimens identified by Spandelas Bigenerina cf. eximia Eichwald and Textulariagibbosa d'Orbigny (sensu Brady) areprobably referrable to the Palaeotextulariidae.Ammodiscus concavus Spandel is reassigned toBrunsiella as B. concava (Spandel). We followprevious authors in elevating Tetrataxis conicaEhrenberg var. lata Spandel to Tetrataxis lataSpandel, and in referring Nodosaria postcarbonicaSpandel to Nodosinelloides. The genusTezaquina Vachard was described originally aspseudoseptate. Re-examination of the type species,T. clivuli Vachard, confirms that it lackssepta but possesses internal wall thickenings thatcrudely partition the test. Primitively septateforms previously identified as Tezaquina arereferred to Vervilleina n. gen., anchored by thetype species Dentalina bradyi Spandel from theHooser locality. The presence of septation delimitsthe Syzraniidae from the Geinitzinidae,both of which are classified here within the Lagenina.According to this interpretation, the Lageninaare probably a monophyletic group thatoriginated in Moscovian time, and then diversifiedthroughout the remaining Late Paleozoicbefore their major radiation in the Early Mesozoic.2008040285西 班 牙 坎 塔 布 连 山 脉 Las Llacerias 剖 面( Moscovian/Kasimovian 界 线 ) 有 孔 虫Fusulinellid 晚 期 分 子 和 Schwagerinid 早 期 分子 的 出 现 及 两 者 关 系 = Late Fusulinellid earlySchwagerinid Foraminifera; relationships andoccurrences in the Las Llacerias Section(Moscovian/Kasimovian), Cantabrian Mountains,Spain. ( 英 文 ). Adriaan C. van Ginke; Villa E.Journal of Foraminiferal Research, 1999, 29(3):263-290 6 图 版 .Several localities in the Cantabrian Mountains(Spain) yield data on the occurrence of the latefusulinellid/early schwagerinid genera Protriticitesand Montiparus, but the Las Llacerias sectionnear Covadonga (Asturias), offers the bestopportunity for a better understanding of the92