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signment is made following a recent emendationfor the polyphyletic group of rotaliporids, withthe generic attribution as follows: Thalmanninellareicheli (Mornod) and Rotalipora montsalvensisMornod.2008040154印 度 尼 西 亚 苏 拉 威 西 岛 东 南 Wakatobi 海 上国 家 公 园 海 平 面 重 建 过 程 中 所 用 现 代 有 孔 虫资 料 研 究 的 进 展 发 展 = The development of amodern foraminiferal data set for sea-level reconstructions,Wakatobi marine national park,southeast Sulawesi, Indonesia. ( 英 文 ). Horton BP; Whittaker J E. Journal of Foraminiferal Research,2006, 35(1): 1-14 1 图 版 .We collected modern foraminiferal samples tocharacterize the foraminiferal environments andinvestigate the role that temporal and spatialvariability may play in controlling the nature andsignificance of foraminiferal assemblages of themangroves of Kaledupa, Wakatobi Marine NationalPark, Southeast Sulawesi, Indonesia. Thestudy of foraminiferal live and dead assemblagesindicates that dead assemblages are least proneto vary in time and space, and furthermore, theyaccurately represent the subsurface assemblagesthat are the focus of paleoenvironmental reconstructions.Further analyses of the dead assemblagesindicate a vertical zonation of foraminiferawithin the intertidal zone. Zone D-Ia isdominated by agglutinated foraminiferaArenoparrella mexicana, Miliammina fusca, M.obliqua and Trochammina inflata. Zone D-Ibhas mixed agglutinated/calcareous assemblageswith species such as T. inflata and Ammoniatepida. Zone D-II is dominated by numerouscalcareous species including A. tepida, Discorbinellabertheloti, Elphidium advenum andQuinqueloculina spp. Zone D-Ia is found to bethe most accurate sea-level indicator and its assemblagesare omnipresent world-wide. ZonesD-Ib and D-II are subject to both spatial andtemporal variations which must be included inany sea-level reconstructions.2008040155深 海 底 栖 有 孔 虫 对 新 鲜 供 给 的 有 机 物 质 的 行为 和 反 应 - 一 个 来 自 对 微 观 环 境 下 供 食 系 统的 实 验 = Behavior and response of deep-seabenthic foraminifera to freshly supplied organicmatter: a laboratory feeding experiment in microcosmenvironments. ( 英 文 ). Nomaki H;Heinz P. Journal of Foraminiferal Research,2005, 35(2): 103-113The behavior of deep-sea benthic foraminiferain response to seasonal inputs of food materialwas examined through feeding experiments. Theexperiments using sediments from Sagami Bay(1425m water depth) containing living foraminiferawere carried out using microcosms(aquaria) with thin-walled glass sides. Threedifferent nutrient levels were tested in order toobserve how benthic foraminifera reacted to depositedorganic matter. Observations of bothbehavior and microhabitat segregation with respectto the sediment-water interface were conductedusing a sideways-mounted binocular microscope.Benthic foraminifera were verticallydistributed according to three types of microhabitatsegregation patterns, comparable to thoseof natural populations in Sagami Bay: shallowinfaunal, intermediate infaunal and deep infaunal.After addition of food into the aquaria, manyforaminifera migrated upwards to a shallowerpart of the sediment and some foraminifera ingestedfood. Shallow and intermediate infaunalspecies reacted faster to newly deposited foodmaterials than deep infaunal species. Amongdeep infaunal species, Globobulimina affinisreacted very slowly to added food, whereas Chilostomellaovoidea did not respond at all. Reactionsto newly deposited organic matter observedin this experiment vary from one microhabitat toanother. These different food preferences are animportant factor for understanding foraminiferalmicrohabitats and the degradation of phytodetritus.The size distribution of foraminiferal testsafter the experiment was completed suggests thatsome species reproduced during the experimentalrun, although there was no significant differencein total numbers of foraminifera betweenfed and unfed aquaria. Our results indicate thatsome benthic foraminifera may reproduce inresponse to organic matter arriving before thespring bloom.2008040156基 于 底 栖 有 孔 虫 大 陆 架 群 落 中 有 机 物 质 脉 动和 氧 气 损 耗 影 响 的 实 验 结 果 = Experimentaleffects of an organic matter pulse and oxygendepletion on a benthic foraminiferal shelf community.( 英 文 ). Ernst S; Bours R. Journal ofForaminiferal Research, 2005, 35(3): 177-197 1图 版 .Foraminiferal assemblages from a shelf environment(32 m water depth) in the northernAdriatic Sea were incubated in 26 mesocosms,in which six different environmental conditionswere created. A number of mesocosms weresealed to initiate anoxic conditions, and differentdoses of organic matter were added under boththe oxygenated and anoxic conditions. Themesocosms were harvested three times during anexperimental period of two months and foraminiferawere studied in the upper 3cm of thesediment. Certain taxa (Stainforthia fusiformis,Nouria polymorphinoides, Hopkinsina pacifica,Nonionella turgida) responded immediately tothe anoxic conditions: standing stocks declined47