The evolution of BioBike: Community adaptation of a biocomputing platform

Programming languages are, at the same time, instruments and communicative artifacts that evolve rapidly through use. In this paper I describe an online computing platform called BioBike. BioBike is a trading zone where biologists and programmers collaborate in the development of an extended vocabulary and functionality for computational genomics. In the course of this work they develop interactional expertise with one another’s domains. The extended BioBike vocabulary operates on two planes: as a working programming language, and as a pidgin in the conversation between the biologists and engineers. The flexibility that permits this community to dynamically extend BioBike’s working vocabulary—to form new pidgins—makes BioBike unique among computational tools, which usually are not themselves adapted through the collaborations that they facilitate. Thus BioBike is itself a crucial feature—which it is tempting to refer to as a participant—in the developing interaction.     

神农架花粉-气候转换函数的建立与初步应用

根据大量孢粉分析与气候观测资料，运用统计方法建立了神农架地区现代花粉一气候转换函数，并以大九湖为例，运用所建回归方程计算出了晚第四纪12500年以来的气候参量值，结果表明，更新世末（10600－12500a,B,P)为寒冷干燥的冷期气候，年均温比今低8度,年降水量比今低150－200mm,7400-10600a,B.P为一气候过渡期，年均温比今高3．5度左右，年降水量最高时比今约高300mm;4000a.B.P以来，气候有所波动，基本以温和湿润为特征。     

星载GMTI稀疏阵雷达的STAP研究

针对稀疏阵的欠采样会引起动目标检测盲区的问题,基于星载GMTI(ground moving targets indica-tion)稀疏线阵雷达,分析了多载频稀疏阵雷达的系统模型和空时自适应处理(space time adaptive processing,STAP)的基本原理,考虑了非周期阵列对减少盲区的作用。仿真结果表明采用多载频模式可有效改善稀疏引起的动目标检测盲区。     

黄骅拗陷滩海地区沙河街组孢粉组合

目的 由于黄骅拗陷滩海地区下第三系沙河街组孢粉化石研究相对较为薄弱。方法 根据沙河街组所产孢粉化石的特征，讨论了孢粉组合的时代。结果 建立了1个孢粉组合和3个亚组合，即栎粉属Q-uercoidites高含量组合(Q．microhenrici-U.minor亚组合，Ephedripites-Rutaceoipollis-Meliaceoidites亚组合和Quercoidites-Labitricolpites亚组合)。结论 该地区古植被类型由落叶针叶林逐渐转变为落叶阔叶草原型的植物群；古气候经历了半干旱、潮湿的亚热带气候到温暖带-亚热带气候至半干旱的暖温型气候。     

泌阳断陷下第三系陆相层序中油气生储盖及其组合特征——以双河-赵凹地区下第三系核三上段为例

运用层序地层学理论和分析方法 ,分析了泌阳断陷下第三系陆相层序中油气生、储、盖以及盐组合特征 .分析结果表明 :第三系陆相层序中极为有利的烃源岩为发育于高水位体系域的半深湖 -深湖泥岩 (属区域性生油层 ) ,其次是水进体系域及水退体系域的湖相泥岩 (属局部性生油层 ) ;有利的储集体分布于水进体系域和水退体系域的冲积扇——扇三角洲砂体及前扇三角洲斜坡带的滑塌性重力流扇体中 ,尤其是扇三角洲的 (水下 )分流河道、河口砂坝 (远砂坝 )及前缘席状砂体 .区域性盖层为高水位体系域的深水湖相泥岩 ,而水进和水退体系域的湖相泥岩亦可构成局部性盖层     

北京平原区第四纪软体动物化石组合

本文对北京平原区第四纪软体动物化石进行了初步的研究，建立了１４个组合带，反映了本区第四纪时期经历了大约１１个古气候演变阶段。在冷期因气候干燥，环境中水量减少，腹足类化石以陆生肺螺类最为发育；在暖期水生双壳类较为发育，腹足类群明显繁盛，以水生种类的大量出现为特征。冷暖交替的软体动物组合，反映了本区第四纪时古气候的变动特点。     

Late Glacial and Holocene vegetation history and paleoclimate of the Tengger Desert,northwestern China

With a total area of 36000 km2, the Tengger Desert is the fourth largest desert in China. The Qilian Mountains demarcate the southwestern boundary of the desert andthe Helan Mountain on the east separates the desert from the Mo Us Desert. The Yabulai Mountain on thenorthwest borders the Tengger Desert and the BadainJaran Desert and the Loess Plateau touch its southern tip (Fig. 1). Climatically, the area is situated at the junction of the hyper-arid northwest, the arid to semi-arid sou…     

The white schist assemblage in the kyanite quartzite from the ultrahigh-pressure metamorphic belt, eastern Dabie Mountains

The kyanite quartzite from the ultrahigh-pressure metamorphic belt in the eastern Dabie Mountains is composed mainly of quartz, kyanite, talc and epidote, which contains a typical mineral assemblage of white schist. It suffered an eclogite facies metamorphism of P =(2 4±0 3) GPa and T =630℃ together with coexisting eclogite. The protolith may be an aplite replaced by high-pressure fluid of eclogite facies.     

柴达木盆地第三系碎屑岩中粘土矿物特征及储层保护措施

柴达木盆地第三系碎屑岩中粘土矿物含量较低,一般小于４％大多数介于１％－２％,故对也孔隙度影响不明显,经Ｘ射线衍射分析可知,粘土矿物主要有４大类：伊／蒙混层粘土,伊利石,绿泥石和高岭石。它们的相对含量及形态产状,对不同地区不同层位的储层有着不同的潜在危害。