New Data of Macrofossils in the Ediacaran Wenghui Biota from Guizhou,South China

The abundance and diversity of macrofossils in the Ediacaran have attracted much attention.The upper Doushantuo macrobiotas in South China,including the Miaohe biota from Hubei and the Wenghui biota from Guizhou,are mainly preserved as the carbonaceous compressions and dominated by macroscopic algae and metazoans.Here,we describe 10 genera and 10 species（including 6 new genera and species） of macrofossils from the Wenghui biota.At present,the Wenghui biota yields macrofossils in more than 31 genera and 33 species,excluding those given no image and established on a few unascertained specimens.Based on the occurrence and distribution of macrofossils in both Miaohe and Wenghui areas,the middle-late Ediacaran（back shales of the upper Doushantuo Formation） in South China can be subdivided into two assemblage biozones in biostratigraphy：（i） the Protoconites-Linbotulitaenia-Eoandromeda Anomalophton assemblage biozone characterized by abundant and diverse macrofossils and by the ranges of Protoconites,Linbotulitaenia and Anomalophton;and（ii） the Baculiphyca-Gesinella-Cucullus-Beltanelliformis assemblage biozone characterized by the acme of the longer macrofossils Baculiphyca and Gesinella,and by few shorter and discoidal macrofossils.

Weng旋回参数求解的简单方法

基于对Ｗｅｎｇ旋回的研究，提出了一种Ｗｅｎｇ旋回参数求解的简单、适用方法。该方法只需要进行两次简单的线性回归即可实现，克服了Ｗｅｎｇ旋回参数求取的麻烦，方便了油气藏现场工作者，具有一定的实际意义和使用价值。

New Macroalgal Fossils from Middle Cambrian Kaili Biota in Guizhou Province, China

Abundant and well-preserved remains of noncalcareous algae and soft-bodied metazoans were collected from Middle Cambrian Kaili biota in Taijiang county, Guizhou Province, China. These remains provide further evidence for the wide geographic distribution of many Burgess Shale taxa. Among the algae, 5 genera (including two new genera) and 5 species are described. They are Marpolia spissa Walcott, Acinocricus stichus Conway Morris and Robison, Udotealga erecta Yang, Eosargassum sawata Yang, and Rhizophyton zhaoyuanlongii Yang. Contrasting the macroalgal fossil assemblage in the Kaili biota with one in the Burgess Shale biota, it is clear that similarity of the Kaili biota and the Burgess Shale biota is reflected by the same content of not only the soft-bodied metazoans, but also the noncalcareous algae.

预测油气田产量的Weng旋回及其参数求解方法

论述了油气田动态系统的非线性特征，介绍了Weng旋回模型结构及性质。同时，对Weng旋回传统求解方法进行了研究、分析和对比，提出了Weng旋回求解的新方法，即联立方程求解法。新方法简单方便，不受人为因素的影响，具有单一解的特点，只需要最基本的加减乘除运算即可确定模型参数，通过实例验证了新方法的可靠性。

对Weng旋回模型预测可采储量方法的修正

Weng旋回模型在油气田长期产量预测中起着非常重要的作用,已在国内油气田产量预测中得到广泛应用.可采储量是油气田预测中的一个重要组成部分,在目前有关Weng旋回模型文献中,油气田可采储量的预测方法存在着错误和不足.本文对Weng旋回模型预测油气田可采储量的方法存在的错误进行了修正,建立了预测可采储量的可靠方法,从而完善了Weng旋回模型.

Weng旋回与Poisson、Gamma分布的对比与分析

通过对Ｗｅｎｇ旋回与Ｐｏｉｓｏｎ、Ｇａｍｍａ（亦记为Γ）分布模型的对比和分析表明，Ｗｅｎｇ旋回模型原式的自变量为特定的时间变量，即其时间为实际发生时间的１／Ｂ故模型原式在自变量从０～＋∞积分，其结果并非是真正的可采储量，而是对应于特定时间的积分值，这一数值等于可采储量的１／Ｂ；Ｗｅｎｇ氏模型原式与Ｐｏｉｓｏｎ分布尽管具有相似的表现形式，但却是两个完全不同的模型，因为二者的自变量不具有同一数学意义；Ｗｅｎｇ旋回模型的本质符合连续型Ｇａｍｍａ随机分布的数学原理，以往对模型参数ｎ规定取正整数的假设是不妥和多余的。在上述研究的基础上，给出了Ｗｅｎｇ旋回模型的简明式和结构式，使其上升到了一定的理论高度，更加具有实际意义和Ｗｅｎｇ氏特色，同时给应用者带来了方便。

Discovery of Enteromophites in the Chengjiang Biota and Its Ecological Significance

The paper deals with a new species of megaalgal fossil-Enteromophites intestinalis sp. nov. found in Chenejiang Biota in the early Cambrian. A morphological comparison of the living Enteromorpha and fossil Enteromophites indicates that there probably is a close relationship between these two genera. Based on a study on the surroundings of living Enteromorpha, Enteromophites intestinalis sp. nov. might have lived in the environment of sea or salt water.

使用RESRAD-BIOTA程序和ERICA程序计算某核电厂址附近水域中华鲟剂量的对比

根据某核电厂址附近水域的部分放射性核素浓度,使用美国能源部开发的RESRAD-BIOTA程序和欧洲原子能共同体开发的ERICA程序对该水域中的中华鲟进行剂量计算,同时使用蒙特卡罗方法进行了模拟计算,并将3种方法的计算参数和结果进行对比和分析。结果显示,ERICA程序的计算过程更符合实际情况,对于未知要素进行保守假设,其计算结果更具参考价值。

二苯基碘Weng盐引发阳离子与自由基光固化的研究

以合成的二苯基碘Ｗｅｎｇ六氟磷酸盐作光引发剂，对合成的有机硅环氧树脂（ＥＰＳ）和丙烯酸酯化环氧树脂（ＡＥＰＳ ＡＥ７１１、ＡＥ４４）及其混合物进行了两种没机理的光固化研究，并与安息香二甲醚引发的两烯酸酯化环氧树脂的自由基光固化进行了比较。结果表明，二苯基碘Ｗｅｎｇ盐具有同时引发阳离子和自由基光固化的双重功能。

实现k=18的Brezing-Weng曲线的最优配对

研究了嵌入次数为18的Brezing-Weng椭圆曲线上的最优配对的构造与实现。给出配对的Miller算法的循环长度为log2r/6,达到了Miller算法循环长度的猜想下界log2r/φ(18)。使用6次扭转映射实现了点的压缩表示,并减少了Miller算法中的除法运算,从而使得配对中的大多数计算只需要在Fq或Fq3上进行。给出了一个有效计算最优配对的算法。最后使用有限域上的Frobenius映射简化了配对算法中最终的幂运算。

Kaili Biota: A Taphonomic Window on Diversification of Metazoans from the Basal Middle Cambrian: Guizhou, China

A Burgess Shale-type biota is, in part, characterized by a wide diversity of taxa and soft-part preservation. Each provides unique historical insights into early metazoan evolution. Among the more than 40 globally distributed biotas, the early Cambrian Chengjiang and Middle Cambrian Burgess-type biotas are the largest. The Kaili Biota, from the earliest Middle Cambrian of Guizhou, China, contains representatives of 110 metazoan genera belonging to 10 phyla. It contains many well-persevered soft-bodied specimens. This Chinese biota has become the third most taxonomically diverse Burgess Shale-type fauna. Because the Kaili Biota formed in an outer-shelf environment, its main faunal character is large numbers of eocrinoids and planktoic trilobites. The Kaili is younger than the Chengjiang Biota but older than the Canadian Burgess Shale Biota; it shares 30 genera with the Chengjiang and 38 genera with the Burgess Biota. The Kaili Biota displays a taphonomic window to the diversification and evolution of marine offshore organisms covering 5.13 million years between the Early and Middle Cambrian.

Guanling Biota: A Marker of Triassic Biotic Recovery from the end-Permian Extinction in the Ancient Guizhou Sea

After a slow recovery from the end-Permian extinction during the Early Triassic and rapid radiation in the Middle Triassic, evolution of organisms reached a new peak phase in the Late Triassic. The Guanling Biota from the Wayao Member （conodont Paragondolella polygnathiformis Zone）, Falang Formation, Xinpu, Guanling County, Guizhou Province, southwestern China corresponds to this peak that marks the full recovery from the end-Permian extinction of marine ecosystems. The biota is of high diversity, containing well preserved and completely articulated skeletons of vertebrates comprising marine reptiles, fishes, and invertebrates including crinoids, ammonites, bivalves, and other fossils, and is one of the best examples of marine ecosystem records in life history. The fossil marine reptiles and crinoids are most significant in this biota, especially the marine reptiles, which provide an important link between the Triassic Pacific and Tethys, and between Triassic basal forms and the Jurassic-Cretaceous marine top predators. The most remarkable fossils are the large completely articulated ichthyosaur skeletons up to and more than 10 m, and the first recorded thalattosaurs and placodonts in China. Following our review, of the 17 named reptilian taxa the eight listed here are considered to be valid： three ichthyosaurs （Qianichthyosaurus zhoui Li, 1999; Guizhouichthyosaurus tangae Cao and Luo in Yin et al., 2000, Guanlingsaurus liangae Yin in Yin et al., 2000）, three thalattosaurs （Anshunsaurus huangguoshuensis Liu, 1999, Xinpusaurus suni Yin in Yin et al., 2000, Xinpusaurus kohi Jiang et al., 2004）, and two placodonts （Sinocyamodus xinpuensis Li, 2000, Psephochelys polyosteoderma Li and Rieppel, 2002）. Mixosaurus guanlingensis Cao in Yin et al., 2000 might be a junior synonym of Qianichthyosaurus zhoui Li, 1999, and Cymbospondylus asiaticus Li and You, 2002 and Panjiangsaurus epicharis Chen and Cheng, 2003 might be junior synonyms of Guizhouichthyosaurus tangae Cao and Luo in Yin et al., 2000. It needs to re-describe the holotypes after a complete preparation for clarifying the taxonomic status of Typicusichthyosaurus tsaihuae Yu in Yin et al., 2000, Xinpusaurus bamaolinensis Cheng, 2003, Neosinosaurus hoangi （Zhou in Yin et al., 2000）, Wayaosaurus geei Zhou in Yin et al., 2000, Wayaosaurus bellus Zhou in Yin et al., 2000 and Placochelys ？ minutus Yin and Luo in Yin et al., 2000.

New Localities and Palaeoscolecid Worms from the Cambrian(Stage 4,Series 2)Guanshan Biota in Kunming,Yunnan,South China

The Guanshan Biota from the Cambrian Stage 4 Wulongqing Formation is a typical Burgess-shale type Lagerst？tte that had witnessed the Cambrian explosion. Here we report two new localities of the Guanshan Biota, which is located at Baimei village, south of Kunming and Xinglong village, Wuding County, Yunnan Province respectively. Both localities produce soft-body fossils and several new taxa, e.g. a new species of palaeoscolecidans （Palaeoscolex xinglongensis sp. nov.） reported herein. The comparative study of the new species with similar form not only indicates that there is a diversification of palaeoscolecid species in Guanshan Biota, but also strengthens the ties between the older Chengjiang Biota and the younger Kaili Biota （and also the coeval Burgess Shale community）. Three paleoecological features, including high diversity, little disparity and richness of palaeoscolecid worms, are summarized as a case study to represent the differences between Guanshan and Chengjiang Biota.

First report on Guanshan Biota(Cambrian Stage 4) at the stratotype area of Wulongqing Formation in Malong County, Eastern Yunnan, China

Exceptionally preserved fossils,such as those from Cambrian Burgess Shale-type fossil-Lagerstatten are critical because of their unique contributions to knowledge of the phylogenetic radiation and palaeoecological expansion of metazoans during the Cambrian explosion.Critically,these deposits provide information that is usually unobtainable from shelly and skeletonized fossils alone.The Guanshan Biota(Cambrian Series 2,Stage 4)in the Yunnan Province of South China,has produced abundant and diverse,exquisitely preserved fossils that often retain soft tissues and organs.To date,most fossils from the Guanshan Biota have been collected from localities such as Gaoloufang and Gangtoucun,which have become inaccessible due to new urban expansions and constructions of residential buildings.Here we present the first report of soft bodied fossils from a new section at Kanfuqing,close to the Wulongqing village in Malong County,approximately 3 km east of the Wulongqing Formation stratotype section.Fossils retain soft morphology,and include brachiopods with delicate marginal setae,priapulids with well-preserved sclerites and vetulicolians with entire sections of body.In addition,this fauna includes rare occurrences of trilobites preserved with soft tissues replicated as pyrite pseudomorphs after weathering.This discovery represents an important palaeogeographical extension of soft-bodied fossils of the Guanshan fauna to the east of the Xiaojiang Fault(related to Tsinning tectonic movements ca.700 Ma).The fauna from the new Kanfuqing section is similar to that reported from the Wulongqing Formation west of the Xiaojiang Fault,and thus has significant implications for early Cambrian palaeogeography,faunal successions and palaeoenvironments of eastern Yunnan.

Neogene Paleoseismic Events and the Shanwang Biota's Burial in the Linqu Area,Shandong Province,China

Several paleoseismic events are recorded in the Neogene Linqu Group, exposed in the Linqu area, Shandong Province, China. The events were interpreted on the basis of fleldwork and laboratory analysis, which showed the presence of seismites with plastically deformed soft-sediment deformation structures in the Shanwang Formation, and of seismic volcanic rocks in the Yaoshan Formation which show brittle deformation. The earthquake-triggered soft-sediment deformations in the seismites include load structures, ball-and-pillow structures, flame structures, piUow-like beds, boudinage structures, slump folds, syn-depositional faults, veins of liquefied sand, and dikes of liquefied sandy lime-mud. The seismic activity is also reflected in what might be called ＇brittle seismites＇; these originated when, under the influence of seismic vibrations, semi-consolidated conglomerate was shattered. Moreover, volcanic activity is related to intense earthquakes that affected basalts intercalated with sand layers; these successions are known as ＇seismic volcanic rocks＇, which are characterized by veins of liquefied sand intruding the basalts. AH above traces of paleoseismic activity were left from one single time span of 4 Ma with active seismicity that took place 14-10 Ma. This time span is known as ＇the Linqu Neogene Paleoseismic Active Period＇, which is divided into four paleoseismic episodes, which were responses to tectonic extension and basin rifting in this area. It even includes the activity of the Yishu Fault Zone during the Miocene and the Neogene. The ratios of trace elements in the seismites, w（La）/w（Sc） and w （La）/w（Th） are higher than the average value of the upper crust, but w（Th）/w（Sc） is lower; this is geochemical evidence for the basin rifting that resulted in a high sedimentation rate. The intense and frequent paleo-earthquakes are held responsible for the rapid burial of the Shanwang Biota. Secondary earthquake-induced processes （e.g. slumping of a lake shore and the strongly increased lacustrine sedimentation rate） contributed to the rapid burial of the biota.