Volume 57,Issue 2,2018 Table of Contents

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  • 1  A REVIEW OF PROTEROZOIC ORGANIC-WALLED MICROFOSSILS-TAPPANIA AND ITS BIOLOGIC AND GEOLOGIC IMPLICATIONS
    YIN Lei-ming NIU Chang-tai KONG Fan-fan
    2018, 57(2):147-156. DOI: 10.19800/j.cnki.aps.2018.02.001 CSTR:
    [Abstract](250) [HTML](0) [PDF 807.12 K](1623)
    Abstract:
    Organic-walled microfossil-Tappania was firstly described and reported from the Beidajian Formation of the Ruyang Group in the Yongji area,Shanxi Province,North China,which was deposited during the period of late Paleoproterozoic-early Mesoproterozoic in the period from about 1 700—1 400 Ma.So far,Tappania has been widely found in roughly coeval sediments distributed in India,Australia,Siberia,America,etc.Certainly,it becomes significant microfossil evidence of stratigraphic correlation in the geological time.Furthermore,it is recognized as a complex eukaryotic microfossil by possessing features like dynamic cytoskeleton and membrane system,and forms the evidence of indicating the divergence of stem group eukaryotes during the geological period. The paper is aimed to understand morphological features and biological affinity of Tappania and to discuss its ecological environment and relative geological background.In combination with paleogeographic and geochemical research data,it could be suggested that the appearance of Tappania was relevant with important geological events that happened in the geological interval. Though cyanobacteria and unicellular algae dominated in late Paleoproterozoic-early Neoproterozoic marine basins,some multicellular organisms with function of osmotrophy were already actively reproductive in the suitable ecological niche.
    2  HIGH-RESOLUTION TOMOGRAPHY OF MILLIMETER-TO CENTIMETER-SIZED FOSSILS USING THREE-DIMENSIONAL X-RAY MICROSCOPY
    WU Su-ping YIN Zong-jun SUN Wei-chen ZHAO Duo-duo WU Ruo-lin
    2018, 57(2):157-167. DOI: 10.19800/j.cnki.aps.2018.02.002 CSTR:
    [Abstract](336) [HTML](0) [PDF 1.17 M](1579)
    Abstract:
    Among imaging techniques for paleontology,computed tomography(CT)is an unparallel one when comparing to conventional optical and electronic imaging methods, because it can reconstruct both external and internal structures of fossils without destroying them.As a powerful non-destructive three-dimensional imaging technique,CT is widely used in paleontological community recent years. Here,we introduce a new micro-CT technique,three-dimensional X-ray microscopy(3 D-XRM). Different from the conventional micro-CT characterized by geometric magnification and absorption contrast,this new technique has four merits:(1)it can provide micron to sub-micron spatial resolution due to a CCD-based optical system;(2)it can reconstruct centimeter-to millimeter-sized specimens with lowZ materials using propagation phase contrast imaging mode;(3)based on the new architecture and specific algorithms,the system has a"zoom-in function" which can precisely reconstruct any"region of interests(ROIs)"located inside a comparatively large specimen with micron to submicron resolution;(4)contrary to conventional micro-CT,this new system can reconstruct small size high aspect-ratio flat specimens(width <10 cm) and tubular microfossils with high resolution.Owing to the merits,3 D-XRM can provide high quality reconstructions for millimeterto centimeter-sized fossils with three-dimensional preservation.
    3  PRELIMINARY STUDY ON PALEOECOLOGICAL CHARACTERISTICS OF BALANG FAUNA(STAGE 4,CAMBRIAN)IN JIANHE,EASTERN GUIZHOU PROVINCE,CHINA
    LIU Shuai PENG Jin WEN Rong-qin WANG Qiu-jun DU Guang-ying
    2018, 57(2):168-180. DOI: 10.19800/j.cnki.aps.2018.02.003 CSTR:
    [Abstract](270) [HTML](0) [PDF 1.30 M](1568)
    Abstract:
    The Lazizhai section of the Balang Formatiom near Lazhizhai village,Jianhe,Guizhou,China is the most prolific locality of the Balang Fauna.Body fossil remains from this locality have been recognized in at least eight major groups of organisms, including sponges, chancelloriids,cnidarians, "worms", brachiopods, hyoliths,arthropods,echinoderms and"algae",a total of 63 genera and 80 species.Here,based on the fossil assemblage from the Lower Fossil Bed of the Laizizhai section of the Balang Formation(Cambrian Stage 4)and their paleoecological groups and taphonomic groups and sedimentary characters,the ecosystem of the Balang Fauna is recognized.Its ecological groups include the benthic,nektonbenthic and nektonic to planktonic organisms.The characters of ecological groups and sedimentary evidences of the Lower Fossil Bed suggest that the Balang Fauna lived in an open sea basin north of the equator,where a deep shelf of rapid depositional event often developed.It is a biotope to have oxygenated and normal salinity,and photic environment,but,to be an aerobic to dysaerobic on the seabed.The ecosystem of the Balang Fauna includes carnivores(predators and scavengers), deposit-feeders and filter-feeders.Analysis of the predator-prey systems reveals a complex food web with a trophic structure containing several trophic levels, with obvious pyramidal nutritional structure.
    4  DUYUNASPIS ZHANG AND QIANIN ZHOU ET AL.,1977(TRILOBITA)FROM THE “TSINGHSUTUNG FORMATION”(SERIES 2,STAGE 4)OF EASTERN GUIZHOU,SOUTH CHINA
    CHEN Zheng-peng ZHAO Yuan-long YANG Xing-lian WANG Ming-kun
    2018, 57(2):181-191. DOI: 10.19800/j.cnki.aps.2018.02.004 CSTR:
    [Abstract](218) [HTML](0) [PDF 1.64 M](1530)
    Abstract:
    A new oryctocephalid species Duyunaspis jianheensis sp. nov. is described from the Cambrian "Tsinghsutung Formation"(Series 2,Stage 4)at Songshan,Jianhe,eastern Guizhou,South China,revealing that the genus Duyunaspis ranges up from the slightly older Balang Formation(Cambrian Stage 4).The Balang Formation is widely exposed in the border area between eastern Guizhou and western Hunan and is dominated by oryctocephalids including Duyunaspis. Duyunaspis jianheensis sp.nov.is characterized by having aglabella that is more or less expanded at its mid-lengtha,aproparian suture,and a thorax with 10 segments in holaspids. Detailed exploration of ontogeny of D.jianheensis sp.nov.shows that the new species seems to be a descendent of Duyunaspis duyunensis of the Balang Formation.
    5  ON THE TAXONOMIC PROBLEM OF THE ABADIELLATRILOBITES
    LIN Tian-rui
    2018, 57(2):192-201. DOI: 10.19800/j.cnki.aps.2018.02.005 CSTR:
    [Abstract](254) [HTML](0) [PDF 467.11 K](1472)
    Abstract:
    In the present paper,the method of"Q-mode cluster analysis"is used in a taxonomic study of 18 cranidia belonging to abadiellid trilobite genera(subgenera)of traditional early Cambrian age.The statistical measurement of similarity is incremental sum of error squares(ΔE). The author uses the variables in the eight quantitative ratio form(see table 1).The resemblance relation matrices of all specimens are formed through calculation of the increments of sum of error squares between those specimens(see table 2).Finally,the two-dimensional dendrogram is drawn by stepwise calculation(see text-fig.2).The dendrogram(text-fig.2)shows nine specific groups by the association line having a value of increments of sum of error squares 0.1.They correspond as follows:Group A(= Abadiella huoi)—containing 5 species:Parabadiella huoi Zhang,1966(1),Parabadiella shaanxiensis Zhang and Lin,1980(7),Parabadiella obscurata Zhang and Lin,1980(9),Parabadiella(Danangouia)quadrata Chen,1985(3),Parabadiella tenuilimbata Zhang and Lin,1980(8).Group B(=Abadiella elegans)—containing 2 species:Guangyuanaspis elegans Lee,1978(14),Guangyuanaspis fandianensis Zhang and Lin,1980(15).Group C(= Abadiella longmenshanensis)—containing only 1 species: Parabadiella longmenshanensis Lee,1978(11).Group D(= Abadiella yunnanensis)—containing 2 species:Parabadiella yunnanensis Luo,1981(17),Parabadiella zhongliangsiensis Chen,1985(6).Group E(=Abadiella elevata)—containing 2 species:Parabadiella elevata Lee,1978(12),Parabadiella conica Luo,1981(16).Group F(= Abadiella hanzhongensis)—containing 3 species:Parabadiella(Danangouia)transversa Chen, 1985(2), Parabadiella hanzhongensis Chen, 1985(4), Parabadiella nanzhengensis Chen,1985(5).Group G(= Abadiella modaoyaensis)—containing only 1 species: Guangyuanaspis modaoyaensis Chang and Qian,1974(13).Group H(= Abadiella shaanxiensis)—containing only 1 species too:Guangyuanaspis shaanxiensis Zhang and Lin,1980(10).Group I(= Abadiella wudingensis)—containing also only 1 species:Guangyuanaspis wudingensis Zhang and Lin,1980(18).Through the application of combined cluster analysis with traditional qualitative analysis in the study of 18 species of abadiellid trilobites in this paper,the opinion on lumping and transferring the studied species is proposed(see table 3).
    6  EXPLORATION OF CAMBRIAN FOSSILS BY MICRO X-RAY FLUORESCENCE SPECTROMETER
    LIANG Yue ZHANG Zhi-fei
    2018, 57(2):202-211. DOI: 10.19800/j.cnki.aps.2018.02.006 CSTR:
    [Abstract](231) [HTML](0) [PDF 1.64 M](1695)
    Abstract:
    With the increasing emphasis on basic research in China,great achievements have been made in paleontology,especially in the study of early life and the Cambrian explosion.Research facilities have been improved,such as Scanning Electron Microscopy(SEM)and X-ray microtomography Scanner(Micro-CT)have been used extensively in researches. Micro X-ray Fluorescence(μ-XRF) is a non-destructive technique used to study those exceptionally preserved brachiopod fossils from the lower Cambrian lagerst?tten in South China.Here we present the first μ-XRF mapping of exquisite fossils with soft-part preservation recovered from the Wulongqing Formation of two important localities,the Jianshan section and the Gaoloufang section in eastern Yunnan.Due to the Penetrative capabilities of this technique,some fine details,such as lophophore, which is invisible under optical microscope, can be observed. Semiquantitative analysis of chemical elements(Na-U)and compounds in the matrix also reveals subtle differences in sedimentary mineral characteristics between the Chengjiang and the Guanshan deposits.μ-XRF does not require any sample preparation before testing and scanning,which is a useful and non-destructive technique for surface scanning of specimens,and micro-area analysis at different scales.μ-XRF is providing critical new information for comparative studies of the preservation and sedimentary environment of fauna in critical deposits such as the Chengjiang and the Guanshan deposits.
    7  TAPHONOMIC CHARACTERISTICS OF A PERMIAN CALCISPONGE REEF IN LICHUAN,HUBEI PROVINCE AND ITS PALEOENVIRONMENTAL SIGNIFICANCE
    LI Yang WU Ya-sheng JIANG Hong-xia
    2018, 57(2):212-227. DOI: 10.19800/j.cnki.aps.2018.02.007 CSTR:
    [Abstract](211) [HTML](0) [PDF 2.58 M](1611)
    Abstract:
    The calcisponge reefs in Lichuan, western Hubei Province is analyzed for reef-building organism composition, preservation status of calcisponges,size of calcisponges,contents of Archaeolithoporellaencrustations and micrites.A total of 17 genera of calcisponges and one genus of hydrozoan are found in the reef-core facies(Layers8-10).The 8 th to 9 th layers are mainly composed of toppled sponges and have little content of Archaeolithoporellaencrustations,while the 10 th layer has more contents of erect calcisponges and Archaeolithoporella encrustations. The average diameters of the calcisponges in the 8 th to 10 th layers increase a little,but the content of micrites gradually declines.Thus we infer that the reefbuilding organisms in the 8 th to 9 th layers formed under less strong hydrodynamic conditions,and were mostly toppled.For the 10 th layer,the hydrodynamic conditions are stronger,but,the Archaeolithoporella encrustations enhanced the anti-wave capability of the reef-building organisms,and they were preserved in erect positions.
    8  A NEW TYPE OF LACUSTRINE ICHNOFOSSILS FROM THE LOWER JURASSIC ZILIUJING FORMATION IN WANZHOU OF CHONGQING AND ITS PALEOENVIRONMENTAL SIGNIFICANCES
    ZHANG Feng ZHOU Yu-xuan GE Run-qing HU Xu-feng XIONG Can YI Wan-cheng
    2018, 57(2):228-236. DOI: 10.19800/j.cnki.aps.2018.02.008 CSTR:
    [Abstract](214) [HTML](0) [PDF 877.62 K](1511)
    Abstract:
    The Early Jurassic trace fossil is reported for the first time from the Da’nanzhai Member of the Lower Jurassic Ziliujing Formation in Tiefeng Mountain of Wanzhou,Chongqing.The newlyfound trace fossil is attributed to a new ichnospecies-Palaeophycus tiefengshanensis, which differs from other ichnospecies of Palaeophycus by its large size and nodular surface.Ichnofabric analysis shows that the bedding-plane bioturbation indice of the Palaeophycus ichnofabric is 5 representing the highest level of bioturtation,which suggests abundant food supply,high level of oxygen content and frequent animal activities.Based on the sedimentary facies changes of the Tiefengxiang section,the eastern region of Sichuan Basin experienced a similar environmental transformation of lake regression as the northern region of Sichuan Basin;the differences are the locally more habitable environment for ichnofauna in the studied area.
    9  LATE EOCENE BIVALVIA FOSSILS FROM THE SHUANGHE FORMATION IN JIANCHUAN BASIN,YUNNAN PROVINCE AND ITS GEOLOGICAL IMPLICATION
    ZHENG Guo-dong XU Ya-dong ZHANG Ke-xin QIN Qiong WU Jing WU Shun-bao
    2018, 57(2):237-248. DOI: 10.19800/j.cnki.aps.2018.02.009 CSTR:
    [Abstract](269) [HTML](0) [PDF 1.15 M](1579)
    Abstract:
    The southeastern Tibetan Plateau is considered as the main region where material escalation caused by the Tibetan Plateau,and it records the sedimentary,tectonic and biological events reflecting the uplift of the plateau.The Jianchuan Basin is one of the pull-apart basins in the southeastern Tibetan Plateau.The Shuanghe Formation is the main sedimentary strata of the Jianchuan Basin.The bivalve fossils from this formation lack detailed study,and only limited reports had been documented.In this paper,nine species and four genera of bivalves are found under systematic specification in the Jianchuan Basin.Four genera are Unio,Acuticosta,Cuneopsis and Anodota,and nine species include Acuticosta huoerguosica, Acuticosta sp., Acuticosta subimmutata,Cuticosta cf.chinensis,Acuticosta cf.cuspidata,Acuticosta cf.semiretiaria,Unio cf.subparallelus,Cuneopsis cf.subceltiformis and Anodontacf.subpiscinalis.All of the species belong to the family Unionidae. The genus Acuticostaand Cuneopsis are modern characteristic genera in eastern Asia,and A.chinensis and C.subceltiformis are present existing species south of the Yangtze River.However,A.chinensis was just reported in Xinjiang before.Based on ages of intrusive veins and standard Ostracoda fossil zones, the Shuanghe Formation could be constrained in late Eocene.Therefore,this paper not only provides new evidence of bivalve fossils in western Yunnan Province, but also reveals a subtropical fresh-water delta-front and prodelta environment of the Jianchuan Basin during the late Eocene.
    10  POLLEN/CHARCOAL RECORD OVER THE PAST 13 300YEARS FROM FUXIAN LAKE IN THE YUNNAN-GUIZHOU PLATEAU
    SUN Qi-fa SHEN Cai-ming WANG Min MENG Hong-wei ZHANG Hu-cai
    2018, 57(2):249-259. DOI: 10.19800/j.cnki.aps.2018.02.010 CSTR:
    [Abstract](366) [HTML](0) [PDF 910.00 K](1610)
    Abstract:
    Fuxian Lake is a well-known rift deep-water lake on the Yunnan-Guizhou Plateau. Its sediments contain abundant environmental information in its drainage region during geologic times.Pollen/charcoal analysis on 46 samples from a 900 cm core of this lake provides a history of vegetation,climate,and forest fire in its drainage region during the last 13 300 years.The results of pollen/charcoal analysis and principal component analysis on pollen data show five-stage vegetation succession,climate change,and forest fire:1)13 300-10 400 cal.a BP,the vegetation was dominated by pine forests,accompanied by dark coniferous forests and evergreen broadleaved forests,indicating cold and wet conditions;high frequent forest fires occurred in this stage,and especially more fires appeared as the humidity decreased in its late period.2)10 400-5 700 cal.a BP,the shrinkage in pine forest,expansion in evergreen broadleaved forest,and appearance of deciduous broadleaved forest indicated relatively warm and dry conditions;forest fires occurred frequently like the previous stage as climatic conditions became warm and dry at the early period of this stage until 9 500 cal.a BP,when relative humidity increased and forest fires decreased obviously.3)5 700-1 800 cal.a BP,the pine and evergreen broadleaved forests still dominated,but Liquidambar forests favoring warm and hot climate first appeared,showing warm and wet conditions;the occurrence frequency of forest fire was low.4)1 800-500 cal.a BP,the expansion of pine forest and the shrinkage of deciduous broadleaved forest with an increase of upland herbaceous plants indicated relatively cold and dry conditions;forest fires were more than the preceding stage but less than the first stage.5)500 cal.a BP to the present,the shrinkage of pine forests and a significant increase of upland herbs showed cool and dry conditions,and suggested increasing human activities.
    11  THE LATEST TILIA SOFTWARE:CHINESE MANUAL AND PRACTISE SKILLS
    SHU Jun-wu HUANG Xiao-zhong XU De-ke CHEN Wei SONG Bing CUI An-ning Eric Grimm
    2018, 57(2):260-272. DOI: 10.19800/j.cnki.aps.2018.02.011 CSTR:
    [Abstract](812) [HTML](0) [PDF 1.78 M](1879)
    Abstract:
    The Tilia software has been the most common professional computer programs used in the micropaleontology studies, particularly in the palynological field. This software primarily functions to make statistic analyses of counted microfossil data and then to create a stratigraphic diagram showing quantities of fossil taxa in each sample,that is, graphing fossil data. Tilia facilitates the zonation of fossil assemblages determined by the variation of taxa especially the dominant or constructive taxa in stratigraphic order to vividly show the evolution history of ecological communities in response to environmental changes. However,it is usually not easy for Chinese new users to learn and master it due to the facts that this software is performed in an English context with diverse and complex functions.Based on our experiences of Tilia performance,this paper aims at producing a Chinese manual for the latest Tilia 2.0.45 version to illustrate each step in detail with a simple example trying to make it easier to be understood in a Chinese context.Therefore,two versions are generated,i.e."basic-level"and"advanced-level". The former is made for beginners to practice Tilia basic skills to construct apercentage pollen diagram easily,while the latter is for skilled users to broaden its span especially in building apollen concentration diagram,apollen influx diagram, depth-chronology models,and exploring the Neotoma database.

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