Volume 58,Issue 4,2019 Table of Contents

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  • 1  INJURED TRILOBITE EOREDLICHIA INTERMEDIA FROM THE EARLY CAMBRIAN CHENGJIANG BIOTA
    CHENG Mei-rong HAN Jian OU Qiang ZHANG Zhi-fei GUO Jin ZHANG Xing-liang
    2019, 58(4). DOI: 10.19800/j.cnki.aps.2019.04.001 CSTR:
    [Abstract](1085) [HTML](0) [PDF 124.26 M](3817)
    Abstract:
    Trilobites are common fossil animals in the Cambrian. The fossil record of their healed exoskeletons can provide important information on the competitive arms-race relationship between trilobite prey and their potential predators in the Cambrian ecosystem. The early Cambrian Chengjiang biota from South China, well known for its exceptional fossil preservation, allows us to study the ancient ecological interactions in marine communities during the Cambrian explosion. However, there is no record of healed trilobites so far known from the Chengjiang biota. The trilobite Eoredlichia intermedia Lu, 1940, an index fossil of the second trilobite biozone in eastern Yunnan of China, is one of the commonest arthropods in the deposits. Of more than 2 000 specimens of E. intermedia in our collection, two adult specimens are revealed with deformities in the lateral margin of cephalon, genal spine, and the pleural region. We suggest that such injuries were most likely caused by unknown predators. The scalloped fractures or cracks on these two adult individuals were marginally thickened and smoothed at the edges, indicating obvious signs of healing. If interpreted exactly, these fossils lend some supports for the view that the victim Eoredlichia intermedia was capable of repairing their fractured exoskeletons from sub-lethal attack by unknown predators. Therefore, this research presents the thus-far oldest fossil record of trilobites with injuries and the first report of the trilobite exoskeleton with healed injuries from the Chengjiang biota, signifying an existing escalating arms race between durophagous predators and prey since Cambrian Stage 3.
    2  ON THE TAXONOMIC PROBLEM OF THE MUFUSHANIA TRILOBITES
    LIN Tian-rui
    2019, 58(4). DOI: 10.19800/j.cnki.aps.2019.04.002 CSTR:
    [Abstract](954) [HTML](0) [PDF 10.70 M](14511)
    Abstract:
    In accordance with the cranidia structures, the method of “Q-mode cluster analysis” used in the present paper for a taxonomic study of 18 species of the genus Mufushania, that was established or adopted by Lin Tian-rui (1965), Li Shan-ji (1978),Zhang Wen-tang et al. (1980), Sun Zhen-hua (1982), Zhou Zhi-qiang et al. (1982), Guo Hong-jun et al. (1996), Yuan Jin-liang and Li Yue (1999), Peng Shan-chi et al. (2001), Yuan Jin-liang et al. (2002). The statistical measurement of similarity is incremental sum of error squares (ΔE). The use of the variability by the author is the eight quantitative ratio values (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). These data show that M. shalangensis Zhang and Zhou in Zhang et al. 1980(5), M. angustilimbata Zhang and Zhou in Zhang et al.,1980 (7) and M. kailiensis (Yuan in Yuan et al., 2002) (13) species should not be a member of the Mufushania, not belonging to species of Mufushania. Finally, through the application of combined cluster analysis with traditional qualitative analysis in the study of fifteen species of Mufushania trilobites in this paper, of which M. changi Lin, 1965 (2) is regarded as a junior synonym of the type species (1) and M. zhanjiaxiangensis Sun, 1982 (10) is regarded as a junior synonym of M. ezhongensis Sun, 1982 (9), too, the other thirteen species of Mufushania in the opinion on lumping and transferring the studied species is proposed (see table 3).
    3  FRAMBOIDAL PYRITES IN THALASSINOIDES BACAE FROM THE ZHANGXIA FORMATION (CAMBRIAN MIAOLINGIAN SERIES) IN HENAN PROVINCE: GENESIS AND ITS ECOLOGICAL SIGNIFICANCE
    LI Kai-nan WANG Min QI Yong-an YANG Wen-tao ZHONG Cong-cong
    2019, 58(4). DOI: 10.19800/j.cnki.aps.2019.04.003 CSTR:
    [Abstract](442) [HTML](0) [PDF 81.40 M](2244)
    Abstract:
    Amounts of Thalassinoides bacae are preserved in micrite of the Zhangxia Formation in western Henan Province. In order to illuminate the element distribution and microscopic characteristics of Thalassinoides bacae, they are observed under micro-X-ray fluorescence spectrometer and scanning electron microscope (SEM) and analyzed by energy dispersive X-ray spectroscopy (EDS). The results show that: the elements in the lining are similar with that in the surrounding sediments, Fe and Mg are enriched in the diagenetic halo indicating that this part was preferentially flowed by the dolomitizing fluids and was dolomitized; Fe is also enriched in the boundary between fill and lining; abundant of framboidal pyrites (microcrystalline pyrites occur as octahedrons, pyritohedrons, cubes, spheres and irregular shapes), single idiomorphic crystals and iron oxides are only found in the boundary of fill and lining. The characters of the framboidal pyrites show that they are likely to be related to biogenesis, and they are an important evidence of the trace maker growing microbes for supply nutrient materials to live in the restricted marine, indicating the behavior evolution and the ecological space radiation in the middle Cambrian period.
    4  THE TRILOBITE BIOSTRATIGRAPHY OF THE BALANG FORMATION, DUYUNIAN STAGE, QIANDONG SERIES (CAMBRIAN SERIES 2, STAGE 4) FROM HUANGLIAN AREA IN SONGTAO COUNTY, GUIZHOU PROVINCE AND ITS CORRELATION SIGNIFICANCE
    WU Meng-yin,ZHAO Yuan-long,YANG Xing-lian,CHEN Zheng-peng
    2019, 58(4). DOI: 10.19800/j.cnki.aps.2019.04.004 CSTR:
    [Abstract](429) [HTML](0) [PDF 34.79 M](2103)
    Abstract:
    The Huanglian section located in the west of Huanglian village, Songtao County, Guizhou Province was the basic section for establishing the Nangaoan Stage and the Duyunian Stage by Peng Shanchi et al. in 2000. We restudy some materials collected from the Balang Formtion of the Huanglian section eighteen years ago. The Balang Formtion in Huanglian section consists of dark gray and grayish black silty mudstone. Its thickness is 417.8 m. The lithology of the Balang Formation in Huanglian is similar to that of the Balang Formation in east Guizhou and west Hunan. The trilobites are very abundant except the lower part from the base boundary to 38 m and two trilobite zones are defined according to the collected data: Oryctocarella duyunensis Zone, occupies lower part of the Balang Formation from 38 m to 83 m above the base; Arthricocephlus chauveaui Zone, occupies middle-upper part of the Balang Formation from 83 m to the upper unit, the “Tsinghsutung Formation”, including Arthricocephlus chauveaui, A. xinzhaiheensis, Oryctocarella duyunensis, O. sibirica, O. balangensis, Duyunaspis duyunensis, Changaspis elongata and Redlichia (Pteroredlichia) murakamii. The trilobite biostratigraphy of the Balang Formation at the Huanglian section is exactly the same as that of the Balang Formation at the Jiaobang section which is the potential Global standard stratotype-section and point (GSSP) for the base of the Cambrian Stage 4 and can correlate with the Henson Gletscher Formation in Freachen land and Peary land of North Greenland. The Huanglian section is a good supplementary section of the Jiaobang section for the Palang Formation.
    5  LOWER ORDOVICIAN GRAPTOLITES FROM THE DACHENGSI FORMATION IN HANYUAN-YINGJING AREA, WESTERN SICHUAN, CHINA
    ZHANG Di.) YU Qian.) FENG Xin-tao.) WANG Xiao-fei.) ZHAO An-kun.) LEI Zi-hui.) ZHOU Ye-xin.)
    2019, 58(4). DOI: 10.19800/j.cnki.aps.2019.04.005 CSTR:
    [Abstract](309) [HTML](0) [PDF 22.70 M](2130)
    Abstract:
    A graptolite fauna of the Baltogratus deflexus Biozone (Dachengsi Formation, Lower Ordovician) was obtained recently from the Well-CYD2 cores from Hanyuan-Yingjing area, western Sichuan. Five species belonging to two genera of graptolites have been identified and described in the present paper. They include Baltograptus deflexus (Elles and Wood, 1901), B. enshiensis (Ni, 1979), B. scanicus (Tjernvik, 1960), B. stratus (Chen and Xia, 1979), and Corymbograptus v-fractus minor (Li, 1979). The terminologies for the development types of the proximal end of the turbaria in the present material are after Malatz (1994, 2018). The validity of the genus Norvegiograptus Li, 2014 is discussed herein. The low diversity of the B. deflexus fauna in the Hanyuan-Yingjing area might be due to the limited specimens obtained from drilling core. The B. deflexus Biozone marks the top of the Dachengsi Formation in the studied area. It is overlain directly by the Lower Permian Liangshan Formation. This disconformity extends eastwards to the Emeishan area of SW Sichuan, indicating a regional, long-term erosion.
    6  Early-Middle Ordovician graptolite Phyllograptus from the Yiyang area, Hunan Province
    LI Li-xia.),FENG Hong-zhen) WANG Wen-hui)
    2019, 58(4). DOI: 10.19800/j.cnki.aps.2019.04.006 CSTR:
    [Abstract](367) [HTML](0) [PDF 18.92 M](2062)
    Abstract:
    Five species of Early-Middle Ordovician graptolite genus Phyllograptus are reported from the Nanba section in the Yiyang area, Hunan Province, South China, including Phyllograptus anna Hall, 1865, P. anna longus Ruedemann, 1947, P. anna ultimus Ruedemann, 1904, P. claviger Monsen, 1937, and P. claviger acuminatus (Chen and Xia, 1979). This study indicates that Phyllograptus is distributed in the interval from the upper Floian to the middle Dapingian. As the early indicator of graptolite with scandent stipes, this genus first appeared at the end of the first phase (Corymbograptus deflexus Biozone) of graptolite diversification during the Early-Middle Ordovician, and became increasingly dominant in the Dichograptid fauna during the second phase (Pseudophyllograptus angustifolius elongatus Biozone-Isograptus victoriae divergens Biozone), directly affected the replacement between different groups within the Dichograptid fauna, implying that the evolution within the Dichograptid fauna significantly contributed to the graptolite diversification during the Early-Middle Ordovician.
    7  CHARACTERISTICS OF PALEOENVIRONMENTAL EVOLUTION AND ICHNOCOENOSIS IN THE 55 SUBMEMBER OF THE MIDDLE ORDOVICIAN MAJIAGOU FORMATION, XINGXIAN, SHANXI
    LIU Meng-yao ),SHI Yun-he ),DONG Guo-dong ),WANG Yan-qing ),ZHANG Xin ),SU Zhong-tang ) ZHANG Li-jun )
    2019, 58(4). DOI: 10.19800/j.cnki.aps.2019.04.007 CSTR:
    [Abstract](304) [HTML](0) [PDF 24.43 M](2172)
    Abstract:
    A large number of invertebrate fossils are preserved in the stratum of the 55 Submember of Ordovician Majiagou Formation in the Guanjiaya section, eastern margin of Ordos Basin, identified types of domichnia, fodinichnia and grazing traces, 8 ichnogenera and 15 ichnospecies, Arenicolites isp., Cylindricum isp., Helminthopsis abeli, Helminthopsis isp. 1, Helminthopsis isp. 2, Lorenzinia isp. , Planolites isp., Planolites beverleyensis, Planolites montanus, Teichichnus rectus, Thalassinoides isp.1, Thalassinoides isp.2, Thalassinoides isp.3, Thalassinoides isp.4. Three trace fossil assemblages under different sedimentary environments have been recognized as follows: 1) Helminthopsis-Planolites trace fossil assemblages mainly consists of fodinichnia and domichnia from intertidal and subtidal zone; 2) Thalassinoides-Teichichnus trace fossil assemblages, its trace fossils are relatively simple mainly consists of fodinichnia from intertidal and supratidal zone; 3) Thalassinoides-Helminthopsis trace fossil assemblages from intertidal zone. Based on the distribution characteristics of the trace fossil assemblages, the sedimentary environment model of the submember 55 of Middle Ordovician Majiagou Formation in the eastern margin of Ordos Basin was proposed.
    8  Cladistic analysis of Waagenophyllum(Waagenophyllum) in China
    WANG Xiao-juan,LIN Wei
    2019, 58(4). DOI: 10.19800/j.cnki.aps.2019.04.008 CSTR:
    [Abstract](404) [HTML](0) [PDF 14.86 M](2057)
    Abstract:
    A preliminary cladistic analysis of some species of the subgenus Waagenophyllum (Waagenophyllum) in China is presented to understand their evolutionary relationships. Parsimony analysis was conducted on PAUP4.0b10, with the Waagenophyllum (Liangshanophyllum) wengchengense as an outgroup. The result provides a hypothesis of relationship for the selected species within the subgenus, and suggests that the view that Liangshanophyllum is a genus is worth discussing.
    9  THE WEATHERING MECHANISM OF SURROUNDING ROCKS IN HAMIPTERUS FOSSIL
    LI Ying LUO Wu-gan YANG Yi-min WANG Xiao-lin
    2019, 58(4). DOI: 10.19800/j.cnki.aps.2019.04.009 CSTR:
    [Abstract](724) [HTML](0) [PDF 16.78 M](14022)
    Abstract:
    The value of the discoveries of Hamipterus tianshanensis and their 3D eggs fossils?are of?great importance.?These fossils preserved in Beijing for several years, the surrounding rocks have been powdering and flaking, which seriously endanger the safety to fossils. This paper intends to use XRF and other methods to detect surrounding rock to explore its corrosion mechanism. The analysis shows that the surrounding rock of fossils is composed of sandstone with boulder clay, which contains some clay minerals such as montmorillonite. The?sandstone?with?calcareous?and?salt?cementation contains large amounts of soluble ions such as Cl-, NO3-, Na+ and Mg2+. The mechanism of the deterioration is as followed, when the humidity changes, the soluble salt also generates large crystal pressure, as well as the expansion of clay minerals produces huge pressing force, leading the surrounding rocks to powder and flake gradually. The?solution?of?salt?existing?as the cement results in the escape and?migration of?particles, which?is?an important reason for fossil deterioration.?Based on the above understanding, this paper also gives suggestions about the protection of fossils.
    10  Pattern of Leaf epidermal characters in Cycas and its significance of taxonomy and paleoecology
    LIANG Shui-qing.) SU Tao) HU Jin-jin) LI Nan)
    2019, 58(4). DOI: 10.19800/j.cnki.aps.2019.04.010 CSTR:
    [Abstract](648) [HTML](0) [PDF 20.65 M](2110)
    Abstract:
    Cycas is a group of gymnosperms with a long evolutionary history. This study is to investigate the relationship between the leaf epidermal morphology of Cycas and the environment to provide fundamental evidences for palaeoenvironmental reconstructions. In this study, we compared the epidermal characters and stomatal parameters of 27 Cycas species in the garden culturing environment and then analyzed the phylogenetic signals of stomatal parameters. The present study mainly found that: 1) the epidermal characters of Cycas were generally conservative within species and it has taxonomic significance. These 27 Cycas species could be classified into four types according to their epidermal cells pattern and other characters of stomata apparatus. The above result indicated that leaf epidermal characters can be used for identifying extant or fossil Cycas species; 2) Four leaf epidermal types were related to their natural habitats; therefore, the combination of different leaf epidermal characters may be a good indicator for palaeoenvironment; 3) Species included in this study varied in stomatal parameters despite they grew under the same cultivating environment. The variation of Stomatal Index (SI) within Cycas was associated with phylogeny: the SI presented with significant phylogenetic signal, whereas the phylogenetic signals of other stomatal parameters were weak. This study indicated that, when using the stomatal density/index method to reconstruct palaeo-atmospheric CO2 concentration, it should be cautiously considered to choose nearest living species as proxies, especially these with similar morphology, habitat and close phylogenetic relationship. In addition, the relationship between stomatal parameters and CO2 partial pressure (pCO2) should be clarified within a genus so as to improve the effectiveness of this method.
    11  The Morphological Characteristics of Fan-Shaped Phytolith of Rice Based on Large Sample
    TANG Xian-gan .) XIE Jin-shui ) CHEN Da-zhou ) LIU Guang-rong )
    2019, 58(4). DOI: 10.19800/j.cnki.aps.2019.04.011 CSTR:
    [Abstract](484) [HTML](0) [PDF 10.18 M](2038)
    Abstract:
    Bulliform phytoliths plays an important role in researching rice origins. However, its application was limited in the early studies of rice planting culture due to an uncertainty in distinguishing the bulliform phytoliths between wild rice and cultivated rice. Through the investigation and statistical analysis based on the large sample data, the authors found that the size of the bulliform phytoliths of the common wild rice was larger than that of the cultivated rice, and that japonica rice was larger than indica rice; the B/A value of common wild rice was significantly higher than that of cultivated rice while the Japonica rice was significantly lower than that of indica rice; the length (VL) and width (HL) of bulliform phytoliths were positively correlated to each other, and the investigated bulliform phytoliths was mainly distributed in the range of VL < 41 μm & HL < 39 μm and VL > 41 μm & HL >39 μm. In the identification of rice site, if most B/A of the rice bulliform phytoliths was less than or equal to 1.20, it was likely to be japonica rice; if B/A was greater than 1.2, we can distinguish wild rice from indica rice according to the size of bulliform phytoliths, it might be indica rice if most of bulliform phytoliths in the range of VL < 41 μm & HL < 39 μm, or it might be wild rice if that’s in the range of VL > 41 μm & HL > 39 μm.

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