Second Circular
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Landscape Analysis of Geographical Names in Hubei Province, China
Entropy 2014, 16, 6313-6337; doi:10.3390/e16126313 OPEN ACCESS entropy ISSN 1099-4300 www.mdpi.com/journal/entropy Article Landscape Analysis of Geographical Names in Hubei Province, China Xixi Chen 1, Tao Hu 1, Fu Ren 1,2,*, Deng Chen 1, Lan Li 1 and Nan Gao 1 1 School of Resource and Environment Science, Wuhan University, Luoyu Road 129, Wuhan 430079, China; E-Mails: [email protected] (X.C.); [email protected] (T.H.); [email protected] (D.C.); [email protected] (L.L.); [email protected] (N.G.) 2 Key Laboratory of Geographical Information System, Ministry of Education, Wuhan University, Luoyu Road 129, Wuhan 430079, China * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel: +86-27-87664557; Fax: +86-27-68778893. External Editor: Hwa-Lung Yu Received: 20 July 2014; in revised form: 31 October 2014 / Accepted: 26 November 2014 / Published: 1 December 2014 Abstract: Hubei Province is the hub of communications in central China, which directly determines its strategic position in the country’s development. Additionally, Hubei Province is well-known for its diverse landforms, including mountains, hills, mounds and plains. This area is called “The Province of Thousand Lakes” due to the abundance of water resources. Geographical names are exclusive names given to physical or anthropogenic geographic entities at specific spatial locations and are important signs by which humans understand natural and human activities. In this study, geographic information systems (GIS) technology is adopted to establish a geodatabase of geographical names with particular characteristics in Hubei Province and extract certain geomorphologic and environmental factors. -
Fulu Biota, a New Exceptionally Preserved Cambrian Fossil Assemblage from the Longha Formation in Southeastern Yunnan
Fulu biota, a new exceptionally preserved Cambrian fossil assemblage from the Longha Formation in southeastern Yunnan Shanchi Penga, b*, Xianfeng Yangc, Liu Yuc, Xuejin Zhua, b, Haijing Sund, Samuel Zamorae, Yingyan Maoa, and Yuchen Zhanga aState Key Laboratory of Palaeobiology and Stratigraphy (Chinese Academy of Sciences), Nanjing 210008, China bNanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China cYunnan Key Laboratory for Palaeobiology, Yunnan University, Kunming 650091, ChinaeNational Maritime Museum of China, Tianjin 300467, China dNational Maritime Museum of China, Tianjin 300467, China eInstituto Geológico y Minero de España, C/ Manuel Lasala, 44 - 9º B, 50006 Zaragoza, Spain Abstract A new exceptionally preserved Cambrian biota, with fossils belonging to multiple phyla, has recently been found from the middle part of the Longha Formation, near Fulu Village, southeastern Yunnan, South China, and is named the Fulu biota. Groups recovered so far include polymerid trilobites, agnostoids, large bivalved arthropods, bradoriid arthropods, echinoderms, brachiopods, priapulids (worms), hyoliths, macroscopic algae, and trace fossils. The arthropods dominate and are highly diverse with echinoderms second in diversity. The associated agnostoids provide a precise late Guzhangian Age (late Miaolingian Epoch) for the biota, indicating that the biota occurs stratigraphically about halfway between the occurrences of the Kaili and the Guole biotas of South China, from both of which the new Fulu biota differs significantly in faunal components. Guzhangian biotas preserving poorly mineralized tissues and complete echinoderms were previously unknown in Gondwana until now, providing a unique window into life at this critical time interval. Keywords: Fulu biota; Fossils of multiple phyla; Longha Formation; Guzhangian; Yunnan, South China 1. -
Supplemental Information
Supplemental information Table S1 Sample information for the 36 Bactrocera minax populations and 8 Bactrocera tsuneonis populations used in this study Species Collection site Code Latitude Longitude Accession number B. minax Shimen County, Changde SM 29.6536°N 111.0646°E MK121987 - City, Hunan Province MK122016 Hongjiang County, HJ 27.2104°N 109.7884°E MK122052 - Huaihua City, Hunan MK122111 Province 27.2208°N 109.7694°E MK122112 - MK122144 Jingzhou Miao and Dong JZ 26.6774°N 109.7341°E MK122145 - Autonomous County, MK122174 Huaihua City, Hunan Province Mayang Miao MY 27.8036°N 109.8247°E MK122175 - Autonomous County, MK122204 Huaihua City, Hunan Province Luodian county, Qiannan LD 25.3426°N 106.6638°E MK124218 - Buyi and Miao MK124245 Autonomous Prefecture, Guizhou Province Dongkou County, DK 27.0806°N 110.7209°E MK122205 - Shaoyang City, Hunan MK122234 Province Shaodong County, SD 27.2478°N 111.8964°E MK122235 - Shaoyang City, Hunan MK122264 Province 27.2056°N 111.8245°E MK122265 - MK122284 Xinning County, XN 26.4652°N 110.7256°E MK122022 - Shaoyang City,Hunan MK122051 Province 26.5387°N 110.7586°E MK122285 - MK122298 Baojing County, Xiangxi BJ 28.6154°N 109.4081°E MK122299 - Tujia and Miao MK122328 Autonomous Prefecture, Hunan Province 28.2802°N 109.4581°E MK122329 - MK122358 Guzhang County, GZ 28.6171°N 109.9508°E MK122359 - Xiangxi Tujia and Miao MK122388 Autonomous Prefecture, Hunan Province Luxi County, Xiangxi LX 28.2341°N 110.0571°E MK122389 - Tujia and Miao MK122407 Autonomous Prefecture, Hunan Province Yongshun County, YS 29.0023°N -
Your Paper's Title Starts Here
2020 International Conference on Economic Development and Education Innovation (EDEI 2020) An Analysis on the Evolutionary Path of Scattered Clusters of Commercial Space around Sea Ports Xiaoliang Xiong, Wan Shao, Huxiao Li Wuhan Technology And Business University, Wuhan, Hubei China [email protected] Keywords: Sea Ports, Commerce and Trade, Clusters, Evolution. Abstract: The scattered villages and town communities around sea ports are the window of modern Chinese economic changes, and the changes in the economic spatial structure of the country’s economic development reflect the spatial pattern of the country’s economic development, -promoting the channel optimization of the rural economy and the optimization of the spatial structure of urban clusters. Based on the evolution trajectory of the economic space of sea ports, this paper studies the characteristics and systems of the evolution of the economic space of tea ports, and analyses the dynamic mechanism of the evolution of the economic space of tea ports, trying to demonstrate the spatial optimization principles of the sea ports and clusters from the system and structure aspects. 1. Introduction Organizations of regional traffic function have a great influence on the formation and development of the town and city. In the ancient era of traffic shortage, clusters often become the first choice for the development of the market city. By virtue of the location advantage as the intersection of the river and sea, the port town has become an important local trade distribution centre with the flow of people and logistics, where all kinds of cultural collision and fusion give birth to the regional economic modernization transformation. -
This Article Was Published in an Elsevier Journal. the Attached Copy
This article was published in an Elsevier journal. The attached copy is furnished to the author for non-commercial research and education use, including for instruction at the author’s institution, sharing with colleagues and providing to institution administration. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Available online at www.sciencedirect.com Earth-Science Reviews 85 (2007) 47–81 www.elsevier.com/locate/earscirev A review of the Late Cambrian (Furongian) palaeogeography in the western Mediterranean region, NW Gondwana ⁎ J. Javier Álvaro a,b, , Annalisa Ferretti c, Cristina González-Gómez a, Enrico Serpagli d, M. Franco Tortello e, Marco Vecoli b, Daniel Vizcaïno f a Departamento Ciencias de la Tierra, Universidad de Zaragoza, 50009-Zaragoza, Spain b Laboratoire ‘Paléontologie et Paléogéographie du Paléozoïque’, UMR 8014 CNRS, Université de Lille I, 59655-Villeneuve d'Ascq, France c Dipartimento di Scienze della Terra, Università di Modena e Reggio Emilia, largo S. Eufemia 19, 41100-Modena, Italy d Dipartimento del Museo di Paleobiologia e dell'Orto Botanico, Università di Modena e Reggio Emilia, Via Università 4, 41100-Modena, Italy e Departamento Paleozoología Invertebrados, Museo de Ciencias Naturales, Paseo del Bosque s/n°, 1900-La Plata, Argentina f 7 rue Jean-Baptiste Chardin, Maquens, 11090-Carcassonne, France Received 18 December 2006; accepted 25 June 2007 Available online 6 August 2007 Abstract The Cambrian–Ordovician transition of the western Mediterranean region (NW Gondwana) is characterized by the record of major erosive unconformities with gaps that range from a chronostratigraphic stage to a series. -
Proposed Global Standard Stratotype-Section And
PROPOSED GLOBAL STANDARD STRATOTYPE-SECTION AND POINT FOR THE DRUMIAN STAGE (CAMBRIAN) Prepared for the International Subcommission on Cambrian Stratigraphy by: Loren E. Babcock School of Earth Sciences The Ohio State University, 125 South Oval Mall Columbus, OH 43210, USA [email protected] Richard A. Robison Department of Geology, University of Kansas Lawrence, KS 66045, USA [email protected] Margaret N. Rees Department of Geoscience University of Nevada, Las Vegas Las Vegas, NV 89145, USA [email protected] Peng Shanchi Nanjing Institute of Geology and Palaeontology Chinese Academy of Sciences 39 East Beijing Road, Nanjing 210008, China [email protected] Matthew R. Saltzman School of Earth Sciences The Ohio State University, 125 South Oval Mall Columbus, OH 43210, USA [email protected] 31 July 2006 CONTENTS Introduction …………………………………………………………………………. 2 Proposal: Stratotype Ridge, Drum Mountains (Millard County, Utah, USA) as the GSSP for the base of the Drumian Stage ……………………………………………………. 3 1. Stratigraphic rank of the boundary …………………..…………………………… 3 2. Proposed GSSP – geography and physical geology ……………………………… 3 2.1. Geographic location …………………………………………………...….. 3 2.2. Geological location ………………..……………………...…………...….. 4 2.3. Location of level and specific point ……………………..……………...… 4 2.4. Stratigraphic completeness ………………...……………………………… 5 2.5. Thickness and stratigraphic extent …………………...……………...……. 5 2.6. Provisions for conservation, protection, and accessibility ……………..…. 5 3. Motivation for selection of the boundary level and of the potential stratotype section ………………………………………………………………………………. 6 3.1. Principal correlation event (marker) at GSSP level ………...…………..… 6 3.2. Potential stratotype section …………………………………………....….. 7 3.3. Demonstration of regional and global correlation ………………………... 8 3.3.1. Agnostoid trilobite biostratigraphy ………………………………… 9 3.3.2. Polymerid trilobite biostratigraphy …………....…………….……. -
Table of Codes for Each Court of Each Level
Table of Codes for Each Court of Each Level Corresponding Type Chinese Court Region Court Name Administrative Name Code Code Area Supreme People’s Court 最高人民法院 最高法 Higher People's Court of 北京市高级人民 Beijing 京 110000 1 Beijing Municipality 法院 Municipality No. 1 Intermediate People's 北京市第一中级 京 01 2 Court of Beijing Municipality 人民法院 Shijingshan Shijingshan District People’s 北京市石景山区 京 0107 110107 District of Beijing 1 Court of Beijing Municipality 人民法院 Municipality Haidian District of Haidian District People’s 北京市海淀区人 京 0108 110108 Beijing 1 Court of Beijing Municipality 民法院 Municipality Mentougou Mentougou District People’s 北京市门头沟区 京 0109 110109 District of Beijing 1 Court of Beijing Municipality 人民法院 Municipality Changping Changping District People’s 北京市昌平区人 京 0114 110114 District of Beijing 1 Court of Beijing Municipality 民法院 Municipality Yanqing County People’s 延庆县人民法院 京 0229 110229 Yanqing County 1 Court No. 2 Intermediate People's 北京市第二中级 京 02 2 Court of Beijing Municipality 人民法院 Dongcheng Dongcheng District People’s 北京市东城区人 京 0101 110101 District of Beijing 1 Court of Beijing Municipality 民法院 Municipality Xicheng District Xicheng District People’s 北京市西城区人 京 0102 110102 of Beijing 1 Court of Beijing Municipality 民法院 Municipality Fengtai District of Fengtai District People’s 北京市丰台区人 京 0106 110106 Beijing 1 Court of Beijing Municipality 民法院 Municipality 1 Fangshan District Fangshan District People’s 北京市房山区人 京 0111 110111 of Beijing 1 Court of Beijing Municipality 民法院 Municipality Daxing District of Daxing District People’s 北京市大兴区人 京 0115 -
GSSP) of the Drumian Stage (Cambrian) in the Drum Mountains, Utah, USA
Articles 8585 by Loren E. Babcock1, Richard A. Robison2, Margaret N. Rees3, Shanchi Peng4, and Matthew R. Saltzman1 The Global boundary Stratotype Section and Point (GSSP) of the Drumian Stage (Cambrian) in the Drum Mountains, Utah, USA 1 School of Earth Sciences, The Ohio State University, 125 South Oval Mall, Columbus, OH 43210, USA. Email: [email protected] and [email protected] 2 Department of Geology, University of Kansas, Lawrence, KS 66045, USA. Email: [email protected] 3 Department of Geoscience, University of Nevada, Las Vegas, Las Vegas, NV 89145, USA. Email: [email protected] 4 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing 210008, China. Email: [email protected] The Global boundary Stratotype Section and Point correlated with precision through all major Cambrian regions. (GSSP) for the base of the Drumian Stage (Cambrian Among the methods that should be considered in the selection of a GSSP (Remane et al., 1996), biostratigraphic, chemostratigraphic, Series 3) is defined at the base of a limestone (cal- paleogeographic, facies-relationship, and sequence-stratigraphic cisiltite) layer 62 m above the base of the Wheeler For- information is available (e.g., Randolph, 1973; White, 1973; McGee, mation in the Stratotype Ridge section, Drum Moun- 1978; Dommer, 1980; Grannis, 1982; Robison, 1982, 1999; Rowell et al. 1982; Rees 1986; Langenburg et al., 2002a, 2002b; Babcock et tains, Utah, USA. The GSSP level contains the lowest al., 2004; Zhu et al., 2006); that information is summarized here. occurrence of the cosmopolitan agnostoid trilobite Pty- Voting members of the International Subcommission on Cam- chagnostus atavus (base of the P. -
Ecosystem Services Value Assessment and Uneven Development of the Qingjiang River Basin in China
sustainability Article Ecosystem Services Value Assessment and Uneven Development of the Qingjiang River Basin in China Zhengsong Lin 1,2 ID , Xinyue Ye 3,4,* ID , Qian Wei 2, Fan Xin 5, Zhang Lu 2, Sonali Kudva 6 ID and Qiwen Dai 4,* 1 School of Environmental Studies, China University of Geosciences (Wuhan), Wuhan 430074, China; [email protected] 2 School of Arts Communication, China University of Geosciences (Wuhan), Wuhan 430074, China; [email protected] (Q.W.); [email protected] (Z.L.) 3 Department of Geography, Kent State University, Kent, OH 44242, USA 4 School of Economics and Management, Guangxi Normal University, Guilin 541004, China 5 School of Public Administration, China University of Geosciences (Wuhan), Wuhan 430074, China; [email protected] 6 School of Information, Kent State University, Kent, OH 44242, USA; [email protected] * Correspondence: [email protected] (X.Y.); [email protected] (Q.D.); Tel.: +1-419-494-7825 (X.Y.); +86-773-5816858 (Q.D.); Fax: +1-330-672-4034 (X.Y.); +86-773-5816858 (Q.D.) Received: 11 August 2017; Accepted: 8 December 2017; Published: 18 December 2017 Abstract: As an important ecological barrier in Southwest China, the Qingjiang river basin plays a vital role in shaping the mountainous terrain. This paper analyzes the Ecosystem Services Value (ESV) using a series of methods based on the data of changes in land use from 2000 to 2015 and the statistical yearbook. The changes in land use between 2000 and 2015 were dominated by forest land, which accounted for 60.63% of the total area, followed by arable landwhich accounted for about 22.26%, while grassland and other land use contribution rates were the lowest, accounting for only about 17.11%. -
Petrography and Origin of the Lower Ordovician Microbial Carbonates in the Songzi Area of Hubei Province, Middle Yangtze Region, China
Petroleum Science (2019) 16:956–971 https://doi.org/10.1007/s12182-019-0346-2 ORIGINAL PAPER Petrography and origin of the Lower Ordovician microbial carbonates in the Songzi Area of Hubei Province, middle Yangtze region, China Chuan‑Tao Xiao1 · Guo‑Qi Wei2 · Zhen‑Yu Song1 · Yun‑Peng Xiao1 · Wei Yang2 · Man Dong1 · Yun‑Fei Huang1 · Da Gao1 Received: 15 May 2018 / Published online: 16 August 2019 © The Author(s) 2019 Abstract This study is the frst systematic assessment of the Lower Ordovician microbial carbonates in Songzi, Hubei Province, China. This paper divides the microbial carbonates into two types according to growth patterns, namely nongranular and granular. The nongranular types include stromatolites, thrombolites, dendrolites, leiolites and laminites; the granular types are mainly oncolites and may include a small amount of microbiogenic oolite. According to their geometric features, the stromatolites can be divided into four types: stratiform, wavy, columnar and domal. Additionally, dipyramidal columnar stromatolites are identifed for the frst time and represent a new type of columnar stromatolite. The thrombolites are divided into three types: speckled, reticulated and banded. The grazing gastropod Ecculiomphalus and traces of bioturbation are observed in the speckled and reticulated thrombolites. This paper considers these two kinds of thrombolites to represent bioturbated thrombolites. These fndings not only fll gaps in the feld of domestic Ordovician bioturbated thrombolites but also provide new information for the study of thrombolites. Based on the analysis of the sedimentary characteristics of microbialites, the depositional environments of the various types of microbialites are described, and the distribution patterns of their depo‑ sitional environments are summarized. -
Network Group Psychological Education of College Students
Journal of Psychological Research | Volume 02 | Issue 03 | July 2020 Journal of Psychological Research https://ojs.bilpublishing.com/index.php/jpr REVIEW Network Group Psychological Education of College Students Zhenzi Han* Yonggang Li Babao Township Hospital, Songzi, Jingzhou, Hubei, 434000, China ARTICLE INFO ABSTRACT Article history Based on the perspective of psychology, this paper analyzes the causes and Received: 23 June 2020 characteristics of college students’ network mass incidents, explores the psychological factors of college students’ network mass incidents, and puts Accepted: 23 June 2020 forward the educational strategies to solve college students’ network mass Published Online: 30 July 2020 incidents: No.1. Adhere to humanism and take appeals as the center; Keywords: No.2. To improve the campus network public opinion guidance mechanism College students network group event psychological under the guidance of relevant social cognition theories; No.3. Strengthen communication and improve communication skills; analysis No.4. Promote information disclosure and transparency, and eliminate Education countermeasures uncertainty and ambiguity. 1. Foreword behavior, network group events is formed under the background of a certain social network community is a n recent years, with the frequent occurrence of mass social phenomenon and social issues of mutual interest incidents and related reports in various parts of China, focus in the discussion, through the network publishing, IPeople pay more and more attention to network group disseminating information and manufacturing network events, With the popularization and application of the net- public opinion, make the development of social events work, the network mass incidents of college students have conform to the collective behavior of his desire. -
One-Dimensional Steady Flow-Sediment Mathematic Models Helius and Their Application in the Three Gorges Project
US-CHINA WORKSHOP ON ADVANCED COMPUTATIONAL MODELLING IN HYDROSCIENCE & ENGINEERING September 19-21, Oxford, Mississippi, USA ONE-DIMENSIONAL STEADY FLOW-SEDIMENT MATHEMATIC MODELS HELIUS AND THEIR APPLICATION IN THE THREE GORGES PROJECT Yue Huang1 and Yuling Huang2 ABSTRACT In order to investigate the sediment problem of the Three Gorges Project (TGP), two 1-D steady flow-sediment mathematic models (i.e., HELIU-1 and HELIU-2) are developed gradually by Changjiang River Scientific Research Institute (CRSRI). Through calculation and verification for in situ measured data of large and medium scale reservoirs and channel reaches downstream of the dams in the Changjiang River Basin, it is found that they can give reasonable results to simulate reservoirs sedimentation and the downstream channel reaches’ deformation due to scour in long time period and long distance. Especially, after completion of TGP the models are also used to predict reservoir sedimentation in the TGP Reservoir (780 km long) and the channel reach (over 1100 km long) downstream of the TGP Dam. The calculated results have been referred by the technical design department of TGP. 1. INTRODUCTION At the beginning of the 1970s, a 1-D steady flow-sediment mathematic model HELIU-1 was developed for studying the sediment problem of the Three Gorges Project (TGP). This model was mainly used to study the scour and deposition of suspended sediment. It simulate reservoir sedimentation well, but it falls short of modeling the scour of river channel. Therefore, the model HELIU-2 was developed in the early 1990s. For HELIU-2, technical problems such as exchange of bed sediment and suspended sediment, river bed deformation and bed sediment composition have been taken into account.