Protection Efficacy of National Wetland Reserves in China

Total Page:16

File Type:pdf, Size:1020Kb

Protection Efficacy of National Wetland Reserves in China Article Ecology April 2012 Vol.57 No.10: 11161134 doi: 10.1007/s11434-011-4942-9 Protection efficacy of national wetland reserves in China ZHENG YaoMin1, ZHANG HaiYing1, NIU ZhenGuo1* & GONG Peng1,2,3* 1 State Key Laboratory of Remote Sensing Science, Jointly Sponsored by Institute of Remote Sensing Applications, Chinese Academy of Sciences and Beijing Normal University, Beijing 100101, China; 2 Ministry of Education Key Laboratory for Earth System Modeling, Center for Earth System Science, Institute for Global Change Studies, Tsing- hua University, Beijing 100084, China; 3 Department of Environmental Science, Policy and Management, University of California, Berkeley, California 94720-3114, USA Received August 10, 2011; accepted November 28, 2011 Wetlands have the most abundant biodiversity, the highest carbon sequestration capacity, and the highest values for ecological services per unit area, of all the world’s ecosystems. Practice has shown that establishing reserves is the most effective way of protecting typical ecosystems and their biodiversity, and saving rare or endangered wildlife. The Chinese government’s policy is to protect wetland systems by establishing reserves that encompass a massive network of wetlands, including wetland nature re- serves, internationally important wetlands, and wetland parks. Many are already established. The effect of protecting wetland nature reserves at the national level has not yet been reported. We used the latest database evaluating the protection value of wet- land reserves, and remotely sensed wetland maps (1978–2008), developed by the same mapping specialists and based on the same classification system, and related environmental data, to evaluate the effects of protecting China’s national wetland reserves over the last 30 years. We conclude that (i) the total area of wetland in the national wetland reserves has decreased over the last 30 years to 8152.47 km2, and just 8% of China’s net decrease in wetlands; (ii) about 79% of the 91 national wetland reserves are in a poor condition. These are generally located around the Yangtze River, Eastern Coast, the Three Rivers Source, and Southwest China. Protection measures should be undertaken urgently in these areas. Only 15% of national wetland reserves are under sound protection, and these are generally located in the upper reaches of the Songhua River; (iii) although 88% of national wetland re- serves are primitive (relatively natural), implying that the site selection has been scientific, a high percentage of national wetland reserves show early warning signs of decline and require urgent attention; (iv) based on our evaluation of protection effects and pressures on ecology, we have made a priority list of national wetland reserves, and propose several protection strategies. remote sensing, wetlands, protection, ecology, early warning signs Citation: Zheng Y M, Zhang H Y, Niu Z G, et al. Protection efficacy of national wetland reserves in China. Chin Sci Bull, 2012, 57: 11161134, doi: 10.1007/s11434-011-4942-9 Wetlands have the highest ecological value per unit area on change [8]. earth [1], the strongest carbon sequestration capability [2], Through over 140 years of practice, the establishment of and the greatest biodiversity protection significance [3–7]. nature reserves has been shown to be the best method of Protecting wetlands and their biodiversity has attracted sig- protecting biodiversity, and an effective measure for main- nificant attention from the international community (http:// taining the ecological security of a region [9]. Prior to 2008, www.wetlands.org, 2010). However, the effectiveness of there were 1.2×105 protected areas around the world, occu- wetland protection has rarely been considered. There is a pying about 2.1×107 km2 in total area (http://www.unep- great need for quantitative assessment of wetland ecosys- wcmc.org/wdpa/statistics, 2010), and accounting for 14% of tems to aid understanding of likely global environmental the world’s total land area. There has been no agreement on the classification of the *Corresponding authors (email: [email protected]; [email protected]) world’s protected areas. After several rounds of discussion © The Author(s) 2012. This article is published with open access at Springerlink.com csb.scichina.com www.springer.com/scp Zheng Y M, et al. Chin Sci Bull April (2012) Vol.57 No.10 1117 and revision by the International Union for Conservation of wetland reserves, and suggested a ranked list of national and Nature and Natural Resources (IUCN) in 1969, 1972, 1978 provincial wetland reserves based on 16 categories of wet- and 1994, protected areas have been divided into 6 types, land reserves across China, depending on their protection including Strict Nature Reserve (Ia), Wilderness Area (Ib), value. National Park (II), Natural Monument or Feature (III), Habi- Gong et al. [9] revised the wetland classification system tat Species management Area (IV), Protected Landscape/sea- suggested by Niu et al. [21] and completed wetland maps of scape (V) and Protected Area with sustainable use of natural China for the past 30 years based on remotely sensed data resources (VI) (http://www.iucn.org, 2010). [22]. These wetland-related data have laid the foundations Studies on nature reserve classification were carried out for assessment of the effectiveness of wetland protection at in China during the 20th century [10]. In 1993, the “Chinese the national level. Nature Reserves Classification and Ranking Principle” was We analyzed changes in wetland reserves and assessed published jointly by the former State Environmental Protec- the effects of protection and human pressure over the last 30 tion Agency and the State Administration of Technological years, mainly by using wetland maps, national wetland re- Supervision, and this was accepted as a national standard serve boundary data, protection value data, and related data. (GB/T 14529-93) [11]. By consideration of the main protec- tion roles, this document divided Chinese nature reserves into 3 categories and 9 types: the natural ecosystem class 1 Methods (forest, prairie and meadow, wilderness, interior wetland, 1.1 Data sources and preparation and marine/coast), the wildlife class (wild animals and wild plants), and the natural vestige class (geological vestige and 1.1.1 Chinese wetland maps based on satellite data extinct organism vestige). Prior to 2011, China had estab- The Chinese wetland maps were developed primarily by lished 614 wetland reserves [12,13], and 91 of these are manual interpretation [8,21], in which the narrowest river national wetland reserves. width was 90 m and the area of the minimum mapping unit A wetland protection network has been established. This was about 9×104 m2. Four different maps at 20 m (2008), 30 m is made up of mostly wetland reserves, along with interna- (2000, 1990), and 80 m (1978) resolutions were resampled tional important wetlands, wetland parks, special marine into maps with the same cell size (240 m×240 m) for com- reserves, small wetland reserves and wetland multipurpose parative purposes. reserves. However, no report has evaluated the effects of wetland protection, or assessed the spatial distribution of 1.1.2 Database of wetland reserves China’s wetland reserves. Data for 182 wetland reserves were collected [23–26], the Assessment of protection value refers to research into database for protection value evaluation of wetland reserves natural resources and the importance of nature reserves, was established and distribution maps of wetland reserves including the relative diversity, rarity, representativeness, were created. The websites of the nature reserve authorities suitability, naturalness, and human disturbance of reserves were used for checking data and updating it in real time. For [13,14]. Protection effect evaluation is comprehensive research details see Zheng [13]. into the levels of protection of national wetland reserves The distribution maps of wetland reserves were scanned, from the perspective of protection value, dynamic change, adjusted, and quantified based on the general plan of wet- the expansion of species, and the functional zoning suggested land reserves. Basic information about the reserves from sci- by conservation biology, ecology, and nature reserve science. entific reports was input into an Excel spreadsheet and then There has been no appropriate definition of ecological loaded into a special database. Data from the “1:4000000 security [15]. Some believe that ecological security is as Chinese wetland distribution map” (State Forest Admin- important as national and economic security (http://www. istration, 2003), the “1:4000000 Chinese river system dis- cctv.com/news/ocus/story/story0423.html, 2010). Ecological tribution map” (https://219.238.166.215/mcp/index.asp, 2011), security can be explained as comprising two aspects. First, “the Chinese map” (Map Publishing House, 2010), “the re- degeneration of the ecological environment poses a threat to mote sensing data of Beijing Smallsat”, and “the announce- sustainable economic development; and second, public dis- ment material on the website of the reserves authorities” were affection raised by environmental problems poses a threat to used as supplementary material for checking and analysis. social stability [15,16]. Combining remote sensing (RS) and geographic infor- 1.1.3 Database of ecological pressure mation system (GIS) has created a powerful analytical Charts of Chinese population density and land use were method for exploring the dynamics of wetlands and devel- downloaded from the Internet (http://www.igsnrr.ac.cn/xxgx/ oping an influential model for change [17–20]. There is 200909/t20090904_2464203.html, 2011) and Chinese road, currently no literature relating to the effects of protecting rail, and residential areas were taken from the China Na- wetlands at the national level because of the lack of data. tional 1:1000000 terrain database (State Administration of Zheng [13] completed maps of the boundaries of national Surveying, Mapping, and Geoinformation, 2002). 1118 Zheng Y M, et al. Chin Sci Bull April (2012) Vol.57 No.10 1.2 Research methods and data processing reserves has not been published.
Recommended publications
  • Environmental Changes in Chaohu Lake (Southeast, China) Since the Mid 20Th Century: the Interactive Impacts of Nutrients, Hydrology and Climate
    Limnologica 43 (2013) 10–17 Contents lists available at SciVerse ScienceDirect Limnologica journal homepage: www.elsevier.com/locate/limno Environmental changes in Chaohu Lake (southeast, China) since the mid 20th century: The interactive impacts of nutrients, hydrology and climate Xu Chen a,b, Xiangdong Yang a,∗, Xuhui Dong a, Enfeng Liu a a State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, People’s Republic of China b Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, People’s Republic of China article info abstract Article history: Chaohu Lake, the fifth largest freshwater lake in the Yangtze floodplain, is faced with multiple stresses Received 21 June 2011 from anthropogenic disturbances and climate change. To explore the ecological changes in Chaohu Lake Received in revised form 31 October 2011 since the mid 20th century, we examined diatoms, geochemical indicators and particle size in 210Pb- Accepted 6 March 2012 dated sediment core from the lake. Diatom succession revealed that the lake had switched to a eutrophic Available online 11 June 2012 state since the late 1970s. Redundancy analysis using limnological data, hydrological and meteorological variables showed that sedimentary total phosphorus (TP) and total organic carbon (TOC), annual mean Keywords: temperature, annual mean wind velocity, and water-level amplitude (WLA) were five significant factors Diatoms Nutrient loading influencing diatom succession. Diatom assemblages from 1950 till 1978 were driven by WLA and wind. Hydrological alteration The establishment of Chaohu Dam baffled hydrological connectivity between the lake and the Yangtze Climate warming River in 1962, and reducing water exchange-induced flow.
    [Show full text]
  • Supplement of a Systematic Examination of the Relationships Between CDOM and DOC in Inland Waters in China
    Supplement of Hydrol. Earth Syst. Sci., 21, 5127–5141, 2017 https://doi.org/10.5194/hess-21-5127-2017-supplement © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Supplement of A systematic examination of the relationships between CDOM and DOC in inland waters in China Kaishan Song et al. Correspondence to: Kaishan Song ([email protected]) The copyright of individual parts of the supplement might differ from the CC BY 3.0 License. Figure S1. Sampling location at three rivers for tracing the temporal variation of CDOM and DOC. The average widths at sampling stations are about 1020 m, 206m and 152 m for the Songhua River, Hunjiang River and Yalu River, respectively. Table S1 the sampling information for fresh and saline water lakes, the location information shows the central positions of the lakes. Res. is the abbreviation for reservoir; N, numbers of samples collected; Lat., latitude; Long., longitude; A, area; L, maximum length in kilometer; W, maximum width in kilometer. Water body type Sampling date N Lat. Long. A(km2) L (km) W (km) Fresh water lake Shitoukou Res. 2009.08.28 10 43.9319 125.7472 59 17 6 Songhua Lake 2015.04.29 8 43.6146 126.9492 185 55 6 Erlong Lake 2011.06.24 6 43.1785 124.8264 98 29 8 Xinlicheng Res. 2011.06.13 7 43.6300 125.3400 43 22 6 Yueliang Lake 2011.09.01 6 45.7250 123.8667 116 15 15 Nierji Res. 2015.09.16 8 48.6073 124.5693 436 83 26 Shankou Res.
    [Show full text]
  • Family-Sisoridae-Overview-PDF.Pdf
    FAMILY Sisoridae Bleeker, 1858 - sisorid catfishes SUBFAMILY Sisorinae Bleeker, 1858 - sisorid catfishes [=Sisorichthyoidei, Bagarina, Nangrina] GENUS Ayarnangra Roberts, 2001 - sisorid catfishes Species Ayarnangra estuarius Roberts, 2001 - Irrawaddy ayarnangra GENUS Bagarius Bleeker, 1853 - sisorid catfishes Species Bagarius bagarius (Hamilton, 1822) - goonch, dwarf goonch [=buchanani, platespogon] Species Bagarius rutilus Ng & Kottelat, 2000 - Red River goonch Species Bagarius suchus Roberts, 1983 - crocodile catfish Species Bagarius yarrelli (Sykes, 1839) - goonch, giant devil catfish [=carnaticus, lica, nieuwenhuisii] GENUS Caelatoglanis Ng & Kottelat, 2005 - sisorid catfishes Species Caelatoglanis zonatus Ng & Kottelat, 2005 - Chon Son catfish GENUS Conta Hora, 1950 - sisorid catfishes Species Conta conta (Hamilton, 1822) - Mahamanda River catfish [=elongata] Species Conta pectinata Ng, 2005 - Dibrugarh catfish GENUS Erethistes Muller & Troschel, 1849 - sisorid catfishes [=Hara, Laguvia] Species Erethistes filamentosus (Blyth, 1860) - Megathat Chaung catfish [=maesotensis] Species Erethistes hara (McClelland, 1843) - Hooghly River catfish [=asperus, buchanani, saharsai, serratus] Species Erethistes horai (Misra, 1976) - Terai catfish Species Erethistes jerdoni (Day, 1870) - Sylhet catfish Species Erethistes koladynensis (Anganthoibi & Vishwanath, 2009) - Koladyne River catfish Species Erethistes longissimus (Ng & Kottelat, 2007) - Mogaung catfish Species Erethistes mesembrinus (Ng & Kottelat, 2007) - Langkatuek catfish Species Erethistes
    [Show full text]
  • Determination of Geochronology and Sedimentation Rates of Shallow Lakes in the Middle Yangtze Reaches Using 210Pb, 137Cs and Spheroidal Carbonaceous Particles
    Determination of geochronology and sedimentation rates of shallow lakes in the middle Yangtze reaches using 210Pb, 137Cs and spheroidal carbonaceous particles Xu Chen1*, Qianglong Qiao1, Suzanne McGowan2, Linghan Zeng1,2, Mark A Stevenson3, Lei Xu1, Chunling Huang1, Jia Liang1, Yanmin Cao4 1State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China 2School of Geography, University of Nottingham, Nottingham NG7 2RD, UK 3School of Natural and Environmental Sciences, Newcastle University, Newcastle- upon-Tyne NE1 7RU, UK 4College of Resources and Environmental Science, South-Central University for Nationalities, Wuhan 430074, China *Corresponding author; e-mail address: [email protected] https://doi.org/10.1016/j.catena.2018.11.041 Catena Abstract: Accurate chronologies for recent sediments of shallow lakes in the Yangtze floodplain are critical to calibrate proxy records for reconstructing environmental changes during the past century. This study presents the results of detailed 210Pb analysis from eight lake sediment cores collected from the middle Yangtze reaches, 210 southeast China. Unsupported Pb activities generally declined exponentially with mass depth in the eight cores. The chronologies and sedimentation rates for the sediment cores were calculated using different 210Pb-based mathematical models. The 137Cs chronomarker (i.e. the 1963 fallout peak) and the spheroidal carbonaceous particle (SCP) chronomarker (i.e. the start of the rapid increase in 1970 AD) were selected to validate the 210Pb dating. Sedimentation rates derived from different models were validated using historical data including lake area, arable land area, sediment discharge and reservoir volume in the Yangtze basin. The SCP-corrected CRS (constant rate of supply) model performs better than other models, based on validation using historical documents in the Yangtze basin.
    [Show full text]
  • Flood Control for the Red River [Vietnam]
    Total Disaster Risk Management - Good Practices - Chapter 3 Vietnam Flood Control for the Red River The Red River, the Delta and Floods The history of the development of Vietnamese civilizations is closely linked to the Red River (Hong River) Delta. As the second largest granary of Vietnam, the Delta holds a significant meaning in the life of the Vietnamese people. This is where approximately 15–20 % of Vietnam’s rice is produced. A population of 17 million now inhabits the 16,500-km2 area of the Red River Delta. The catchment area of the Red River is estimated at 169,000 km2, half of which lies in China. The Red River at Hanoi comprises three major tributary systems, the Da, Thao and Lo Rivers. The river is the source of various positive aspects for human life, such as water resources and rich alluvium (it is called the Red River as the large amount of alluvium it carries colors it red all year round). However, these go hand in hand with a much less expected occurrence: floods. Increased flash floods as a result of deforestation in the upstream parts of the Red River basin, and raised bed levels of the rivers due to the deposition of sediment, are causing higher flood levels, endangering the ever increasing socio-economic value of the capital. The land in low-lying areas of the river delta is protected against flooding by river dyke systems. According to official historical records, in 1108, King Ly Nhan Tong ordered the construction of the first dyke with solid foundations on a large scale aimed at protecting the capital of Thang Long (now Hanoi).
    [Show full text]
  • Diatom Community Succession and Nutrient Evolution Recorded from a Sediment Core of the Longgan Lake, a Large Shallow Lake in East China
    第 30 卷 第 6 期 水 生 生 物 学 报 Vol . 30 ,No . 6 2 0 0 6 年 1 1 月 ACTA HYDROBIOLOGICA SINICA Nov. , 2 0 0 6 DIATOM COMMUNITY SUCCESSION AND NUTRIENT EVOLUTION RECORDED FROM A SEDIMENT CORE OF THE LONGGAN LAKE, A LARGE SHALLOW LAKE IN EAST CHINA DONG Xu2Hui and YANG Xiang2Dong ( Nanjing Institute of Geography &Limnology , the Chinese Academy of Sciences , Nanjing 210008 , China) Abstract :The Longgan Lake is a shallow mesotrophic macrophyted2ominated lake. According to the high2resolution diatom research from its sediment core , the diatom community succession was built , and the total phosphorus (TP) and chlorophyll2a (Chl2a) con2 centration were quantitatively reconstructed for the past 2000 years , based on the diatom2TP and diatom2Chla transfer functions. The shifts of diatom assemblages also mirrored the developments of aquatic plant , reflecting the characters of aquatic ecosystem evolution. The inferred epilimnetic TP concentration fluctuated within a small range of 36 to 62μg/ L , indicating the lake remained a relative stable mesotrophic status in the long historical period. The periodical variations of the diatom assemblage and trophic sta2 tus suggest a mitigating function of shallow macrophyte2dominated lakes to nutrient input. The changes of lakesptrophic status donpt linearly respond to the human disturbance in the catchment. The dynamics mechanism of phosphorus in macrophyte2dominated lakes , as inferred from diatoms , will provide a scientific foundation for the prediction of trophic status change in a shallow lake , as well as the lake ecological restoration and management decisions. Key words :Diatom assemblage ; Nutrient ; Quantitative reconstruction ; Aquatic macrophyte ; Longgan Lake CLC number :X172 Document code :A Article ID :100023207(2006) 0620702209 The importance of aquatic vegetation to the ecologi2 on the environment reconstruction based on the sediment cal restoration has been recognized commonly by limnolo2 biomarker such as diatom have made rapid gists and lake managements[1 —4 ] .
    [Show full text]
  • APPENDIX 6D Profile of the Inland Waterway Master Plan Projects
    APPENDIX 6D Profile of the Inland Waterway Master Plan Projects ANNEX 6D Profile of the Inland Waterway Master Plan Projects A. Ongoing/Committed Project Profile Project Name: Sector: Upgrading of Northern Trans Mekong corridor (to Class III) (253km) CW01 Project Background & Objective: None of the corridors provide good transport continuity at present , and improvements will help improve region – wide accessibility re- lieve congestion on the main corridors, reduce transportation costs and supports economic development in the provinces. Project Description: (i) To improve the standard (up to Class III/300DWT vessels) and connectivity of the canal network in Northern Trans Mekong corri- dor(253km):Dredging, bank protection, ship lock, bridge improvements, navigation aids for 24-hour navigation, as one of the com- ponents of Development of transport infrastructure of Mekong River Delta. (ii) Main Project Components is Dredging, Bank protection, Improving and building bridges, Enhancing alarming system, Building Rach Chanh Dock and Building Tan Chau Port: Estimated Cost (2009): Original Schedule: US 99.3 million (including CW02) 2009–2015 Financial Source: Implementation Agency World Bank , Vietnam VIWA 6D-1 Project Name: Sector: Updating of Southern coastal corridor (to Class III) (153km) CW02 Project Background & Objective: This improvements will help improve region –wide accessibility, relieve congestion on the main corridors, reduce transportation costs and support economic development in the province. Project Description: (i) To improve the standard (up to Class III/300DWT vessels) and connectivity of the canal network in the southern coastal corri- dor(153km) (ii) Location is Gia Rai–Bac Liec–Dai Ngai (103km) and Cho Gao Canal (50km) (iii) Main components are as follows: Dredging, bank protections, ship lock, bridge improvements, navigation aids for 24-hour naviga- tion .These are one of the components of Development of transport infrastructure of Mekong River Delta.
    [Show full text]
  • Next Tier 3 Suppliers 2020
    TIER 3 SUPPLIER SITES - Produced March 2021 SUPPLIER NAME ADDRESS SPINNING KNITTING WEAVING DYEING PRINTING Bangladesh A One Polar Ltd Vulta, Rupgonj, Nrayangonj ✓ ✓ ✓ AA Spinning Mill Ltd Nagar Howla, Sreepur, Gazipur District, Dhaka ✓ Aaron Denim Ltd Sukran, Mirzanagar, Nobinagar, Savar, Dhaka 1347 ✓ ✓ Abanti Colour Tex Ltd S A-646, Shashongaon, Enayetnagar, Fatullah, Narayanganj 1400 ✓ ✓ ✓ ACS Textiles Ltd Tetlabo, Rupgonj, Ward 3, Narayangonj, Dhaka 1400 ✓ ✓ ✓ Adury Knit Composite Ltd Karadi, Shibpur, Narsingdi Narshingdi Dhaka ✓ ✓ ✓ Akij Textile Mills Ltd Golora, Charkhanda, Manikgonj ✓ ✓ ✓ Al Haj Karim Textiles Ltd Kalampur, Dhamrai, Savar, Dhaka 1351 ✓ Alim Knit BD Ltd Nayapara, Kashimpur, Zitar Moor, Gazipur ✓ ✓ ✓ Alliance Knit Composite Ltd 8/118, Pukurpar, Zirabo, Ashulia, Savar, Dhaka-1341 ✓ ✓ ✓ Aman Spinning Mills Ltd Ashulia Highway, Zirabo, Ashulia, Savar, Dhaka ✓ Amantex Limited Boiragi Challa, Shreepur, Gazipur 1740, Dhaka ✓ ✓ ✓ Amber Cotton Mills Ltd Banglabazar, Bahadurpur, Razendrapur, Gazipur, Dhaka ✓ Amber Denim Mills Ltd (Unit 2) Unit 2, Banglabazar, Bahadurpur, Razendrapur, Gazipur, Dhaka ✓ ✓ Anjum Textile Mills Birampur, Madhobdi, Norshingd ✓ ✓ Anwar Silk Mills Ltd 186 Tongi Industrial Area, Tongi, Gazipur ✓ Apex Weaving and Finishing Mills Ltd East Chundora, Shafipur, Kaliakoar, Gazipur 1751 ✓ ✓ ✓ APS Group Kamar Gaon Pubail Road Gazipur ✓ ✓ Argon Denims Ltd Beraider Chala Po Gilaberaid Ps Sripur, Gazipur, 1742, Gazipur ✓ ✓ ✓ Arif Spinning Mill Ltd Mastarbari, Jamirdia, Valuka, Mymensingh ✓ Armada Spinning Mills
    [Show full text]
  • Report on the State of the Environment in China 2016
    2016 The 2016 Report on the State of the Environment in China is hereby announced in accordance with the Environmental Protection Law of the People ’s Republic of China. Minister of Ministry of Environmental Protection, the People’s Republic of China May 31, 2017 2016 Summary.................................................................................................1 Atmospheric Environment....................................................................7 Freshwater Environment....................................................................17 Marine Environment...........................................................................31 Land Environment...............................................................................35 Natural and Ecological Environment.................................................36 Acoustic Environment.........................................................................41 Radiation Environment.......................................................................43 Transport and Energy.........................................................................46 Climate and Natural Disasters............................................................48 Data Sources and Explanations for Assessment ...............................52 2016 On January 18, 2016, the seminar for the studying of the spirit of the Sixth Plenary Session of the Eighteenth CPC Central Committee was opened in Party School of the CPC Central Committee, and it was oriented for leaders and cadres at provincial and ministerial
    [Show full text]
  • Back Matter (PDF)
    Index Page numbers in italics refer to Figures. Page numbers in bold refer to Tables. acoustic Doppler current profiler (ADCP) 156, 182 Bulimina spp. 202, 202, 205, 206 agriculture, impact on weathering 48 butterfly delta 2, 90 anthropogenic impact 5–6, 15 Diaokou lobe 191–192, 192 13C isotope analysis 198 Lingdingyang Bay 182 14C age measurement Pearl River delta sediments 48 Beibu Gulf 92, 92, 95, 96 apatite fission track (AFT), provenance evidence southern mud depocentre 90 18–20, 23 Diaokou lobe sediments 188 40Ar/39Ar dating, role in provenance studies 20–21 Gulf of Tonkin 75 offshore cores 212, 215 Baiyun Sag 32, 33 offshore Hainan Island Bashi Straits 9, 10 method 102 10Be date 199 results 104, 104 Beibu Gulf 100, 101 Cangzhou rise 186 geological setting 88–90 carbonate location 87 offshore Hainan Island sediment study map 88 methods 104 sea-level change post glacial 101–102 results 110 sediment movement 2 South China Sea sediment 200 southern mud depocentre 89 Cassidulina carinata 202, 205, 206 sediment study Cathaysia Block 123, 124 methods 90 Cathaysia (South China) terrane 11, 12,19 results Central Yellow Sea Mud 88 14C dating 92, 92, 95, 96 Changjiang (Yangtze) River 88, 224, 225, 225, 226 geochemistry 93–95, 94 catchment climate 140 lithology 93 catchment geology 139–140 seismic profiles 90, 91,92–93 delta sedimentary system 233, 234, 236, 237, 248, 249 results discussed 96–97 discharge pattern 156, 230, 231 Beijiang River 32, 33 gravity flow 231 Beipanjiang River 32, 33 history of inputs to East China Sea 140 Bohai Basin 186
    [Show full text]
  • Ge/Si Ratios Indicating Hydrothermal and Sulfide Weathering Input To
    Chemical Geology 410 (2015) 40–52 Contents lists available at ScienceDirect Chemical Geology journal homepage: www.elsevier.com/locate/chemgeo Ge/Si ratios indicating hydrothermal and sulfide weathering input to rivers of the Eastern Tibetan Plateau and Mt. Baekdu Yeongcheol Han a,1, Youngsook Huh a,⁎, Louis Derry b a School of Earth and Environmental Sciences, Seoul National University, Seoul 151-747, Korea. b Department of Earth and Atmospheric Sciences, Cornell University, Ithaca, NY 14853, USA article info abstract Article history: Concentrations of dissolved silicon in river waters reflect a complex interplay among chemical weathering of pri- Received 6 February 2015 mary silicate minerals, formation and weathering of secondary clay minerals, hydrothermal input and biological Received in revised form 29 May 2015 cycling (formation and dissolution of opal phytoliths and growth of diatoms). We applied the Ge/Si ratio to assess Accepted 1 June 2015 the different sources of dissolved Si in rivers hailing from the eastern Tibetan Plateau — the Salween, Mekong, Available online 3 June 2015 Chang Jiang (Yangtze), Hong (Red) and Huang He (Yellow) and from Mt. Baekdu — the Duman. Elevated riverine Keywords: Ge/Si ratios were observed in arid regions with high geothermal activity in the Salween, Chang Jiang and Mt. fl Germanium Baekdu streams. In the Huang He and Hong River basins geothermal in uence was not as pronounced, but Silicon weathering of sulfide- and coal-bearing minerals may be responsible for the high Ge/Si ratios. In rivers where in- Chang Jiang puts from hydrothermal and sulfide weathering are minimal, our data mostly fall in the weathering-limited re- Mekong gime of high riverine Si concentrations and low Ge/Si ratios.
    [Show full text]
  • • -Depth More Than 1.5M Figure 5C.15 Sai Gon–Moc Hoa Route (Ii) Sai
    • -Depth more than 1.5m Figure 5C.15 Sai Gon–Moc Hoa Route Grade Width Depth No Route Length Obstacle Project Present Target Present Plan Present Plan Sai Gon–Moc Hoa mainly III & improvement: widening, S3-1 96 III 30–150 50–70 1.9–8.0 1.5 bridge (Vam Co River) partially I removal of obstacles (ii) Sai Gon–Ben Suc Route Location • Route from Sai Gon Port along Sai Gon River to Ho Dau Tieng Dam in Tay Ninh Province. • This route lies on Sai Gon River with length of 89km. Main Role • Connection between Binh Duong and Ho Chi Minh City. • Port areas of Sai Gon, Ben Nghe and Tan Cang Ports and channel to Ha Tien ce- ment factory (section from Te channel confluence to Thanh Da) • Transportation of sand, gravel and wood from upstream to ports at Ho Chi Minh and Binh Duong provinces Target • Grade III • Width 50–70m • Depth more than 1.5m 5C-15 Figure 5C.16 Sai Gon–Ben Suc Route Grade Width Depth No Route Length Obstacle Project Present Target Present Plan Present Plan Sai Gon–Ben Suc I and III, improvement: re- S3-2 89 III 70–200 50–70 2.5–13.2 1.5 bridge (SaiGon River) partially II moval of obstacles (iii) Sai Gon–Ben Keo Route Location • Route between the northern area of Dong Thap Muoi with Ho Chi Minh City via rivers of Sai Gon, Nha Be, Soai Rap, Can Giuoc and Vam Co as well as Nuoc Man canal to Ben Keo on Vam Co Dong River with 165.7km in length Main Role • Connection of Tay Ninh and Long An, and Ho Chi Minh City and Mekong through Tay Ninh Province • Transportation of wood and construction materials to Ho Chi Minh City • Transportation
    [Show full text]