Yangtze River, an Insignificant Genetic Boundary in Tufted Deer
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Southwest Guangdong, 28 April to 7 May 1998
Report of Rapid Biodiversity Assessments at Qixingkeng Nature Reserve, Southwest Guangdong, 29 April to 1 May and 24 November to 1 December, 1998 Kadoorie Farm and Botanic Garden in collaboration with Guangdong Provincial Forestry Department South China Institute of Botany South China Agricultural University South China Normal University Xinyang Teachers’ College January 2002 South China Biodiversity Survey Report Series: No. 4 (Online Simplified Version) Report of Rapid Biodiversity Assessments at Qixingkeng Nature Reserve, Southwest Guangdong, 29 April to 1 May and 24 November to 1 December, 1998 Editors John R. Fellowes, Michael W.N. Lau, Billy C.H. Hau, Ng Sai-Chit and Bosco P.L. Chan Contributors Kadoorie Farm and Botanic Garden: Bosco P.L. Chan (BC) Lawrence K.C. Chau (LC) John R. Fellowes (JRF) Billy C.H. Hau (BH) Michael W.N. Lau (ML) Lee Kwok Shing (LKS) Ng Sai-Chit (NSC) Graham T. Reels (GTR) Gloria L.P. Siu (GS) South China Institute of Botany: Chen Binghui (CBH) Deng Yunfei (DYF) Wang Ruijiang (WRJ) South China Agricultural University: Xiao Mianyuan (XMY) South China Normal University: Chen Xianglin (CXL) Li Zhenchang (LZC) Xinyang Teachers’ College: Li Hongjing (LHJ) Voluntary consultants: Guillaume de Rougemont (GDR) Keith Wilson (KW) Background The present report details the findings of two field trips in Southwest Guangdong by members of Kadoorie Farm & Botanic Garden (KFBG) in Hong Kong and their colleagues, as part of KFBG's South China Biodiversity Conservation Programme. The overall aim of the programme is to minimise the loss of forest biodiversity in the region, and the emphasis in the first three years is on gathering up-to-date information on the distribution and status of fauna and flora. -
Mineralogy and Geochemistry of Nephrite Jade from Yinggelike Deposit, Altyn Tagh (Xinjiang, NW China)
minerals Article Mineralogy and Geochemistry of Nephrite Jade from Yinggelike Deposit, Altyn Tagh (Xinjiang, NW China) Ying Jiang 1, Guanghai Shi 1,* , Liguo Xu 2 and Xinling Li 3 1 State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China; [email protected] 2 Geological Museum of China, Beijing 100034, China; [email protected] 3 Xinjiang Uygur Autonomous Region Product Quality Supervision and Inspection Institute, Xinjiang 830004, China; [email protected] * Correspondence: [email protected]; Tel.: +86-010-8232-1836 Received: 6 April 2020; Accepted: 6 May 2020; Published: 8 May 2020 Abstract: The historic Yinggelike nephrite jade deposit in the Altyn Tagh Mountains (Xinjiang, NW China) is renowned for its gem-quality nephrite with its characteristic light-yellow to greenish-yellow hue. Despite the extraordinary gemological quality and commercial significance of the Yinggelike nephrite, little work has been done on this nephrite deposit, due to its geographic remoteness and inaccessibility. This contribution presents the first systematic mineralogical and geochemical studies on the Yinggelike nephrite deposit. Electron probe microanalysis, X-ray fluorescence (XRF) spectrometry, inductively coupled plasma mass spectrometry (ICP-MS) and isotope ratio mass spectrometry were used to measure the mineralogy, bulk-rock chemistry and stable (O and H) isotopes characteristics of samples from Yinggelike. Field investigation shows that the Yinggelike nephrite orebody occurs in the dolomitic marble near the intruding granitoids. Petrographic studies and EMPA data indicate that the nephrite is mainly composed of fine-grained tremolite, with accessory pargasite, diopside, epidote, allanite, prehnite, andesine, titanite, zircon, and calcite. Geochemical studies show that all nephrite samples have low bulk-rock Fe/(Fe + Mg) values (0.02–0.05), as well as low Cr (0.81–34.68 ppm), Co (1.10–2.91 ppm), and Ni (0.52–20.15 ppm) contents. -
Impacts of Re-Vegetation on Surface Soil Moisture Over the Chinese Loess Plateau Based on Remote Sensing Datasets
remote sensing Article Impacts of Re-Vegetation on Surface Soil Moisture over the Chinese Loess Plateau Based on Remote Sensing Datasets Qiao Jiao 1,†, Rui Li 1,2,3,*, Fei Wang 1,2,3,*,†, Xingmin Mu 1,2,3, Pengfei Li 2 and Chunchun An 2 1 College of Natural Resources and Environment, Northwest A&F University, Yangling 712100, China; [email protected] (Q.J.); [email protected] (X.M.) 2 Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, China; [email protected] (P.L.); [email protected] (C.A.) 3 Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, China * Correspondence: [email protected] (R.L.); [email protected] (F.W.); Tel.: +86-29-8701-9829 (R.L. & F.W.); Fax: +86-29-8701-2210 (R.L. & F.W.) † These authors contributed equally to this work. Academic Editors: Angela Lausch, Marco Heurich, Nicolas Baghdadi and Prasad S. Thenkabail Received: 4 November 2015; Accepted: 15 February 2016; Published: 19 February 2016 Abstract: A large-scale re-vegetation supported by the Grain for Green Project (GGP) has greatly changed local eco-hydrological systems, with an impact on soil moisture conditions for the Chinese Loess Plateau. It is important to know how, exactly, re-vegetation influences soil moisture conditions, which not only crucially constrain growth and distribution of vegetation, and hence, further re-vegetation, but also determine the degree of soil desiccation and, thus, erosion risk in the region. In this study, three eco-environmental factors, which are Soil Water Index (SWI), the Normalized Difference Vegetation Index (NDVI), and precipitation, were used to investigate the response of soil moisture in the one-meter layer of top soil to the re-vegetation during the GGP. -
DICTIONARY SUBJ1: Subject Headings
PINYIN CONVERSION SPECIFICATIONS DICTIONARIES FOR SUBJECT HEADINGS DICTIONARY SUBJ-2: Subject headings (geographics) OCTOBER 1, 2000 *AY* = (in former heading) ayn or apostrophe or alif *AP* = (in revised heading) apostrophe *U* = the lower case letter u with umlaut *UU* = the capital letter u with umlaut *N* = the lower case letter n with tilde *E* = the lower case letter e with circumflex Instructions: Replace WG form with PY equivalent 1 Instructions 1.1_ Identify a subject string which should either be converted from Wade-Giles to pinyin, or should not be converted 2.1 Mark and pass these subject strings where appropriate 3.1 In the 651$a subfield, replace these WG forms with PY equivalents: [chronological subdivisions are covered by Dictionary CHRON] Ling Canal (Hsing-an hsien, China) / Ling Canal (Xing*AP*an Xian, China) Chung-nan-hai (Peking, China) / Zhongnan Hai (Beijing, China) Fu ling Site (Shen-yang shih, China) / Fu Ling Site (Shenyang, Liaoning Sheng, China) Fu ling Site (Shenyang, Liaoning Sheng, China) / Fu Ling Site (Shenyang, Liaoning Sheng, China) I Ho Y*U*an (Peking, China) / Yi He Yuan (Beijing, China) Hsin kang kang chan ch*AY*iao (Dairen, China) / Xin Gang Gang Zhan Qiao (Dalian, Liaoning Sheng, China) Lei-ku-tun Site (Sui-chou, China) / Leigudun Site (Suizhou, China) Lei-ku-tun Site (Suizhou, China) / Leigudun Site (Suizhou, China) 2 Lu-chou Ch*AY*ang-chiang ta ch*AY*iao (Lu-chou shih, China) / Luzhou Chang Jiang Da Qiao (Luzhou, Sichuan Sheng, China) Lu-chou Ch*AY*ang-chiang ta ch*AY*iao (Luzhou, Sichuan Sheng, -
Quantifying Trends of Land Change in Qinghai-Tibet Plateau During 2001–2015
remote sensing Article Quantifying Trends of Land Change in Qinghai-Tibet Plateau during 2001–2015 Chao Wang, Qiong Gao and Mei Yu * Department of Environmental Sciences, University of Puerto Rico, Rio Piedras, San Juan, PR 00936, USA; [email protected] (C.W.); [email protected] (Q.G.) * Correspondence: [email protected]; Tel.: +1-787-764-0000 Received: 1 September 2019; Accepted: 17 October 2019; Published: 20 October 2019 Abstract: The Qinghai-Tibet Plateau (QTP) is among the most sensitive ecosystems to changes in global climate and human activities, and quantifying its consequent change in land-cover land-use (LCLU) is vital for assessing the responses and feedbacks of alpine ecosystems to global climate changes. In this study, we first classified annual LCLU maps from 2001–2015 in QTP from MODIS satellite images, then analyzed the patterns of regional hotspots with significant land changes across QTP, and finally, associated these trends in land change with climate forcing and human activities. The pattern of land changes suggested that forests and closed shrublands experienced substantial expansions in the southeastern mountainous region during 2001–2015 with the expansion of massive meadow loss. Agricultural land abandonment and the conversion by conservation policies existed in QTP, and the newly-reclaimed agricultural land partially offset the loss with the resulting net change of 5.1%. Although the urban area only expanded 586 km2, mainly at the expense of agricultural − land, its rate of change was the largest (41.2%). Surface water exhibited a large expansion of 5866 km2 (10.2%) in the endorheic basins, while mountain glaciers retreated 8894 km2 ( 3.4%) mainly in the − southern and southeastern QTP. -
Download From
Designation date: 07/12/2004 Ramsar Site no. 1441 Information Sheet on Ramsar Wetlands (RIS) – 2009-2012 version Available for download from http://www.ramsar.org/ris/key_ris_index.htm. Categories approved by Recommendation 4.7 (1990), as amended by Resolution VIII.13 of the 8th Conference of the Contracting Parties (2002) and Resolutions IX.1 Annex B, IX.6, IX.21 and IX. 22 of the 9th Conference of the Contracting Parties (2005). Notes for compilers: 1. The RIS should be completed in accordance with the attached Explanatory Notes and Guidelines for completing the Information Sheet on Ramsar Wetlands. Compilers are strongly advised to read this guidance before filling in the RIS. 2. Further information and guidance in support of Ramsar site designations are provided in the Strategic Framework and guidelines for the future development of the List of Wetlands of International Importance (Ramsar Wise Use Handbook 14, 3rd edition). A 4th edition of the Handbook is in preparation and will be available in 2009. 3. Once completed, the RIS (and accompanying map(s)) should be submitted to the Ramsar Secretariat. Compilers should provide an electronic (MS Word) copy of the RIS and, where possible, digital copies of all maps. 1. Name and address of the compiler of this form: FOR OFFICE USE ONLY. DD MM YY Name: Yuxiang Li Institution: Bureau of Liaoning Shuangtai Estuary National Nature Reserve Tel: +86-427-2287002 Designation date Site Reference Number Fax: +86-427-2287011 Address: Shiyou Street 121, Panjin City 124010, Liaoning Province, China. Email: [email protected] 2. Date this sheet was completed/updated: June 5, 2012 3. -
Amphibiaweb's Illustrated Amphibians of the Earth
AmphibiaWeb's Illustrated Amphibians of the Earth Created and Illustrated by the 2020-2021 AmphibiaWeb URAP Team: Alice Drozd, Arjun Mehta, Ash Reining, Kira Wiesinger, and Ann T. Chang This introduction to amphibians was written by University of California, Berkeley AmphibiaWeb Undergraduate Research Apprentices for people who love amphibians. Thank you to the many AmphibiaWeb apprentices over the last 21 years for their efforts. Edited by members of the AmphibiaWeb Steering Committee CC BY-NC-SA 2 Dedicated in loving memory of David B. Wake Founding Director of AmphibiaWeb (8 June 1936 - 29 April 2021) Dave Wake was a dedicated amphibian biologist who mentored and educated countless people. With the launch of AmphibiaWeb in 2000, Dave sought to bring the conservation science and basic fact-based biology of all amphibians to a single place where everyone could access the information freely. Until his last day, David remained a tirelessly dedicated scientist and ally of the amphibians of the world. 3 Table of Contents What are Amphibians? Their Characteristics ...................................................................................... 7 Orders of Amphibians.................................................................................... 7 Where are Amphibians? Where are Amphibians? ............................................................................... 9 What are Bioregions? ..................................................................................10 Conservation of Amphibians Why Save Amphibians? ............................................................................. -
Study on the Coniferous Characters of Pinus Yunnanensis and Its Clustering Analysis
Journal of Polymer Science and Engineering (2017) Original Research Article Study on the Coniferous Characters of Pinus yunnanensis and Its Clustering Analysis Zongwei Zhou,Mingyu Wang,Haikun Zhao Huangshan Institute of Botany, Anhui Province, China ABSTRACT Pine is a relatively easy genus for intermediate hybridization. It has been widely believed that there should be a natural hybrid population in the distribution of Pinus massoniona Lamb. and Pinus hangshuanensis Hsia, that is, the excessive type of external form between Pinus massoniana and Pinus taiwanensis exist. This paper mainly discusses the traits and clustering analysis of coniferous lozeng in Huangshan scenic area. This study will provide a theoretical basis for the classification of long and outstanding Huangshan Song and so on. At the same time, it will provide reference for the phenomenon of gene seepage between the two species. KEYWORDS: Pinus taiwanensis Pinus massoniana coniferous seepage clustering Citation: Zhou ZW, Wang MY, ZhaoHK, et al. Study on the Coniferous Characters of Pinus yunnanensis and Its Clustering Analysis, Gene Science and Engineering (2017); 1(1): 19–27. *Correspondence to: Haikun Zhao, Huangshan Institute of Botany, Anhui Province, China, [email protected]. 1. Introduction 1.1. Research background Huangshan Song distribution in eastern China’s subtropical high mountains, more than 700m above sea level. Masson pine is widely distributed in the subtropical regions of China, at the lower reaches of the Yangtze River, vertically distributed below 700m above sea level, the upper reaches of the Yangtze River area, the vertical height of up to 1200 - 1500m or so. In the area of Huangshan Song and Pinus massoniana, an overlapping area of Huangshan Song and Pinus massoniana was formed between 700 - 1000m above sea level. -
Royle Safaris Sichuan Mammals Tour Trip Report
In March 2019 Royle Safaris ran our second specialist Sichuan Mammals Tour with a focus on a particularly special species. The trip was run with Martin Royle, Roland Zeidler & Sid Francis as our guides. We visited 3 different locations (covering the rugged bamboo forests of the greater Wolong ecosystem, the high altitude grasslands of Rouergai and the wonderful forests of Tangjiahe. We were very successful with sightings of 44 different species of mammals and over 100 species of birds including Giant Panda, Red Panda, Pallas’s Cat, Chinese Mountain Cat, Indochinese Leopard Cat, Particoloured Flying Squirrel, Golden Snub-nosed Monkey, Chinese Ferret Badger, Eurasian Otter and Chinese Pipistrelle. We ran a second Sichuan’s Mammals Tour (back to back with this one) in April 2019 and we had even more success in some areas. The sightings log for that trip will follow in a few days. We have started to promote our 2020 Sichuan Mammals Tour (with special focus on a particular special species for half of the trip); we have already received many bookings on these two trips. Our first tour for 2020 (9th – 22nd March 2020) has just one place remaining and our second tour for 2020 (25th April – 8th May 2020) which also has only one place remaining. We have also started offering places on another specialist mammal tour of China, visiting Qinghai and the wonderful Valley of the Cats. This tour is for July 2020 (1st – 15th July 2020) and focuses on Snow leopards, Eurasian lynx, Himalayan wolf, Himalayan brown bear, Tibetan antelope, Wild Yak, White-lipped deer, Alpine musk deer, Glover’s pika, Bharal, McNeil’s deer and many more species. -
Portfolio Investment Opportunities in China Democratic Revolution in China, Was Launched There
Morgan Stanley Smith Barney Investment Strategy The Great Wall of China In c. 220 BC, under Qin Shihuangdi (first emperor of the Qin dynasty), sections of earlier fortifications were joined together to form a united system to repel invasions from the north. Construction of the Great Wall continued for more than 16 centuries, up to the Ming dynasty (1368–1644), National Emblem of China creating the world's largest defense structure. Source: About.com, travelchinaguide.com. The design of the national emblem of the People's Republic of China shows Tiananmen under the light of five stars, and is framed with ears of grain and a cogwheel. Tiananmen is the symbol of modern China because the May 4th Movement of 1919, which marked the beginning of the new- Portfolio Investment Opportunities in China democratic revolution in China, was launched there. The meaning of the word David M. Darst, CFA Tiananmen is “Gate of Heavenly Succession.” On the emblem, the cogwheel and the ears of grain represent the working June 2011 class and the peasantry, respectively, and the five stars symbolize the solidarity of the various nationalities of China. The Han nationality makes up 92 percent of China’s total population, while the remaining eight percent are represented by over 50 nationalities, including: Mongol, Hui, Tibetan, Uygur, Miao, Yi, Zhuang, Bouyei, Korean, Manchu, Kazak, and Dai. Source: About.com, travelchinaguide.com. Please refer to important information, disclosures, and qualifications at the end of this material. Morgan Stanley Smith Barney Investment Strategy Table of Contents The Chinese Dynasties Section 1 Background Page 3 Length of Period Dynasty (or period) Extent of Period (Years) Section 2 Issues for Consideration Page 65 Xia c. -
Article-Lanzhou
13 by He Yuanqing, Yao Tandong, Cheng Guodong, and Yang Meixue Climatic records in a firn core from an Alpine temperate glacier on Mt. Yulong, southeastern part of the Tibetan Plateau Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 73000, China. Mt. Yulong is the southernmost glacier-covered area in Asian southwestern monsoon climate. Their total area is 11.61 km2. Eurasia, including China. There are 19 sub-tropical The glaciers resemble a group of flying dragons, giving Mt. Yulong temperate glaciers on the mountain, controlled by the (white dragon) as its name. Many explorers, tourists, poets and scientists have described southwestern monsoon climate. In the summer of 1999, Mt. Yulong from different points of view (Ward, 1924; Wissmann, a firn core, 10.10 m long, extending down to glacier ice, 1937). However, as they were unable to cross the extremely steep was recovered in the accumulation area of the largest mountain slopes and the forested area to the glacier above 4000 m a.s.l., some reported data were not correct. Most of the literature has glacier, Baishui No.1. Periodic variations of climatic focussed on the alpine landscape and the snow scenery, and there are signals above 7.8 m depth were apparent, and net accu- few accounts of the existing glaciers. Ren et al (1957) and Luo and mulation of four years was identified by the annual Yang (1963) first reported the distribution of these glaciers and of the late Pleistocene glacial landforms. To clarify the scale of glacia- oscillations of isotopic and ionic composition. -
Diversity and Geographical Pattern of Altitudinal Belts in the Hengduan Mountains in China
J. Mt. Sci. (2010) 7: 123–132 DOI: 10.1007/s11629-010-1011-9 Diversity and Geographical Pattern of Altitudinal Belts in the Hengduan Mountains in China YAO Yonghui, ZHANG Baiping*, HAN Fang, and PANG Yu Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China. E-mail: [email protected] * Corresponding author, e-mail: [email protected] © Science Press and Institute of Mountain Hazards and Environment, CAS and Springer-Verlag Berlin Heidelberg 2010 Abstract: This paper analyses the diversity and effect needs further study. In addition, the data spatial pattern of the altitudinal belts in the quality and data accuracy at present also affect to Hengduan Mountains in China. A total of 7 types of some extent the result of quantitative modeling and base belts and 26 types of altitudinal belts are should be improved with RS/GIS in the future. identified in the study region. The main altitudinal belt lines, such as forest line, the upper limit of dark Keywords: Hengduan Mountains; Altitudinal belt coniferous forest and snow line, have similar spectra; Exposure effect; Quadratic model latitudinal and longitudinal spatial patterns, namely, arched quadratic curve model with latitudes and concave quadratic curve model along longitudinal Introduction direction. These patterns can be together called as “Hyperbolic-paraboloid model”, revealing the complexity and speciality of the environment and Globally and generally, the upper and lower ecology in the study region. This result further limits of altitudinal belts vary (increase) from high validates the hypnosis of a common quadratic model latitudes to low latitudes, from continental for spatial pattern of mountain altitudinal belts peripheries to inland areas, and from very humid proposed by the authors.