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Spatiotemporal Changes and the Driving Forces of Sloping Farmland Areas in the Sichuan Region
sustainability Article Spatiotemporal Changes and the Driving Forces of Sloping Farmland Areas in the Sichuan Region Meijia Xiao 1 , Qingwen Zhang 1,*, Liqin Qu 2, Hafiz Athar Hussain 1 , Yuequn Dong 1 and Li Zheng 1 1 Agricultural Clean Watershed Research Group, Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences/Key Laboratory of Agro-Environment, Ministry of Agriculture, Beijing 100081, China; [email protected] (M.X.); [email protected] (H.A.H.); [email protected] (Y.D.); [email protected] (L.Z.) 2 State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100048, China; [email protected] * Correspondence: [email protected]; Tel.: +86-10-82106031 Received: 12 December 2018; Accepted: 31 January 2019; Published: 11 February 2019 Abstract: Sloping farmland is an essential type of the farmland resource in China. In the Sichuan province, livelihood security and social development are particularly sensitive to changes in the sloping farmland, due to the region’s large portion of hilly territory and its over-dense population. In this study, we focused on spatiotemporal change of the sloping farmland and its driving forces in the Sichuan province. Sloping farmland areas were extracted from geographic data from digital elevation model (DEM) and land use maps, and the driving forces of the spatiotemporal change were analyzed using a principal component analysis (PCA). The results indicated that, from 2000 to 2015, sloping farmland decreased by 3263 km2 in the Sichuan province. The area of gently sloping farmland (<10◦) decreased dramatically by 1467 km2, especially in the capital city, Chengdu, and its surrounding areas. -
Crop Systems on a County-Scale
Supporting information Chinese cropping systems are a net source of greenhouse gases despite soil carbon sequestration Bing Gaoa,b, c, Tao Huangc,d, Xiaotang Juc*, Baojing Gue,f, Wei Huanga,b, Lilai Xua,b, Robert M. Reesg, David S. Powlsonh, Pete Smithi, Shenghui Cuia,b* a Key Lab of Urban Environment and Health, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen 361021, China b Xiamen Key Lab of Urban Metabolism, Xiamen 361021, China c College of Resources and Environmental Sciences, Key Laboratory of Plant-soil Interactions of MOE, China Agricultural University, Beijing 100193, China d College of Geography Science, Nanjing Normal University, Nanjing 210046, China e Department of Land Management, Zhejiang University, Hangzhou, 310058, PR China f School of Agriculture and Food, The University of Melbourne, Victoria, 3010 Australia g SRUC, West Mains Rd. Edinburgh, EH9 3JG, Scotland, UK h Department of Sustainable Agriculture Sciences, Rothamsted Research, Harpenden, AL5 2JQ. UK i Institute of Biological and Environmental Sciences, University of Aberdeen, Aberdeen AB24 3UU, UK Bing Gao & Tao Huang contributed equally to this work. Corresponding author: Xiaotang Ju and Shenghui Cui College of Resources and Environmental Sciences, Key Laboratory of Plant-soil Interactions of MOE, China Agricultural University, Beijing 100193, China. Phone: +86-10-62732006; Fax: +86-10-62731016. E-mail: [email protected] Institute of Urban Environment, Chinese Academy of Sciences, 1799 Jimei Road, Xiamen 361021, China. Phone: +86-592-6190777; Fax: +86-592-6190977. E-mail: [email protected] S1. The proportions of the different cropping systems to national crop yields and sowing area Maize was mainly distributed in the “Corn Belt” from Northeastern to Southwestern China (Liu et al., 2016a). -
Science Journals — AAAS
RESEARCH ◥ the lake level could not exceed 1975 m asl (25 to TECHNICAL RESPONSE 50 m lower than we reconstruct) due to a low divide upstream of the dam (3); however, Han’s datum is obtained from Google Earth, whereas ARCHAEOLOGY a more accurate 1:50,000 topographic map shows that it is ~2010 m asl, within our range. More- over, the sharp crest at this site suggests that it Response to Comments on “Outburst mayhavebeenloweredbymasswastingoverthe past 4000 years. flood at 1920 BCE supports Huang et al.(4) argue that there is no sedi- mentary evidence to support the maximum level historicity of China’s Great Flood of the dammed lake. This is true because the lake with level above 1890 m asl only existed for a few months, and at its peak (~2000 to 2025 m and the Xia dynasty” asl), only for a few days, too short to leave behind sediments that would have survived subsequent Qinglong Wu,1,2* Zhijun Zhao,1,2 Li Liu,3† Darryl E. Granger,4 Hui Wang,5 subaerial exposure. The lacustrine (not fluvial) sediments in Jishi Gorge represent the remnant David J. Cohen,6† Xiaohong Wu,7 Maolin Ye,5 Ofer Bar-Yosef,8 Bin Lu,9 Jin Zhang,10 lake, which persisted long after the breach and Peizhen Zhang,11 Daoyang Yuan,12 Wuyun Qi,5 Linhai Cai,13 Shibiao Bai1,2 was gradually filled in (1). Lacustrine sediment in Jishi Gorge was previ- Downloaded from Wu et al., Han, and Huang et al. question our reconstruction of a large outburst flood ously dated to ~8000 to 5500 years before the and its possible relationship to China’s Great Flood and the Xia dynasty. -
Ceramic's Influence on Chinese Bronze Development
Ceramic’s Influence on Chinese Bronze Development Behzad Bavarian and Lisa Reiner Dept. of MSEM College of Engineering and Computer Science September 2007 Photos on cover page Jue from late Shang period decorated with Painted clay gang with bird, fish and axe whorl and thunder patterns and taotie design from the Neolithic Yangshao creatures, H: 20.3 cm [34]. culture, H: 47 cm [14]. Flat-based jue from early Shang culture Pou vessel from late Shang period decorated decorated with taotie beasts. This vessel with taotie creatures and thunder patterns, H: is characteristic of the Erligang period, 24.5 cm [34]. H: 14 cm [34]. ii Table of Contents Abstract Approximate timeline 1 Introduction 2 Map of Chinese Provinces 3 Neolithic culture 4 Bronze Development 10 Clay Mold Production at Houma Foundry 15 Coins 16 Mining and Smelting at Tonglushan 18 China’s First Emperor 19 Conclusion 21 References 22 iii The transition from the Neolithic pottery making to the emergence of metalworking around 2000 BC held significant importance for the Chinese metal workers. Chinese techniques sharply contrasted with the Middle Eastern and European bronze development that relied on annealing, cold working and hammering. The bronze alloys were difficult to shape by hammering due to the alloy combination of the natural ores found in China. Furthermore, China had an abundance of clay and loess materials and the Chinese had spent the Neolithic period working with and mastering clay, to the point that it has been said that bronze casting was made possible only because the bronze makers had access to superior ceramic technology. -
Chinese Research Perspectives on the Environment, Volume 1 Chinese Research Perspectives: Environment
Chinese Research Perspectives on the Environment, Volume 1 Chinese Research Perspectives: Environment International Advisory Board Judith Shapiro, American University Guobin Yang, University of Pennsylvania Erika Scull VOLUME 1 The titles published in this series are listed at brill.com/crp Chinese Research Perspectives on the Environment, Volume 1 Urban Challenges, Public Participation, and Natural Disasters Edited by Yang Dongping Friends of Nature LEIDEN • bOSTON 2013 This book is the result of a copublication agreement between Social Sciences Academic Press and Koninklijke Brill NV. These articles were selected and translated into English from the original 《中国 环境发展报告 (2011)》(Zhongguo huanjing fazhan baogao 2011) and《中国 环境发展 报告 (2012)》(Zhongguo huanjing fazhan baogao 2012) with the financial support of the Chinese Fund for the Humanities and Social Sciences. This publication has been typeset in the multilingual “Brill” typeface. With over 5,100 characters covering Latin, IPA, Greek, and Cyrillic, this typeface is especially suitable for use in the humanities. For more information, please see www.brill.com/brill-typeface. ISSN 2212-7496 ISBN 978-90-04-24953-0 (hardback) ISBN 978-90-04-24954-7 (e-book) Copyright 2013 by Koninklijke Brill NV, Leiden, The Netherlands. Koninklijke Brill NV incorporates the imprints Brill, Global Oriental, Hotei Publishing, IDC Publishers and Martinus Nijhoff Publishers. All rights reserved. No part of this publication may be reproduced, translated, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, without prior written permission from the publisher. Authorization to photocopy items for internal or personal use is granted by Koninklijke Brill NV provided that the appropriate fees are paid directly to The Copyright Clearance Center, 222 Rosewood Drive, Suite 910, Danvers, MA 01923, USA. -
Originally, the Descendants of Hua Xia Were Not the Descendants of Yan Huang
E-Leader Brno 2019 Originally, the Descendants of Hua Xia were not the Descendants of Yan Huang Soleilmavis Liu, Activist Peacepink, Yantai, Shandong, China Many Chinese people claimed that they are descendants of Yan Huang, while claiming that they are descendants of Hua Xia. (Yan refers to Yan Di, Huang refers to Huang Di and Xia refers to the Xia Dynasty). Are these true or false? We will find out from Shanhaijing ’s records and modern archaeological discoveries. Abstract Shanhaijing (Classic of Mountains and Seas ) records many ancient groups of people in Neolithic China. The five biggest were: Yan Di, Huang Di, Zhuan Xu, Di Jun and Shao Hao. These were not only the names of groups, but also the names of individuals, who were regarded by many groups as common male ancestors. These groups first lived in the Pamirs Plateau, soon gathered in the north of the Tibetan Plateau and west of the Qinghai Lake and learned from each other advanced sciences and technologies, later spread out to other places of China and built their unique ancient cultures during the Neolithic Age. The Yan Di’s offspring spread out to the west of the Taklamakan Desert;The Huang Di’s offspring spread out to the north of the Chishui River, Tianshan Mountains and further northern and northeastern areas;The Di Jun’s and Shao Hao’s offspring spread out to the middle and lower reaches of the Yellow River, where the Di Jun’s offspring lived in the west of the Shao Hao’s territories, which were near the sea or in the Shandong Peninsula.Modern archaeological discoveries have revealed the authenticity of Shanhaijing ’s records. -
The Impacts of Climate Change on the Neolithic Cultures of Gansu-Qinghai Region During the Late Holocene Megathermal
See discussions, stats, and author profiles for this publication at: http://www.researchgate.net/publication/225224713 The impacts of climate change on the Neolithic cultures of Gansu-Qinghai region during the late Holocene Megathermal ARTICLE in JOURNAL OF GEOGRAPHICAL SCIENCES · JUNE 2010 Impact Factor: 1.34 · DOI: 10.1007/s11442-010-0417-1 CITATIONS READS 12 31 6 AUTHORS, INCLUDING: Hou Guangliang Qinghai Normal University 14 PUBLICATIONS 40 CITATIONS SEE PROFILE Available from: Hou Guangliang Retrieved on: 02 December 2015 J. Geogr. Sci. 2010, 20(3): 417-430 DOI: 10.1007/s11442-010-0417-1 © 2010 Science China Press Springer-Verlag The impacts of climate change on the Neolithic cultures of Gansu-Qinghai region during the late Holocene Megathermal LIU Fenggui1,2,3, ZHANG Yili3, FENG Zhaodong4, HOU Guangliang2, ZHOU Qiang2, ZHANG Haifeng2 1. School of Geography, Beijing Normal University, Beijing 100875, China; 2. School of Life and Geographic Science, Qinghai Normal University, Xining 810008, China; 3. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China; 4. Key Laboratory of Western China's Environmental Systems (Ministry of Education), Lanzhou University, Lanzhou 730000, China Abstract: The Holocene Megathermal is divided into early, middle and late periods, each having different impacts on the Neolithic cultures due to their different climate changing trends. This study is based on a comparative analysis of the environmental evolution information recorded in the Qinghai Lake, the western edge of the Loess Plateau and Zoige and the spa- tial distribution of Neolithic sites of the Gansu-Qinghai region. Results show that the early and middle periods towards warm and humid promoted the development of Neolithic cultures with agriculture as the main sector in the Gansu-Qinghai region, furthermore a heyday of Yang- shao Culture prosperity emerged. -
Adaptation and Invention During the Spread of Agriculture to Southwest China
Adaptation and Invention during the Spread of Agriculture to Southwest China The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation D'Alpoim Guedes, Jade. 2013. Adaptation and Invention during the Spread of Agriculture to Southwest China. Doctoral dissertation, Harvard University. Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:11002762 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA Adaptation and Invention during the Spread of Agriculture to Southwest China A dissertation presented by Jade D’Alpoim Guedes to The Department of Anthropology in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the subject of Anthropology Harvard University Cambridge, Massachusetts March 2013 © 2013 – Jade D‘Alpoim Guedes All rights reserved Professor Rowan Flad (Advisor) Jade D’Alpoim Guedes Adaptation and Invention during the Spread of Agriculture to Southwest China Abstract The spread of an agricultural lifestyle played a crucial role in the development of social complexity and in defining trajectories of human history. This dissertation presents the results of research into how agricultural strategies were modified during the spread of agriculture into Southwest China. By incorporating advances from the fields of plant biology and ecological niche modeling into archaeological research, this dissertation addresses how humans adapted their agricultural strategies or invented appropriate technologies to deal with the challenges presented by the myriad of ecological niches in southwest China. -
The Zhuan Xupeople Were the Founders of Sanxingdui Culture and Earliest Inhabitants of South Asia
E-Leader Bangkok 2018 The Zhuan XuPeople were the Founders of Sanxingdui Culture and Earliest Inhabitants of South Asia Soleilmavis Liu, Author, Board Member and Peace Sponsor Yantai, Shangdong, China Shanhaijing (Classic of Mountains and Seas) records many ancient groups of people (or tribes) in Neolithic China. The five biggest were: Zhuan Xu, Di Jun, Huang Di, Yan Di and Shao Hao.However, the Zhuan Xu People seemed to have disappeared when the Yellow and Chang-jiang river valleys developed into advanced Neolithic cultures. Where had the Zhuan Xu People gone? Abstract: Shanhaijing (Classic of Mountains and Seas) records many ancient groups of people in Neolithic China. The five biggest were: Zhuan Xu, Di Jun, Huang Di, Yan Di and Shao Hao. These were not only the names of individuals, but also the names of groups who regarded them as common male ancestors. These groups used to live in the Pamirs Plateau, later spread to other places of China and built their unique ancient cultures during the Neolithic Age. Shanhaijing reveals Zhuan Xu’s offspring lived near the Tibetan Plateau in their early time. They were the first who entered the Tibetan Plateau, but almost perished due to the great environment changes, later moved to the south. Some of them entered the Sichuan Basin and became the founders of Sanxingdui Culture. Some of them even moved to the south of the Tibetan Plateau, living near the sea. Modern archaeological discoveries have revealed the authenticity of Shanhaijing ’s records. Keywords: Shanhaijing; Neolithic China, Zhuan Xu, Sanxingdui, Ancient Chinese Civilization Introduction Shanhaijing (Classic of Mountains and Seas) records many ancient groups of people in Neolithic China. -
2 Days Leshan Giant Buddha and Mount Emei Tour
[email protected] +86-28-85593923 2 days Leshan Giant Buddha and Mount Emei tour https://windhorsetour.com/emei-leshan-tour/leshan-emei-2-day-tour Chengdu Mount Emei Leshan Chengdu A classic trip to Leshan and Mount Emei only takes 2 days. Leshan Grand Buddha is the biggest sitting Buddha in the world and Mount Emei is one of the four Buddhist Mountains in China. Type Private Duration 2 days Theme Culture and Heritage Trip code WS-302 From £ 214 per person £ 195 you save £ 19 (10%) Itinerary Mt.Emei lies in the southern area of Sichuan basin. It is one of the four sacred Buddhist Mountains in China. It is towering, beautiful, old and mysterious and is like a huge green screen standing in the southwest of the Chengdu Plain. Its main peak, the Golden Summit, is 3099 meters above the sea level, seemingly reaching the sky. Standing on the top of it, you can enjoy the snowy mountains in the west and the vast plain in the east. In addition in Golden Summit there are four spectacles: clouds sea, sunrise, Buddha rays and saint lamps. Leshan Grand Buddha is the biggest sitting Buddha in the world. It was begun to built in 713AD in Tang Dynasty, took more than 90 years to finish this huge statue. And it sits at Lingyue Mountain, at the Giant Buddha Cliff, you will find out a lot of stunning small buddha caves, you will be astonished by this human project. Leshan Grand Buddha and Mt.Emei both were enlisted in the world natural and cultural heritage by the UNESCO in 1996. -
Cultic Practices of the Bronze Age Chengdu Plain
SINO-PLATONIC PAPERS Number 149 May, 2005 A Sacred Trinity: God, Mountain and Bird. Cultic Practices of the Bronze Age Chengdu Plain by Kimberley S. Te Winkle Victor H. Mair, Editor Sino-Platonic Papers Department of East Asian Languages and Civilizations University of Pennsylvania Philadelphia, PA 19104-6305 USA [email protected] www.sino-platonic.org SINO-PLATONIC PAPERS FOUNDED 1986 Editor-in-Chief VICTOR H. MAIR Associate Editors PAULA ROBERTS MARK SWOFFORD ISSN 2157-9679 (print) 2157-9687 (online) SINO-PLATONIC PAPERS is an occasional series dedicated to making available to specialists and the interested public the results of research that, because of its unconventional or controversial nature, might otherwise go unpublished. The editor-in-chief actively encourages younger, not yet well established, scholars and independent authors to submit manuscripts for consideration. Contributions in any of the major scholarly languages of the world, including romanized modern standard Mandarin (MSM) and Japanese, are acceptable. In special circumstances, papers written in one of the Sinitic topolects (fangyan) may be considered for publication. Although the chief focus of Sino-Platonic Papers is on the intercultural relations of China with other peoples, challenging and creative studies on a wide variety of philological subjects will be entertained. This series is not the place for safe, sober, and stodgy presentations. Sino- Platonic Papers prefers lively work that, while taking reasonable risks to advance the field, capitalizes on brilliant new insights into the development of civilization. Submissions are regularly sent out to be refereed, and extensive editorial suggestions for revision may be offered. Sino-Platonic Papers emphasizes substance over form. -
Holocene Environmental Archaeology of the Yangtze River Valley in China: a Review
land Review Holocene Environmental Archaeology of the Yangtze River Valley in China: A Review Li Wu 1,2,*, Shuguang Lu 1, Cheng Zhu 3, Chunmei Ma 3, Xiaoling Sun 1, Xiaoxue Li 1, Chenchen Li 1 and Qingchun Guo 4 1 Provincial Key Laboratory of Earth Surface Processes and Regional Response in the Yangtze-Huaihe River Basin, School of Geography and Tourism, Anhui Normal University, Wuhu 241002, China; [email protected] (S.L.); [email protected] (X.S.); [email protected] (X.L.); [email protected] (C.L.) 2 State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China 3 School of Geograpy and Ocean Science, Nanjing University, Nanjing 210023, China; [email protected] (C.Z.); [email protected] (C.M.) 4 School of Environment and Planning, Liaocheng University, Liaocheng 252000, China; [email protected] * Correspondence: [email protected] Abstract: The Yangtze River Valley is an important economic region and one of the cradles of human civilization. It is also the site of frequent floods, droughts, and other natural disasters. Conducting Holocene environmental archaeology research in this region is of great importance when studying the evolution of the relationship between humans and the environment and the interactive effects humans had on the environment from 10.0 to 3.0 ka BP, for which no written records exist. This Citation: Wu, L.; Lu, S.; Zhu, C.; review provides a comprehensive summary of materials that have been published over the past Ma, C.; Sun, X.; Li, X.; Li, C.; Guo, Q.