Pan-Third Pole region; human activities; Eastern and Western cultural exchanges; environmental change; Silk Road
The Third Pole Region mainly includes the Tibetan Plateau and the arid central Asia, spanning from the Caucasus mountains to the Loess plateau. Located in the hinterland of the Eurasian continent, different ethnic groups and cultures in this area experienced complex and long-term contact, communication, fusion, and sedimentary accretion, opening up a convenient channel for exchanges between Eastern and Western civilizations, profoundly influencing the development process of human civilization. Study on the human activities, change of environment and their relationship between the rise and fall of the Silk Road, and analysis of social environment development of this key area, will benefit the countries along the Silk Road to built mutual trust and cultural identity. Such study has very important theoretical and practical significance, providing the historical reference for the construction of green Silk Road.
Bulletin of Chinese Academy of Sciences
Chen F, Yu Z, Yang M, et al. Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history. Quaternary Science Reviews, 2008, 27(3-4):351-364.
Dennell R W. The Nihewan Basin of North China in the Early Pleistocene:Continuous and flourishing, or discontinuous, infrequent and ephemeral occupation? Quaternary International, 2013, 295:223-236.
Madsen D B, Li J Z, Brantingham P J, et al. Dating Shuidonggou and the Upper Palaeolithic blade industry in North China. Antiquity, 2001, 75(290):706-716.
Li F, Kuhn S L, Gao X, et al. Re-examination of the dates of large blade technology in China:A comparison of Shuidonggou Locality 1 and Locality 2. J Hum Evol, 2013, 64(2):161-168.
Arnason U. A phylogenetic view of the Out of Asia/Eurasia and Out of Africa hypotheses in the light of recent. molecular and palaeontological finds. Gene, 2017, 627:473-476.
Meyer M C, Aldenderfer M S, Wang Z, et al. Permanent human occupation of the central Tibetan Plateau in the early Holocene. Science, 2017, 355(6320):64-67.
Zhang D, Zhang N, Wang J, et al. Comment on "Permanent human occupation of the central Tibetan Plateau in the early Holocene". Science, 2017, 357(6351):64-67.
Madsen D B, Haizhou M, Brantingham P J, et al. The Late Upper Paleolithic occupation of the northern Tibetan Plateau margin. Journal of Archaeological Science, 2006, 33(10):1433-1444.
Zhao M, Kong Q-P, Wang H-W, et al. Mitochondrial genome evidence reveals successful Late Paleolithic settlement on the Tibetan Plateau. PNAS, 2009, 106(50):21230-21235.
张东菊, 董广辉, 王辉, 等.史前人类向青藏高原扩散的历史过程和可能驱动机制.中国科学:地球科学, 2016, 46(8):1007-1023.
Zeder M A. Domestication and early agriculture in the Mediterranean Basin:Origins, diffusion, and impact. PNAS, 2008, 105:11597-11604.
Zhao Z J. New archaeobotanic data for the study of the origins of agriculture in China. Current Anthropology, 2011, 52:S295-S306.
Jones M K, Hunt H, Lightfoot E, et al. Food globalization in prehistory. World Archaeology, 2011, 43:665-675.
Dong G H, Yang Y S, Han J Y, et al. Exploring the history of cultural exchange in prehistoric Eurasia from the perspectives of crop diffusion and consumption. Science China Earth Sciences, 2017, 60:1-14.
Frachetti M D, Smith C E, Traub C M, et al. Nomadic ecology shaped the highland geography of Asia's Silk Roads. Nature, 2017, 543:193-198.
Frankopan P. The Silk Roads:A New History of the World. London:Bloomsbury Publishing, 2015.
Wood F. The Silk Road:Two Thousand Years in the Heart of Asia. Oakland:University of California Press, 2002.
Sun X J, Wang P X. How old is the Asian monsoon system? -Palaeobotanical records from China. Palaeogeography, Palaeoclimatology, Palaeoecology, 2005, 222(4):181-222.
Guo Z T, Ruddiman W F, Hao Q Z, et al. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China. Nature, 2002, 416:159-163.
姚檀栋, 施雅风, 秦大河, 等.古里雅冰芯中末次间冰期以来气候变化记录研究.中国科学:地球科学, 1997, 27(5):447-452.
Ding Z L, Ranov V, Yang S L, et al. The loess record in southern Tajikistan and correlation with Chinese loess. Earth and Planetary Science Letters, 2002, 200(3):387-400.
李吉均.中国西北地区晚更新世以来环境变迁模式.第四纪研究, 1990, 10(3):197-204.
Li G, Rao Z, Duan Y, et al. Paleoenvironmental changes recorded in a luminescence dated loess/paleosol sequence from the Tianshan Mountains, arid central Asia, since the Penultimate Glaciation. Earth and Planetary Science Letters, 2016, 448:1-12.
Zhao Y, An C B, Mao L, et al. Vegetation and climate history in arid western China during MIS2:New insights from pollen and grain-size data of the Balikun Lake, eastern Tien Shan. Quaternary Science Reviews, 2015, 126:112-125.
Wang W, Feng Z D. Holocene moisture evolution across the Mongolian Plateau and its surrounding areas:A synthesis of climatic records. Earth Science Reviews, 2013, 122:38-57.
Chen F H, Jia J, Chen J H, et al. A persistent Holocene wetting trend in arid central Asia, with wettest conditions in the late Holocene, revealed by multi-proxy analyses of loess-paleosol sequences in Xinjiang, China. Quaternary Science Reviews, 2016, 146:134-146.
安成邦, 王伟, 段阜涛, 等.亚洲中部干旱区丝绸之路沿线环境演化与东西方文化交流.地理学报, 2017, 72(5):875-891.
Chen F, Dong G, Zhang D, et al. Agriculture facilitated permanent human occupation of the Tibetan Plateau after 3600 B.P. Science, 2015, 60:1-14.
周伟洲, 丁景泰.丝绸之路大辞典.西安:陕西人民出版社, 2006:1-2.
Fahu, Chen; Chengbang, An; Guanghui, Dong; and Dongju, Zhang
"Human Activities, Environmental Changes, and Rise and Decline of Silk Road Civilization in Pan-Third Pole Region,"
Bulletin of Chinese Academy of Sciences (Chinese Version): Vol. 32
, Article 6.
Available at: https://bulletinofcas.researchcommons.org/journal/vol32/iss9/6