2021 Vol. 41, No. 3
Article Contents

ZHANG Ling, YANG Xiaoqiang, SHANG Shengtan, ZHANG Tingwei, LI Guanhua, RUAN Jiaoyang. Tropical rainfall variations and human activities of last 1 000 years recorded by lake deposits on the Dongdao Island, Xisha Islands[J]. Marine Geology & Quaternary Geology, 2021, 41(3): 182-192. doi: 10.16562/j.cnki.0256-1492.2021031603
Citation: ZHANG Ling, YANG Xiaoqiang, SHANG Shengtan, ZHANG Tingwei, LI Guanhua, RUAN Jiaoyang. Tropical rainfall variations and human activities of last 1 000 years recorded by lake deposits on the Dongdao Island, Xisha Islands[J]. Marine Geology & Quaternary Geology, 2021, 41(3): 182-192. doi: 10.16562/j.cnki.0256-1492.2021031603

Tropical rainfall variations and human activities of last 1 000 years recorded by lake deposits on the Dongdao Island, Xisha Islands

More Information
  • A series of paleoclimate researches have been made in the South China Sea for the past 1000 years, that provided the insights to the understanding of regional climate change pattern and served as the basis to predict and evaluate the future trends of climate change under the joint actions of the human and the nature. Numerous natural archives and proxies are adopted to reveal the climate changes in different regions of China influenced by monsoon and tropical ocean processes. However, due to the lack of high-resolution climate records, our knowledge about the link between precipitation patterns and monsoon variability remains incomplete, particularly in the tropical region. In order to study the rainfall patterns and the history of anthropogenic activities in tropical zones during the time of AD 1000—1700, we studied such proxies as grain-size distribution and magnetic parameters collected from the sediments of the Cattle Pond on the Dongdao Island of the Xisha Islands. The results show that the precipitation on the Dongdao Island is mainly influenced by ENSO activities and the movements of the Intertropical Convergence Zone. Both of the factors will increase rainfall in the study area, which is opposed to the pattern of the Monsoon system. Human activities on the island were vigorous during the Southern Song Dynasty and the Late Ming Dynasty when the climate is humid and rich in rainfall. There are two periods characterized by sandstorms occurred in northern China during the time of AD 1000—1200 and AD 1450—1600 respectively in the Xisha Islands, reflecting the long-distance migration and precipitation of dust by air.

  • 加载中
  • [1] Oppo D W, Rosenthal Y, Linsley B K. 2, 000-year-long temperature and hydrology reconstructions from the indo-pacific warm pool [J]. Nature, 2009, 460(7259): 1113-1116. doi: 10.1038/nature08233

    CrossRef Google Scholar

    [2] Mann M E, Zhang Z H, Rutherford S, et al. Global signatures and dynamical origins of the little ice age and medieval climate anomaly [J]. Science, 2009, 326(5957): 1256-1260. doi: 10.1126/science.1177303

    CrossRef Google Scholar

    [3] Yan H, Sun L G, Wang Y H, et al. A record of the southern oscillation index for the past 2, 000 years from precipitation proxies [J]. Nature Geoscience, 2011, 4(9): 611-614. doi: 10.1038/ngeo1231

    CrossRef Google Scholar

    [4] Yan H, Wei W, Soon W, et al. Dynamics of the intertropical convergence zone over the western pacific during the little ice age [J]. Nature Geoscience, 2015, 8(4): 315-320. doi: 10.1038/ngeo2375

    CrossRef Google Scholar

    [5] Wang Y J, Cheng H, Edwards R L, et al. The holocene asian monsoon: links to solar changes and north atlantic climate [J]. Science, 2005, 308(5723): 854-857. doi: 10.1126/science.1106296

    CrossRef Google Scholar

    [6] Gu Y S, Liu H Y, Traoré D D, et al. ENSO-related droughts and ISM variations during the last millennium in tropical southwest China [J]. Climate Dynamics, 2020, 54(1): 649-659.

    Google Scholar

    [7] Tan L C, Cai Y J, Cheng H, et al. High resolution monsoon precipitation changes on southeastern tibetan plateau over the past 2300 years [J]. Quaternary Science Reviews, 2018, 195: 122-132. doi: 10.1016/j.quascirev.2018.07.021

    CrossRef Google Scholar

    [8] Yamoah K A, Chabangborn A, Chawchai S, et al. A 2000-year leaf wax-based hydrogen isotope record from southeast asia suggests low frequency ENSO-like teleconnections on a centennial timescale [J]. Quaternary Science Reviews, 2016, 148: 44-53. doi: 10.1016/j.quascirev.2016.07.002

    CrossRef Google Scholar

    [9] 陈德亮, 徐柏青, 姚檀栋, 等. 青藏高原环境变化科学评估: 过去、现在与未来[J]. 科学通报, 2015, 60(32):3023-3035 doi: 10.1360/csb2015-60-32-3023

    CrossRef Google Scholar

    CHEN Deliang, XU Baiqing, YAO Tandong, et al. Assessment of past, present and future environmental changes on the tibetan plateau [J]. Chinese Science Bulletin, 2015, 60(32): 3023-3035. doi: 10.1360/csb2015-60-32-3023

    CrossRef Google Scholar

    [10] Roxy M K, Ritika K, Terray P, et al. Drying of Indian subcontinent by rapid Indian ocean warming and a weakening land-sea thermal gradient [J]. Nature Communications, 2015, 6: 7423. doi: 10.1038/ncomms8423

    CrossRef Google Scholar

    [11] Kumar K K, Rajagopalan B, Hoerling M, et al. Unraveling the mystery of Indian monsoon failure during el niño [J]. Science, 2006, 314(5796): 115-119. doi: 10.1126/science.1131152

    CrossRef Google Scholar

    [12] Zhang J P, Lu H Y, Jia J W, et al. Seasonal drought events in tropical east asia over the last 60, 000 y [J]. Proceedings of the National Academy of Sciences of the United States of America, 2020, 117(49): 30988-30992. doi: 10.1073/pnas.2013802117

    CrossRef Google Scholar

    [13] Weiss H, Courty M A, Wetterstrom W, et al. The genesis and collapse of third millennium north mesopotamian civilization [J]. Science, 1993, 261(5124): 995-1004. doi: 10.1126/science.261.5124.995

    CrossRef Google Scholar

    [14] Kidder T R, Henry E R, Arco L J. Rapid climate Change-induced collapse of hunter-gatherer societies in the lower mississippi river valley between ca. 3300 and 2780 cal yr BP [J]. Science China Earth Sciences, 2017, 61(2): 178-189.

    Google Scholar

    [15] Chen F H, Dong G H, Zhang D J, et al. Agriculture facilitated permanent human occupation of the tibetan plateau after 3600 B.P [J]. Science, 2015, 347(6219): 248-250. doi: 10.1126/science.1259172

    CrossRef Google Scholar

    [16] Young K R. Biogeography of the anthropocene: domestication [J]. Progress in Physical Geography: Earth and Environment, 2016, 40(1): 161-174. doi: 10.1177/0309133315598724

    CrossRef Google Scholar

    [17] Heitkamp F, Sylvester S P, Kessler M, et al. Inaccessible andean sites reveal human-induced weathering in grazed soils [J]. Progress in Physical Geography: Earth and Environment, 2014, 38(5): 576-601. doi: 10.1177/0309133314544918

    CrossRef Google Scholar

    [18] Vannière B, Blarquez O, Rius D, et al. 7000-year human legacy of elevation-dependent european fire regimes [J]. Quaternary Science Reviews, 2016, 132: 206-212. doi: 10.1016/j.quascirev.2015.11.012

    CrossRef Google Scholar

    [19] Yasuda Y, Kitagawa H, Nakagawa T. The earliest record of major anthropogenic deforestation in the Ghab Valley, northwest Syria: a palynological study [J]. Quaternary International, 2000, 73-74: 127-136. doi: 10.1016/S1040-6182(00)00069-0

    CrossRef Google Scholar

    [20] Chen F H, Chen S Q, Zhang X, et al. Asian dust-storm activity dominated by Chinese dynasty changes since 2000 BP [J]. Nature Communications, 2020, 11: 992. doi: 10.1038/s41467-020-14765-4

    CrossRef Google Scholar

    [21] 赵三平. 南海西沙群岛海鸟生态环境演变[D]. 中国科学技术大学硕士学位论文, 2006:1-117.

    Google Scholar

    ZHAO Sanping. Evolution of seabird eco-environment on Xisha Islands of South China Sea[D]. Master Dissertation of University of Science and Technology of China, 2006:1-117.

    Google Scholar

    [22] Yan H, Sun L G, Oppo D W, et al. South China Sea hydrological changes and Pacific Walker Circulation variations over the last millennium [J]. Nature Communications, 2011, 2: 293. doi: 10.1038/ncomms1297

    CrossRef Google Scholar

    [23] Blaauw M, Christen J A. Bacon Manual-v2.3.3[Z]. 2013: 1-15.

    Google Scholar

    [24] Thompson R, Oldfield F. Environmental Magnetism[M]. London, Boston: Allen & Unwin, 1986:1-237.

    Google Scholar

    [25] Liu Q S, Roberts A P, Torrent J, et al. What do the HIRM and S‐ratio really measure in environmental magnetism? [J]. Geochemistry, Geophysics, Geosystems, 2007, 80(9): Q09011.

    Google Scholar

    [26] Evans M E, Heller F. Environmental Magnetism: principles and applications of enviromagnetics[M]. Amsterdam: Academic Press, 2003:1-299.

    Google Scholar

    [27] Zhang D E. Evidence for the existence of the medieval warm period in China [J]. Climatic Change, 1994, 26(2-3): 289-297. doi: 10.1007/BF01092419

    CrossRef Google Scholar

    [28] Chen J A, Wan G J, Zhang D D, et al. Environmental records of lacustrine sediments in different time scales: sediment grain size as an example [J]. Science in China Series D: Earth Sciences, 2004, 47(10): 954-960. doi: 10.1360/03yd0160

    CrossRef Google Scholar

    [29] 孙立广, 晏宏, 王玉宏. 南海西沙过去千年降雨变化及其影响因素[J]. 科学通报, 2012, 57(19):1730-1738 doi: 10.1360/972011-1842

    CrossRef Google Scholar

    SUN Liguang, YAN Hong, WANG Yuhong. South China Sea hydrological changes over the past millennium [J]. Chinese Science Bulletin, 2012, 57(19): 1730-1738. doi: 10.1360/972011-1842

    CrossRef Google Scholar

    [30] Zhang P Z, Cheng H, Edwards R L, et al. A test of climate, Sun, and Culture relationships from an 1810-Year Chinese cave record [J]. Science, 2008, 322(5903): 940-942. doi: 10.1126/science.1163965

    CrossRef Google Scholar

    [31] Conroy J L, Overpeck J T, Cole J E, et al. Holocene changes in eastern tropical pacific climate inferred from a galápagos lake sediment record [J]. Quaternary Science Reviews, 2008, 27(11-12): 1166-1180. doi: 10.1016/j.quascirev.2008.02.015

    CrossRef Google Scholar

    [32] Yang X Q, Wei G J, Yang J, et al. Paleoenvironmental shifts and precipitation variations recorded in tropical maar lake sediments during the Holocene in southern China [J]. The Holocene, 2014, 24(10): 1216-1225. doi: 10.1177/0959683614540962

    CrossRef Google Scholar

    [33] Tan L C, Shen C C, Löwemark L, et al. Rainfall variations in central Indo-Pacific over the past 2, 700 y [J]. Proceedings of the National Academy of Sciences of the United States of America, 2019, 116(35): 17201-17206. doi: 10.1073/pnas.1903167116

    CrossRef Google Scholar

    [34] 孟原召. 华光礁一号沉船与宋代南海贸易[J]. 博物院, 2018(2):11-26 doi: 10.3969/j.issn.2096-1715.2018.02.003

    CrossRef Google Scholar

    MENG Yuanzhao. Research on Huaguang reef shipwreck I and overseas trade on the maritime silk road in the song dynasty [J]. Museum, 2018(2): 11-26. doi: 10.3969/j.issn.2096-1715.2018.02.003

    CrossRef Google Scholar

    [35] 包春磊. 南海“华光礁Ⅰ号”沉船水下考古试析[J]. 南海学刊, 2015, 1(3):55-59

    Google Scholar

    BAO Chunlei. An archaeological analysis of underwater wreck of Huaguang Reef Ⅰ in South China Sea [J]. The Journal of South China Sea Studies, 2015, 1(3): 55-59.

    Google Scholar

    [36] 陈冲. 南澳Ⅰ号沉船所见景德镇民窑青花瓷的生产年代[J]. 华夏考古, 2018(4):85-96

    Google Scholar

    CHEN Chong. The year of production of blue-and-white porcelain made in Civilian Kiln in Jingdezhen Discovered on the Shipwreck Nan'ao Ⅰ [J]. Huaxia Archaeology, 2018(4): 85-96.

    Google Scholar

    [37] 崔勇. 广东汕头市“南澳Ⅰ号”明代沉船[J]. 考古, 2011(7):39-46

    Google Scholar

    CUI Yong. The Sunken Ship "Nan'ao Ⅰ" of the Ming dynasty in Shantou City, Guangdong [J]. Archaeology, 2011(7): 39-46.

    Google Scholar

    [38] 中国国家博物馆水下考古研究中心, 海南省文物局. 西沙群岛北礁19号水下遗存的考古调查[J]. 中国国家博物馆馆刊, 2011(11):47-53

    Google Scholar

    Underwater Archaeology Research Centre of National Museum of China, Hainan Provincial Bureau of Cultural Relics. Archaeological survey of the Beijiao 19 underwater site in the paracel islands [J]. Journal of National Museum of Chinese History, 2011(11): 47-53.

    Google Scholar

    [39] 刘晓瞳, 葛晨东, 邹欣庆, 等. 西沙群岛东岛潟湖沉积物碳、氮元素地球化学特征及其指示的环境变化[J]. 海洋学报, 2017, 39(6):43-54

    Google Scholar

    LIU Xiaotong, GE Chendong, ZOU Xinqing, et al. Carbon, Nitrogen geochemical characteristics and their implications on environmental change in the lagoon sediments of the Dongdao Island of Xisha Islands in South China Sea [J]. Acta Oceanologica Sinica, 2017, 39(6): 43-54.

    Google Scholar

    [40] 孙立广, 赵三平, 刘晓东, 等. 西沙群岛生态环境报告[J]. 自然杂志, 2005, 27(2):79-84 doi: 10.3969/j.issn.0253-9608.2005.02.004

    CrossRef Google Scholar

    SUN Liguang, ZHAO Sanping, LIU Xiaodong, et al. An eco-environmental report on xisha archipelago, South China Sea [J]. Chinese Journal of Nature, 2005, 27(2): 79-84. doi: 10.3969/j.issn.0253-9608.2005.02.004

    CrossRef Google Scholar

    [41] Iwasaka Y, Minoura H, Nagaya K. The transport and spacial scale of asian dust-storm clouds: a case study of the dust-storm event of april 1979 [J]. Tellus B: Chemical and Physical Meteorology, 1983, 35(3): 189-196. doi: 10.3402/tellusb.v35i3.14594

    CrossRef Google Scholar

    [42] Liu Y, Sun L G, Zhou X, et al. A 1400-year terrigenous dust record on a coral island in South China Sea [J]. Scientific Reports, 2014, 4: 4994.

    Google Scholar

  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(8)

Tables(1)

Article Metrics

Article views(1153) PDF downloads(15) Cited by(0)

Access History

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint