地球科学进展 ›› 2004, Vol. 19 ›› Issue (5): 699 -705. doi: 10.11867/j.issn.1001-8166.2004.05.0699

发展战略论坛 上一篇    下一篇

浅谈固体地球科学与地球系统科学
郭正堂 1,2;吴海斌 1   
  1. 中国科学院地球环境研究所,陕西 西安 710075;中国科学院地质与地球物理研究所,北京 100029
  • 收稿日期:2004-06-01 修回日期:2004-08-02 出版日期:2004-12-20
  • 通讯作者: 郭正堂(1964-),男,研究员,主要从事新生代环境与全球变化研究. E-mail:E-mail:ztguo@mail.igcas.ac.cn

ON THE SOLID EARTH SCIENCE AND 
EARTH SYSTEM SCIENCE

GUO Zheng-tang 1,2,WU Hai-bin 1   

  1. 1.Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075,China;2.Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029,China
  • Received:2004-06-01 Revised:2004-08-02 Online:2004-12-20 Published:2004-10-01

地球科学在20世纪的诸多进展中,对后来科学发展具有深远影响的基本认识之一是地球演化的行为具有整体性,其不同的圈层确实通过多种途径相互作用,且人类活动已成为地球演化的重要营力之一。这些认识导致地球系统科学思想的产生和发展,并使不同圈层相互作用的过程和机理、人与环境的相互作用研究成为21世纪基础科学研究的前沿。地球系统科学强调地球不同圈层、不同单元相互作用的整体性和关联性,因而科学研究必须从"整体地球系统"的视野出发,但研究过程又必须从关键区域入手。我国是地球系统科学研究的关键地区之一,未来研究应立足地域优势和特色,攻克全球性重大科学问题,解决社会对地球科学的知识需求。

The advances during the 20th century in the field of Solid Earth Science have numerously contributed to the emergence of Earth System Science (ESS). ESS aims at understanding the Earth as a synthetic system driven by complex internal and external processes, with special emphasis given to the interactions of geosphere, atmosphere, hydrosphere and biosphere. It should answer a series of questions about the Earth, such as (1) How the Earth system evolved in the past? What are the driving forces and mechanisms of these changes? What occurs presently in the system with numerous human disturbances and what will be its future? The fundamental of the Earth System Science is to view the Earth as a whole system, but approaches of ESS need to start by key regions. China is located within a crucial region for understanding the basic Earth system processes. The study of ESS also meets China's social requirements as it is likely faced with most serious natural environmental and resource problems. We suggest a number of issues relevant to the traditional Solid Earth Science, which appear to be of importance in the ESS studies in China.

中图分类号: 

[1]中国科学院地学部“中国地球科学发展战略”研究组.地球科学:世纪之交的回顾与展望[M]. 济南:山东教育出版社,2002.
[2]Tackley P J. Mantle convection and plate tectonics: Toward an integrated physical and chemical theory[J].Science, 2000, 288: 2 002-2 007.
[3]Buffett B A. Earth's core and the geodynamo[J].Science, 2000, 288: 2 007-2 012.
[4]Flower B P, Kennett J P. Middle Miocene ocean-climate transition: High-resolution oxygen and carbon isotopic records from Deep Sea Drilling Project site 588A, southwest Pacific[J].Palaeoceanography, 1993, 8: 811-843.
[5]Ruddiman W F, Prell W L, Raymo M E. Late Cenozoic uplift in southern Asia and the American West: Rational for general circulation modeling experiments[J].Journal of Geophysical Research, 1989, 94:18 379-18 391.
[6]Raymo M E, Ruddiman W F, Froelich P N. The influence of late Cenozoic mountain building on oceanic geochemical cycle[J].Geology, 1988, 16: 649-653.
[7]Zhang P, Molnar P, Downs W R. Increased sedimentation rates and grain sizes 2~4 Ma ago due to the influence of climate change on erosion rates[J].Nature, 2001, 410: 891-897.
[8]Lamb S, Davis P. Cenozoic climate changes as a possible cause for the rise of the Andes[J]. Nature, 2003, 425: 792-797.
[9]Broecker W S. Paleocean circulation during the last deglaciation: A bipolar seesaw?[J].Paleoceanography, 1998, 13: 119-121.
[10]Stocker T F. Past and future reorganizations in the climate system[J].Quaternary Science Reviews, 2000, 19: 301-319.
[11]Wignall P B. Large igneous provinces and mass extinction[J].Earth Science Reviews,2001, 53: 1-33.
[12]Quade J, Cerling T E, Bowman J R. Development of Asian monsoon revealed by marked ecological shift during the latest Miocene in the northern Pakistan[J].Nature, 1989, 342: 163-166
[13]Cerling T E, Wang Y, Quade J. Expansion of C4 ecosystems as an indictor of global ecological change in the late Miocene[J].Nature, 1993, 361:344-345.
[14]Pagani M, Freeman K H, Arthur M A. Late Miocene atmospheric CO2concentrations and the expansion of C4 grasses[J].Science, 1999, 285: 876-879.
[15]Van derMerve N JTschauner HC4 plants and the development of human societies[A]. In: Sage R F, Monson R K,eds.C4 Plant Biology[C].San Diego:Academy Press, 1999.509-538.
[16]Shackleton N J. A new Late Neogene time scale: Application to Log 138 sites[J].Proceeding ODP, Science Results, 1995, 138: 73-91
[17]Kashiwaya K, Ochiai S, Sakai H, et al. Orbital-related long-term climate cycles revealed in a 12 Ma continental record from Baikal[J].Nature, 2001,410:71-74.
[18]Bond G, Kromer B, Beer J, et al. Persistent solar influence on north Atlantic climate during the Holocene[J].Science, 2001, 294: 2 130-2 136.
[19]Guydo Y, Valet J P. Global changes in intensity of the Earth's magnetic field during the past 800 ka[J].Nature, 1999, 399: 249-252.
[20]Alvarezl W, Alvarez W M, Asaro F,et al. Extraterrestrial cause for the Cretaceous-Tertiary extinction[J].Science, 1980, 208: 1 095-1 108.
[21]IPCC. Climate Change: The IPCC Scientific Assessment[M]. Cambridge: Cambridge University Press,2000
[22]Chen Panqin(陈泮勤), Ma Zhenhua(马振华), Wang Genchen(王庚辰) translated. Earth System Science[M]. Beijing: Seismetic Press, 1992(in Chinese).
[23]赵生才.固体地球科学的研究现状和趋势[J].地球科学进展,2000,15(6):757-759.
[24]Martin J H. Glacial-interglacial CO2 changes: The iron hypothesis[J].Paeoceanography, 1990, 5: 1-13.

[1] 魏梦美,符素华,刘宝元. 青藏高原水力侵蚀定量研究进展[J]. 地球科学进展, 2021, 36(7): 740-752.
[2] 范成新, 刘敏, 王圣瑞, 方红卫, 夏星辉, 曹文志, 丁士明, 侯立军, 王沛芳, 陈敬安, 游静, 王菊英, 盛彦清, 朱伟. 20年来我国沉积物环境与污染控制研究进展与展望[J]. 地球科学进展, 2021, 36(4): 346-374.
[3] 吴佳梅,彭秋志,黄义忠,黄亮. 中国植被覆盖变化研究遥感数据源及研究区域时空热度分析[J]. 地球科学进展, 2020, 35(9): 978-989.
[4] 李侠祥, 刘昌新, 王芳, 郝志新. 中国投资对“一带一路”地区经济增长和碳排放强度的影响[J]. 地球科学进展, 2020, 35(6): 618-631.
[5] 刘凯,聂格格,张森. 中国 19512018年气温和降水的时空演变特征研究[J]. 地球科学进展, 2020, 35(11): 1113-1126.
[6] 谢彦君, 任福民, 李国平, 王铭杨, 杨慧. 影响中国双台风活动气候特征研究[J]. 地球科学进展, 2020, 35(1): 101-108.
[7] 郝志新,吴茂炜,张学珍,刘洋,郑景云. 过去千年中国年代和百年尺度冷暖阶段的干湿格局变化研究[J]. 地球科学进展, 2020, 35(1): 18-25.
[8] 蒋诗威,周鑫. 中国东南地区中世纪暖期和小冰期夏季风降水研究进展[J]. 地球科学进展, 2019, 34(7): 697-705.
[9] 吴泽燕,章程,蒋忠诚,罗为群,曾发明. 岩溶关键带及其碳循环研究进展[J]. 地球科学进展, 2019, 34(5): 488-498.
[10] 高峰,赵雪雁,宋晓谕,王宝,王鹏龙,牛艺博,王伟军,黄春林. 面向 SDGs的美丽中国内涵与评价指标体系[J]. 地球科学进展, 2019, 34(3): 295-305.
[11] 张宸嘉, 方一平, 陈秀娟. 基于文献计量的国内可持续生计研究进展分析[J]. 地球科学进展, 2018, 33(9): 969-982.
[12] 陈亮, 段建平, 马柱国. 大气环流形势客观分型及其与中国降水的联系[J]. 地球科学进展, 2018, 33(4): 396-403.
[13] 王建, 车涛, 李震, 李弘毅, 郝晓华, 郑照军, 肖鹏峰, 李晓峰, 黄晓东, 钟歆玥, 戴礼云, 李红星, 柯长青, 李兰海. 中国积雪特性及分布调查[J]. 地球科学进展, 2018, 33(1): 12-15.
[14] 吴绍洪, 高江波, 戴尔阜, 赵东升, 尹云鹤, 杨琳, 郑景云, 潘韬, 杨勤业. 中国陆地表层自然地域系统动态研究:思路与方案[J]. 地球科学进展, 2017, 32(6): 569-576.
[15] 陈晓龙, 周天军. 使用订正的“空间型标度”法预估1.5 ℃温升阈值下地表气温变化[J]. 地球科学进展, 2017, 32(4): 435-445.
阅读次数
全文


摘要