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生态学杂志 ›› 2023, Vol. 42 ›› Issue (3): 736-747.doi: 10.13292/j.1000-4890.202303.002

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长江流域水环境碳循环研究进展

王威1,郭庆军2,3*,杜陈军2,3,邓义楠1,4   

  1. 1云南大学地球科学学院, 古生物研究院深时陆地生态研究所, 昆明 650500; 2中国科学院地理科学与资源研究所, 北京 100101; 3中国科学院大学, 北京 100049; 4广州海洋地质调查局, 广州 510075)

  • 出版日期:2023-03-10 发布日期:2023-03-10

Research advances in water environmental carbon cycle in the Yangtze River Basin.

WANG Wei1, GUO Qingjun2,3*, DU Chenjun2,3, DENG Yinan1,4   

  1. (1Institute of Deep Time Terrestrial Ecology, Institute of Paleonto-logy, College of Earth Sciences, Yunnan University, Kunming 650500, China; 2Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 3University of Chinese Academy of Sciences, Beijing 100049, China; 4Guangzhou Marine Geological Survey, Guangzhou 510075, China).

  • Online:2023-03-10 Published:2023-03-10

摘要: 碳循环是地球系统中最重要的物质循环之一,对全球气候变化和人类生存发展具有根本性的意义。河流中的碳物质常常反映了流域气候与环境的变化,是全球碳循环的关键组成部分。长江流域是我国最大的流域,广泛分布碳酸盐岩,具有巨大的生态系统固碳潜力。由于长江流域的自然环境变化的复杂性,我们对全球变化背景下长江流域水环境碳循环的认识还十分有限。本文对长江流域水环境碳物质的时空分布与来源以及流域岩石风化碳汇等资料进行了回顾和梳理,发现有机碳的来源和分布主要受人类活动的影响,而无机碳主要来源于长江流域岩石的化学风化,同时岩石风化具有巨大的碳汇潜力。在全球变化影响下,这些碳物质发生迁移转化,可能引发新的生态环境问题,这对预测未来的环境变化具有重要意义,也为长江流域碳循环研究提供了基础。


关键词: 碳循环, 同位素, 岩石风化, 全球变化, 长江流域

Abstract: As one most important material cycling on the earth, carbon cycling has great implications for global climate change and human well-being. Carbon in rivers could reflect the changes in climate and environment in river basins, and is a key part of the global carbon cycle. The Yangtze River Basin is the largest basin in China, with wide distribution of carbonate rocks, which has huge carbon sequestration potential. Due to the complexity of natural environment change in the Yangtze River Basin, our understanding of water environment carbon cycle under the background of global change is still limited. Here we review the temporal and spatial variations and source of carbon in the water environment and the carbon sink data of rock weathering in the Yangtze River Basin. The source and distribution of organic carbon are mainly affected by human activities. Inorganic carbon mainly comes from the chemical weathering of rocks in the Yangtze River Basin. Rock weathering has great potential in carbon sink. Under the influence of global change, the migration and transformation of these carbonic materials may lead to new ecolo-gical and environmental problems, which is of great significance for predicting future environmental changes. Our work provides a basis for the study of carbon cycle in the Yangtze River Basin.


Key words: carbon cycle, isotope, rock weathering, global change, Yangtze River Basin.