深部碳循环的环境气候效应

宗克清, 何德涛, 陈春飞, 陈唯, 虞凯章, 刘勇胜. 2022. 深部碳循环的环境气候效应. 岩石学报, 38(5): 1389-1398. doi: 10.18654/1000-0569/2022.05.08
引用本文: 宗克清, 何德涛, 陈春飞, 陈唯, 虞凯章, 刘勇胜. 2022. 深部碳循环的环境气候效应. 岩石学报, 38(5): 1389-1398. doi: 10.18654/1000-0569/2022.05.08
ZONG KeQing, HE DeTao, CHEN ChunFei, CHEN Wei, YU KaiZhang, LIU YongSheng. 2022. The effect of the deep carbon cycle on environment and climate. Acta Petrologica Sinica, 38(5): 1389-1398. doi: 10.18654/1000-0569/2022.05.08
Citation: ZONG KeQing, HE DeTao, CHEN ChunFei, CHEN Wei, YU KaiZhang, LIU YongSheng. 2022. The effect of the deep carbon cycle on environment and climate. Acta Petrologica Sinica, 38(5): 1389-1398. doi: 10.18654/1000-0569/2022.05.08

深部碳循环的环境气候效应

  • 基金项目:

    本文受国家重点研发计划项目(2019YFA0708400)和国家自然科学基金项目(41922021)联合资助

详细信息
    作者简介:

    宗克清,男,1982年生,教授,从事岩石地球化学研究,E-mail: zongkeqing@cug.edu.cn

  • 中图分类号: P531.2;P542;P595

The effect of the deep carbon cycle on environment and climate

  • 地球表层温度主要由接收的太阳辐射能量及大气温室气体的保温能力共同控制。CO2等温室气体通过对大气温度的调节影响着全球环境气候变化,工业革命以来全球CO2排放量的增加被认为是全球变暖的重要原因,地质历史时期大气CO2浓度的波动与温室和冰室气候的交替出现相对应。地球超过90%的碳赋存于深部,因此地球深部过程的些许波动便会影响到地表碳含量,进而深刻影响着地球的环境气候变化。以往的研究注重地表碳循环对环境气候的影响,对深部碳的贡献考虑不足。最近十余年全球开展了详细的深部碳循环研究,基于已经取得的重要成果,本文从大火成岩省、裂谷和俯冲带的视角对深部碳循环驱动的环境气候效应进行了系统回顾。认为未来的研究需要对地球深部碳循环通量和碳同位素组成进行更精确的定量,这是我们认识深部碳循环对地表环境气候影响的基础;除了碳元素本身我们还需要关注其他挥发性元素和有害金属元素的综合效应;俯冲带作为全球壳-幔相互作用和物质交换循环最重要的场所,应该是进行深部碳循环观察和环境气候效应研究的重点。

  • 加载中
  • 图 1 

    大气CO2浓度随时间的变化趋势

    Figure 1. 

    Variation of atmospheric CO2 concentration with time

    图 2 

    全球深部碳循环示意图(据Wong et al., 2019修改)

    Figure 2. 

    Schematic illustration of the global deep carbon cycle (modified after Wong et al., 2019)

    图 3 

    裂谷对古大气中CO2浓度的控制(据Brune et al., 2017修改)

    Figure 3. 

    CO2 concentration in the paleo-atmosphere is controlled by rifts (modified after Brune et al., 2017)

    图 4 

    全球成冰纪(Cryogenian)以来沉积物中年轻碎屑锆石年龄统计结果揭示的大陆弧活动强度与气候和大气CO2浓度变化的耦合关系(据McKenzie et al., 2016修改)

    Figure 4. 

    The statistical results of young detrital zircon ages in sediments demonstrate the coupled continental arc activity and climate and atmospheric CO2 concentration since the Cryogenian (modified after McKenzie et al., 2016)

    图 5 

    碳酸盐岩在俯冲带发生脱碳、熔融与喷发再沉积模型(据Liu et al., 2021修改)

    Figure 5. 

    A model of decarbonation, melting, eruption, and redeposition of carbonate rocks in the subduction zone (modified after Liu et al., 2021)

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出版历程
收稿日期:  2022-01-15
修回日期:  2022-03-21
刊出日期:  2022-05-01

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