生物多样性 ›› 2020, Vol. 28 ›› Issue (11): 1405-1416. DOI: 10.17520/biods.2020262 cstr: 32101.14.biods.2020262
收稿日期:
2020-06-30
接受日期:
2020-10-24
出版日期:
2020-11-20
发布日期:
2020-10-30
通讯作者:
骆亦其
作者简介:
* E-mail: Yiqi.Luo@nau.edu基金资助:
Received:
2020-06-30
Accepted:
2020-10-24
Online:
2020-11-20
Published:
2020-10-30
Contact:
Yiqi Luo
摘要:
生态系统维持物质与能量的动态平衡是地球系统孕育与维持生物多样性的重要基础。自工业革命以来, 人类活动导致陆地生态系统的碳循环转变为动态非平衡,进而使陆地生态系统的结构与功能出现许多难以预测的变化动态。本文阐释了陆地生态系统碳循环的动态非平衡假说。该假说构建于陆地碳循环内部过程的四点基本特征和五类外部驱动因素。基于这些内部特征与外部因素, 本文归纳了陆地生态系统碳循环动态非平衡在不同时间与空间尺度的表达现象, 并从观测、实验与模型的角度讨论了其检测方法。陆地生态系统碳循环的动态非平衡假说不仅有助于我们理解复杂的陆地碳循环现象, 也为预测未来陆地碳汇动态提供了新的理论框架。
骆亦其, 夏建阳 (2020) 陆地碳循环的动态非平衡假说. 生物多样性, 28, 1405-1416. DOI: 10.17520/biods.2020262.
Yiqi Luo, Jianyang Xia (2020) A dynamic disequilibrium hypothesis for terrestrial carbon cycle. Biodiversity Science, 28, 1405-1416. DOI: 10.17520/biods.2020262.
图1 陆地碳循环动态非平衡假说中包含的外部驱动因素、内部碳循环过程及其在不同时空尺度上的表达现象。图片中的公式为正文中的公式(1), 其变量解释见正文。
Fig. 1 External forcing, internal processes, and complex phenomena of dynamic disequilibrium hypothesis for terrestrial carbon cycle. The equation in the figure is cited from Luo et al (2003) and the details of equation can be found in the text.
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