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综合内陆水体中的碳排放、积累和输移,以了解它们在全球碳循环中的作用。

Integrating carbon emission, accumulation and transport in inland waters to understand their role in the global carbon cycle.

机构信息

Climate Impacts Research Centre (CIRC), Department of Ecology and Environmental Science, Umeå University, Umeå, Sweden.

出版信息

Glob Chang Biol. 2021 Feb;27(4):719-727. doi: 10.1111/gcb.15448. Epub 2020 Dec 9.

Abstract

Inland waters receive a significant quantity of carbon (C) from land. The fate of this C during transit, whether it is emitted to the atmosphere, accumulated in sediments or transported to the ocean, can considerably reshape the landscape C balance. However, these different fates of terrestrial C are not independent but are instead linked via several catchment and aquatic processes. Thus, according to mass conservation, any environmental change inducing a shift in a particular C fate should come at the expense of at least one other fate. Nonetheless, studies that have investigated C emission, accumulation and transport concertedly are scarce, resulting in fragmented knowledge of the role of inland waters in the global C cycle. Here, we propose a framework to understand how different C fates in aquatic systems are interlinked and covary under environmental changes. First, to explore how C fates are currently distributed in streams, rivers, reservoirs and lakes, we compiled data from the literature and show that 'C fate allocation' varies widely both within and among inland water systems types. Secondly, we developed a framework that integrates C fates in any inland water system by identifying the key processes underlying their linkages. Our framework places the partitioning between the different C forms, and how this is controlled by export from land, internal transformations and hydrology, as central to understanding C fate allocation. We argue that, by focusing on a single fate, studies could risk drawing misleading conclusions regarding how environmental changes will alter the role of inland waters in the global C cycle. Our framework thus allows us to holistically assess the consequences of such changes on coupled C fluxes, setting a foundation for understanding the contemporary and future fate of land-derived C in inland water systems.

摘要

内陆水体从陆地接收大量的碳 (C)。在传输过程中,这些 C 的命运——是排放到大气中、积累在沉积物中还是输送到海洋中——可以极大地改变景观碳平衡。然而,这些陆地 C 的不同命运并不是独立的,而是通过几个流域和水生过程相互关联的。因此,根据质量守恒定律,任何导致特定 C 命运发生变化的环境变化都应该以至少另一个命运为代价。尽管如此,很少有研究同时调查 C 的排放、积累和运输,这导致了人们对内陆水域在全球碳循环中的作用的认识碎片化。在这里,我们提出了一个框架,以了解水生系统中的不同 C 命运在环境变化下是如何相互关联和共同变化的。首先,为了探索当前 C 命运在溪流、河流、水库和湖泊中的分布情况,我们从文献中汇编了数据,并表明“C 命运分配”在不同的内陆水系统类型内和之间差异很大。其次,我们开发了一个框架,通过确定其联系的关键过程,将任何内陆水系统中的 C 命运整合在一起。我们的框架将不同 C 形态之间的分配以及这种分配如何受到陆地出口、内部转化和水文学的控制作为理解 C 命运分配的核心。我们认为,通过关注单一命运,研究可能会得出关于环境变化将如何改变内陆水域在全球碳循环中作用的误导性结论。因此,我们的框架使我们能够全面评估这些变化对耦合 C 通量的影响,为了解内陆水系统中陆地衍生 C 的当代和未来命运奠定基础。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/417d/7898617/e494bab3bdc8/GCB-27-719-g001.jpg

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