Redox-driven biogeochemical element cycles play a central role in converting organic matter in aquatic ecosystems. They also perform key functions such as removing nitrate, mitigating the formation of greenhouse gases and weakening the effects of contaminants. Recent research has revealed the presence of redox-active compounds in these ecosystems with hitherto unknown redox properties. These substances are metastable (that is, non-equilibrium solid phases), which can both donate and accept electrons. They are highly redox reactive and recyclable and may act as biogeobatteries by temporarily storing electrons. Their lifetime, however, is limited, and with time they become more crystalline and less reactive. In this Review, we argue that these redox-active metastable phases require activation by fluctuating redox conditions to maintain their high reactivity. In aquatic ecosystems, switching between oxidizing and reducing conditions can be achieved only through hydrological perturbations at hydrological interfaces (for example, water level fluctuations). We present a novel framework that links microscale biogeochemical processes to large-scale hydrological processes, and discuss implications and future research directions for biogeochemical element cycles in aquatic systems exposed to frequent hydrological disturbances.
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This article is the outcome of discussions that took place in a series of workshops organized by the authors on the role of redox-active compounds in aquatic ecosystems.
The authors declare no competing interests.
Peer review information Nature Geoscience thanks Matthew Kirk and the other, anonymous, reviewer(s) for their contribution to the peer review of this work. Primary Handling Editors: Tamara Goldin; Xujia Jiang.
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Peiffer, S., Kappler, A., Haderlein, S.B. et al. A biogeochemical–hydrological framework for the role of redox-active compounds in aquatic systems. Nat. Geosci. 14, 264–272 (2021). https://doi.org/10.1038/s41561-021-00742-z