Global lake phytoplankton proliferation intensifies climate warming.

Shi, Wenqing; Qin, Boqiang; Zhang, Qingji; Paerl, Hans W; Van Dam, Bryce; Jeppesen, Erik; Zeng, Chenjun · Nat Commun · 2024

basic_science · Level V

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Abstract

In lakes, phytoplankton sequester atmospheric carbon dioxide (CO<sub>2</sub>) and store it in the form of biomass organic carbon (OC); however, only a small fraction of the OC remains buried, while the remaining part is recycled to the atmosphere as CO<sub>2</sub> and methane (CH<sub>4</sub>). This has the potential effect of adding CO<sub>2</sub>-equivalents (CO<sub>2</sub>-eq) to the atmosphere and producing a warming effect due to the higher radiative forcing of CH<sub>4</sub> relative to CO<sub>2</sub>. Here we show a 3.1-fold increase in CO<sub>2</sub>-eq emissions over a 100-year horizon, with the effect increasing with global warming intensity. Climate warming has stimulated phytoplankton growth in many lakes worldwide, which, in turn, can feed back CO<sub>2</sub>-eq and create a positive feedback loop between them. In lakes where phytoplankton is negatively impacted by climate warming, the CO<sub>2</sub>-eq feedback capacity may diminish gradually with the ongoing climate warming.

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