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Endogenous circadian regulation of carbon dioxide exchange in terrestrial ecosystems

机译:陆地生态系统中二氧化碳交换的内源性昼夜节律

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摘要

It is often assumed that daytime patterns of ecosystem carbon assimilation are mostly driven by direct physiological responses to exogenous environmental cues. Under limited environmental variability, little variation in carbon assimilation should thus be expected unless endogenous plant controls on carbon assimilation, which regulate photosynthesis in time, are active. We evaluated this assumption with eddy flux data, and we selected periods when net ecosystem exchange (NEE) was decoupled from environmental variability in seven sites from highly contrasting biomes across a 74 degrees latitudinal gradient over a total of 36 site-years. Under relatively constant conditions of light, temperature, and other environmental factors, significant diurnal NEE oscillations were observed at six sites, where daily NEE variation was between 20% and 90% of that under variable environmental conditions. These results are consistent with fluctuations driven by the circadian clock and other endogenous processes. Our results open a promising avenue of research for a more complete understanding of ecosystem fluxes that integrates from cellular to ecosystem processes.
机译:通常认为,生态系统碳同化的白天模式主要是由对外源环境线索的直接生理反应驱动的。因此,在有限的环境可变性下,除非能够及时调节光合作用的内源植物对碳同化的控制有效,否则应预期碳同化的变化很小。我们用涡流数据评估了这一假设,并选择了在36个站点年中,跨越74度纬度梯度的高度相反的生物群落,从七个站点的净生态系统交换(NEE)与环境变异脱钩的时期。在相对恒定的光照,温度和其他环境因素条件下,六个地点观测到明显的昼夜NEE振荡,其中每日NEE的变化介于可变环境条件下的20%至90%。这些结果与昼夜节律和其他内生过程引起的波动一致。我们的结果为更完整地了解从细胞到生态系统过程整合的生态系统通量开辟了有希望的研究途径。

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