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Prolonged suppression of ecosystem carbon dioxide uptake after an anomalously warm year

机译:异常温暖的一年后,长期抑制了生态系统二氧化碳的吸收

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Terrestrial ecosystems control carbon dioxide fluxes to and from the atmosphere through photosynthesis and respiration, a balance between net primary productivity and heterotrophic respiration, that determines whether an ecosystem is sequestering carbon or releasing it to the atmosphere. Global and site-specific data sets have demonstrated that climate and climate variability influence biogeochemical processes that determine net ecosystem carbon dioxide exchange (NEE) at multiple timescales. Experimental data necessary to quantify impacts of a single climate variable, such as temperature anomalies, on NEE and carbon sequestration of ecosystems at interannual timescales have been lacking. This derives from an inability of field studies to avoid the confounding effects of natural intra-annual and interannual variability in temperature and precipitation. Here we present results from a four-year study using replicate 12,000-kg intact tallgrass prairie monoliths located in four 184-m enclosed lysimeters. We exposed 6 of 12 monoliths to an anomalously warm year in the second year of the study and continuously quantified rates of ecosystem processes, including NEE. We find that warming decreases NEE in both the extreme year and the following year by inducing drought that suppresses net primary productivity in the extreme year and by stimulating heterotrophic respiration of soil biota in the subsequent year. Our data indicate that two years are required for NEE in the previously warmed experimental ecosystems to recover to levels measured in the control ecosystems. This time lag caused net ecosystem carbon sequestration in previously warmed ecosystems to be decreased threefold over the study period, compared with control ecosystems. Our findings suggest that more frequent anomalously warm years, a possible consequence of increasing anthropogenic carbon dioxide levels, may lead to a sustained decrease in carbon dioxide uptake by terrestrial ecosystems.
机译:陆地生态系统通过光合作用和呼吸作用控制着进入和流出大气的二氧化碳通量,这是净初级生产力与异养呼吸之间的平衡,它决定了生态系统是否在隔离碳或将其释放到大气中。全球和特定地点的数据集表明,气候和气候变化会影响生物地球化学过程,这些过程决定了多个时间尺度上的净生态系统二氧化碳交换量(NEE)。缺乏量化单个气候变量(例如温度异常)对NEE和年际尺度上的生态系统碳固存的影响所必需的实验数据。这是由于无法进行实地研究而避免温度和降水的自然年内和年际变化的混杂影响。在这里,我们介绍了一项为期四年的研究结果,该研究使用了位于四个184 m封闭式溶渗仪中的12,000 kg完整的高草草原整块生物。在研究的第二年,我们将12个整体中的6个暴露在异常温暖的一年中,并不断量化生态系统过程的速率,包括NEE。我们发现变暖会在极端年份和第二年降低NEE,原因是干旱导致极端年份的净初级生产力受到抑制,第二年又通过刺激土壤生物的异养呼吸。我们的数据表明,先前变暖的实验生态系统中的NEE需要两年时间才能恢复到对照生态系统中测得的水平。与对照生态系统相比,这种时滞导致先前变暖的生态系统中的净生态系统碳固存在研究期内减少了三倍。我们的发现表明,异常温暖的年份更为频繁,这是人为二氧化碳水平增加的可能结果,可能导致陆地生态系统对二氧化碳的吸收持续减少。

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