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中国沿海湿地温室气体通量的格局和环境驱动因素:系统评价与综合。

Patterns and environmental drivers of greenhouse gas fluxes in the coastal wetlands of China: A systematic review and synthesis.

机构信息

Key Laboratory of Humid Sub-tropical Eco-geographical Process of Ministry of Education, Fujian Normal University, Fuzhou, 350007, Fujian, China; College of the Environment and Ecology, Xiamen University, Xiamen, 361102, Fujian, China.

CSIC, Global Ecology CREAF-CSIC-UAB, Bellaterra, 08193, Barcelona, Catalonia, Spain; CREAF, Cerdanyola del Vallès, 08193, Barcelona, Catalonia, Spain.

出版信息

Environ Res. 2020 Jul;186:109576. doi: 10.1016/j.envres.2020.109576. Epub 2020 Apr 25.

Abstract

Coastal wetlands play an increasingly important role in regulating greenhouse gas (GHG) fluxes and thus affecting climate change. However, the overall magnitude, trend, and environmental drivers of GHG fluxes in these wetlands of China remain uncertain. Herein, we synthesized data from 70 publications involving 187 field observations to identify patterns and drivers of GHG fluxes across coastal wetlands in China. Average methane (CH), nitrous oxide (NO) fluxes, and carbon dioxide (CO) emissions (ecosystem respiration) across coastal wetlands were estimated as 2.20±0.31 mg·m·h, 16.44±2.96 μg·m·h, and 388.76±42.28 mg·m·h, respectively. GHG emissions varied with tidal inundation, where CH and CO emissions during tidal inundation were lower than during ebbing. CH and CO emissions from wetlands decreased linearly with increasing latitude, while NO did not. CH fluxes were positively related to air temperature and aboveground biomass, and CO emissions were positively related to soil organic carbon. NO fluxes were lower with increasing soil pH, and CH and CO emissions were greater with increasing soil moisture. Based on the results of sustained-flux global warming potential and sustained-flux global cooling potential models, our paper indicate that the fluxes of CH and NO in coastal wetlands have a positive feedback to global warming, which is mainly driven by the CH emission. Our synthesis improved understanding of the roles of coastal wetlands in the ecosystem C cycle under global change. We suggest that long-term field observations of GHG fluxes across a wider range of spatiotemporal scales are urgently required to improve the prediction accuracy in GHG fluxes and the assessment of net GHG balance and its contribution to the GWP of coastal wetlands.

摘要

沿海湿地在调节温室气体(GHG)通量方面发挥着越来越重要的作用,从而影响气候变化。然而,中国沿海湿地 GHG 通量的整体幅度、趋势和环境驱动因素仍不确定。在此,我们综合了 70 篇文献的数据,这些文献涉及 187 个实地观测,以确定中国沿海湿地 GHG 通量的模式和驱动因素。中国沿海湿地的平均甲烷(CH)、氧化亚氮(NO)通量和二氧化碳(CO)排放(生态系统呼吸)分别估计为 2.20±0.31mg·m·h、16.44±2.96μg·m·h 和 388.76±42.28mg·m·h。GHG 排放随潮汐淹没而变化,潮汐淹没期间的 CH 和 CO 排放低于退潮期间。CH 和 CO 排放随纬度增加呈线性下降,而 NO 则不然。CH 通量与空气温度和地上生物量呈正相关,CO 排放与土壤有机碳呈正相关。NO 通量随土壤 pH 值升高而降低,CH 和 CO 排放随土壤湿度升高而增大。基于持续通量全球变暖潜势和持续通量全球冷却潜势模型的结果,我们的论文表明,沿海湿地的 CH 和 NO 通量对全球变暖具有正反馈作用,主要由 CH 排放驱动。我们的综合研究提高了对全球变化下沿海湿地在生态系统 C 循环中作用的认识。我们建议迫切需要在更广泛的时空尺度上进行长期的 GHG 通量实地观测,以提高 GHG 通量的预测精度,并评估净 GHG 平衡及其对沿海湿地全球变暖潜势的贡献。

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