National Plateau Wetlands Research Center, Southwest Forestry University, Kunming, Yunnan, China.
State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling, Shaanxi, China.
Glob Chang Biol. 2019 Jun;25(6):2061-2076. doi: 10.1111/gcb.14621. Epub 2019 Apr 7.
Wetlands contain a large proportion of carbon (C) in the biosphere and partly affect climate by regulating C cycles of terrestrial ecosystems. China contains Asia's largest wetlands, accounting for about 10% of the global wetland area. Although previous studies attempted to estimate C budget in China's wetlands, uncertainties remain. We conducted a synthesis to estimate C uptake and emission of wetland ecosystems in China using a dataset compiled from published literature. The dataset comprised 193 studies, including 370 sites representing coastal, river, lake and marsh wetlands across China. In addition, C stocks of different wetlands in China were estimated using unbiased data from the China Second Wetlands Survey. The results showed that China's wetlands sequestered 16.87 Pg C (315.76 Mg C/ha), accounting for about 3.8% of C stocks in global wetlands. Net ecosystem productivity, jointly determined by gross primary productivity and ecosystem respiration, exhibited annual C sequestration of 120.23 Tg C. China's wetlands had a total gaseous C loss of 173.20 Tg C per year from soils, including 154.26 Tg CO -C and 18.94 Tg CH -C emissions. Moreover, C stocks, uptakes and gaseous losses varied with wetland types, and were affected by geographic location and climatic factors (precipitation and temperature). Our results provide better estimation of the C budget in China's wetlands and improve understanding of their contribution to the global C cycle in the context of global climate change.
湿地在生物圈中储存了大量的碳(C),通过调节陆地生态系统的碳循环在一定程度上影响着气候。中国拥有亚洲最大的湿地,占全球湿地面积的 10%左右。尽管之前的研究试图估算中国湿地的碳预算,但仍存在不确定性。我们利用已发表文献中的数据集进行了综合分析,以估算中国湿地生态系统的碳吸收和排放。该数据集包括 193 项研究,涉及中国沿海、河流、湖泊和沼泽湿地的 370 个地点。此外,我们还利用中国第二次湿地调查的无偏数据来估算中国不同湿地的碳储量。结果表明,中国湿地固碳 16.87 Pg C(315.76 Mg C/ha),约占全球湿地碳储量的 3.8%。净生态系统生产力由总初级生产力和生态系统呼吸共同决定,表现为每年 120.23 Tg C 的碳固存。中国湿地土壤每年的气态碳损失总量为 173.20 Tg C,包括 154.26 Tg CO -C 和 18.94 Tg CH -C 的排放。此外,碳储量、吸收量和气态损失随湿地类型而变化,并受地理位置和气候因素(降水和温度)的影响。我们的研究结果为更好地估算中国湿地的碳预算提供了依据,并在全球气候变化背景下,提高了对其在全球碳循环中贡献的认识。
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