Zhu Jianxiao, Hu Huifeng, Tao Shengli, Chi Xiulian, Li Peng, Jiang Lai, Ji Chengjun, Zhu Jiangling, Tang Zhiyao, Pan Yude, Birdsey Richard A, He Xinhua, Fang Jingyun
Department of Ecology, College of Urban and Environmental Science, and Key Laboratory for Earth Surface Processes of the Ministry of Education, Peking University, Beijing, 100871, China.
State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing, 100093, China.
Nat Commun. 2017 Jul 28;8(1):151. doi: 10.1038/s41467-017-00207-1.
Forests play an important role in global carbon cycles. However, the lack of available information on carbon stocks in dead organic matter, including woody debris and litter, reduces the reliability of assessing the carbon cycles in entire forest ecosystems. Here we estimate that the national DOM carbon stock in the period of 2004-2008 is 925 ± 54 Tg, with an average density of 5.95 ± 0.35 Mg C ha. Over the past two decades from periods of 1984-1988 to 2004-2008, the national dead organic matter carbon stock has increased by 6.7 ± 2.2 Tg carbon per year, primarily due to increasing forest area. Temperature and precipitation increase the carbon density of woody debris, but decrease that of litter. Additionally, the woody debris increases significantly with above ground biomass and forest age. Our results can improve estimates of the carbon budget in China's forests and for better understanding of effects of climate and stand characteristics on dead organic matter distribution.Reliable estimates of the total forest carbon (C) pool are lacking due to insufficient information on dead organic matter (DOM). Here, the authors estimate that the current DOM C stock in China is 925 ± 54 Tg and that it grew by 6.7 ± 2.2 Tg C/yr over the past two decades primarily due to increasing forest area.
森林在全球碳循环中发挥着重要作用。然而,由于缺乏关于包括木质残体和凋落物在内的死有机物质碳储量的可用信息,降低了评估整个森林生态系统碳循环的可靠性。在此,我们估计2004 - 2008年期间全国死有机物质碳储量为925±54太克,平均密度为5.95±0.35兆克碳/公顷。在1984 - 1988年至2004 - 2008年的过去二十年中,全国死有机物质碳储量每年增加6.7±2.2太克碳,主要原因是森林面积增加。温度和降水增加了木质残体的碳密度,但降低了凋落物的碳密度。此外,木质残体随地上生物量和林龄显著增加。我们的结果可以改进对中国森林碳预算的估计,并更好地理解气候和林分特征对死有机物质分布的影响。由于关于死有机物质(DOM)的信息不足,目前缺乏对森林总碳(C)库的可靠估计。在此,作者估计中国目前的DOM碳储量为925±54太克,并且在过去二十年中每年增长6.7±2.2太克碳,主要原因是森林面积增加。