Department of Ecology, College of Urban and Environmental Sciences, 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;
Research Faculty of Agriculture, Hokkaido University, Sapporo, Hokkaido 060-8589, Japan;
Proc Natl Acad Sci U S A. 2014 Jul 1;111(26):9527-32. doi: 10.1073/pnas.1402333111. Epub 2014 Jun 16.
Forests in the middle and high latitudes of the northern hemisphere function as a significant sink for atmospheric carbon dioxide (CO2). This carbon (C) sink has been attributed to two processes: age-related growth after land use change and growth enhancement due to environmental changes, such as elevated CO2, nitrogen deposition, and climate change. However, attribution between these two processes is largely controversial. Here, using a unique time series of an age-class dataset from six national forest inventories in Japan and a new approach developed in this study (i.e., examining changes in biomass density at each age class over the inventory periods), we quantify the growth enhancement due to environmental changes and its contribution to biomass C sink in Japan's forests. We show that the growth enhancement for four major plantations was 4.0∼7.7 Mg C⋅ha(-1) from 1980 to 2005, being 8.4-21.6% of biomass C sequestration per hectare and 4.1-35.5% of the country's total net biomass increase of each forest type. The growth enhancement differs among forest types, age classes, and regions. Our results provide, to our knowledge, the first ground-based evidence that global environmental changes can increase C sequestration in forests on a broad geographic scale and imply that both the traits and age of trees regulate the responses of forest growth to environmental changes. These findings should be incorporated into the prediction of forest C cycling under a changing climate.
北半球中高纬度地区的森林是大气二氧化碳(CO2)的重要汇。这个碳(C)汇归因于两个过程:土地利用变化后的年龄相关生长和环境变化(如 CO2 升高、氮沉积和气候变化)导致的生长增强。然而,这两个过程之间的归因在很大程度上存在争议。在这里,我们使用了来自日本六个国家森林清查的独特年龄类数据集时间序列和本研究中开发的一种新方法(即检查清查期间每个年龄类别的生物量密度变化),量化了环境变化引起的生长增强及其对日本森林生物量 C 汇的贡献。我们表明,1980 年至 2005 年期间,四大人工林的生长增强为 4.0∼7.7 Mg C⋅ha(-1),占每公顷生物量 C 封存的 8.4-21.6%,占每个森林类型的全国净生物量增加的 4.1-35.5%。生长增强因森林类型、年龄类和地区而异。我们的结果提供了,据我们所知,第一个基于地面的证据,表明全球环境变化可以在广泛的地理范围内增加森林的碳封存,并暗示树木的特征和年龄调节了森林生长对环境变化的响应。这些发现应纳入气候变化下森林 C 循环预测。