Ecological restoration enhances dryland carbon stock by reducing surface soil carbon loss due to wind erosion
成果类型:
Article
署名作者:
Song, Jian; Wan, Shiqiang; Zhang, Kesheng; Hong, Songbai; Xia, Jianyang; Piao, Shilong; Wang, Ying-Ping; Cheni, Jiquan; Hui, Dafeng; Luo, Yiqi; Niul, Shuli; Ru, Jingyi; Xu, Hao; Zheng, Mengmei; Liun, Weixing; Wang, Haidao; Tan, Menghao; Zhou, Zhenxing; Feng, Jiayin; Qiu, Xueli
署名单位:
Hebei University; Luoyang Institute of Science & Technology; Peking University; Peking University Shenzhen Graduate School (PKU Shenzhen); East China Normal University; East China Normal University; Peking University; Chinese Academy of Sciences; Institute of Tibetan Plateau Research, CAS; Commonwealth Scientific & Industrial Research Organisation (CSIRO); CSIRO Environment; Michigan State University; Tennessee State University; Cornell University; Chinese Academy of Sciences; Institute of Geographic Sciences & Natural Resources Research, CAS; Henan Normal University; Chinese Academy of Agricultural Sciences; Institute of Agricultural Resources & Regional Planning, CAAS
刊物名称:
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
ISSN/ISSBN:
0027-11555
DOI:
10.1073/pnas.2416281121
发表日期:
2024-11-12
关键词:
organic-carbon
northern china
CLIMATE-CHANGE
plant
sequestration
ecosystems
grassland
storage
摘要:
Enhancing terrestrial carbon (C) stock through ecological restoration, one of the prominent approaches for natural climate solutions, is conventionally considered to be achieved through an ecological pathway, i.e., increased plant C uptake. By conducting a comprehensive regional survey of 4279 1 x 1 m2 plots at 517 sites across China's drylands and a 13- y manipulative experiment in a semiarid grassland within the same region, we show that greater soil and ecosystem C stocks in restored than degraded lands result predominantly from decreased surface soil C loss via suppressed wind erosion. This biophysical pathway is always overlooked in model evaluation of land- based C mitigation strategies. Surprisingly, stimulated plant growth plays a minor role in regulating C stocks under ecological restoration. In addition, the overall enhancement of C stocks in the restored lands increases with both initial degradation intensity and restoration duration. At the national scale, the rate of soil C accumulation (7.87 Tg C y-1) due to reduced wind erosion and surface soil C loss under dryland restoration is equal to 38.8% of afforestation and 56.2% of forest protection in China. Incorporating this unique but largely missed biophysical C- conserving mechanism into land surface models will greatly improve global assessments of the potential of land restoration for mitigating climate change.