固碳
生物量(生态学)
环境科学
陆地生态系统
碳循环
土壤碳
碳纤维
植被(病理学)
陆生植物
生态系统
生态学
二氧化碳
土壤科学
生物
土壤水分
医学
材料科学
病理
复合数
复合材料
作者
Yinon M. Bar-On,Xiaojun Li,Michael O’Sullivan,Jean‐Pierre Wigneron,Stephen Sitch,Philippe Ciais,Christian Frankenberg,Woodward W. Fischer
出处
期刊:Science
[American Association for the Advancement of Science]
日期:2025-03-20
卷期号:387 (6740): 1291-1295
标识
DOI:10.1126/science.adk1637
摘要
Terrestrial sequestration of carbon has mitigated ≈30% of anthropogenic carbon emissions. However, its distribution across different pools, live or dead biomass and soil and sedimentary organic carbon, remains uncertain. Analyzing global observational datasets of changes in terrestrial carbon pools, we found that ≈35 ± 14 gigatons of carbon (GtC) have been sequestered on land between 1992 and 2019, whereas live biomass changed by ≈1 ± 7 GtC. Global vegetation models instead imply that sequestration has been mostly in live biomass. We identify key processes not included in most models that can explain this discrepancy. Most terrestrial carbon gains are sequestered as nonliving matter and thus are more persistent than previously appreciated, with a substantial fraction linked to human activities such as river damming, wood harvest, and garbage disposal in landfills.
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