The enduring world forest carbon sink

作者：Yude Pan, Richard A. Birdsey, Oliver L. Phillips, R. A. Houghton, Jingyun Fang, Pekka E. Kauppi, Heather Keith, Werner A. Kurz, Akihiko Ito, Simon L. Lewis, G.J. Nabuurs, А. Shvidenko, Shoji Hashimoto, Bas Lerink, Dmitry Schepaschenko, Andrea Castanho, Daniel Murdiyarso · 发表于：Nature · 年份：2024 · DOI：10.1038/s41586-024-07602-x · 被引用次数：686 · 研究领域：Forest Management and Policy、Conservation, Biodiversity, and Resource Management、Climate Change Policy and Economics

The uptake of carbon dioxide (CO2) by terrestrial ecosystems is critical for moderating climate change1. To provide a ground-based long-term assessment of the contribution of forests to terrestrial CO2 uptake, we synthesized in situ forest data from boreal, temperate and tropical biomes spanning three decades. We found that the carbon sink in global forests was steady, at 3.6 ± 0.4 Pg C yr−1 in the 1990s and 2000s, and 3.5 ± 0.4 Pg C yr−1 in the 2010s. Despite this global stability, our analysis revealed some major biome-level changes. Carbon sinks have increased in temperate (+30 ± 5%) and tropical regrowth (+29 ± 8%) forests owing to increases in forest area, but they decreased in boreal (−36 ± 6%) and tropical intact (−31 ± 7%) forests, as a result of intensified disturbances and losses in intact forest area, respectively. Mass-balance studies indicate that the global land carbon sink has increased2, implying an increase in the non-forest-land carbon sink. The global forest sink is equivalent to almost half of fossil-fuel emissions (7.8 ± 0.4 Pg C yr−1 in 1990–2019). However, two-thirds of the benefit from the sink has been negated by tropical deforestation (2.2 ± 0.5 Pg C yr−1 in 1990–2019). Although the global forest sink has endured undiminished for three decades, despite regional variations, it could be weakened by ageing forests, continuing deforestation and further intensification of disturbance regimes1. To protect the carbon sink, land management policies are neede...