Cargando…

Pervasive decreases in living vegetation carbon turnover time across forest climate zones

Forests play a major role in the global carbon cycle. Previous studies on the capacity of forests to sequester atmospheric CO(2) have mostly focused on carbon uptake, but the roles of carbon turnover time and its spatiotemporal changes remain poorly understood. Here, we used long-term inventory data...

Descripción completa

Detalles Bibliográficos
Autores principales: Yu, Kailiang, Smith, William K., Trugman, Anna T., Condit, Richard, Hubbell, Stephen P., Sardans, Jordi, Peng, Changhui, Zhu, Kai, Peñuelas, Josep, Cailleret, Maxime, Levanic, Tom, Gessler, Arthur, Schaub, Marcus, Ferretti, Marco, Anderegg, William R. L.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6900527/
https://www.ncbi.nlm.nih.gov/pubmed/31740604
http://dx.doi.org/10.1073/pnas.1821387116
Descripción
Sumario:Forests play a major role in the global carbon cycle. Previous studies on the capacity of forests to sequester atmospheric CO(2) have mostly focused on carbon uptake, but the roles of carbon turnover time and its spatiotemporal changes remain poorly understood. Here, we used long-term inventory data (1955 to 2018) from 695 mature forest plots to quantify temporal trends in living vegetation carbon turnover time across tropical, temperate, and cold climate zones, and compared plot data to 8 Earth system models (ESMs). Long-term plots consistently showed decreases in living vegetation carbon turnover time, likely driven by increased tree mortality across all major climate zones. Changes in living vegetation carbon turnover time were negatively correlated with CO(2) enrichment in both forest plot data and ESM simulations. However, plot-based correlations between living vegetation carbon turnover time and climate drivers such as precipitation and temperature diverged from those of ESM simulations. Our analyses suggest that forest carbon sinks are likely to be constrained by a decrease in living vegetation carbon turnover time, and accurate projections of forest carbon sink dynamics will require an improved representation of tree mortality processes and their sensitivity to climate in ESMs.