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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...

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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
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author 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.
author_facet 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.
author_sort Yu, Kailiang
collection PubMed
description 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.
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spelling pubmed-69005272019-12-12 Pervasive decreases in living vegetation carbon turnover time across forest climate zones 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. Proc Natl Acad Sci U S A Biological Sciences 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. National Academy of Sciences 2019-12-03 2019-11-18 /pmc/articles/PMC6900527/ /pubmed/31740604 http://dx.doi.org/10.1073/pnas.1821387116 Text en Copyright © 2019 the Author(s). Published by PNAS. https://creativecommons.org/licenses/by-nc-nd/4.0/ https://creativecommons.org/licenses/by-nc-nd/4.0/This open access article is distributed under Creative Commons Attribution-NonCommercial-NoDerivatives License 4.0 (CC BY-NC-ND) (https://creativecommons.org/licenses/by-nc-nd/4.0/) .
spellingShingle Biological Sciences
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.
Pervasive decreases in living vegetation carbon turnover time across forest climate zones
title Pervasive decreases in living vegetation carbon turnover time across forest climate zones
title_full Pervasive decreases in living vegetation carbon turnover time across forest climate zones
title_fullStr Pervasive decreases in living vegetation carbon turnover time across forest climate zones
title_full_unstemmed Pervasive decreases in living vegetation carbon turnover time across forest climate zones
title_short Pervasive decreases in living vegetation carbon turnover time across forest climate zones
title_sort pervasive decreases in living vegetation carbon turnover time across forest climate zones
topic Biological Sciences
url 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
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