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Drought stress and tree size determine stem CO (2) efflux in a tropical forest

CO (2) efflux from stems (CO (2_stem)) accounts for a substantial fraction of tropical forest gross primary productivity, but the climate sensitivity of this flux remains poorly understood. We present a study of tropical forest CO (2_stem) from 215 trees across wet and dry seasons, at the world'...

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Detalles Bibliográficos
Autores principales: Rowland, Lucy, da Costa, Antonio C. L., Oliveira, Alex A. R., Oliveira, Rafael S., Bittencourt, Paulo L., Costa, Patricia B., Giles, Andre L., Sosa, Azul I., Coughlin, Ingrid, Godlee, John L., Vasconcelos, Steel S., Junior, João A. S., Ferreira, Leandro V., Mencuccini, Maurizio, Meir, Patrick
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2018
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5969101/
https://www.ncbi.nlm.nih.gov/pubmed/29397028
http://dx.doi.org/10.1111/nph.15024
Descripción
Sumario:CO (2) efflux from stems (CO (2_stem)) accounts for a substantial fraction of tropical forest gross primary productivity, but the climate sensitivity of this flux remains poorly understood. We present a study of tropical forest CO (2_stem) from 215 trees across wet and dry seasons, at the world's longest running tropical forest drought experiment site. We show a 27% increase in wet season CO (2_stem) in the droughted forest relative to a control forest. This was driven by increasing CO (2_stem) in trees 10–40 cm diameter. Furthermore, we show that drought increases the proportion of maintenance to growth respiration in trees > 20 cm diameter, including large increases in maintenance respiration in the largest droughted trees, > 40 cm diameter. However, we found no clear taxonomic influence on CO (2_stem) and were unable to accurately predict how drought sensitivity altered ecosystem scale CO (2_stem), due to substantial uncertainty introduced by contrasting methods previously employed to scale CO (2_stem) fluxes. Our findings indicate that under future scenarios of elevated drought, increases in CO (2_stem) may augment carbon losses, weakening or potentially reversing the tropical forest carbon sink. However, due to substantial uncertainties in scaling CO (2_stem) fluxes, stand‐scale future estimates of changes in stem CO (2) emissions remain highly uncertain.