Climatic influences on leaf phenology, xylogenesis and radial stem changes at hourly to monthly scales in two tropical dry forests

© 2015 Elsevier B.V. Assessing the effects of climate on leaf phenology and xylem development will improve our understanding of how wood formation and carbon uptake occur in tropical tree species. Wood formation depends on how tree stems enlarge, shrink or swell at multiple temporal scales. To address these issues we analyzed climate data, leaf phenology, xylogenesis and radial increment at hourly to monthly scales of ten tree species in two tropical dry forests with different drought seasonality and severity (the wet Tuluá site is located in Colombia and the dry INPA site is situated in Bolivia). Leaf flushing and radial growth occurred during the wet season at both sites, reflecting the influence of high precipitation, a positive water balance and low vapor pressure deficit on the development of new leaves and xylem cells. In Tuluá, the xylem growing season was associated with low air temperatures, while in INPA it was related to high air temperatures. At both sites, the high air temperatures registered throughout the day negatively affected radial-increment rates at hourly scales, probably by rising vapor pressure deficit and enhancing evapotranspiration rates. Tree species could face adverse dry conditions by growing in periods of the day when temperatures decrease and water loss due to evapotranspiration is reduced, particularly at dry INPA site. Stem shrinkage and swelling were observed at hourly to daily scales in all tree species, but most INPA species also registered strong reversible shrinkage at monthly scales. The strength of the positive association between leaf flushing and radial-increment rates was species-specific and it related to sapwood density. Thus, Cedrela fissilis, a pioneer deciduous species with low sapwood density showed the strongest associations between leaf flushing and radial-increment rates, whereas Acosmium cardenasii, a shade-tolerant deciduous species showed the reverse characteristic. The time-dependent growth responses of tree species to water availability should be explicitly considered to properly forecast their responses to climate warming and to evaluate their relevance as carbon sinks under warmer and drier conditions.We are grateful to all the staff of the Jardín Botánico “Juan María Céspedes” (INCIVA, Colombia) and the Instituto Boliviano de Investigación Forestal (IBIF, Bolivia) for their support, particularly to M. Toledo and W. Devia. We sincerely acknowledge P. Roosenboom (INPA PARKET Ltda) and his staff at Concepción (G. Urbano) for their help in Bolivia. We also thank J. Chamo for his help in the field and M. Sancho and O. Romero for their help in the laboratory. We would also like to thank P.A. Zuidema, J.D. Fuentes, and an anonymous reviewer for their constructive comments on an earlier version of this manuscript. This study was supported by the following research projects “Análisis retrospectivos mediante dendrocronología para profundizar en la ecología y mejorar la gestión de los bosques tropicales secos” (financed by Fundación BBVA) and “Regeneración, crecimiento y modelos dinámicos de bosques tropicales secos: herramientas para su conservación y para el uso sostenible de especies maderables” (AECID 11-CAP2-1730, Spanish Ministry of Foreign Affairs).Peer Reviewe