Seasonal trends of Amazonian rainforest phenology, net primary productivity, and carbon allocation

dc.contributor.authorCécile Girardin
dc.contributor.authorYadvinder Malhi
dc.contributor.authorChristopher E. Doughty
dc.contributor.authorDaniel B. Metcalfe
dc.contributor.authorPatrick Meir
dc.contributor.authorJhon del Águila Pasquel
dc.contributor.authorAlejandro Araujo‐Murakami
dc.contributor.authorAntônio C. L. da Costa
dc.contributor.authorJavier E. Silva‐Espejo
dc.contributor.authorFilio Farfán Amézquita
dc.coverage.spatialBolivia
dc.date.accessioned2026-03-22T14:03:58Z
dc.date.available2026-03-22T14:03:58Z
dc.date.issued2016
dc.descriptionCitaciones: 74
dc.description.abstractAbstract The seasonality of solar irradiance and precipitation may regulate seasonal variations in tropical forests carbon cycling. Controversy remains over their importance as drivers of seasonal dynamics of net primary productivity in tropical forests. We use ground data from nine lowland Amazonian forest plots collected over 3 years to quantify the monthly primary productivity ( NPP ) of leaves, reproductive material, woody material, and fine roots over an annual cycle. We distinguish between forests that do not experience substantial seasonal moisture stress (“humid sites”) and forests that experience a stronger dry season (“dry sites”). We find that forests from both precipitation regimes maximize leaf NPP over the drier season, with a peak in production in August at both humid (mean 0.39 ± 0.03 Mg C ha −1 month −1 in July, n = 4) and dry sites (mean 0.49 ± 0.03 Mg C ha −1 month −1 in September, n = 8). We identify two distinct seasonal carbon allocation patterns (the allocation of NPP to a specific organ such as wood leaves or fine roots divided by total NPP ). The forests monitored in the present study show evidence of either (i) constant allocation to roots and a seasonal trade‐off between leaf and woody material or (ii) constant allocation to wood and a seasonal trade‐off between roots and leaves. Finally, we find strong evidence of synchronized flowering at the end of the dry season in both precipitation regimes. Flower production reaches a maximum of 0.047 ± 0.013 and 0.031 ± 0.004 Mg C ha −1 month −1 in November, in humid and dry sites, respectively. Fruitfall production was staggered throughout the year, probably reflecting the high variation in varying times to development and loss of fruit among species.
dc.identifier.doi10.1002/2015gb005270
dc.identifier.urihttps://doi.org/10.1002/2015gb005270
dc.identifier.urihttps://andeanlibrary.org/handle/123456789/44339
dc.language.isoen
dc.publisherWiley
dc.relation.ispartofGlobal Biogeochemical Cycles
dc.sourceUniversity of Oxford
dc.subjectPrimary production
dc.subjectDry season
dc.subjectSeasonality
dc.subjectAmazonian
dc.subjectEnvironmental science
dc.subjectProductivity
dc.subjectPhenology
dc.subjectRainforest
dc.subjectWet season
dc.subjectPrecipitation
dc.titleSeasonal trends of Amazonian rainforest phenology, net primary productivity, and carbon allocation
dc.typearticle

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