ArticlePlant-environment interactions (Hoboken, N.J.)2024
Historical tree phenology data reveal the seasonal rhythms of the Congo Basin rainforest.
Article in Plant-environment interactions (Hoboken, N.J.), 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 5 papers.
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Who cites it
5 citing papers in PubMed.
- Historical tree phenology data across contrasting sites in the Congo Basin.Scientific data · 2026Article
- Congo Basin Carbon Cycle Responses to Global Change.Global change biology · 2026Review
- Asynchronous xylogenesis among and within tree species in the central Congo Basin.BMC plant biology · 2025Article
- Growth periodicity in semi-deciduous tropical tree species from the Congo Basin.Plant-environment interactions (Hoboken, N.J.) · 2024Article
- Historical tree phenology data reveal the seasonal rhythms of the Congo Basin rainforest.Plant-environment interactions (Hoboken, N.J.) · 2024Article
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18 authors.
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Abstract
Tropical forest phenology directly affects regional carbon cycles, but the relation between species-specific and whole-canopy phenology remains largely uncharacterized. We present a unique analysis of historical tropical tree phenology collected in the central Congo Basin, before large-scale impacts of human-induced climate change. Ground-based long-term (1937-1956) phenological observations of 140 tropical tree species are recovered, species-specific phenological patterns analyzed and related to historical meteorological records, and scaled to characterize stand-level canopy dynamics. High phenological variability within and across species and in climate-phenology relationships is observed. The onset of leaf phenophases in deciduous species was triggered by drought and light availability for a subset of species and showed a species-specific decoupling in time along a bi-modal seasonality. The majority of the species remain evergreen, although central African forests experience relatively low rainfall. Annually a maximum of 1.5% of the canopy is in leaf senescence or leaf turnover, with overall phenological variability dominated by a few deciduous species, while substantial variability is attributed to asynchronous events of large and/or abundant trees. Our results underscore the importance of accounting for constituent signals in canopy-wide scaling and the interpretation of remotely sensed phenology signals.
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