Article Synopsis

  • Mounting evidence suggests that human-induced climate change is altering plant species composition in tropical forests, with a focus on a 28-year study of tropical flower phenology.
  • An increase in flower activity is mainly linked to rising atmospheric CO levels, which have a much stronger effect on flowering compared to other climate factors like rainfall and solar radiation.
  • While flowering activity has decreased for lianas and canopy trees in the last decade, some species like midstory trees and shrubs continue to see increases, potentially lasting until limited by nutrients or further climate changes.

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Article Abstract

Mounting evidence suggests that anthropogenic global change is altering plant species composition in tropical forests. Fewer studies, however, have focused on long-term trends in reproductive activity, in part because of the lack of data from tropical sites. Here, we analyze a 28-year record of tropical flower phenology in response to anthropogenic climate and atmospheric change. We show that a multidecadal increase in flower activity is most strongly associated with rising atmospheric CO concentrations using yearly aggregated data. Compared to significant climatic factors, CO had on average an approximately three-, four-, or fivefold stronger effect than rainfall, solar radiation, and the Multivariate ENSO Index, respectively. Peaks in flower activity were associated with greater solar radiation and lower rainfall during El Niño years. The effect of atmospheric CO on flowering has diminished over the most recent decade for lianas and canopy trees, whereas flowering of midstory trees and shrub species continued to increase with rising CO . Increases in flowering were accompanied by a lengthening of flowering duration for canopy and midstory trees. Understory treelets did not show increases in flowering but did show increases in duration. Given that atmospheric CO will likely continue to climb over the next century, a long-term increase in flowering activity may persist in some growth forms until checked by nutrient limitation or by climate change through rising temperatures, increasing drought frequency and/or increasing cloudiness and reduced insolation.

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http://dx.doi.org/10.1111/gcb.14004DOI Listing

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