Causes of reduced leaf-level photosynthesis during strong El Niño drought in a Central Amazon forest

dc.contributor.authorSantos, Victor Alexandre Hardt Ferreira dos
dc.contributor.authorFerreira, Marciel José
dc.contributor.authorRodrigues, J. V. F. C.
dc.contributor.authorGarcia, Maquelle Neves
dc.contributor.authorCeron, João Vitor Barbosa
dc.contributor.authorNelson, Bruce Walker
dc.contributor.authorSaleska, Scott Reid
dc.date.accessioned2020-06-15T21:36:51Z
dc.date.available2020-06-15T21:36:51Z
dc.date.issued2018
dc.description.abstractSustained drought and concomitant high temperature may reduce photosynthesis and cause tree mortality. Possible causes of reduced photosynthesis include stomatal closure and biochemical inhibition, but their relative roles are unknown in Amazon trees during strong drought events. We assessed the effects of the recent (2015) strong El Niño drought on leaf-level photosynthesis of Central Amazon trees via these two mechanisms. Through four seasons of 2015, we measured leaf gas exchange, chlorophyll a fluorescence parameters, chlorophyll concentration, and nutrient content in leaves of 57 upper canopy and understory trees of a lowland terra firme forest on well-drained infertile oxisol. Photosynthesis decreased 28% in the upper canopy and 17% in understory trees during the extreme dry season of 2015, relative to other 2015 seasons and was also lower than the climatically normal dry season of the following non-El Niño year. Photosynthesis reduction under extreme drought and high temperature in the 2015 dry season was related only to stomatal closure in both upper canopy and understory trees, and not to chlorophyll a fluorescence parameters, chlorophyll, or leaf nutrient concentration. The distinction is important because stomatal closure is a transient regulatory response that can reverse when water becomes available, whereas the other responses reflect more permanent changes or damage to the photosynthetic apparatus. Photosynthesis decrease due to stomatal closure during the 2015 extreme dry season was followed 2 months later by an increase in photosynthesis as rains returned, indicating a margin of resilience to one-off extreme climatic events in Amazonian forests. © 2018 John Wiley & Sons Ltden
dc.identifier.doi10.1111/gcb.14293
dc.identifier.urihttps://repositorio.inpa.gov.br/handle/1/16864
dc.language.isoenpt_BR
dc.publisher.journalGlobal Change Biologypt_BR
dc.relation.ispartofVolume 24, Número 9, Pags. 4266-4279pt_BR
dc.rightsRestrito*
dc.subjectChlorophyllen
dc.subjectClimate Changeen
dc.subjectDrought Stressen
dc.subjectEl Ninoen
dc.subjectExtreme Eventen
dc.subjectPhotosynthesisen
dc.subjectStomatal Conductanceen
dc.subjectTropical Foresten
dc.subjectWarmingen
dc.subjectAmazoniaen
dc.subjectDroughten
dc.subjectEl Ninoen
dc.subjectForesten
dc.subjectPhotosynthesisen
dc.subjectPhysiologyen
dc.subjectPlant Leafen
dc.subjectSeasonen
dc.subjectTreeen
dc.subjectDroughtsen
dc.subjectEl Nino-southern Oscillationen
dc.subjectForestsen
dc.subjectPhotosynthesisen
dc.subjectPlant Leavesen
dc.subjectSeasonsen
dc.subjectTreesen
dc.titleCauses of reduced leaf-level photosynthesis during strong El Niño drought in a Central Amazon foresten
dc.typeArtigopt_BR

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