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Species-Specific Shifts in Diurnal Sap Velocity Dynamics and Hysteretic Behavior of Ecophysiological Variables During the 2015-2016 El Niño Event in the Amazon Forest.
Gimenez, Bruno O; Jardine, Kolby J; Higuchi, Niro; Negrón-Juárez, Robinson I; Sampaio-Filho, Israel de Jesus; Cobello, Leticia O; Fontes, Clarissa G; Dawson, Todd E; Varadharajan, Charuleka; Christianson, Danielle S; Spanner, Gustavo C; Araújo, Alessandro C; Warren, Jeffrey M; Newman, Brent D; Holm, Jennifer A; Koven, Charles D; McDowell, Nate G; Chambers, Jeffrey Q.
Affiliation
  • Gimenez BO; National Institute of Amazonian Research (INPA), Manaus, Brazil.
  • Jardine KJ; Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, United States.
  • Higuchi N; National Institute of Amazonian Research (INPA), Manaus, Brazil.
  • Negrón-Juárez RI; Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, United States.
  • Sampaio-Filho IJ; National Institute of Amazonian Research (INPA), Manaus, Brazil.
  • Cobello LO; National Institute of Amazonian Research (INPA), Manaus, Brazil.
  • Fontes CG; Department of Integrative Biology, University of California, Berkeley, Berkeley, CA, United States.
  • Dawson TE; Department of Integrative Biology, University of California, Berkeley, Berkeley, CA, United States.
  • Varadharajan C; Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, United States.
  • Christianson DS; Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, United States.
  • Spanner GC; National Institute of Amazonian Research (INPA), Manaus, Brazil.
  • Araújo AC; Embrapa Amazônia Oriental, Belém, Brazil.
  • Warren JM; Environmental Sciences Division and Climate Change Science Institute, Oak Ridge National Laboratory, Oak Ridge, TN, United States.
  • Newman BD; Earth and Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos, NM, United States.
  • Holm JA; Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, United States.
  • Koven CD; Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, United States.
  • McDowell NG; Pacific Northwest National Laboratory, Richland, WA, United States.
  • Chambers JQ; Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, United States.
Front Plant Sci ; 10: 830, 2019.
Article de En | MEDLINE | ID: mdl-31316536
ABSTRACT
Current climate change scenarios indicate warmer temperatures and the potential for more extreme droughts in the tropics, such that a mechanistic understanding of the water cycle from individual trees to landscapes is needed to adequately predict future changes in forest structure and function. In this study, we contrasted physiological responses of tropical trees during a normal dry season with the extreme dry season due to the 2015-2016 El Niño-Southern Oscillation (ENSO) event. We quantified high resolution temporal dynamics of sap velocity (Vs), stomatal conductance (gs) and leaf water potential (ΨL) of multiple canopy trees, and their correlations with leaf temperature (Tleaf) and environmental conditions [direct solar radiation, air temperature (Tair) and vapor pressure deficit (VPD)]. The experiment leveraged canopy access towers to measure adjacent trees at the ZF2 and Tapajós tropical forest research (near the cities of Manaus and Santarém). The temporal difference between the peak of gs (late morning) and the peak of VPD (early afternoon) is one of the major regulators of sap velocity hysteresis patterns. Sap velocity displayed species-specific diurnal hysteresis patterns reflected by changes in Tleaf. In the morning, Tleaf and sap velocity displayed a sigmoidal relationship. In the afternoon, stomatal conductance declined as Tleaf approached a daily peak, allowing ΨL to begin recovery, while sap velocity declined with an exponential relationship with Tleaf. In Manaus, hysteresis indices of the variables Tleaf-Tair and ΨL-Tleaf were calculated for different species and a significant difference (p < 0.01, α = 0.05) was observed when the 2015 dry season (ENSO period) was compared with the 2017 dry season ("control scenario"). In some days during the 2015 ENSO event, Tleaf approached 40°C for all studied species and the differences between Tleaf and Tair reached as high at 8°C (average difference 1.65 ± 1.07°C). Generally, Tleaf was higher than Tair during the middle morning to early afternoon, and lower than Tair during the early morning, late afternoon and night. Our results support the hypothesis that partial stomatal closure allows for a recovery in ΨL during the afternoon period giving an observed counterclockwise hysteresis pattern between ΨL and Tleaf.
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Texte intégral: 1 Collection: 01-internacional Base de données: MEDLINE Type d'étude: Prognostic_studies Langue: En Journal: Front Plant Sci Année: 2019 Type de document: Article Pays d'affiliation: Brésil

Texte intégral: 1 Collection: 01-internacional Base de données: MEDLINE Type d'étude: Prognostic_studies Langue: En Journal: Front Plant Sci Année: 2019 Type de document: Article Pays d'affiliation: Brésil