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A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...

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WATER POTENTIAL OF PLANTS IN DIFFERENT CONDITIONS OF LIGHTINTENSITY IN ATROPICAL RAIN FOREST – SAVANNA ECOTONE OF MATOGROSSOPedro Correto Priante 1 (Rua dos Eucaliptos, n. 7 Quadra 15, J. das Palmeiras – Cuiabá-MT –Brazil pedropri@terra.com.br), Eduardo Jacusiel Miranda 1 , Clóvis Lasta Fritzen 2 , NicolauPriante Filho 1 , José de Souza Nogueira 1 and George Louis Vourlitis 31 Universidade Federal de M<strong>at</strong>o Grosso; 2 Universidade Federal de M<strong>at</strong>o Grosso do Sul;3 California St<strong>at</strong>e University San MarcosMeasurements of <strong>the</strong> w<strong>at</strong>er potential of transitional tropical forest understorey plants weremade seasonally to determine <strong>the</strong> effect of seasonal vari<strong>at</strong>ions in rainfall on plant-w<strong>at</strong>erst<strong>at</strong>us. The study was conducted in an intact transitional forest stand loc<strong>at</strong>ed near Sinop,M<strong>at</strong>o Grosso, and we chose plants th<strong>at</strong> were common to <strong>the</strong> region, Quiina pteridophyllaand Dinizia excelsa, in different conditions of luminosity (plants loc<strong>at</strong>ed in gap and shadedareas). The measurements were made in 2 young and 3 adult individuals per species during<strong>the</strong> wet season, transition wet-dry season, dry season, and transition dry-wet season. The Q.pteridophylla individuals presented large season vari<strong>at</strong>ion in w<strong>at</strong>er potential. The Q.pteridophylla in <strong>the</strong> wet season had an average w<strong>at</strong>er potential of –0.5MPa, 1.7 MPa in <strong>the</strong>transition from <strong>the</strong> wet-dry season, -2.7 MPa in <strong>the</strong> dry season and, –1.7MPa in <strong>the</strong> transitionbetween <strong>the</strong> dry-wet season. Adult trees had an average w<strong>at</strong>er potential of –0.9MPa in <strong>the</strong>wet season;-1.2 MPa during <strong>the</strong> wet-dry season transition, and a –3.8MPa w<strong>at</strong>er potential <strong>at</strong><strong>the</strong> end dry season. The loc<strong>at</strong>ion of plants bene<strong>at</strong>h <strong>the</strong> canopy (gap vs. shaded areas) had astrong influence on <strong>the</strong> w<strong>at</strong>er potential of D. excelsa and Q. pteridophylla individuals. Forexample, D. excelsa plants growing in shaded areas had a w<strong>at</strong>er potential of -1.1 MPa in <strong>the</strong>transition wet-dry season while D exelsa individuals growing in gaps had a w<strong>at</strong>er potential of–1.5MPa. Following <strong>the</strong> same tendency, Q. pteridophylla plants growing in shade had anaverage w<strong>at</strong>er potential of –2.1MPa while plants growing in gaps had a w<strong>at</strong>er potential of –3.4MPa during <strong>the</strong> dry season. These d<strong>at</strong>a suggest th<strong>at</strong> plant w<strong>at</strong>er potential is stronglycontrolled by seasonal vari<strong>at</strong>ions in rainfall and <strong>the</strong> canopy light regime. These sp<strong>at</strong>ial andtemporal trends have important implic<strong>at</strong>ions for <strong>the</strong> seasonal vari<strong>at</strong>ions in leaf and canopygas exchange.

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