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

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Where are <strong>the</strong> oldest of <strong>the</strong> forest? Radiocarbon use to determine <strong>the</strong> age andgrowth r<strong>at</strong>e of trees from <strong>the</strong> Brazilian <strong>Amazon</strong>ian ForestSimone A. Vieira 1 , Plínio B. de Camargo 1 , Susan E. Trumbore 2 , Diogo Selhorst 3 ,Niro Higuchi 4 , Luiz A. Martinelli 1 , John Southon 5savieira@cena.usp.br,pcamargo@cena.usp.br,setrumbo@uci.edu,selhorst@bol.com.br, niro@inpa.gov.br, zebu@cena.usp.br, southon@llnl.gov(1)Centro de Energia Nuclear na Agricultura/USP, Av. Centenário 303,Piracicaba, SP 13416-000 – Brazil (2) University of Califórnia, Irvine, CA, USA (3)Parque Zoobotânico-UFAC-Brazil (4) Instituto Nacional de Pesquisas da Amazônia –Manaus - Brasil (5) Center for Acceler<strong>at</strong>or Mass Spectrometry, Lawrence LivermoreN<strong>at</strong>ional Labor<strong>at</strong>ory, Livermore, CA, USAIt has been reported th<strong>at</strong> trees can survive over 1000 years in <strong>the</strong> <strong>Amazon</strong>ian tropicalforest. This fact apparently contradicts <strong>the</strong> idea th<strong>at</strong> tropical rain forests are highlydynamic systems. This contradiction can be clarified by determining <strong>the</strong> age structureof <strong>the</strong> forest through <strong>the</strong> residence time of <strong>the</strong> Carbon in <strong>the</strong> veget<strong>at</strong>ion. The first stepto estim<strong>at</strong>e <strong>the</strong> C residence time in <strong>the</strong> forest is to determine <strong>the</strong> amount of 14 C oftrees. We followed <strong>the</strong> diameter tree growth <strong>at</strong> three sites in <strong>the</strong> <strong>Amazon</strong>ian tropicalforest in order to provide a better understanding of <strong>the</strong> carbon dynamics in this regionand its vari<strong>at</strong>ions according to <strong>the</strong> clim<strong>at</strong>e gradient. We also collected trunk samplesfrom 100 individuals and <strong>the</strong> radiocarbon measurements of tree cores purifiedcellulose were used to determine <strong>the</strong> ages and radial growth r<strong>at</strong>es of various species oftrees <strong>with</strong> different diameter classes. The studied sites were loc<strong>at</strong>ed in <strong>the</strong> Tapajósforest (FLONA) near Santarém (PA), <strong>the</strong> EEST-ZF2 site near Manaus (AM) and <strong>the</strong>C<strong>at</strong>uaba Experimental Farm near Rio Branco (AC). The amount and distribution of<strong>the</strong> precipit<strong>at</strong>ion, <strong>the</strong> tree diameter distribution and <strong>the</strong> aboveground biomass aredifferent among <strong>the</strong> studied areas. The dry biomass is 360 t.ha -1 , 281 t.ha -1 and244 t.ha -1 in Manaus, Santarém and Rio Branco, respectively. The DHB of <strong>the</strong>sampled trees ranged from 11 to 143 cm. The maximum age obtained fromradiocarbon was 760 years and <strong>the</strong> minimum was 20 years. The annual diametergrowth r<strong>at</strong>e ranged between 0.01 and 0.9 cm.year -1 . It seems th<strong>at</strong> <strong>the</strong> bigger trees tendto have higher growth r<strong>at</strong>es than smaller trees in all studied sites.

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