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

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Carbon Release from Stems and Branches in a <strong>Seasonal</strong>ly Flooded <strong>Amazon</strong> ForestViviana Horna 1,2) and Reiner Zimmermann 1,2)1) Max Planck Institute for Biogeochemistry, Carl Zeiss Promenade 10, D-07701 JenaGermany2) Forest Ecology and Remote Sensing Group, Ecological-Botanical Gardens, Universityof Bayreuth, D-95440 Bayreuth, Germanyvhorna@bgc-jena.mpg.de Phone: ++49-3641-686731 Fax: ++49-3641-686710Release of CO 2 from woody tree tissue was measured in eight major tree species of a central<strong>Amazon</strong>ian “Varzea” white w<strong>at</strong>er inund<strong>at</strong>ion forest. Varzea forests are believed to have a highcarbon release since net wood productivity is low in spite of favorable nutrient supply andclim<strong>at</strong>e. Consecutive daily courses of carbon release were measured starting in March 1999,using stem and branch chambers in an open system <strong>with</strong> an integr<strong>at</strong>ed infrared gas analyzerrunning in differential mode. Deciduous tree species (Albizia multiflora, Tabebuia barb<strong>at</strong>a,Pseudobombax munguba, Cr<strong>at</strong>aeva benthamii, Vitex cymosa) and evergreen tree species(Nectandra amazonum, Laetia corymbulosa, Pouteria glomer<strong>at</strong>a) were compared. The resultswere analyzed for different flooding conditions of increasing w<strong>at</strong>er level (February-April),maximum w<strong>at</strong>er level (May-July), decreasing w<strong>at</strong>er level (August-October) and underconditions of no flooding (November-January).Trees showed maximum r<strong>at</strong>es of woody tissue CO 2 release during early flooding and variedfrom 2 to 14 µmol CO 2 m -2 s -1 in <strong>the</strong> lower part of <strong>the</strong> main stem during <strong>the</strong> day. These valuesare higher than those reported in <strong>the</strong> liter<strong>at</strong>ure for broad-leaved species. The highest values ofcarbon release were observed in <strong>the</strong> main stem of <strong>the</strong> evergreen Nectandra amazonum. For<strong>the</strong> remaining seasons daily vari<strong>at</strong>ion of main stem CO 2 release was smaller <strong>with</strong> a maximumof 4 µmol CO 2 m -2 s -1 between night and midday hours. CO 2 release r<strong>at</strong>es in <strong>the</strong> upper stemwere r<strong>at</strong>her constant throughout <strong>the</strong> year. Branch CO 2 release was high during new leafdevelopment indic<strong>at</strong>ing a tight rel<strong>at</strong>ionship <strong>with</strong> leaf phenology.The up-scaled values of CO 2 release from above-ground woody parts per season showed alinear rel<strong>at</strong>ionship <strong>with</strong> tree basal area: lowest correl<strong>at</strong>ion (r 2 =0.53) was found for <strong>the</strong> seasonof increasing w<strong>at</strong>er level and highest correl<strong>at</strong>ion (r 2 =0.68) during <strong>the</strong> season of decreasingw<strong>at</strong>er level. Annual stand carbon release from above-ground tree woody biomass wasestim<strong>at</strong>ed to be 1870 g C ha -1 a -1 . This value is 5 to 6 times higher than stand carbon releasevalues reported for o<strong>the</strong>r non-flooded neotropical forest (Odum, 1970, Ryan et al. 1994, Meir1996).The results of this study support <strong>the</strong> hypo<strong>the</strong>sis of a high respir<strong>at</strong>ion in seasonally floodedtropical forests. A close rel<strong>at</strong>ionship exists between apparent carbon release in branches andtree leaf phenology.

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