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

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Rel<strong>at</strong>ionship between soil nutrient availability and carbon fix<strong>at</strong>ion in seedlings andtrees in central <strong>Amazon</strong>iaRomilda M. Q. Paiva; Claudio Y. Yano; Flávio J. Luizão. INPA-Ecology. E-mail:romilda@inpa.gov.brTropical rain forests generally grow on nutrient-poor soils. Despite of efficient mechanismsfor nutrient conserv<strong>at</strong>ion and recycling, developed by <strong>the</strong> forest, nutrient limit<strong>at</strong>ions mayprevent higher carbon fix<strong>at</strong>ion, and consequent plant growth. The present study aim to test<strong>the</strong> hipo<strong>the</strong>sis th<strong>at</strong> soil nutrient limit<strong>at</strong>ions can influence both, <strong>the</strong> initial growth ofseedlings as well as carbon sequestr<strong>at</strong>ion and additional growth in adult trees. The studyhas been conducted <strong>at</strong> <strong>the</strong> ZF-2 INPA’s Reserve, ca. 80 km north of Manaus, in two phases:i) test of <strong>the</strong> effect of fertilizer additions (N + P and Ca + Mg) on <strong>the</strong> growth of seedlings ofpioneer and climax species; and, ii) study of <strong>the</strong> rel<strong>at</strong>ionship between C and nutrientconcentr<strong>at</strong>ions, and <strong>the</strong> possible nutrient limit<strong>at</strong>ion to <strong>the</strong> <strong>at</strong>mospheric CO 2 uptake by adulttrees in <strong>the</strong> forest. In a toposequence (pl<strong>at</strong>eau, slope and valley), <strong>the</strong> r<strong>at</strong>ios C/N, C/P,C/bases, were calcul<strong>at</strong>ed in selected trees and surrounding soil. The addition of N+P to <strong>the</strong>soil induced a higher seedling mortality; however, <strong>the</strong>re was a positive effect on <strong>the</strong> growthof surviving seedlings, suggesting a possible N and P limit<strong>at</strong>ion to <strong>the</strong> establishment ofseedlings. Adult trees loc<strong>at</strong>ed in <strong>the</strong> valley plots showed <strong>the</strong> most favorable C/bases(K+Ca+Mg) r<strong>at</strong>io: 83, against 145 in both, pl<strong>at</strong>eau and slope plots. Mean N concentr<strong>at</strong>ionswere similar in tree leaves <strong>at</strong> pl<strong>at</strong>eau (1.9%) and slope (2%); however, both were higherthan in <strong>the</strong> valley (1.3%). Th<strong>at</strong> is also reflected in <strong>the</strong> C/N r<strong>at</strong>io, significantly lower in <strong>the</strong>pl<strong>at</strong>eau and slope than in <strong>the</strong> valley plots (26.1%, 26% and 36.6%, respectively). Carbonconcentr<strong>at</strong>ions in m<strong>at</strong>ure leaves were higher (49.2%) in <strong>the</strong> slope than in both, pl<strong>at</strong>eau andvalley (47.5% and 47.8% respectively). Suggestions are made th<strong>at</strong>: (i) lower CO 2 fix<strong>at</strong>ionin <strong>the</strong> valley plots may be influenced by low soil nutrient availability for plants; and, (ii)slopes may have better supplies of o<strong>the</strong>r elements (e.g., w<strong>at</strong>er in soil) which favor Cfix<strong>at</strong>ion in trees.

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