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

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Soil microbial biomass and respir<strong>at</strong>ion in an Eastern <strong>Amazon</strong>ian regrowth forestLívia G. T. R. Vasconcelos 1 , Daniel J. Zarin 2 , Claudio José R. de Carvalho 3 , Steel S.Vasconcelos 4 , Maria M. de L. S. Santos 11 Department of Soil Science, Faculdade de Ciências Agrárias do Pará (FCAP), P. O. Box917, Belém, PA, 66077-530, Brazil, E-mail: lgabrig@amazon.com.br; 2 University ofFlorida, USA, E-mail: zarin@ufl.edu; 3 EMBRAPA Amazônia Oriental, Brazil, E-mail:carvalho@cp<strong>at</strong>u.embrapa.br;manflora@amazon.com.br4Projeto MANFLORA, FCAP, Brazil, E-mail:Soil microbial biomass is an important component in forest ecosystems and itsmeasurement provides an estim<strong>at</strong>e of <strong>the</strong> size of <strong>the</strong> most dynamic fraction of soil organicm<strong>at</strong>ter and associ<strong>at</strong>ed nutrients. We measured soil microbial biomass in a fourteen-year-oldregrowth forest in Eastern <strong>Amazon</strong>ia (Pará, Brazil) during early November 2000 (dryseason) and l<strong>at</strong>e April 2001 (wet season). Microbial biomass carbon (C mic ) and respir<strong>at</strong>ionwere determined using <strong>the</strong> fumig<strong>at</strong>ion-extraction method and an adapt<strong>at</strong>ion of <strong>the</strong>fumig<strong>at</strong>ion-incub<strong>at</strong>ion method, respectively. We also calcul<strong>at</strong>ed <strong>the</strong> metabolic quotient(respir<strong>at</strong>ion:C mic r<strong>at</strong>io, qCO 2 ) and <strong>the</strong> soil microbial carbon:soil organic carbon r<strong>at</strong>io(C mic :C org ). During <strong>the</strong> dry season, soil moisture was significantly lower (12.9 ± 0.3 %) thanin <strong>the</strong> wet season (28.5 ± 0.8 %). C mic was significantly higher in <strong>the</strong> dry (937 ± 55 µg g -1 )than in <strong>the</strong> rainy season (454 ± 26 µg g -1 ); C mic :C org showed <strong>the</strong> same p<strong>at</strong>tern. However,microbial respir<strong>at</strong>ion was significantly higher in <strong>the</strong> rainy than in <strong>the</strong> dry season (2.74 ±0.15 vs. 1.61 ± 0.06 µg C-CO 2 g -1 soil hr -1 ), and rainy season qCO2 values (0.006 ± 0.0004)were also significantly higher than dry season values (0.002 ± 0.0001). Our results indic<strong>at</strong>eth<strong>at</strong> soil moisture influences soil microbial biomass which was more efficient during <strong>the</strong>dry season due to substantial carbon immobiliz<strong>at</strong>ion during this period. The increase inqCO2 in <strong>the</strong> rainy season suggests a higher carbon mineraliz<strong>at</strong>ion by <strong>the</strong> soil microbialbiomass, resulting in less efficiency in this period.

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