A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...
A Look at Amazon Basin Seasonal Dynamics with the Biophysical ... A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...
Autotrophic X heterotrophic respiration in Western Amazonia, Acre-BrazilCI Salimon; JW Pereira; Victoria, RL; EA Davidson; AWF Melo; IF BrownConversion of forest to cattle pastures and subsequent abandonment of those pastures isoccurring throughout the Amazon Basin, and although there is a lot of research on theconsequences that come from this land cover change, there are still many questions to beanswered about biogeochemical processes associated with them. In this study we try todetermine the effects of land-use change on soil respiration in pastures, secondary forestsand mature forests near Rio Branco, Acre. Data analyses from June/99 to July/00 showsthat the greatest CO 2 fluxes are observed in pastures and not in mature forests. In searchof a better understanding of these results, we sampled soils for carbon stocks down to60cm depth and conducted some respirometry essays, and also sampled CO 2 fordetermination of its δ 13 C value, by using keeling plots. Carbon stocks are higher inpastures than in mature and secondary forests. Heterotrophic respiration is lower or equalin pasture compared to primary and secondary forests, showing that autotrophicrespiration is probably the main cause of higher fluxes in pastures. δ 13 C of heterotrophicrespired CO 2 in pasture was -15‰. Since δ 13 C from pasture soil is -21‰,microorganisms in the pasture soil are feeding basically on carbon from grasses and notfrom remaining forest carbon.
- Page 220: COMPARISION THE SOIL RESPIRATION IN
- Page 224: WATER POTENTIAL OF PLANTS IN DIFFER
- Page 228: CO2 FLUXES OVER PANTANAL REGION UND
- Page 232: Radiation Budget over the forest ne
- Page 236: MODELING INTERCEPTED SOLAR RADIATIO
- Page 240: Tower- and Biometry-based Measureme
- Page 244: A METHODOLOGICAL APPROACH TO STUDY
- Page 248: Ecophysiological characteristics re
- Page 252: Ecological Classification of Soils
- Page 256: C Sequestration Dynamics: Biomass,
- Page 260: Simone PereiraMuseu ParaenseEmílio
- Page 264: Effects of land use change and tree
- Page 268: The contribution of pioneer tree sp
- Page 274: Submitted to: II_ISC_LBA - 2 ND INT
- Page 278: Fine root dynamics from radiocarbon
- Page 282: SEASONAL CHANGES IN LEAF LITTER NUT
- Page 286: Variability of Soil Microbial Bioma
- Page 290: composite. We can also use several
- Page 294: Soil microbial biomass and respirat
- Page 298: Tree ring studies to estimate carbo
- Page 302: Litter decomposition rate estimatio
- Page 306: cardinot@amazon.com.britohver@yahoo
- Page 310: VARIABILITY OF SOIL RESPIRATION OVE
- Page 314: Fine litter fall and standing tree
- Page 318: LATERAL VARIATIONS IN THE CHEMICAL
Autotrophic X heterotrophic respir<strong>at</strong>ion in Western <strong>Amazon</strong>ia, Acre-BrazilCI Salimon; JW Pereira; Victoria, RL; EA Davidson; AWF Melo; IF BrownConversion of forest to c<strong>at</strong>tle pastures and subsequent abandonment of those pastures isoccurring throughout <strong>the</strong> <strong>Amazon</strong> <strong>Basin</strong>, and although <strong>the</strong>re is a lot of research on <strong>the</strong>consequences th<strong>at</strong> come from this land cover change, <strong>the</strong>re are still many questions to beanswered about biogeochemical processes associ<strong>at</strong>ed <strong>with</strong> <strong>the</strong>m. In this study we try todetermine <strong>the</strong> effects of land-use change on soil respir<strong>at</strong>ion in pastures, secondary forestsand m<strong>at</strong>ure forests near Rio Branco, Acre. D<strong>at</strong>a analyses from June/99 to July/00 showsth<strong>at</strong> <strong>the</strong> gre<strong>at</strong>est CO 2 fluxes are observed in pastures and not in m<strong>at</strong>ure forests. In searchof a better understanding of <strong>the</strong>se results, we sampled soils for carbon stocks down to60cm depth and conducted some respirometry essays, and also sampled CO 2 fordetermin<strong>at</strong>ion of its δ 13 C value, by using keeling plots. Carbon stocks are higher inpastures than in m<strong>at</strong>ure and secondary forests. Heterotrophic respir<strong>at</strong>ion is lower or equalin pasture compared to primary and secondary forests, showing th<strong>at</strong> autotrophicrespir<strong>at</strong>ion is probably <strong>the</strong> main cause of higher fluxes in pastures. δ 13 C of heterotrophicrespired CO 2 in pasture was -15‰. Since δ 13 C from pasture soil is -21‰,microorganisms in <strong>the</strong> pasture soil are feeding basically on carbon from grasses and notfrom remaining forest carbon.