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 ...
CHARCOAL DEPOSITION FROM TROPICAL VEGETATION IN BRAZIL: ACOMPARISON IN DIFFERENT REGIONS AND TIME SCALE1 Cordeiro, R.C., 3,1 Turcq, B., 1,3 Sifeddine, A., 1 Albuquerque, A.L.S., 2,1 Simões-Filho, F.F.L.(1) PROFIX/CNPq/ Departamento de Geoquímica, Universidade Federal Fluminense, Outeiro S.João Batista, Niterói, R.J., Brazil.rcampello@yahoo.com, tel/fax: 55216207025(2) Institute de Recherche pour le development(3) Instituto de Radioproteção e Dosimetria. Conselho de Energia NuclearFires records were obtained through the charcoal particles flux analyses in lacustrine sediments (daPata Lake, São Gabriel da Cachoeira (AM); N4 Lake, Carajás, PA; Dom Helvécio Lake, ParqueEstadual do Vale do Rio Doce, MG; and Caracaranã Lake, RR), resevoir sediment (Alta Floresta,MT), and an anual cicle of atmospheric deposition (Porto Velho, RO). The deposition of charcoals inthe sediments results from local or regional burns, caused by dry climates, associated or not toanthropogenic action. The highest charcoal fluxes values were obtained in the period of intenseland use change in Alta Floresta and in sediments that represent the medium Holocene in Serra SulCarajás region. The lowest values were found Lagoa da Pata in São Gabriel da Cachoeira, apronounced humid region in Amazon and in Porto Velho region, atmospheric deposition in a humidseason. Paleofires The deposition of charcoals in the sediments results from local or regional burns,caused by dry climates, associated or not to anthropogenic action. Thus, the charcoal analysescould have also a great importance in evaluating the impact of dry climates and human in differenttropical ecosystems. Determination of fire frequencies and dimensions in key areas of SouthAmerica, is a first step to understand the global carbon transference between terrestrial andatmospheric systems.
- Page 640: Abstract for the 2 nd international
- Page 644: the mature forest by about 6 years
- Page 648: Litter standing crop and mycorrhiza
- Page 652: Diversity and vertical distribution
- Page 656: The effect of lime and phosphorus o
- Page 660: ROOT CARBON AND NUTRIENT STOCKS IN
- Page 664: The Influence of Prescribed Burning
- Page 668: NUTRIENT USE EFFICIENCY IN ABANDONE
- Page 672: The fate of phosphorus in a lowland
- Page 676: Relationship between soil nutrient
- Page 680: LITTER DYNAMICS IN AN UPLAND FOREST
- Page 684: Abstract submitted to the 2 nd LBA
- Page 688: Pleistocene Amazonia: forest cover,
- Page 694: River water as a medium for transpo
- Page 698: Organic and inorganic carbon dynami
- Page 702: Control of stream water cations by
- Page 706: Project:Title:Authors:LBA-CARBONSIN
- Page 712: Transport of Particulate Carbon and
- Page 716: Dynamic of Gran Sabana forest-savan
- Page 720: Submitted to: II_ISC_LBA - 2 ND INT
- Page 724: Influence of land use in aquatic me
- Page 728: CHEMICAL COMPOSITION OF SOIL SOLUTI
- Page 732: Water surface and river bottom long
- Page 736: CHANGES TO INORGANIC NITROGEN IN SO
- Page 740: Scenarios of land use change: what
CHARCOAL DEPOSITION FROM TROPICAL VEGETATION IN BRAZIL: ACOMPARISON IN DIFFERENT REGIONS AND TIME SCALE1 Cordeiro, R.C., 3,1 Turcq, B., 1,3 Sifeddine, A., 1 Albuquerque, A.L.S., 2,1 Simões-Filho, F.F.L.(1) PROFIX/CNPq/ Departamento de Geoquímica, Universidade Federal Fluminense, Outeiro S.João B<strong>at</strong>ista, Niterói, R.J., Brazil.rcampello@yahoo.com, tel/fax: 55216207025(2) Institute de Recherche pour le development(3) Instituto de Radioproteção e Dosimetria. Conselho de Energia NuclearFires records were obtained through <strong>the</strong> charcoal particles flux analyses in lacustrine sediments (daP<strong>at</strong>a Lake, São Gabriel da Cachoeira (AM); N4 Lake, Carajás, PA; Dom Helvécio Lake, ParqueEstadual do Vale do Rio Doce, MG; and Caracaranã Lake, RR), resevoir sediment (Alta Floresta,MT), and an anual cicle of <strong>at</strong>mospheric deposition (Porto Velho, RO). The deposition of charcoals in<strong>the</strong> sediments results from local or regional burns, caused by dry clim<strong>at</strong>es, associ<strong>at</strong>ed or not toanthropogenic action. The highest charcoal fluxes values were obtained in <strong>the</strong> period of intenseland use change in Alta Floresta and in sediments th<strong>at</strong> represent <strong>the</strong> medium Holocene in Serra SulCarajás region. The lowest values were found Lagoa da P<strong>at</strong>a in São Gabriel da Cachoeira, apronounced humid region in <strong>Amazon</strong> and in Porto Velho region, <strong>at</strong>mospheric deposition in a humidseason. Paleofires The deposition of charcoals in <strong>the</strong> sediments results from local or regional burns,caused by dry clim<strong>at</strong>es, associ<strong>at</strong>ed or not to anthropogenic action. Thus, <strong>the</strong> charcoal analysescould have also a gre<strong>at</strong> importance in evalu<strong>at</strong>ing <strong>the</strong> impact of dry clim<strong>at</strong>es and human in differenttropical ecosystems. Determin<strong>at</strong>ion of fire frequencies and dimensions in key areas of SouthAmerica, is a first step to understand <strong>the</strong> global carbon transference between terrestrial and<strong>at</strong>mospheric systems.