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

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

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Secondary forest recovery on degraded pastures in Central <strong>Amazon</strong>ia: carbon,nutrients, and light-captureTed R. Feldpausch 1,3 , Erick C.M. Fernandes 1 , Susan J. Riha 2 , Marco A. Rondon 11 Department of Crop and Soil Sciences, Cornell University, Ithaca, NY, 14853, USA2 Department of Earth and Atmospheric Sciences, Cornell University, Ithaca, NY, 14853USA3 Department of Crop and Soil Sciences, 612 Bradfield Hall, Cornell University, Ithaca,NY, 14853, USA; trf2@cornell.eduLarge areas of <strong>the</strong> <strong>Amazon</strong> <strong>Basin</strong> have been cleared for pasture. Depending on regionand management, <strong>the</strong> pastures may degener<strong>at</strong>e be abandoned to invading secondaryveget<strong>at</strong>ion. We examined post-pasture forest recovery in ten secondary forests (SF)ranging in age from 0 to 14 years since abandonment to determine <strong>the</strong> dynamics ofnutrient and C accumul<strong>at</strong>ion and forest structure in redeveloping SF. Within <strong>the</strong> SFchronosequence, we measured aboveground biomass and nutrient storage, soil C andnutrients, leaf area index (LAI), and canopy cover by dominant genera and growth-form.After 12 to 14 years of recovery, <strong>the</strong> colonizing secondary veget<strong>at</strong>ion rapidly sequesteredC, rebuilt total nutrient capital, and returned some, but not all components of foreststructure. Compared to primary forests values, LAI was about 50%, canopy cover wassimilar, and <strong>the</strong> rapid Vismia-domin<strong>at</strong>ed aboveground biomass accrual was 25 to 50% in<strong>the</strong> oldest forests. Carbon accumul<strong>at</strong>ion r<strong>at</strong>es were comparable or higher than r<strong>at</strong>esreported from o<strong>the</strong>r studies. Although <strong>the</strong> veget<strong>at</strong>ion is Ca demanding, <strong>the</strong> low Ca soilsadequ<strong>at</strong>ely replenished immobilized Ca. There was a net loss of soil P over time, whichcan be <strong>at</strong>tributed to reloc<strong>at</strong>ion of P from soil to growing veget<strong>at</strong>ion. Slow leaf areaaccumul<strong>at</strong>ion rel<strong>at</strong>ive to forests recovering from o<strong>the</strong>r land-use, demonstr<strong>at</strong>es differencesin canopy development, which could neg<strong>at</strong>ively influence soil w<strong>at</strong>er uptake,evapotranspir<strong>at</strong>ion, and primary productivity. Although aboveground C gains were rapid,<strong>the</strong> soil pool represents <strong>the</strong> gre<strong>at</strong>est potential for long-term C gains; however, soil nutrientdeficits may limit future productivity.

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