Management effects on carbon stocks and fluxes across the Orinoco savannas

Across the physiognomic types of the Orinoco llanos, periodic inventories and changes in land-use between 1982–1992 are estimated. Results indicate that the area under pastures and forest plantations is increased by 0.005337×10 6 km 2, whilts reducing the area of croplands by 0.000119×10 6 km 2. This is a net increase of 0.005218×10 6 km 2. The gross carbon release is 174.66 Tg C per year to the atmosphere and transferring from cultivated and native vegetation to wood products (1.62 Tg C per year) and slash (1.18 Tg C per year). The processes of land preparation contribute 1.40 Tg C per year to the atmosphere. From the tree savannas, woodlands and forests 0.73 Tg C per year are estimated to have been transferred to the soil following clearance and burning over this period, and 1.05 Tg C per year from herbaceous savannas when were buried and decomposed at 0.84 Tg C per year. The estimate of carbon balance here by inventories and changes in land-use approach indicates that the Orinoco llanos is a sink of −17.53 Tg C per year. The carbon turnover time in the Orinoco system is 68 years, which provides a limited route for carbon sequestration. The calculated potential of the Orinoco llanos for storing carbon is 8300 Tg C. Ecological options to achieve this potential value are addressed. However, nutrient deficiency and seasonal water supply are serious drawbacks to take into account for increasing carbon accretion. These results are particular for the Orinoco llanos, even though described processes could be similar to world-wide savannas, where a gradient of carbon heterogeneity exists.