CARBON SEQUESTRATION AND TURNOVER IN SEMIARID SAVANNAS AND DRY FOREST

Citation
H. Tiessen et al., CARBON SEQUESTRATION AND TURNOVER IN SEMIARID SAVANNAS AND DRY FOREST, Climatic change, 40(1), 1998, pp. 105-117
Citations number
56
Categorie Soggetti
Environmental Sciences","Metereology & Atmospheric Sciences
Journal title
ISSN journal
01650009
Volume
40
Issue
1
Year of publication
1998
Pages
105 - 117
Database
ISI
SICI code
0165-0009(1998)40:1<105:CSATIS>2.0.ZU;2-R
Abstract
Data on carbon and biomass budgets under different land use in tropica l savannas and some dry forests are reviewed. Global data show wide ra nges of biomass carbon stocks (20-150 Mg C ha(-1)), net primary produc tion (2-15 Mg C ha(-1)y(-1)) and litter production (2-10 Mg C ha(-1)y( -1)) for the semiarid tropics. Although ranges for soil carbon are als o wide, an average figure for the top 20 cm is probably 10 g C kg(-1), or about 25 Mg C ha(-1). In order to arrive at a better understanding of C budgets and their controls, two regional reviews are presented f or NE Brazil and W. Africa. In NE Brazil approximately 40% of the land s have ''near-climax'' native vegetation. Less than 10% of the area is planted annually, but about 3-4 times that area is affected by shifti ng cultivation which has an average cycle of 5 y arable use followed b y 20 y or more recovery. Standing biomass of native caatinga shows nea rly the full global range with 2-50 Mg C ha(-1), Litter fall around 1- 2 Mg C ha(-1)y(-1) is partly decomposed and partly consumed by animals , resulting in low average soil C levels near 8 g kg(-1), or 20 Mg C h a(-1). Under cultivation, C sequestration is decreased, and soils lose approximately half their C stocks before being abandoned. In W. Afric a between 50-70% of the land is under a management regime with minimal C returns to the soils. Overgrazing and over-exploitation for fuel wo od has resulted in land degradation. Short fallow periods on cultivate d lands have caused serious declines in soil C stocks. Both C sequestr ation and stocks are therefore lower in W. Africa than in NE Brazil. I mprovements in the C sequestration in these semi arid regions depend o n an increase in crop production under suitable rotations, improved fa llow and animal husbandry, and a limitation on biomnass burning. Use o f fertilizer is required for improved productivities but socioeconomic constraints largely prevent such improvements, resulting in a very li mited scope for changes in soil C management.