Restoration Ecology · 2000 · 593 citations · 67 references
Natural ResourcesEcologyForestryForest ManagementSoil EcologyTerrestrial EcologyCarbon CycleCarbon SequestrationForest SuccessionReforestationAboveground Carbon StocksCarbon Sequestration During SuccessionLand-use Change Carbon DynamicsReforestation Carbon SequestrationReforestation EffectsReforestation OffsettingSoil Carbon Dioxide FluxTropical Secondary Forests
"Literature review shows above‑ground biomass accumulates at 6.2 Mg ha⁻¹ yr⁻¹ in the first 20 years (2.9 Mg ha⁻¹ yr⁻¹ over 80 years), with wet zones fastest, while soil carbon builds at 1.30 Mg ha⁻¹ yr⁻¹ initially and 0.41 Mg ha⁻¹ yr⁻¹ over a century; rates vary by land use, and reforestation can sequester carbon for 40–80 years or more." Ensure each sentence ends with period. No extra sentences. Count 4. Good.
Abstract Approximately half of the tropical biome is in some stage of recovery from past human disturbance, most of which is in secondary forests growing on abandoned agricultural lands and pastures. Reforestation of these abandoned lands, both natural and managed, has been proposed as a means to help offset increasing carbon emissions to the atmosphere. In this paper we discuss the potential of these forests to serve as sinks for atmospheric carbon dioxide in aboveground biomass and soils. A review of literature data shows that aboveground biomass increases at a rate of 6.2 Mg ha − 1 yr − 1 during the first 20 years of succession, and at a rate of 2.9 Mg ha − 1 yr − 1 over the first 80 years of regrowth. During the first 20 years of regrowth, forests in wet life zones have the fastest rate of aboveground carbon accumulation with reforestation, followed by dry and moist forests. Soil carbon accumulated at a rate of 0.41 Mg ha − 1 yr − 1 over a 100‐year period, and at faster rates during the first 20 years (1.30 Mg carbon ha − 1 yr − 1 ). Past land use affects the rate of both above‐ and belowground carbon sequestration. Forests growing on abandoned agricultural land accumulate biomass faster than other past land uses, while soil carbon accumulates faster on sites that were cleared but not developed, and on pasture sites. Our results indicate that tropical reforestation has the potential to serve as a carbon offset mechanism both above‐ and belowground for at least 40 to 80 years, and possibly much longer. More research is needed to determine the potential for longer‐term carbon sequestration for mitigation of atmospheric CO 2 emissions.
67
Carbon Pools and Flux of Global Forest Ecosystems
Robert K. Dixon, A. M. Solomon, Sandra Brown et al. · Science · 1994 · 3.4K citations
Natural Sciences, Ecology, Forestry +17
ECOLOGY OF TROPICAL DRY FOREST
Peter G. Murphy, A. E. Lugo · Annual Review of Ecology and Systematics · 1986 · 1.7K citations
Organic Carbon in Soils of the World
H. Eswaran, Evert van den Berg, Paul F. Reich · Soil Science Society of America Journal · 1993 · 1.5K citations
The role of deep roots in the hydrological and carbon cycles of Amazonian forests and pastures
Daniel C. Nepstad, Eric A. Davidson, P. Jipp et al. · Nature · 1994 · 1.4K citations · Full text
Agriculture, Ecology, Hydrology +16