Large changes in carbon storage under different land-use regimes in subtropical seasonally dry forests of southern South America

• Published in: Agriculture, ecosystems & environment ecosystems & environment, 2014-12, Vol.197, p.68-76
• Main Authors: Conti, Georgina, Pérez-Harguindeguy, Natalia, Quètier, Fabien, Gorné, Lucas D., Jaureguiberry, Pedro, Bertone, Gustavo A., Enrico, Lucas, Cuchietti, Aníbal, Díaz, Sandra
• Format: Article
• Language: English
• Subjects: Agronomy. Soil science and plant productions; Americas; Biological and medical sciences; Biomass; Carbon sequestration; Chaco; Deep soil; Drying; Ecosystems; Forestry; Forests; Fundamental and applied biological sciences. Psychology; General agroecology; General agroecology. Agricultural and farming systems. Agricultural development. Rural area planning. Landscaping; General agronomy. Plant production; Generalities. Agricultural and farming systems. Agricultural development; Global change; Land use; Pools; Soil (material); Soil inorganic carbon; Soil organic carbon
• ISSN: 0167-8809; 1873-2305
• DOI: 10.1016/j.agee.2014.07.025

•We detail plant and soil C pools for five ecosystem types of the Chaco region.•Total soil C represents the main compartment, especially below 30cm depth.•Shrubs are an important compartment not previously quantified on these systems (≈30% of aboveground biomass).•The replacement of forests is linked to large losses in organic and inorganic C.•Actual land cover changes in the area may lead to a huge reduction in the stored C. Net emissions of CO2 from land-use conversion represent a significant driver of global climatic change. This is especially true for subtropical seasonally dry Chaco forests from southern South America, now experiencing one of the highest loss rates globally. However, direct quantifications of the effect of accelerated deforestation on carbon (C) pools of these systems are rare. Considering five dominant ecosystem types within the dry Chaco forest of Argentina, derived by land-use change from the same original vegetation, substrate, and climate, we quantified the magnitude and change of total C pools including trees and shrubs, non-woody plants, coarse and fine debris, and soil organic (SOC) and inorganic (SIC) pools up to 2m depth. Soil C pools represented the largest C stocks (>74%). Shrubs also represented a large C pool (at least 28% of the aboveground standing biomass), which we quantified in detail for the first time. The conversion of forests to open shrublands and croplands was associated to large losses of organic C both in aboveground biomass and in soils down to 30cm depth (from 43 to 64%). Although SIC is usually considered as a relatively stable compartment, the forest to crop transition presented here involved carbonate losses of c. 68% at soil depths between 1 and 2m. Our results indicate that the landscape transformations expected in the region under business-as-usual socioeconomic scenarios will probably lead to a marked reduction of the C stored, with a consequent net C emission and a decline in other C storage-related ecosystem services provided by these ecosystems.