PS 92-38 - Soil microbial biomass and activity in a cork oak savanna

Friday, August 6, 2010
Exhibit Hall A, David L Lawrence Convention Center
Maria C. Caldeira, Centre for Forestry Research/ School of Agriculture, Technical University of Lisbon, Lisbon, Portugal, David Fangueiro, Chemistry Department, Technical University of Lisbon, Instituto Superior de Agronomia, Lisbon, Portugal, Xavier Lecomte, Centre of Forest Research, Technical University of Lisbon, Instituto Superior de Agronomia, Lisboa, Portugal, Miguel Nuno Bugalho, Centre for Applied Ecology/ School of Agriculture, Technical University of Lisbon, 1349-017 Lisbon, Portugal, João Filipe Coutinho, Universidade de Trás-os Montes e Alto-Douro Vila Real, Vila Real, Portugal and João S. Pereira, Departamento de Ambiente, Território e Recursos Naturais, Instituto Superior de Agronomia, Universidade de Lisboa, Lisboa, Portugal
Background/Question/Methods

Cork oak savannas are composed by a sparse tree canopy (30-70 trees/ha) and a grassland understory predominantly composed of C3 annuals that survive the hot and dry Mediterranean summers as seeds in the soil. Microbial communities can be more or less efficient at converting organic substrates into microbial biomass carbon depending on the quantity and quality of organic matter inputs. The cork oak savannas have two distinct types of plant litter that can affect soil microbial biomass and activity differently: herbaceous litter and the more recalcitrant woody plant litter resulting from the trees. Spatial variability of soil microbial biomass and activity due to the tree-grassland component of cork oak savannas were evaluated in order to better understand the soil carbon dynamics of these systems.

To quantify changes in soil microbial biomass and activity, measurements were performed in a Cork oak savanna in Southern Portugal. At this site 8 plots were randomly established under mature cork oak trees and paired with 8 open grassland plots. During one year soil cores (0-10 cm) were monthly collected at each site for measuring soil microbial biomass C and other eco-physiology parameters.

Results/Conclusions

Soil microbial biomass carbon (Cmic) and nitrogen (Nmic) were always higher under the tree canopy than in the open grasslands. Organic carbon (Corg) was also higher under the tree canopies. The Cmic/Corg ratio that relates to the microbial activity and its potential to mineralize organic substances was lower under the tree canopies than in the open grasslands. This indicates that less microbial biomass was supported per unit of Corg. The basal microbial activity was always higher under the canopy than in the open grassland.

Trees scattered in the savanna function as islands inducing larger soil microbial communities and higher basal activity under the canopies. Lower Cmic/Corg ratio under the tree canopies suggests a more recalcitrant nature of the litter and a decrease in relative availability of organic matter under the trees.

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