Soil aggregates in a tropical deciduous forest: effects on C and N dynamics, and microbial communities as determined by t-RFLPs |
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Authors: | Ana M. Noguez Ana E. Escalante Larry J. Forney Maribel Nava-Mendoza Irma Rosas Valeria Souza Felipe García-Oliva |
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Affiliation: | (1) Departamento de Ecología Evolutiva, Instituto de Ecología, Universidad Nacional Autónoma de México, México, D.F., México;(2) Department of Biological Sciences, University of Idaho, Moscow, ID, USA;(3) Centro de Investigaciones en Ecosistemas, Universidad Nacional Autónoma de México, AP 27-3 Sta. María se Guido, 58090 Morelia, Michoacán, México;(4) Centro de Ciencias de la Atmósfera, Universidad Nacional Autónoma de México, México, D.F., México |
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Abstract: | The aim of this study was to analyze C and N dynamics, as well as, soil bacterial community structure within soil micro- and macro-aggregates in a tropical deciduous forest in México. We measured, for three landscape positions and three seasons of the year: total, microbial and available forms of C and N; potential C and N mineralization; and soil bacterial communities by using t-RFLPs. The highest total C concentrations were found in the north-slopes and in the dry season (DS) samples. In general, micro-aggregates had higher concentrations than macro-aggregates of available C and N forms, and microbial C. Similarly, micro-aggregates had the highest potential C mineralization and net N mineralization. We detected 149 different OTUs (operational taxonomic units) from which 50% was shared by the two aggregate size fractions, 25% was exclusive to micro-aggregates and the 25% left was found only in macro-aggregates. Top-hills were richer in OTUs than north and south-slopes. The Unweighted Pair Group Method with Arithmetic mean (UPGMA) analysis indicated clear differences in community composition between the two aggregate size-fractions in relation to the presence of OTUs. These results suggest that the main difference between micro- and macro-aggregates is due to the community structure within each soil fraction and this difference could affect soil nutrients dynamics. |
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Keywords: | Macro-aggregates Micro-aggregates Mexico Soil bacteria t-RFLPs |
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