4.7 Article

The use of soil respiration as an ecological indicator in arid ecosystems of the SE of Spain: Spatial variability and controlling factors

Journal

ECOLOGICAL INDICATORS
Volume 14, Issue 1, Pages 40-49

Publisher

ELSEVIER
DOI: 10.1016/j.ecolind.2011.08.013

Keywords

Soil CO2 efflux; Autotrophic and heterotrophic respiration; Soil properties; Land cover; Soil moisture; Soil temperature; Soil respiration index

Funding

  1. Junta de Andalucia
  2. Ministry of Education and Science [CGL2005-00563]
  3. CSIC
  4. Institut Nacional de Investigaciones Agrarias [SUM2006-00018-C02-01]
  5. Cabo de Gata-Nijar Natural Park

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In the context of an ongoing monitoring study of the Cabo de Gata-Nijar Natural Park (SE of Spain), we explored the use of soil respiration as an indicator of ecosystem functioning reflecting changes in ecological processes in semiarid environments. With this purpose, we measured soil CO2 efflux in six different and representative ecosystems of the Natural Park, with different land uses (forest and agricultural sites) and under different soil covers (under plant and bare soil) in two distinctive periods of the year: summer (dry period) and spring (growing season). We also measured the main soil properties and environmental variables. Soil CO2 efflux ranged from 0.40 mu mol m(-2) s(-1) in the dry period to 1.93 mu mol m(-2) s(-1) in the growing season. Soil CO2 efflux showed a large spatial variability, with different behaviour between the measured periods. Whereas in the dry period differences among ecosystems were larger (CVs 75-80%) than within them (CVs 40-55%), in the growing season the CVs were smaller (40-50%) and no differences were observed between or within ecosystem. The factors controlling soil CO2 efflux also differed in the two measurement occasions. Whereas in the dry period soil CO2 efflux was mainly the result of transport processes in the soil and therefore related to local factors (OC content, CN ratio, clay, rock outcrop, etc.) assigned to ecosystem conditions, in the growing season soil CO2 efflux was dominated by soil CO2 production and thus related only to organic carbon content and plant cover. In the growing season environmental variables explained ca. 10% of the variation in soil CO2 efflux. In order to capture these different processes in different times of the year, i.e., diffusion versus production processes we calculated a new index, normalised seasonal difference in soil respiration (SDSR), which is proposed as a good indicator of the state and functioning of the ecosystem. (C) 2011 Elsevier Ltd. All rights reserved.

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