From Microhabitat to Ecosystem: Identifying the Biophysical Factors Controlling Soil CO2 Dynamics in a Karst Shrubland
European Journal of Soil Science, November 2018, 69, 1018–1029 doi: 10.1111/ejss.12710 From microhabitat to ecosystem: identifying the biophysical factors controlling soil CO2 dynamics in a karst shrubland C. J. R. Lopeza , E. P. Sánchez-Cañeteb,c , P. Serrano-Ortizb,d, A. López-Ballesterosa,d,F.Domingoa,A.S.Kowalskib,c & C. Oyonartee aDepartment of Desertification and Geo-Ecology, Experimental Station of Arid Zones (EEZA-CSIC), Ctra. Sacramento s/n, 04120La Cañada, Almería, Spain, bInter-University Institute for Earth System Research (IISTA-CEAMA), Av. del Mediterráneo s/n, 18006, Granada, Spain, cDepartment of Applied Physics, University of Granada (UGR), Av. de Fuente Nueva s/n, 18071, Granada, Spain, dDepartment of Ecology, University of Granada (UGR), Av. de Fuente Nueva s/n, 18071, Granada, Spain, and eDepartment of Agronomy, University of Almería (UAL), Ctra. Sacramento s/n, 04120 La Cañada, Almería, Spain Summary The soil CO2 efflux (Fs) remains the least constrained component of the terrestrial carbon cycle; its estimates are still largely uncertain, mainly because of its considerable variation related to the many factors that interact over different temporal and spatial scales. Therefore, our aims were to: (i) identify the biophysical factors that control the soil CO2 molar fraction ( s) and characterize their time-frequency patterns in a karst shrubland, (ii) explore s variation with soil cover type (microhabitat) and (iii) estimate Fs at the ecosystem scale. Continuous measure- ments of aboveground variables, including net CO2 exchanges at the ecosystem level, were compared with pedo- climatic variables collected from four microhabitats (Festuca scariosa (Lag.) Asch. & Graebn., Hormathophylla spinosa (L.) P.
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