Soil respiration is a very important component of the global carbon cycle, considered as the second most important carbon (C) flux to the atmosphere and is directly affected by global warming (Xu & Qi, 2001; Bond-Lamberty et al., 2004; Arredondo et al., 2018). It is defined as the sum of autotrophic respiration (i.e. roots and fungi) and heterotrophic respiration (i.e. soil microorganisms that break down organic matter and soil fauna) and is influenced by environmental factors, such as soil and ambient temperature, water content and photosynthetically active radiation (Raich & Schlesinger, 1992; Zimmermann et al., 2009; Cueva et al., 2016). Approximately 30% of the emissions of carbon dioxide (CO 2) come from changes in land use, particularly from deforestation to establish pastures for extensive livestock production (Schimel et al., 2001; Villanueva, 2014). In Mexico, it is estimated that 30%-50% of soil organic carbon