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This paper summarized the results of 47 global studies with humid subtropical climates investigating the sources of variation in SOC responses to CA. Overall the effect of CA on SOC accumulation in the plough layer was 12% greater in comparison to conventional agriculture. However, the effect was variable depending on the SOC content under conventional agriculture. For soils with less than 40 Mg C ha(-1), increasing the proportion of crops with bigger residue biomasses in a CA rotation was a solution to increase SOC. The effect of CA on SOC also depended on clay content and became null with a SOC/clay index of 3.2. They conclude that SOC increments due to CA application can be achieved especially in agricultural soils with less than 40 Mg C ha(-1) and located in the middle latitudes or in the dry conditions of Mediterranean and humid subtropical climates.