We assessed DOC sources in small volcanic tropical mountainous watersheds.
Organic carbon in soil organic matter (SOM) and soil solutions were characterized.
TOC and TN decreased with depth, and C/N ratios were constant along soil profile.
13C/12C fractionation of SOM showed organism's activity, or SOM leaching.
DOC sources were soil surface lixiviation (flood) and groundwater (low water level).