24 Selenium (Se) is an essential micronutrient for many organisms. Despite 25 its importance, our current knowledge of the biogeochemical cycling of 26 dissolved Se in tropical estuaries is limited, especially in Southeast Asia. To 27 gain insights into Se cycling in tropical peat-draining rivers and estuaries, 28 samples were collected from the Rajang, Maludam, Sebuyau, Simunjan, 29 Sematan, Samunsam, and Lunda rivers and estuaries in western Sarawak, 30 Malaysia, in March and September 2017 and analysed for various forms of Se 31 (dissolved inorganic and organic). Mean total dissolved Se (TDSe), dissolved 32 inorganic Se (DISe), and dissolved organic Se concentrations (DOSe) were 2.2 33 nmol L −1 (range: 0.7 to 5.7 nmol L −1 ), 0.18 nmol L −1 (range: less than the 34 detection limit to 0.47 nmol L −1 ), and 2.0 nmol L −1 (range: 0.42 to 5.7 nmol L −1 ), 35 respectively. In acidic, low-oxygen, organic-rich blackwater (peatland-draining) 36 rivers, the concentrations of DISe were extremely low, whereas those of DOSe 37 were high. In rivers and estuaries that drained peatland, DOSe/TDSe ratios 38 ranged from 0.67 to 0.99, showing that DOSe dominated. The positive 39 relationship between DISe and salinity and the negative relationship between 40 DOSe and salinity indicate marine and terrestrial origins of DISe and DOSe, 41 respectively. The positive correlations of DOSe with the humification index and 42 humic-like chromophoric dissolved organic matter components in freshwater 43 river reaches suggest that peat soils are probably the main source of DOSe. 44 Discharges of water enriched with DOSe fractions associated with peatland-45 derived high-molecular-weight, high-aromaticity dissolved organic matter 46 discharged from estuaries may promote productivity in the adjoining 47 50 https://doi.