https://doi.org/10.5194/bg-2019-204 Preprint. Discussion started: 18 June 2019 c Author(s) 2019. CC BY 4.0 License. 1 Distribution and Flux of Dissolved Iron of the Rajang and Blackwater 2 Rivers at Sarawak, Borneo 3 Xiaohui Zhang1, Moritz Müller2, Shan Jiang1, Ying Wu1, Xunchi Zhu3, Aazani Mujahid4, Zhuoyi Zhu1, 4 Mohd Fakharuddin Muhamad4, Edwin Sien Aun Sia2, Faddrine Holt Ajon Jang2, Jing Zhang1 5 6 1State Key Laboratory of Estuarine and Coastal Research, East China Normal University, 200241 7 Shanghai, China 8 2Swinburne University of Technology, Faculty of Engineering, Computing and Science, 93350 9 Kuching, Sarawak, Malaysia 10 3School of Ecological and Environmental Sciences, East China Normal University, 200241 11 Shanghai, China 12 4Faculty of Resource Science & Technology, University Malaysia Sarawak, 94300, Sarawak, 13 Malaysia 14 15 Correspondence to: Xiaohui Zhang (
[email protected]) 16 17 1 https://doi.org/10.5194/bg-2019-204 Preprint. Discussion started: 18 June 2019 c Author(s) 2019. CC BY 4.0 License. 18 Abstract Dissolved iron (dFe) is essential for biogeochemical reactions in oceans, such as 19 photosynthesis, respiration and nitrogen fixation. Currently, large uncertainties remain on riverine 20 dFe inputs, especially for tropical rivers in Southeast Asia. In the present study, dFe concentrations 21 and distribution along the salinity gradient in the Rajang River in Malaysia, and three blackwater 22 rivers draining from peatlands, including the Maludam River, the Sebuyau River, and the Simunjan 23 River, were determined. In the Rajang River, the concentration of dFe in fresh water (salinity<1) in 24 the wet season (March 2017) was higher than that in the dry season (Auguest 2016), which might be 25 related to the resuspension of sediment particles and soil erosions from cropland in the watershed.