Distribution and behaviour of dissolved selenium in tropical peatland-draining rivers and estuaries of Malaysia
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Published:2020-02-28
Issue:4
Volume:17
Page:1133-1145
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ISSN:1726-4189
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Container-title:Biogeosciences
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language:en
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Short-container-title:Biogeosciences
Author:
Chang Yan, Müller MoritzORCID, Wu Ying, Jiang Shan, Cao Wan Wan, Qu Jian Guo, Ren Jing Ling, Wang Xiao Na, Rao En Ming, Wang Xiao Lu, Mujahid AazaniORCID, Muhamad Mohd Fakharuddin, Sia Edwin Sien Aun, Jang Faddrine Holt Ajon, Zhang Jing
Abstract
Abstract. Selenium (Se) is an essential micronutrient for aquatic organisms. Despite its importance, our current knowledge of the biogeochemical cycling of
dissolved Se in tropical estuaries is limited, especially in Southeast Asia. To gain insights into Se cycling in tropical peat-draining rivers and
estuaries, samples were collected from the Rajang, Maludam, Sebuyau, Simunjan, Sematan, Samunsam and Lunda rivers and estuaries in western Sarawak,
Malaysia, in March and September 2017 and analysed for various forms of Se (dissolved inorganic and organic). Mean total dissolved Se (TDSe),
dissolved inorganic Se (DISe) and dissolved organic Se concentrations (DOSe) were 2.2 nmol L−1 (range: 0.7 to 5.7 nmol L−1),
0.18 nmol L−1 (range: less than the detection limit to 0.47 nmol L−1) and 2.0 nmol L−1 (range: 0.42 to
5.7 nmol L−1), respectively. In acidic, low-oxygen, organic-rich blackwater (peatland-draining) rivers, the concentrations of DISe were
extremely low (near or below the detection limit, i.e. 0.0063 nmol L−1), whereas those of DOSe were high. In rivers and estuaries that
drained peatland, DOSe ∕ TDSe ratios ranged from 0.67 to 0.99, showing that DOSe dominated. The positive relationship between DISe and salinity and the
negative relationship between DOSe and salinity indicate marine and terrestrial origins of DISe and DOSe, respectively. The positive correlations of
DOSe with the humification index and humic-like chromophoric dissolved organic matter components in freshwater river reaches suggest that peat soils
are probably the main source of DOSe. The DOSe fractions may be associated with high molecular weight peatland-derived aromatic and black carbon
compounds and may photodegrade to more bioavailable forms once transported to coastal waters. The TDSe flux delivered by the peat-draining rivers
exceeded those reported for other small rivers and is quantitatively more significant than previously thought.
Funder
China Postdoctoral Science Foundation National Natural Science Foundation of China
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics
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