Rapid depletion of dissolved organic sulphur (DOS) in freshwaters
Rapid depletion of dissolved organic sulphur (DOS) in freshwaters
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DOI:
10.1007/s10533-020-00669-4
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发表时间:
2020-05
期刊:
影响因子:
4
通讯作者:
F. Brailsford;H. Glanville;D. Wang;P. Golyshin;P. Johnes;C. Yates;D. Jones
中科院分区:
文献类型:
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作者:
F. Brailsford;H. Glanville;D. Wang;P. Golyshin;P. Johnes;C. Yates;D. Jones
Sulphur (S) is a key macronutrient for all organisms, with similar cellular requirements to that of phosphorus (P). Studies of S cycling have often focused on the inorganic fraction, however, there is strong evidence to suggest that freshwater microorganisms may also access dissolved organic S (DOS) compounds (e.g. S-containing amino acids). The aim of this study was to compare the relative concentration and depletion rates of organic35S-labelled amino acids (cysteine, methionine) with inorganic S (Na235SO4) in oligotrophic versus mesotrophic river waters draining from low nutrient input and moderate nutrient input land uses respectively. Our results showed that inorganic SO42−was present in the water column at much higher concentrations than free amino acids. In contrast to SO42−, however, cysteine and methionine were both rapidly depleted from the mesotrophic and oligotrophic waters with a halving time < 1 h. Only a small proportion of the DOS removed from solution was mineralized and excreted as SO42−(< 16% of the total taken up) suggesting that the DOS could be satisfying a demand for carbon (C) and S. In conclusion, even though inorganic S was abundant in freshwater, it appears that the aquatic communities retained the capacity to take up and assimilate DOS.