期刊
FRONTIERS IN MARINE SCIENCE
卷 9, 期 -, 页码 -出版社
FRONTIERS MEDIA SA
DOI: 10.3389/fmars.2022.875415
关键词
sediment trap; biogenic silica; dissolution; underestimation; South China Sea
资金
- State Key R&D Project of China [2016YFC0304105]
- Project of the State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, MNR [SOEDZZ2104]
- National Natural Science Foundation of China [91128212, 41006034, 41876123]
- [SML311019006/311020006]
This study measured dissolved silicate concentrations in sediment trap sampling bottles from four stations in the South China Sea, revealing significant dissolution of particulate bSi and underestimation of bSi flux. It is important to pay attention to bSi dissolution in sampling bottles in low-productivity oligotrophic oceans and calibrate bSi flux via measurement of dissolved silicate.
The dissolved silicate concentrations in the supernatant of sediment trap sampling bottles retrieved from deep water (1000-3000 m) at four stations in the South China Sea (SCS) were measured to calculate the underestimated flux of biogenic silica (bSi) in sinking particles due to bSi dissolution. High dissolved silicate concentrations in the supernatant, ranging from 122.6 to 1365.8 mu mol/L, indicated significant dissolution of particulate bSi in the sampling bottles. Underestimation of the bSi flux in the SCS by similar to 2% to similar to 34% (average: similar to 10%) due to bSi dissolution was revealed, and the degree of underestimation increased with decreasing total bSi flux. The amount of bSi dissolved within the sampling series at each station was generally positively correlated with dissolution time and to a certain extent influenced by the bSi amount collected by the sampling bottles under a low bSi sinking flux. Apparently stronger bSi dissolution was found at two of the four stations due to relatively high bSi dissolution rates, which were possibly related to a higher reactive surface area of the bSi or bacterial activity. Overall, our results demonstrated that the considerable bSi dissolution in sediment trap sampling bottles should not be ignored, especially in the low-productivity oligotrophic ocean, and bSi flux calibration via measurement of the dissolved silicate in sampling bottles is necessary. To reduce bSi flux underestimation due to the deployment of time-series sediment traps, larger-volume sampling bottles should be avoided in the oligotrophic open ocean, and sinking particle samples should be analyzed as soon as the sediment traps are recovered.
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