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Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
Published on: June 13, 2020
Occurrence patterns, spatial heterogeneity, and compositional variation of PFASs in deep-sea cold seep sediments from
Zhuoyun Chen1, Liang Wang1, Didi Liu1
1Laboratory of Marine Ecological Environment Early Warning and Monitoring, Third Institute of Oceanography, Ministry of Natural Resources, Xiamen, 361005, China.
Abstract:
The occurrence and compositional variation of per- and polyfluoroalkyl substances (PFASs) in deep-sea cold seep sediments remain poorly characterized. Here, 25 target PFASs were analyzed in 40 sediment layers from six cores collected in the northern South China Sea. A tiered reporting scheme distinguished quantified concentrations (≥LOQ), detections between LOD and LOQ, and trace-level responses below the method LOD. Quantified ΣPFASs ranged from 0.13 to 6.12 ng g-1 dw, with an overall mean of 1.39 ng g-1 dw; the highest whole-core station-mean concentration occurred at station F (3.06 ng g-1 dw). The dominant contributors to quantified ΣPFASs were PFPeA, PFDS, PFHxA, and 6:2 FTSA, accounting for 40.8%, 26.9%, 13.3%, and 8.1%, respectively. PFDS had a lower quantification frequency than the dominant PFCAs but made a disproportionately high contribution, mainly reflecting elevated PFDS concentrations in selected horizons, including the 4-8 cm interval at station F. Quantified PFASs were dominated by PFCAs (58.3%) and PFSAs (33.6%), whereas Other target PFASs accounted for 8.1% and were almost entirely represented by 6:2 FTSA. PERMANOVA indicated that inter-station variability (R2 = 0.510, p < 0.001) exceeded depth-band effects (R2 = 0.064, p = 0.017). Ordination further linked chain length and functional-group composition to multivariate compositional differences. These results establish a baseline record of PFAS occurrence and compositional heterogeneity in cold seep sediments and provide an occurrence-based context for future testing of chromatographic-like retention during burial.
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