New Insights Into the Virus-to-Prokaryote Ratio (VPR) in Marine Sediments.

At the muddy-sand site M-S, the salinity was much lower and greatly fluctuated (21.77 ± 7.79) than that of site S, and the MGS was also lower and showed an increasing trend (69.66 ± 14.59 μm) ( Figure 3B ).

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The Chla (8.20 ± 2.01 μg/g), Pha (4.20 ± 2.50 μg/g), and TOC (0.73 ± 0.27%) were much higher than those observed at site S, all showing a decreasing trend during the investigated period ( Figure 3D ).

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