Fig. 8From: Deep-sea bottom-water environment change caused by sediment resuspension on the continental slope off Sanriku, Japan, before and after the 2011 Tohoku EarthquakeRelationships between DO (a), AOU (b), PO4 (c), NO3 (d), DIC (e), ANU (f), remineralization-corrected DIC (g), and remineralization-corrected PO4 (h) and LTA value on the studied isopycnal surfaces (27.38σθ: red circles; 27.56σθ: blue circles). Solid (dotted) lines indicate statistically significant (insignificant) regressions (p < 0.05)Back to article page