Production of fluorescent dissolved organic matter in Arctic Ocean sediments.

Sci Rep · 2016 · PMC5159788 · PMID 27982085

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an increasing trendno p-value reported

Similar to CDOM, the fluorescent components at site S1 showed an increasing trend with depth down to an obvious turning point around the SMTZ depth ( ca. 4.1 mbsf) followed by a gradual decrease to the deeper sediments ( Fig. 3 ).

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