Revealing sources and distribution changes of dissolved organic matter (DOM) in pore water of sediment from the Yangtze estuary.

PLoS One · 2013 · PMC3796548 · PMID 24155904

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hedged sentences

0.0100

closest p · 0.2× alpha

0.0100

boldest claim

The sentences

highly significantp<0.01actually significant

Significance levels are reported as non-significant (p>0.05), significant (0.05>p>0.01) or highly significant (p<0.01).

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an increasing trendno p-value reported

For DOM in the pore water from the sediment core, there was an increasing trend along 0 to 26 cm depth ( Fig. 5B ), which was due to higher release of the sedimentary organic material into the pore water during early diagenesis [4] .

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