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. 2016 Mar 4;11(3):e0151110. doi: 10.1371/journal.pone.0151110

Table 5. Results of the multiple linear regression models based on AIC.

Data utilize are from all sampling locations and dates. DO = Bottom water dissolved oxygen concentration; OPD = Oxygen penetration depth; Chl a:Phaeo = Chlorophyll-a to phaeopigments ratio; C:N = Carbon-to-nitrogen ratio; MGS = Sediment mean grain size; Prokabun = Prokaryotic cell abundance; RSE = Residuals standard error; * Not significant term in the model but still provides best AIC.

Flux Intercept Temp DO OPD Chl a: Phaeo (log10) C:N (log10) Porosity MGS Prokabun(log10) r2 (Adj r2) p-values RSE
O2 -44.10 -1.68 0.89 -0.89 N/A N/A -0.14 NA 8.01 0.78 (0.75) <0.001 1.91
NH4+ (log10) 3.76* 0.10 N/A 0.04* 1.76 N/A 0.03 0.01 -0.47* 0.60 (0.54) <0.001 0.37
NO3- 2450.28* -89.95 90.49* -33.91* N/A 703.99 N/A N/A -334.13* 0.47 (0.41) <0.001 253.7
NO2- 20.15* N/A -3.88 2.79 -26.52 15.46* N/A N/A -9.72* 0.39 (0.30) 0.003 9.07
Si(OH)4 -7450.07 N/A 1086.48 N/A -9272.87 3066.59* N/A -11.27* N/A 0.55 (0.51) <0.001 1452
PO43- 1901.99 N/A 97.39 -13.60 -897.19 N/A -17.27 -5.96 -114.90 0.90 (0.88) <0.001 69.49