Linking Carbon Fluxes to Flooding Gradients in Sediments of Mediterranean Wetlands.

However, differences between seasons did not reach statistical significance (H = 5.85, p = 0.054) due to high data dispersion. 4 Discussion The flooding gradient effectively represents varying levels of water coverage within wetlands, where the outermost zones experience infrequent flooding, and the innermost zones are more likely to remain submerged.

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CH 4 fluxes displayed an increasing trend from P1 to P3 ( Figure d), peaking in the intermediate, water-saturated zone (P3) during spring and fall-winter, reaching up to 10 mg C/m 2 /day.

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