Seasonal nitrous oxide and methane emissions across a subtropical estuarine salinity gradient

• Published in: Biogeochemistry 2017-01, Vol.132 (1/2), p.55-69
• Main Authors: Welti, Nina, Hayes, Matt, Lockington, David
• Format: Article
• Language: English
• Subjects: Biogeosciences; Dissolved organic carbon; Earth and Environmental Science; Earth Sciences; Ecosystems; Emissions; Environmental changes; Environmental Chemistry; Estuaries; Greenhouse gases; Landscape; Life Sciences; Mangroves; Marine ecosystems; Methane; Nitrogen; Nitrous oxide; ORIGINAL PAPERS; Salinity; Summer; Wetlands; Winter
• ISSN: 0168-2563; 1573-515X
• DOI: 10.1007/s10533-016-0287-4

Currently, there is a lack of knowledge about GHG emissions, specifically N₂Oand CH₄, in subtropical coastal freshwater wetland and mangroves in the southern hemisphere. In this study, we quantified the gas fluxes and substrate availability in a subtropical coastal wetland off the coast of southeast Queensland, Australia over a complete wet-dry seasonal cycle. Sites were selected along a salinity gradient ranging from marine (34 psu) in a mangrove forest to freshwater (0.05 psu) wetland, encompassing the range of tidal influence. Fluxes were quantified for CH₄ (range -0.4–483 mg C–CH₄ h⁻¹ m⁻²) and N₂O (-5.5–126.4 µg N–N₂Oh⁻¹ m⁻²), with the system acting as an overall source for CH₄ and N₂O (mean N₂O and CH₄ fluxes: 52.8 µgN–N₂Oh⁻¹ m⁻² and 48.7 mg C–CH₄ h⁻¹ m⁻², respectively). Significantly higher N₂O fluxes were measured during the summer months (summer mean 64.2 ± 22.2 µgN–N₂O h⁻¹ m⁻²; winter mean 33.1 ± 24.4 µgN–N₂O h⁻¹ m⁻²) but not CH₄ fluxes (summer mean 30.2 ± 81.1 mg C–CH₄h⁻¹ m⁻²; winter mean 37.4 ± 79.6 mg C–CH₄ h⁻¹ m⁻²). The changes with season are primarily driven by temperature and precipitation controls on the dissolved inorganic nitrogen (DIN) concentration. A significant spatial pattern was observed based on location within the study site, with highest fluxes observed in the freshwater tidal wetland and decreasing through the mangrove forest. The dissolved organic carbon (DOC) varied throughout the landscape and was correlated with higher CH₄ fluxes, but this was a nonlinear trend. DIN availability was dominated by N–NH₄ and correlated to changes in N₂O fluxes throughout the landscape. Overall, we did not observe linear relationships between CH₄ and N₂O fluxes and salinity, oxygen or substrate availability along the fresh-marine continuum, suggesting that this ecosystem is a mosaic of processes and responses to environmental changes.