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Restored and reference coastal wetlands emit elevated levels of methane after an extreme rainfall event, but continue to provide climate benefits
Journal article   Open access   Peer reviewed

Restored and reference coastal wetlands emit elevated levels of methane after an extreme rainfall event, but continue to provide climate benefits

Maria Fernanda Adame, Naima Iram, Jasmine Hall, Nicholas James Grundy, Alex Pearse, Vicki Bennion, Catherine E Lovelock, Ashley Rummell, Sonia Marshall, Graham Webb, …
Environmental Research Letters, Vol.Advanced access
16-Jun-2026
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Adame et al_2026_Environ._Res._Lett._10.1088_1748-9326_ae7e0b769.11 kBDownloadView
Published Version (Advanced Access) Open Access CC BY V4.0

Abstract

Climate change science Greenhouse gas inventories and fluxes floodplain greenhouse gases nitrous oxide mangroves rainfall restoration
Restoration of coastal wetlands provides climate adaptation and mitigation benefits. However, there is still limited information on the effects of climate change on restoration projects. We assessed the changes in soil greenhouse gas fluxes (GHG; methane, CH4, carbon dioxide, CO2, and nitrous oxide, N2O) on a site previously used for sugarcane production, and currently undergoing tidal reinstatement in subtropical Australia. Simultaneously, we sampled two natural reference mangrove sites. Sampling was conducted over three years, encompassing summer and winter seasons, before and after tidal reinstatement, and after an extreme rainfall event. After cessation of agriculture and before tidal reinstatement, GHG emissions at the restoration site were low and similar to those at the reference sites. Nine months after tidal reinstatement, soil conductivity increased from below detection limits to 5.9 ± 2.3 dS m-1, and surface soil organic carbon increased by 38%, while GHG emissions remained low. After the cyclone and the extreme rainfall event, a large peak in CH4 emissions was measured at the restoration site (3,661 ± 1,719 µg m-2 hr-1) and at one reference site (7,588 ± 2,193 µg m-2 hr-1); small N2O uptakes were also recorded in the restoration (-2.2 ± 0.5 µg m-2 hr-1) and reference sites ( -0.7 ± 0.1 µg m-2 hr-1). The fluxes were associated with prolonged freshwater flooding and low soil oxygen. After the waters receded, the emissions returned to baseline levels. Despite the elevated emissions from years with extreme rainfall (1.5 Mg CO2eq ha-1 yr-1), these are still much lower than those from alternative agricultural land uses. Thus, despite the extreme rainfall event, this blue carbon project continues to provide climate benefits.

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