Blue carbon potential of coastal wetland restoration varies with inundation and rainfall

Karita Negandhi*, Grant Edwards, Jeffrey J. Kelleway, Dean Howard, David Safari, Neil Saintilan

*Corresponding author for this work

    Research output: Contribution to journalArticle

    6 Citations (Scopus)
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    Abstract

    There is a growing interest in how the management of ‘blue carbon’ sequestered by coastal wetlands can influence global greenhouse gas (GHG) budgets. A promising intervention is through restoring tidal exchange to impounded coastal wetlands for reduced methane (CH4 ) emissions. We monitored an impounded wetland’s GHG flux (CO2 and CH4 ) prior to and following tidal reinstatement. We found that biogeochemical responses varied across an elevation gradient. The low elevation zone experienced a greater increase in water level and an associated greater marine transition in the sediment microbial community (16 S rRNA) than the high elevation zone. The low elevation zone’s GHG emissions had a reduced sustained global warming potential of 264 g m−2 yr−1 CO2-e over 100 years, and it increased to 351 g m−2 yr−1 with the removal of extreme rain events. However, emission benefits were achieved through a reduction in CO2 emissions, not CH4 emissions. Overall, the wetland shifted from a prior CH4 sink (−0.07 to −1.74 g C m−2 yr−1 ) to a variable sink or source depending on the elevation site and rainfall. This highlights the need to consider a wetland’s initial GHG emissions, elevation and future rainfall trends when assessing the efficacy of tidal reinstatement for GHG emission control.

    Original languageEnglish
    Article number4368
    Pages (from-to)1-9
    Number of pages9
    JournalScientific Reports
    Volume9
    Issue number1
    DOIs
    Publication statusPublished - 13 Mar 2019

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    Copyright the Author(s) 2019. Version archived for private and non-commercial use with the permission of the author/s and according to publisher conditions. For further rights please contact the publisher.

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