Intensified inundation shifts a freshwater wetland from a CO2 sink to a source

© 2019 The Authors. Global Change Biology Published by John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 25(2019), 10 vom: 30. Okt., Seite 3319-3333
1. Verfasser: Zhao, Junbin (VerfasserIn)
Weitere Verfasser: Malone, Sparkle L, Oberbauer, Steven F, Olivas, Paulo C, Schedlbauer, Jessica L, Staudhammer, Christina L, Starr, Gregory
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2019
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article Research Support, Non-U.S. Gov't Research Support, U.S. Gov't, Non-P.H.S. ecosystem respiration flooding gross primary production hydrology net ecosystem CO2 exchange wetland Carbon Dioxide 142M471B3J
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520 |a Climate change has altered global precipitation patterns and has led to greater variation in hydrological conditions. Wetlands are important globally for their soil carbon storage. Given that wetland carbon processes are primarily driven by hydrology, a comprehensive understanding of the effect of inundation is needed. In this study, we evaluated the effect of water level (WL) and inundation duration (ID) on carbon dioxide (CO2 ) fluxes by analysing a 10-year (2008-2017) eddy covariance dataset from a seasonally inundated freshwater marl prairie in the Everglades National Park. Both gross primary production (GPP) and ecosystem respiration (ER) rates showed declines under inundation. While GPP rates decreased almost linearly as WL and ID increased, ER rates were less responsive to WL increase beyond 30 cm and extended inundation periods. The unequal responses between GPP and ER caused a weaker net ecosystem CO2 sink strength as inundation intensity increased. Eventually, the ecosystem tended to become a net CO2 source on a daily basis when either WL exceeded 46 cm or inundation lasted longer than 7 months. Particularly, with an extended period of high-WLs in 2016 (i.e., WL remained >40 cm for >9 months), the ecosystem became a CO2 source, as opposed to being a sink or neutral for CO2 in other years. Furthermore, the extreme inundation in 2016 was followed by a 4-month postinundation period with lower net ecosystem CO2 uptake compared to other years. Given that inundation plays a key role in controlling ecosystem CO2 balance, we suggest that a future with more intensive inundation caused by climate change or water management activities can weaken the CO2 sink strength of the Everglades freshwater marl prairies and similar wetlands globally, creating a positive feedback to climate change 
650 4 |a Journal Article 
650 4 |a Research Support, Non-U.S. Gov't 
650 4 |a Research Support, U.S. Gov't, Non-P.H.S. 
650 4 |a ecosystem respiration 
650 4 |a flooding 
650 4 |a gross primary production 
650 4 |a hydrology 
650 4 |a net ecosystem CO2 exchange 
650 4 |a wetland 
650 7 |a Carbon Dioxide  |2 NLM 
650 7 |a 142M471B3J  |2 NLM 
700 1 |a Malone, Sparkle L  |e verfasserin  |4 aut 
700 1 |a Oberbauer, Steven F  |e verfasserin  |4 aut 
700 1 |a Olivas, Paulo C  |e verfasserin  |4 aut 
700 1 |a Schedlbauer, Jessica L  |e verfasserin  |4 aut 
700 1 |a Staudhammer, Christina L  |e verfasserin  |4 aut 
700 1 |a Starr, Gregory  |e verfasserin  |4 aut 
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