Thursday, August 6, 2020
Hydrology drives the carbon balance of wetlands by controlling the uptake and release of CO2 and CH4. In the Everglades, hydrology has been linked to seasonal and annual patterns in net ecosystem exchange rates. Short-hydroperiod freshwater marsh productivity is higher during the dry season, while long-hydroperiod freshwater marshes exhibit greater productivity during the wet season. Although they exhibit diverging seasonal patterns, freshwater marsh are nearly CO2 neutral (-11– -110 g CO2 m-2 yr-1). While seasonal patterns might be better explained by aboveground activity in the short-hydroperiod freshwater marsh, changes in respiration rates better explain seasonal variation in long-hydroperiod freshwater marsh.