Increased salinity decreases annual gross primary productivity at a Northern California brackish tidal marsh

• Published in: Environmental research letters 2023-03, Vol.18 (3), p.34045
• Main Authors: Russell, Sarah J, Windham-Myers, Lisamarie, Stuart-Haëntjens, Ellen J, Bergamaschi, Brian A, Anderson, Frank, Oikawa, Patty, Knox, Sara H
• Format: Article
• Language: English
• Subjects: Air temperature; Brackish Wetland; Carbon; Carbon cycle; Carbon Dioxide; Carbon sequestration; Climate adaptation; Climate change; Drought; Ecosystems; Environmental impact; ENVIRONMENTAL SCIENCES; Environmental Sciences & Ecology; Extreme drought; Freshwater plants; Gross Primary Productivity; Growing season; Marshes; Meteorology & Atmospheric Sciences; Microbial activity; Microorganisms; Plant communities; Productivity; Saline water; Salinity; Salinity effects; Salinization; Tidal marshes; Wetlands
• ISSN: 1748-9326; 1748-9326
• DOI: 10.1088/1748-9326/acbbdf

Tidal marshes sequester 11.4–87.0 Tg C yr −1 globally, but climate change impacts can threaten the carbon capture potential of these ecosystems. Tidal marshes occur across a wide range of salinity, with brackish marshes (0.5–18 ppt (parts per thousand)) dominating global tidal marsh extents. A diverse mix of freshwater- and saltwater-tolerant plant and microbial communities has led researchers to predict that carbon cycling in brackish wetlands may be less sensitive to changes in salinity than fresh- or saltwater wetlands. Rush Ranch, a well-monitored brackish tidal wetland of the San Francisco Bay National Estuarine Research Reserve, experiences highly variable annual salinity regimes. Within a five-year period (2014–2018), Rush Ranch experienced particularly extreme drought-induced salinization during the 2014 and 2015 growing seasons. During drought years, tidal channel salinity rose from a 15 year baseline of 4.7 ppt to growing season peaks of 10.3 ppt and 12.5 ppt. Continuous eddy covariance data from 2014 to 2018 demonstrate that during drought summers, gross primary productivity (GPP) decreased by 24%, whereas ecosystem respiration remained similar among all five years. Stepwise linear regression revealed that salinity, not air temperature or tidal height, was the dominant driver of annual GPP. A random forest model trained to predict GPP based on environmental data from low salinity years (i.e. naive to salinization) significantly over predicted GPP in drought years. When growing season salinities were doubled, annual estimates of net ecosystem exchange of CO 2 decreased by up to 30%. These results provide ecosystem-scale evidence that increased salinity influences CO 2 fluxes dominantly through reductions in GPP. This relationship provides a starting point for incorporating the effect of changes in salinity in wetland carbon models, which could improve wetland carbon forecasting and management for climate resilience.