ABSTRACT Salt marshes play a vital role in the biogeochemistry of coastal zones, yet the biophysical controls on CO 2 exchange with the atmosphere, or net ecosystem exchange (NEE, positive upwards) remain poorly quantified. We investigated a Spartina alterniflora monoculture salt marsh on the eastern shore of Virginia, United States, by estimating half‐hourly NEE from March 2016 to February 2017 using the eddy‐covariance method. Maximum marsh–atmosphere CO 2 exchanges occurred during June and July when hourly averaged NEE values reached −10.0 ± 2.5 μmol CO 2 m −2 s −1 (mean ±1 standard deviation). During the most productive time of the year, a tidal inundation of 0.7 m reduced daytime CO 2 assimilation and nighttime CO 2 release to the atmosphere by 5.0 ± 1.2 μmol CO 2 m −2 s −1 and 3.0 ± 0.7 μmol CO 2 m −2 s −1 , respectively. Diffuse photosynthetically active radiation (PAR) conditions promoted quantum use efficiencies ( α ) of the ecosystem that were approximately three times greater than under direct PAR conditions ( α Cloudy = 0.012 ± 0.004 versus α Clear = 0.004 ± 0.001 mol CO 2 per (mol photons)). Under diffuse light, NEE increased more rapidly with PAR and photo‐saturation occurred at higher PAR levels compared to clear‐sky conditions. On average, under the influence of diffuse light, the assimilation of CO 2 increased by 30% relative to equivalent PAR levels under direct sunlight. During March 2016 to February 2017 the marsh exchanged −269.1 ± 9.1 g of carbon per m 2 with the atmosphere. The findings demonstrate that tides and light quality are key regulators of carbon cycling in tidal marshes. These factors should be incorporated into models of tidal marsh biogeochemistry, particularly as both are undergoing rapid changes due to sea level rise and atmospheric warming.
Ruiz‐Plancarte et al. (Sun,) studied this question.