The rapid increase in atmospheric CO
2 concentrations (
Ca) has resulted in extensive research efforts to understand its impact on terrestrial ecosystems, especially carbon balance. Despite these efforts, there are relatively few data comparing net ecosystem exchange of CO
2 between the atmosphere and the biosphere (NEE), under both ambient and elevated
Ca. Here we report data on annual sums of CO
2 (NEE
net) for 19 years on a Chesapeake Bay tidal wetland for
Scirpus olneyi (C
3 photosynthetic pathway)‐ and
Spartina patens (C
4 photosynthetic pathway)‐dominated high marsh communities exposed to ambient and elevated
Ca (ambient + 340 ppm). Our objectives were to (i) quantify effects of elevated
Ca on seasonally integrated CO
2 assimilation (NEE
net = NEE
day + NEE
night, kg C m
?2 y
?1) for the two communities; and (ii) quantify effects of altered canopy N content on ecosystem photosynthesis and respiration. Across all years, NEE
net averaged 1.9 kg m
?2 y
?1 in ambient
Ca and 2.5 kg m
?2 y
?1 in elevated
Ca, for the C
3‐dominated community. Similarly, elevated
Ca significantly (
P < 0.01) increased carbon uptake in the C
4‐dominated community, as NEE
net averaged 1.5 kg m
?2 y
?1 in ambient
Ca and 1.7 kg m
?2 y
?1 in elevated
Ca. This resulted in an average CO
2 stimulation of 32% and 13% of seasonally integrated NEE
net for the C
3‐ and C
4‐dominated communities, respectively. Increased NEE
day was correlated with increased efficiencies of light and nitrogen use for net carbon assimilation under elevated
Ca, while decreased NEE
night was associated with lower canopy nitrogen content. These results suggest that rising
Ca may increase carbon assimilation in both C
3‐ and C
4‐dominated wetland communities. The challenge remains to identify the fate of the assimilated carbon.
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