Articles | Volume 12, issue 8
Biogeosciences, 12, 2285–2300, 2015
https://doi.org/10.5194/bg-12-2285-2015
Biogeosciences, 12, 2285–2300, 2015
https://doi.org/10.5194/bg-12-2285-2015

Research article 16 Apr 2015

Research article | 16 Apr 2015

Carbon exchange between the atmosphere and subtropical forested cypress and pine wetlands

W. B. Shoemaker1, F. Anderson2, J. G. Barr3, S. L. Graham4, and D. B. Botkin5 W. B. Shoemaker et al.
  • 1U.S. Geological Survey, Florida Water Science Center, 7500 SW 36th St, Davie, FL 33314, USA
  • 2U.S. Geological Survey, California Water Science Center, Placer Hall, 6000 J Street, Sacramento, CA, USA
  • 3South Florida Natural Resource Center, Everglades National Park, Homestead, FL 33030, USA
  • 4National Institute of Water and Atmospheric Research (NIWA), Christchurch, New Zealand
  • 5Department of Biology, University of Miami, Coral Gables, FL, USA

Abstract. Carbon dioxide exchange between the atmosphere and forested subtropical wetlands is largely unknown. Here we report a first step in characterizing this atmospheric–ecosystem carbon (C) exchange, for cypress strands and pine forests in the Greater Everglades of Florida as measured with eddy covariance methods at three locations (Cypress Swamp, Dwarf Cypress and Pine Upland) for 2 years. Links between water and C cycles are also examined at these three sites, as are methane emission measured only at the Dwarf Cypress site. Each forested wetland showed net C uptake from the atmosphere both monthly and annually, as indicated by the net ecosystem exchange (NEE) of carbon dioxide (CO2). For this study, NEE is the difference between photosynthesis and respiration, with negative values representing uptake from the atmosphere that is retained in the ecosystem or transported laterally via overland flow (unmeasured for this study). Atmospheric C uptake (NEE) was greatest at the Cypress Swampp (−900 to −1000 g C m2 yr−1), moderate at the Pine Upland (−650 to −700 g C m2 yr−1) and least at the Dwarf Cypress (−400 to −450 g C m2 yr−1). Changes in NEE were clearly a function of seasonality in solar insolation, air temperature and flooding, which suppressed heterotrophic soil respiration. We also note that changes in the satellite-derived enhanced vegetation index (EVI) served as a useful surrogate for changes in NEE at these forested wetland sites.

Download
Short summary
Carbon dioxide exchange (NEE) between the atmosphere and forested subtropical wetlands is quantified at three locations for 2 years. Each forested wetland showed net carbon uptake (retained in the soil and biomass or transported laterally via overland flow) from the atmosphere both monthly and annually. Changes in NEE were clearly a function of seasonality in solar insolation, air temperature and flooding, which suppressed heterotrophic soil respiration.
Altmetrics
Final-revised paper
Preprint