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Global change accelerates carbon assimilation by a wetland ecosystem engineer

Bibliographic Data

ID15544808
AuthorsJoshua S Caplan (0000-0003-4624-2956, Bryn Mawr College, corresponding author), Rachel Nia Hager (Bryn Mawr College), J Patrick Megonigal (0000-0002-2018-7883, Smithsonian Environmental Research Center), Thomas J Mozdzer (0000-0002-1053-0967, Smithsonian Environmental Research Center)
Year2015
Volume10
Issue11
Pages115006-115006
Publication date2015-11-01
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/10/11/115006
OpenAlexW2267619387
LanguageEN
Citations received1
References cited74

The primary productivity of coastal wetlands is changing dramatically in response to rising atmospheric carbon dioxide (CO2) concentrations, nitrogen (N) enrichment, and invasions by novel species, potentially altering their ecosystem services and resilience to sea level rise. In order to determine how these interacting global change factors will affect coastal wetland productivity, we quantified growing-season carbon assimilation (≈gross primary productivity, or GPP) and carbon retained in living plant biomass (≈net primary productivity, or NPP) of North American mid-Atlantic saltmarshes invaded by Phragmites australis (common reed) under four treatment conditions: two levels of CO2 (ambient and +300 ppm) crossed with two levels of N (0 and 25 g N added m−2 yr−1). For GPP, we combined descriptions of canopy structure and leaf-level photosynthesis in a simulation model, using empirical data from an open-top chamber field study. Under ambient CO2 and low N loading (i.e., the Control), we determined GPP to be 1.66 ± 0.05 kg C m−2 yr−1 at a typical Phragmites stand density. Individually, elevated CO2 and N enrichment increased GPP by 44 and 60%, respectively. Changes under N enrichment came largely from stimulation to carbon assimilation early and late in the growing season, while changes from CO2 came from stimulation during the early and mid-growing season. In combination, elevated CO2 and N enrichment increased GPP by 95% over the Control, yielding 3.24 ± 0.08 kg C m−2 yr−1. We used biomass data to calculate NPP, and determined that it represented 44%–60% of GPP, with global change conditions decreasing carbon retention compared to the Control. Our results indicate that Phragmites invasions in eutrophied saltmarshes are driven, in part, by extended phenology yielding 3.1× greater NPP than native marsh. Further, we can expect elevated CO2 to amplify Phragmites productivity throughout the growing season, with potential implications including accelerated spread and greater carbon storage belowground

Agronomy · Atmospheric sciences · Biology · Biomass (ecology · Botany · Canopy · Carbon cycle · Carbon dioxide · Carbon sequestration · Climate change · Ecosystem · Growing season · Photosynthesis · Phragmites · Primary production · Productivity · Wetland · Coastal wetland ecosystem dynamics · Environmental Science · Marine and coastal plant biology · Peatlands and Wetlands Ecology · Ecology

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    Open Access•Elizabeth Mcleod, Gail L Chmura et al.•Frontiers in Ecology and the…•2011

  • Nitrogen Cycles

    Open Access•James N Galloway, Frank Dentener et al.•Biogeochemistry•2004

  • Tidal influences on carbon assimilation by a salt marsh

    Open Access•James C Kathilankal, Thomas J Mozdzer et al.•Environmental Research Letters•2008

Citations per year0.1
Citation span2016 - 2016 (1)
Highly citedNo

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