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Biogenic volatile organic compound emissions from a lowland tropical wet forest in Costa Rica
Institution:1. State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing, China;2. School of Natural Resources, Faculty of Geographical Science, Beijing Normal University, Beijing, China;3. Environmental Research, Wageningen University and Research, Wageningen, the Netherlands;4. Environmental Systems Analysis Group, Wageningen University and Research, Wageningen, the Netherlands;1. Metabolomics and Mass Spectrometry Research Group, Amazonas State University - UEA, 690065-130 Manaus, AM, Brazil;2. Department of Chemistry, Federal University of Amazonas - UFAM, 69080-900 Manaus, AM, Brazil;3. Faculty of Pharmacy, Federal University of Amazonas - UFAM, 69077-000 Manaus, AM, Brazil;4. School of Biological and Environmental Sciences, Federal University of Grande Dourados - UFGD, 79825-900 Dourados, MS, Brazil;5. Institute of Chemistry, University of Campinas - UNICAMP, 13083-970 Campinas, SP, Brazil;1. School of Environmental Science and Engineering, Sun Yat-Sen University, Guangzhou 510275, China;2. Foshan Environmental Monitoring Center, Foshan 528000, China;3. School of Environment and Energy, South China University of Technology, Guangzhou 510641, China;4. Department of Earth System Science, University of California, Irvine, CA 92697-3100, USA
Abstract:Twenty common plant species were screened for emissions of biogenic volatile organic compounds (BVOCs) at a lowland tropical wet forest site in Costa Rica. Ten of the species examined emitted substantial quantities of isoprene. These species accounted for 35–50% of the total basal area of old-growth forest on the major edaphic site types, indicating that a high proportion of the canopy leaf area is a source of isoprene. A limited number of canopy-level BVOC flux measurements were also collected by relaxed eddy accumulation (REA). These measurements verify that the forest canopy in this region is indeed a significant source of isoprene. In addition, REA fluxes of methanol and especially acetone were also significant, exceeding model estimates and warranting future investigation at this site. Leaf monoterpene emissions were non-detectable or very low from the species surveyed, and ambient concentrations and REA fluxes likewise were very low. Although the isoprene emission rates reported here are largely consistent with phylogenetic relations found in other studies (at the family, genus, and species levels), two species in the family Mimosaceae, a group previously found to consist largely of non-isoprene emitters, emitted significant quantities of isoprene. One of these, Pentaclethra macroloba (Willd.) Kuntze, is by far the most abundant canopy tree species in the forests of this area, composing 30–40% of the total basal area. The other, Zygia longifolia (Humb. & Bonpl.) Britton & Rose is a common riparian species. Our results suggest that the source strength of BVOCs is important not only to tropical atmospheric chemistry, but also may be important in determining net ecosystem carbon exchange.
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