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.

Highlights

  • Isoprene emission from vegetation is the world’s largest known source of non-methane volatile organic compounds (NMVOCs)

  • Isoprene emission rates were measured at leaf temperatures of 30–351C, emission rates were examined at temperatures as high as 391C during temperature response experiments

  • Wendl. (Poaceae) was examined by measuring isoprene emission as TL was increased in 31C increments from 301C to 391C

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Summary

Introduction

Isoprene emission from vegetation is the world’s largest known source of non-methane volatile organic. Modeling (Guenther et al, 1995) and limited measurement (Guenther et al, 1999, 1996) studies have suggested that at least 50% of the global annual isoprene flux is from tropical. Quantitative studies of tropical biogenic volatile organic compound (BVOC) emission at the plant level have been limited to isoprene in Puerto Rico (Lerdau and Keller, 1997) and Panama (Keller and Lerdau, 1999; Lerdau and Throop, 1999) and isoprene and monoterpenes in Central Africa (Klinger et al, 1998; Guenther et al, 1999) and South Africa (Guenther et al, 1996). Canopy-level fluxes are determined over 30-min periods from morning to midafternoon

Methods
Leaf measurements
Leaf-scale BVOC emissions
Canopy-scale BVOC emissions
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