The effects of water deficit stress and plant water potential (w) on monoterpene and sesquiterpene leaf emissions from Rosmarinus officinalis, Pinus halepensis, Cistus albidus and Quercus coccifera were studied over 11 days of water withholding (from t 1 to t 11 ), after substrates had achieved their field capacity (control pots: t 0 ). Volatile compounds were sampled from the same twig per plant all throughout the study, using a dynamic bag enclosure system. Volatiles, collected in Tenax TA, were studied by means of GC-FID and GC-MS. Monoterpene emissions of water stressed plants (t 1 -t 11 ) were either similar to those of control seedlings (R. officinalis and Q. coccifera)or higher (P. halepensis and C. albidus). By contrast, sesquiterpene emissions were strongly reduced or inhibited after four days of water withholding, particularly for R. officinalis, thus altering terpene emission composition. Despite the positive effect of water stress on leaf monoterpene emissions of P. halepensis and C. albidus, the significant correlation between these emissions and w showed a slow decrease of these emissions over long term water deficit periods. This contrasted with the rapid decline of sesquiterpene emissions of R. officinalis according to lower values of w. These results provide an overall picture of the different responses of monoterpene and sesquiterpene emissions to progressive water loss. They also reveal the utility of using w for estimating some emission rates of some species according to drought conditions.
Abstract. The CANOPEE project aims to better understand the biosphere–atmosphere exchanges of biogenic volatile organic compounds (BVOCs) in the case of Mediterranean ecosystems and the impact of in-canopy processes on the atmospheric chemical composition above the canopy. Based on an intensive field campaign, the objective of our work was to determine the chemical composition of the air inside a canopy as well as the net fluxes of reactive species between the canopy and the boundary layer. Measurements were carried out during spring 2012 at the field site of the Oak Observatory of the Observatoire de Haute Provence (O3HP) located in the southeast of France. The site is a forest ecosystem dominated by downy oak, Quercus pubescens Willd., a typical Mediterranean species which features large isoprene emission rates. Mixing ratios of isoprene, its degradation products methylvinylketone (MVK) and methacrolein (MACR) and several other oxygenated VOC (OxVOC) were measured above the canopy using an online proton transfer reaction mass spectrometer (PTR-MS), and fluxes were calculated by the disjunct eddy covariance approach. The O3HP site was found to be a very significant source of isoprene emissions, with daily maximum ambient concentrations ranging between 2–16 ppbv inside and 2–5 ppbv just above the top of the forest canopy. Significant isoprene fluxes were observed only during daytime, following diurnal cycles with midday net emission fluxes from the canopy ranging between 2.0 and 9.7 mg m−2 h1. Net isoprene normalized flux (at 30 °C, 1000 μmol quanta m−2 s−1) was estimated at 7.4 mg m−2 h−1. Evidence of direct emission of methanol was also found exhibiting maximum daytime fluxes ranging between 0.2 and 0.6 mg m−2 h−1, whereas flux values for monoterpenes and others OxVOC such as acetone and acetaldehyde were below the detection limit. The MVK+MACR-to-isoprene ratio provided useful information on the oxidation of isoprene, and is in agreement with recent findings proposing weak production yields of MVK and MACR, in remote forest regions where the NOx concentrations are low. In-canopy chemical oxidation of isoprene was found to be weak and did not seem to have a significant impact on isoprene concentrations and fluxes above the canopy.
Fertilizer effects on terpene production have been noted in numerous reports. In contrast, only a few studies have studied the response of leaf terpene content to naturally different soil fertility levels. Terpene content, as determined by gas chromatography/mass spectrometry/flame ionization detector, and growth of Pinus halepensis, Rosmarinus officinalis, and Cistus albidus were studied on calcareous and siliceous soils under field conditions. The effect of nitrogen (N) and extractable phosphorus (P(E)) from these soils on terpenes was also investigated since calcareous soils mainly differ from siliceous soils in their higher nutrient loadings. Rich terpene mixtures were detected. Twenty-one terpenes appeared in leaf extracts of R. officinalis and C. albidus and 20 in P. halepensis. Growth of all species was enhanced on calcareous soils, while terpene content showed a species-specific response to soil type. The total monoterpene content of P. halepensis and that of some major compounds (e.g., delta-terpinene) were higher on calcareous than on siliceous soils. A significant and positive relationship was found between concentration of N and P(E) and leaf terpene content of this species. These findings suggest that P. halepensis may respond to an environment characterized by increasing soil deposition, by allocating carbon resources to the synthesis of terpene defense metabolites without growth reduction. Results obtained for R. officinalis showed high concentrations of numerous major monoterpenes (e.g., myrcene, camphor) in plants growing on calcareous soils, while alpha-pinene, beta-caryophyllene, and the total sesquiterpene content were higher on siliceous soils. Finally, only alloaromadendrene and delta-cadinene of C. albidus showed higher concentrations on siliceous soils. Unlike P. halepensis, soil nutrients were not involved in terpene variation in calcareous and siliceous soils of these two shrub species. Possible ecological explanations on the effect of soil type for these latter two species as well as the ecological explanation of rich terpene mixtures are discussed.
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