Influence of volcanic gases on the epidermis of Pinus halepensis Mill. in Campi Flegrei, Southern Italy: A possible tool for detecting volcanism in present and past floras

• Published in: Journal of volcanology and geothermal research 2012-07, Vol.233-234, p.1-17
• Main Authors: Bartiromo, Antonello, Guignard, Gaëtan, Lumaga, Maria Rosaria Barone, Barattolo, Filippo, Chiodini, Giovanni, Avino, Rosario, Guerriero, Giulia, Barale, Georges
• Format: Article
• Language: English
• Subjects: Campi Flegrei; Cuticle ultrastructure; Epidermis; Hydrogen sulphide (H2S); Pinus halepensis; Volcanic gases
• ISSN: 0377-0273; 1872-6097
• DOI: 10.1016/j.jvolgeores.2012.04.002

Cuticle micromorphology together with epidermal and epistomatal wax, in both current- and first-year-old needles of conifer Pinus halepensis (Aleppo pine) trees growing under volcanic gas fumigation was analysed in Pisciarelli area, Campi Flegrei, Southern Italy. As a control, current- and first-year-old needles growing far from volcanic gas emission were also sampled. Using a multidisciplinary approach with SEM, TEM and X-ray, volcanic gases were shown to cause degradation on epicuticular and epistomatal waxes. Significant statistical variations of ultrastructural components of the cuticle, with 30 measurements, including total thickness of the cuticle, and details and proportions of all different layers, and use of confidence interval, revealed a high degree of sensitivity of Aleppo pine to this extreme environment. In the present study, non-significant thickness variations of the cell wall plus cuticle among current- and first-year-old needles of both fumigated and non fumigated trees have been found. However, at the ultrastructural level, significant variations in cell wall and total cuticle thickness, especially within the three zones of B1 fibrillar layer, revealed different equilibria for each of the four types of material. Using energy dispersive X-ray microanalysis, no sulphur was found in either cuticle or epidermal cells, but the presence of H2S in the fumarole gas is suspected to cause indirect and/or direct cuticle alterations of wax structure. Ultrastructural characters of plant cuticles related to emission of volcanic gases during the geological past are also discussed. Among these considerations, an identification key enabling distinction between non fumigated and fumigated materials with 9 characters, provides a good tool detecting the influence of volcanism for extant and fossil plants. ► Epidermal micro-morphology of Pinus halepensis growing under volcanic gas fumigation. ► Volcanic gases cause degradation on epicuticular and epistomatal waxes. ► At ultrastructural level, significant variations for cell wall and total cuticle thickness have been found. ► An identification key provides a good tool for extant and fossil material studies.