Nuclear and non-nuclear techniques for assessing the differential uptake of anthropogenic elements by atmospheric biomonitors

• Published in: Nuclear instruments & methods in physics research. Section A, Accelerators, spectrometers, detectors and associated equipment Accelerators, spectrometers, detectors and associated equipment, 2007-08, Vol.579 (1), p.499-502
• Main Authors: Pacheco, Adriano M.G., Freitas, Maria do Carmo, Sarmento, Susana
• Format: Article
• Language: English
• Subjects: AAS; Airborne elements; Biological monitoring; Epiphytic lichens; ICP-MS; INAA; Nickel; Tree bark; Vanadium; Wet–dry cycles
• ISSN: 0168-9002; 1872-9576
• DOI: 10.1016/j.nima.2007.04.110

The present study brings into focus tree-bark and lichen-thalli data from Parmelia caperata (L.) Ach. (syn. Flavoparmelia caperata (L.) Hale) and Platanus hybrida Brot. (syn. Platanus acerifolia (Ait.) Willd.), respectively, whose samples have been exposed at (transplanted into) a coastal location of south-western Portugal, impacted by urban-industrial emissions—Sines. Results for nickel (atomic absorption spectrophotometry; AAS) and vanadium (instrumental neutron activation analysis; INAA) are assessed and discussed here in terms of relative bioaccumulation, as well as in view of an influence of the precipitation regime on the corresponding elemental levels. Comparisons with similar experiments further afield suggest that enhanced levels of V in lichens could be due to an association of increased availability and alternate wet–dry periods. An overall reconciliation of [V] data from lichens seems therefore possible by assuming the former influence. Rainfall cycles did not appear to hinder or ease the Ni uptake though. Differential retention in lichens may thus be related to dissimilar mechanisms of accumulation, with Ni under some sort of homeostatic control and ionic forms of V competing for extracellular binding sites. Even if more conservative in absolute terms, bark indication closely follows lichens’ in either case. Mechanism(s) of elemental uptake are arguably different in bark, an aspect that requires further elucidation. Nickel and vanadium are signature elements that fingerprint fossil-fuel combustion, and have shown a typical [Ni]/[V] ratio around 0.3 in the Portuguese native lichen P. sulcata Taylor. Such ratio is approached by the present organisms in an exposed condition, after going through changes that may be viewed to reflect the above differential behaviour. The ratio is remarkably consistent in bulk deposition, pointing to a coal-burning signal superimposed on a general profile of oil-related industries.