F. Riget et al., The use of lichen (Cetraria nivalis) and moss (Rhacomitrium lanuginosum) as monitors for atmospheric deposition in Greenland, SCI TOTAL E, 245(1-3), 2000, pp. 137-148
Concentrations of Pb, Cd, Hg, Zn, Cu, Cr, Ni, As, V, Al and Fe are reported
from soil, humus, moss (Rhacomitrium lanuginosum) and lichen (Cetraria niv
alis) sampled at four locations in Greenland. For Al, Fe, Cr and V the leve
ls in soil were highest followed by humus and R. lanuginosum and with the l
owest levels in C. nivalis. The same was true for Pb, Cu and Ni but without
as great a difference between medias. For Cd and Hg, the lowest levels wer
e found in soil. For Zn and As, the media with highest levels differed betw
een locality. Data were examined by a principal component analysis. Three p
rincipal components explained 87% of the total variation. The dominant elem
ents in the first component were Fe, Al, V, Ni, Cr, Cu and Pb. This compone
nt is interpreted as a soil dust factor. The concentrations in R. lanuginos
um and C. nivalis of these elements are believed to be highly influenced by
soil dust. Pb concentrations in moss and lichen may also be influenced by
other sources as Pb also had some correlation's with the third component. Z
n and Cd and to a lesser extent As were the dominant elements in the second
component. The third component was highly dominated by Hg with a lesser in
fluence of Pb and As. Zn, Cd and Hg concentrations in R lanuginosum and C.
nivalis are believed to be influenced by other sources than soil dust which
may be long-range atmospheric transport. In general, both the within local
ity and the between locality variability in the values of the three compone
nts decreased in the order soil, humus, R. lanuginosum and C. nivalis. The
lichen C. nivalis is looked at as an indicator with greater potential for m
onitoring atmospheric deposition of elements than the moss R lanuginosum. (
C) 2000 Elsevier Science B.V. All rights reserved.