The acidification chronology of Gr. Arbersee (Bavarian Forest, Germany
) was studied by means of subrecent diatom, and chrysophyte as well as
metal (Al, Cu, Cd, Mg, Ca) stratigraphies. pH was inferred by diatom
assemblages so that the simultaneous effects of acid and accompanying
metals on chrysophytes could be evaluated. The occurrence of seven dom
inant Mallomonadacean taxa was related to the environmental variables
by applying Spearman rank correlation and factor analysis. During the
post-glacial period of natural acidification, increases in organic car
bon and declining pH favor Mallomonas crassisquama and disfavor M. het
erospina and M. caudata. Potentially toxic metals (Al, Cu, Cd) and the
two alkaline earth metals (Ca, Mg) impact the occurrence as well. Alt
hough acidity appears to be also the major driving force during the re
cent acidification period, the occurring Mallomonadacean species may b
e differentiated by their tolerance toward Al and heavy metals.