“…The accumulation of filamentous green algae in various growth forms (epiphytic, epilithic, as well as metaphytic) is a widespread phenomenon in acidic lakes, having been identified in southern Sweden (Grahn et al, 1984 ;Lazerek, 1980), southern Norway (Hendrey, 1982), the Adirondack Mountains of New York (Hendrey & Vertucci, 1980) and New Hampshire (Roberts & Boyle, 1989), in addition to south-central Ontario (Stokes, 1981(Stokes, , 1984Howell et al 1990). Experimental acidification of stream channels (Hendrey, 1976 ;Parent et al, 1986 ;Griffiths, 1987), limnocorrals (Muller, 1980), small streams (Hall et al, 1980), and whole lakes (Brezonik et al, 1986 ;Turner et al, 1987) have also resulted in increases in biomass of filamentous green algae following treatment .…”