Nj. Anderson et al., AN EXPERIMENTAL AND PALEOECOLOGICAL STUDY OF ALGAL RESPONSES TO LAKE ACIDIFICATION AND LIMING IN 3 CENTRAL SWEDISH LAKES, European journal of phycology, 32(1), 1997, pp. 35-48
Contemporary phytoplankton and palaeolimnological studies were made of
the algal response to acidification and liming in three lakes in Hals
ingland, central Sweden (Njupfatet, Sjosjon, Djuptjarn). Surveys and e
xperimental studies of the phytoplankton response to liming were under
taken at Njupfatet, together with an experiment designed to determine
the possible role of lake sediments as an inoculum for any new species
arriving in the water column. Liming had little quantitative or quali
tative effect on the phytoplankton diversity at Njupfatet, but did res
ult in the loss of the dominant contributor to algal biomass, Merismop
edia tenuissima. None of the four new species recorded in the lake fol
lowing liming was hatched from the sediment inoculum experiment. A fre
eze core from Njupfatet was dated by Pb-210 and carbonaceous fly-ash p
article profiles were also determined for Njupfatet and Sjosjon, which
provided an approximate chronology for the latter lake. Diatom analys
es were made of the three lakes and pH and dissolved organic carbon in
ferred using weighted averaging methodology. Njupfatet had no plankton
ic diatoms over the last 200-300 years, and was dominated by benthic d
iatoms, but the diatom-inferred pH suggests that the lake was acidifie
d to pH < 5 prior to liming in 1989. Both Djuptjarn and Sjosjon were d
ominated by planktonic diatoms, and were acidifying from (c. 1970) pri
or to liming, Sjosjon from pH 6 to similar to 5 and Djuptjarn from 65
to similar to 5.5. These pH inferences suggest that at least some lake
s in this region are susceptible to atmospheric acidification. The res
ponse of the diatoms to liming is discussed, in particular the rapid e
xpansion at Njupfatet, of Cyclotella glomerata a diatom which was also
present in Sjosjon for a period prior to acidification, and at other
lakes in south-west Sweden. Possible reasons for the expansion of this
small centric diatom are discussed.