K. Torigai et al., A variable lacustrine environment in Lake Winnipeg, Manitoba: Evidence from modern thecamoebian distribution, J PALEOLIMN, 23(3), 2000, pp. 305-318
Thecamoebians (testate protozoan) were examined in 18 surface sediment samp
les from the North and South basins and the Narrows of Lake Winnipeg, Manit
oba. Significantly higher numbers of thecamoebians and tintinnids in the No
rth Basin compared to the Narrows and South Basin are attributed to the eff
ects of urban development around the South Basin of Lake Winnipeg. Human po
pulation growth in this area has led to increased nutrient concentration in
runoff, causing eutrophication of the southern lake, which in turn allows
for increased algal productivity. Cucurbitella tricuspis is found in large
abundances in the South Basin, particularly close to the inlet of the Red a
nd Assiniboine rivers. High abundances of this species have been attributed
to eutrophic conditions, which this species appears to withstand more succ
essfully than other species. Increases in domestic waste output, that have
led to elevated heavy metal concentrations in lake bottom sediments of the
South Basin, may have resulted in lower abundances of thecamoebians, furthe
r reducing competition.
Strong currents in the Narrows cause a slightly coarser substrate and sweep
away food sources such as phytoplankton. This results in a lower faunal ab
undance and slightly lower species richness of thecamoebians. Robust specie
s such as the coarse-grained Difflugia viscidula and species which feed on
bacteria such as Centropyxis aculeata show increased abundances.
Modern thecamoebian assemblages are comparable to Late Holocene faunal asso
ciations in terms of species composition. Individual species abundances, ho
wever, have changed. For example, in the North Basin the Late Holocene domi
nance of Difflugia manicata is replaced by various strains of Difflugia obl
onga during recent times. A common species of the South Basin from Late Hol
ocene to recent times is Difflugia globulus. It would appear that faunal di
fferences between basins are the result of differences in algal food source
s.