Development of a diatom-based specific conductivity model for the glacio-isostatic lakes of Truelove Lowland: implications for paleoconductivity and paleoenvironmental reconstructions in Devon Island lakes, NWT, Canada
Sl. Ng et Rh. King, Development of a diatom-based specific conductivity model for the glacio-isostatic lakes of Truelove Lowland: implications for paleoconductivity and paleoenvironmental reconstructions in Devon Island lakes, NWT, Canada, J PALEOLIMN, 22(4), 1999, pp. 367-382
Diatoms are identified and enumerated from the surface sediments of 100 lak
es of Truelove Lowland, Devon Island, N.W.T., Canada. These lakes range fro
m large oligotrophic lakes, to small tundra ponds, to coastal marine lagoon
s which are diverse in terms of ionic concentration and composition. The re
lationship between diatoms and 15 limnological variables is examined using
Canonical Correspondence Analysis (CCA). Specific conductivity is identifie
d as the most important variable influencing the distribution of diatoms in
the Truelove lakes. A Weighted Averaging (WA) calibration model is develop
ed to predict diatom-inferred specific conductivity. The reliability of the
model is tested by evaluating the correlation between observed and diatom-
inferred values and determining the error of prediction by bootstrapping. T
he applicability of the predictive conductivity equation is demonstrated by
reconstructing the paleoconductivity history of Fish Lake.