Related Experiment Video
Updated: Aug 29, 2025

Methods of Soil Resampling to Monitor Changes in the Chemical Concentrations of Forest Soils
Published on: November 25, 2016
∼14 000 years of geochemical and isotopic data from Lake Simcoe, Canada
R M Doyle1,2, N Bumstead1, C F M Lewis3
1Department of Earth Sciences, Biological and Geological Sciences, The University of Western Ontario, 1151 Richmond St N, London, ON N6A 5B7, Canada.
Abstract:
This dataset contains measurements of modern water and ancient core materials from Lake Simcoe, the fourth largest lake wholly in Ontario, Canada. These data consist of: (i) oxygen, hydrogen and carbon isotope (δ 18O, δ 2H and δ 13C) compositions for modern water samples; (ii) physical measurements of one piston core, PC-5; (iii) δ 13C and δ 18O values of ostracods collected from PC-5, and (iv) δ 13C and δ 18O values of ancient DIC and water, respectively, inferred from item (iii). Physical measurements performed on core PC-5 include magnetic susceptibility, mineralogy and grain size. Mass accumulation rates are also reported. These data will be of interest to those aiming to better characterize the timing and pathway of meltwater flow during and following deglaciation of the Laurentide Ice Sheet in the Laurentian Great Lakes region. These data will also be useful to researchers investigating the influence of deglaciation on the oxygen and carbon isotope systematics of ancient lake environments. A discussion of these data is available in "A ∼14 000-year record of environmental change from Lake Simcoe, Canada" [1].
Related Concept Videos
Global Climate Change
Radioactive Decay and Radiometric Dating
The Fossil Record
Testing Water Quality

