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Multi-proxy paleoenvironmental record of colonial land-use change in the lower Rideau Canal system (Colonel By Lake), Ontario, Canada

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Abstract

The construction of the Rideau Canal was one of the greatest engineering accomplishments of the nineteenth century, creating a navigable waterway linking the Ottawa River with Lake Ontario. Colonel By Lake, located at the southern end of the canal near Kingston Mills, was created by the damming of the lower Cataraqui River. The canal flooding in 1831 raised water levels by almost 8 m, inundating former wetlands and lowland areas. European settlement in the pre-canal-era (ca. 1780s) was associated with widespread deforestation and limited flooding of wetlands by construction of mill dams. A detailed sediment coring program was conducted in Colonel By Lake to reconstruct the pre-canal environment and to document water level and land-use changes associated with European settlement and canal construction. The paleoenvironmental record was obtained through analysis of multiple environmental indicators including sediment facies, particle size, magnetic susceptibility and downcore changes in testate amoebae (thecamoebian) diversity. The core lithostratigraphy consists of organic-rich muds overlying peaty gyttja and a lowermost unit of fine to coarse silts. The canal flooding surface (ca. 1831) is clearly defined by a shift to finer grain sizes and increased magnetic susceptibility within the upper 40–60 cm. The shift is associated with an overall increase in thecamoebian abundance and diversity, and high numbers of Difflugia oblonga and Cucurbitella tricuspis that indicate a shift to a deeper and more eutrophic environment. In contrast, the pre-canal environment has lower thecamoebian abundance with assemblages characteristic of marsh environments (Centropyxis constricta, Centropyxis aculeata). The onset of canal flooding (ca. 1790s) is identified by an increase in Pontigulasia compressa (~50 cm), recording a higher water flow rate. The study shows that a multi-proxy paleoenvironmental approach can clearly define different environmental changes due to land-use changes during colonisation and canal-era construction activities.

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Acknowledgments

Research work was supported by Natural Science and Engineering Research Council of Canada grants to Boyce and Reinhardt and a GSA Claude J. Britton award to E. Sonnenburg. The authors thank P. J. van Hengstum and two anonymous reviewers for valuable feedback on the manuscript, and Jonathon Moore and staff of Parks Canada Underwater Archaeological Services for assistance with coring and access to reference materials. Ken Watson is thanked for discussions and assistance with field data collection.

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  1. School of Geography and Earth Sciences, McMaster University, Hamilton, ON, L8S 4K1, Canada

    E. P. Sonnenburg, J. I. Boyce & E. G. Reinhardt

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  1. E. P. Sonnenburg
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  2. J. I. Boyce
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  3. E. G. Reinhardt
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Correspondence to E. P. Sonnenburg.

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Sonnenburg, E.P., Boyce, J.I. & Reinhardt, E.G. Multi-proxy paleoenvironmental record of colonial land-use change in the lower Rideau Canal system (Colonel By Lake), Ontario, Canada. J Paleolimnol 42, 515–532 (2009). https://doi.org/10.1007/s10933-008-9302-7

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