The Canada Seed Company was formed in 1913 by Mr. R. C. (Clark) Steele at Hagersville, Ontario with the intent to process and export farm seeds. However, in later years, the company branched out into the Garden Seed business. Early in the 1930's, R. C. Steele merged his company with the Steele Briggs Seed Co., which was owned by his brother Walter D. Steele. Following the deaths of W. D. Steele and E. F. Crossland, R. C. Steele was elected President of Steele Briggs.
A few years later, Vancouver interests took over the seed companies under Steele Briggs, including the Canada Seed Company. At this time, R. C. Steele retired from the company to form Steele Robertson Co., headquartered in Edmonton. W. D. Dack was appointed President of Steele Briggs. In June 1951, W. D. Dack took control of company operations from the Vancouver interests and, in 1961, the Steele Briggs Seed Co. purchased the Rennie Seed Co.
Custodial History
See fonds level description of custodial history of A. E. McKenzie Seed Co. Ltd.
Scope and Content
This sub-series contains the resignation of A.J. Maruca as an officer and director of
Canada Seeds Ltd. and a report on operating results for the nine-month period ending
February 28,1967. The remainder of the records in this sub-series are financial
statements prepared by Meyers Norris Penny & Co.
The sub sub series is divided into two sub sub sub series, including: (1) Financial; and (2) Miscellaneous.
Historical information regarding Canada Seeds Ltd. is located in Series 2 (Office of the President/GM), sub-series 2 (J. Lasby Lowes), Historical Topics file 10 (Tape 23) and file 11 (Tape 24) of the A.E. McKenzie Seed Co. Ltd. fonds.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
North Lauder Radiocarbon Date report by Beta Analytic Inc. for Flintstone Hill #109529 and #109530.
Radiocarbon dating
The technique of radiocarbon dating was developed by Willard Libby and his colleagues at the University of Chicago in 1949.
Radiocarbon dating is used to estimate the age of organic remains from archaeological sites. Organic matter has a radioactive form of carbon (C14) that begins to decay upon death. C14 decays at a steady, known rate of a half life of 5,730 years. The technique is useful for material up to 50,000 years. Fluctuations of C14 in the atmosphere can affect results so dates are calibrated against dendrochronology. Radiocarbon dates are calibrated to calendar years.
Dates are reported in radiocarbon years or Before Present. Before Present refers to dates before 1950. The introduction of massive amounts of C14, due to atomic bomb and surface testing of atomic weapons, has widely increased the standard deviation on all dates after A.D. 1700 causing these dates to be unreliable.
Accelerated mass spectrometry can more accurately measure C14 with smaller samples and can date materials to 80,000 years.
Scope and Content
Sub sub series contains radiocarbon dates from: Atkinson site and Flintstone Hill.
