The surficial geology, sedimentology and geochemistry of the late glacial sediments and Paleozoic bedrock in the Campbellford area, Ontario, with special reference to the Dummer Complex /

The Dummer Complex extends 180 km along the Precambrian - Paleozoic contact from Tamworth to Lake Simcoe. It is composed of coarse, angular Paleozoic clasts in discontinuous, pitted, hummocky deposits. Deposits are usually separated by bare or boulder strewn bedrock, but have been found in the southern drumlinized till sheet. Dummer Complex deposits show rough alignment with ice-flow. Eskers cross-cut many of the deposits. Dummer sediment subfacies are defined on the basis of dominant coarse grain size and lithology, which relate directly to the underlying Paleozoic formation. Three subglacial tills are identified based on the degree of comminution and distance of transport; the immature facies of the Dummer Complex; the mature facies of the drumlinized till sheet and; the submature facies which is transitional. Carbonate geochemistry was used for till-bedrock correlation in various grain sizes. Of the 3 Paleozoic formations underlying the Dummer Complex, the Gull River Fm. is geochemically distinctive from the Bobcaygeon and Verulam Formations using Ca, Mg, Sr, Cu, Mn, Fe and Na. The Bobcaygeon Fm. and Verulam Fm. can be differentiated using Ca and the Sr/Ca ratio. The immature facies from 1.0 phi and finer is dominated by the non-carbonate, long distance transported component which decreases slightly downice. The submature till facies contains more long distance material than the immature facies. Sr and Mn can be used to correlate the Gull River immature till facies to the underlying bedrock the other subfacies could not be distinguished from each other or their respective source formation. This method proved to be ineffective for sediments with greater than 35% non-carbonate component, due to leaching of elements by the dissolving acid.The Dummer Complex is produced subglacially , as the compressional ice encounters the permeable Paleozoic carbonates. The increased shear strength of the ice and pore pressures in the carbonates results in the basal ice zones becoming debris ladden. Cleaner ice overrides the basal debris . laden dead ice which then acts as the glacier bed. During retreat, the Simcoe lobe stagnates as flow is cut-off by the Algonquin Highlands.

Schram Family of Wainfleet Township documents, 1839-1901 (not inclusive)

George William Schram (1809-1885), son of Garrett Schram and Leah Van Etten, married Orpha Pearson on Nov.13, 1835. His son Marsena John Schram (farmer) was born in May of 1840, in Canada. He died on Nov. 17, 1926 in Wexford County, Michigan. He was married in 1867 to Sarah (1825-1887).Marsena married again on April 18, 1910 to Ann Clarinda Warner (1861-1924). He was working as a carpenter at this time. They had another son, William who was born about 1838 and he married Sabina Chambers on Jan. 21, 1862. The 1861 census for Wainfleet lists siblings of Marsena John Schram as Sarah J. (age 14), Georgiana (age 5), and William (age 21). The Schrams lived on Concession 5 and owned approximately 144 acres of land. David Thompson was born Feb. 4, 1873 and died Feb. 19, 1951. He married Sally Ann Wilson on Sept. 7, 1825 in Pelham. She died about 1840 in Indiana Ontario (near Cayuga). Lemuel Victor Hogue was born Dec.1, 1854 and died Jan. 12, 1929. He was married to Elizabeth Wills who was born Aug. 2, 1861 and died Mar. 8, 1926. Sources: http://www.findagrave.com/cgi-bin/fg.cgi?page=gr&GRid=99294842 http://wc.rootsweb.ancestry.com/cgi-bin/igm.cgi?op=GET&db=seadragon5&id=I91708

A Study of Ordered Gene Problems Featuring DNA Error Correction and DNA Fragment Assembly with a Variety of Heuristics, Genetic Algorithm Variations, and Dynamic Representations

Ordered gene problems are a very common classification of optimization problems. Because of their popularity countless algorithms have been developed in an attempt to find high quality solutions to the problems. It is also common to see many different types of problems reduced to ordered gene style problems as there are many popular heuristics and metaheuristics for them due to their popularity. Multiple ordered gene problems are studied, namely, the travelling salesman problem, bin packing problem, and graph colouring problem. In addition, two bioinformatics problems not traditionally seen as ordered gene problems are studied: DNA error correction and DNA fragment assembly. These problems are studied with multiple variations and combinations of heuristics and metaheuristics with two distinct types or representations. The majority of the algorithms are built around the Recentering- Restarting Genetic Algorithm. The algorithm variations were successful on all problems studied, and particularly for the two bioinformatics problems. For DNA Error Correction multiple cases were found with 100% of the codes being corrected. The algorithm variations were also able to beat all other state-of-the-art DNA Fragment Assemblers on 13 out of 16 benchmark problem instances.