Marriage Bond between Henry Chambers of Ancaster and Sarah Smith of Ancaster

Marriage Bond between Henry Chambers of Ancaster and Sarah Smith of Ancaster signed by Charles Anderson of Grimsby and Robert F. Nelles of Grimsby, Dec. 27, 1836.

Senate Chamber

Senate Chambers in A Block of the MacKenzie Chown Complex.

Petrography, geochemistry and structure of the Timmins area, Ontario

Regional structural analysis of the Timmins area indicates four major periods of tectonic deformation. The DI deformation is characterized by a series of isoclinal FI folds which are outlined in the study area by bedding, pillow tops and variolitic flows. The D2 deformation developed the Porcupine Syncline and refolded the Fl folds about a NE. axis. A pervasive S2 foliation developed during low grade (greenschist) regional metamorphism associated with the D2 deformation. The S2 foliation developed south of the Destor-Porcupine Break. The third phase of tectonic D3 deformation is recognized by the development of a S3 sub-horizontal crenulation cleavage which developed on the plane of the S2 foliation. No meso scopic folds are associated with this deformation. The 8 3 crenulation cleavage is observed south of the Destor-Porcupine Break. The D4 tectonic deformation is recorded as a subvertical S4 crenulation cleavage which developed on the plane of the S2 foliation and also offsets the S3 crenulation cleavage. Macroscopic F4 folds have refolded the F2 axial plane. No metamorphic recrystallization is associated with this deformation. The S4 crenulation cleavage is observed south of the Destor-Porcupine Break. Petrographic evidence indicates that the Timmins area has been subjected to pervasive regional low grade (greenschist) metamorphism which has recrystallized the original mineralogy. South of the study are~ the Donut Lake ultramafic lavas have been subjected to contact medium grade (amphibolite facies) metamorphism associated with the intrusion of the Peterlong Lake Complex. The Archean volcanic rocks of the Timmins area have been subdivided into komatiitic, tholeiitic and calcalkaline suites based on Zr, Ti0 2 and Ni. The three elements were used because of their r e lative immobility during subsequent metamorphic events. Geochemical observations in the Timmins area indicates that the composition of the Goose Lake and Donut Lake Formations are a series of peridotitic, pyroxenitic and basaltic komatiites. The Lower Schumacher Formation is a sequence of basaltic komatiites while the upper part of the Lower Schumacher Formation is an intercalated sequence of basaltic komatiites and low Ti0 2 tholeiites. The variolitic flows are felsic tholeiites in composition and geochemical evidenc e sugg ests that they developed as a n immiscible splitting of a tholeiitic magma. The Upper Schumacher Formation is a sequence of tholeiitic rocks dis p laying a mild iron enrichment. The Krist and Boomerang Formations are the felsic calc-alkaline rocks of the study area which are characteristically pyroclastic. The Redstone Fo rmation is dominantly a calc-alkali ne sequence of volcani c rocks whose minor mafic end me mbers exposed in 1t.he study hav e basaltic komatiitic compositions. Geochemical evidence sugges ts that the Keewatin-type se dimentary rocks have a composition similar to a quartz diorite or a granodiorite. Fi e l d obs ervations and petrographic evidence suggests that they were derived fr om a distal source and now repr esent i n part a turbidite sequence. The Timiskaming-type sedimentary rocks approach the c omp osi t ion of the felsic calc-alkaline rocks of the study area . The basal conglomerate in the study are a sugge s ts that th e uni t was derived fr om a proximal source. Petrographic and ge ochemical evidence suggests that the peridotitic and pyroxenitic komatiites originated as a 35-55% partial melt within the mantle, in excess of 100 Km. depth. The melt ros e as a diapir with the subsequent effusion of the ultramafic lavas, The basaltic komatiites and tholeiitic rocks originated in the mantle from lesser degrees of partial melting and fractionated in low pressure chambers. Geochemical evidence suggests a "genetic link" between the basaltic komatiites and tholeiites, The calc-alkaline rocks developed as a result of the increa.se In PO in the magma chamber. The felsic calcalkaline rocks are a late stage effusion possibly the last major volcanic eruptions in the area.

Niagara Resort and Tourist Association Records, 1975-1976, 1978-1983, 1985, 1987-1989, n.d.

Ontario Editorial Bureau (O.E.B.)

Account book from the Wilcox Estate, 1882-1886

This may be the account book of someone in the wholesale dry goods or grocery business. The account book includes balance sheets for a Waterford store and a Dunnville store. The accounts include clients from several southwestern Ontario communities. Names include Leitch, Turner, Auger, McKim, Beatty, Hewetson, Murton, Bell, Greig, Duggan, Kirk, and Logie. Local Niagara names include: W.B. Chambers of Welland and B.F. Morely of Thorold. Also includes deposit accounts held with Traders Bank of Canada and investments in the Temperance Colonization Society.

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

Photograph - Unidentified Male in Uniform

A photograph of a male in uniform standing in front of a horse. In background are tents and trees.

Chamber's Historical Questions with Answers

The book is hardcover and inscribed with an illegible signature, dated 1880 and below that is the signature Margaret J. Woodruff. The preface of the book begins, "The present work is designed to fulfil an important purpose in Education - that of bringing clearly into view the leading facts which are supposed to be gained through a long course of instruction. Without proposing to supersede the elementary books usually employed, it offers a certain test of what is presumed to have been previously learned. With such a work in their hands, Schoolmasters, Tutors, Governesses, or Parents, may at once satisfy themselves as to the degree of knowledge on a variety of subjects attained by the young person under their charge, and for whose intellectual culture they feel a special interest." The full text is available in the Brock University Special Collections and Archives.

Trading nitrogen for carbon: Nitrogen and carbon translocation in a plant/fungal (Metarhizium spp.) symbiosis

While nitrogen is critical for all plants, they are unable to utilize organically bound nitrogen in soils. Therefore, the majority of plants obtain useable nitrogen through nitrogen fixing bacteria and the microbial decomposition of organic matter. In the majority of cases, symbiotic microorganisms directly furnish plant roots with inorganic forms of nitrogen. More than 80% of all land plants form intimate symbiotic relationships with root colonizing fungi. These common plant/fungal interactions have been defined largely through nutrient exchange, where the plant receives limiting soil nutrients, such as nitrogen, in exchange for plant derived carbon. Fungal endophytes are common plant colonizers. A number of these fungal species have a dual life cycle, meaning that they are not solely plant colonizers, but also saprophytes, insect pathogens, or plant pathogens. By using 15N labeled, Metarhizium infected, wax moth larvae (Galleria mellonella) in soil microcosms, I demonstrated that the common endophytic, insect pathogenic fungi Metarhizium spp. are able to infect living soil borne insects, and subsequently colonize plant roots and furnish ts plant host with useable, insect-derived nitrogen. In addition, I showed that another ecologically important, endophytic, insect pathogenic fungi, Beauveria bassiana, is able to transfer insect-derived nitrogen to its plant host. I demonstrated that these relationships between various plant species and endophytic, insect pathogenic fungi help to improve overall plant health. By using 13C-labeled CO2, added to airtight plant growth chambers, coupled with nuclear magnetic resosnance spectroscopy, I was able to track the movement of carbon from the atmosphere, into the plant, and finally into the root colonized fungal biomass. This indicates that Metarhizium exists in a symbiotic partnership with plants, where insect nitrogen is exchanged for plant carbon. Overall these studies provide the first evidence of nutrient exchange between an insect pathogenic fungus and plants, a relationship that has potentially useful implications on plant primary production, soil health, and overall ecosystem stability.

Clippings - Road Allowances, Lock 2 Bridge, Toronto Railway Company, St. Davids' History

Clipping regarding the original road allowance which was part of Mr. Woodruff’s property, n.d. Clipping regarding the Lock 2 Bridge. This is a letter to the editor of the Journal from Calvin Phelps of Lockport, Nov. 13, 1889. Clipping entitled “Settled beyond a Dispute”: a letter to the Editor of the Star from J. G. Currie regarding the road allowance in the 5th Concession of Grantham, Nov. 16, 1889. Clipping entitled “That Old Road Allowance” which is a rebuttal to Mr. Currie’s letter, [1889] 2 newspaper clippings regarding: “Reg. vs. Toronto Railway Company”. These 2 articles are glued to a piece of paper. Beneath the newspaper articles is the name M. Chambers, Nov. 18, 1898. Notes regarding the clippings are enclosed with the articles. These notes and written on the back of “Pattison, Collier and Shaw Barristers, Solicitors, Etc.” stationary (notes are 2 pages, handwritten), Nov. 18, 1898. Clipping entitled “History on the Site: St. Davids’ Students Learn Lessons where Events Occurred” (2 copies), n.d.