Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
The Crepeele locale is located within the larger Lauder Sandhills area, located in southwestern Manitoba. The area is a complex region of high biodiversity made up of stabilized sand dunes and wetlands that encourage the development of mixed forest and grass prairie. This area provided a variety of subsistence resources for pre-European hunter-gatherers. At the present time the grass prairie is now farm land but the areas of vegetated sand dunes have not been cultivated and have revealed numerous pre-contact archaeological sites.
Archaeological surveying was conducted in 2003. The results of the 2003 Casselman survey showed over 300 test uints contained cultural material and indicated several areas for further examination including the Crepeele site DiMe-29, Sarah site DiMe-28 and Graham sites DiMe-30.
From 2003 to 2008 field work took place at the locale with 75 - 1m x1m units excavated. The Crepeele locale is a complex region of high biodiversity made up of stabilized sand dunes and wetlands that encourage the development of mixed forest and grass prairie. This area provided a variety of subsistence resources for pre-European hunter-gatherers. At the present time the grass prairie is now farm land but the areas of vegetated sand dunes have not been cultivated and have revealed numerous pre-contact archaeological sites.
To help establish the cultural sequence at the locale Radiocarbon dates were obtained from the three sites in the Crepeele locale.
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: Crepeele, Sarah and Graham sites.
The Sarah site was chosen for excavation based on the results of the Casselman survey. The survey recovered significant amounts of faunal remains, some ceramics and lithics from the test pits. Excavations took place in 2003 at Crepeele West (Units 1-5) and Crepeele East (Units 6-9). The site was subsequently renamed the Sarah site DiMe-28. In 2004 another 9 units were excavated (Units 10-18).
Based on the recoveries it was determined that the Sarah site is a stratified site with woodland ceramics in the upper occupation and late woodland points in both of the upper occupations. These upper occupations produced abundant bison bone including foetal bone. The lower occupations produced less bone and no foetal bone, although absence of foetal bone in the lower occupations does not necessarily indicate a warm season occupation. This could be due to sample error or perthotaxic factors such as scavenging of the fragile bone by dogs or other carnivores.
The dates from the Sarah site include 550+/-40 B.P.; 1430+/-80 B.P; 2810+/-80 B.P.; 3120+/-130 B.P. The lower occupations did not yield any diagnostic materials although debitage was abundant. These occupations were most productive at the edge of the large sand dune at the southern edge of the excavations. It is assumed that the major portion of these occupations have been overridden by the dune in the past 3000 years. Heavy earthmoving equipment would be required to remove this overburden which limits the possibility of future excavation.
Environment
The Sarah site is a large area located at the eastern end of the Crepeele locale. Ground cover is a mosaic of aspen poplar groves and patches of mesic grass prairie. Excavation profiles indicate that this has been the situation since early precontact times, although as local climatic conditions change (primarily rainfall), the relative size of these areas and where they may have occurred also changed. The soil is aeolian sand sheet derived from delta outwash deposits along the western edge of glacial Lake Hind. The present topography is a variable dune landscape reworked by aeolian activity that creates a mosaic of microhabitats. These include forested patches in the lee of sand dunes with grassland on the southern and western exposures and small damp lowlands that support balsam poplar, willows, red osier dogwood, high-bush cranberry and water birch. There is no permanent water source in the area although a small seasonal stream meanders through a damp lowland to the east of the Sarah site.
Scope and Content
Sub-series has been divided into sub sub series including: Sarah 2003 and Sarah 2004,
The Graham site is a located adjacent to the Crepeele site towards the western end of the Crepeele locale. The Graham site was initially designated as a separate site early in the testing of the Crepeele locale due to what appeared to be a distinction between Early and Late Woodland ceramics. Subsequent testing has shown that this distinction was premature and that the cultural mosaic represented in the western section of the Crepeele locale may not readily separate in this manner. However, due to the records management that was already in place, the original separate designations have been retained.
Environment
Ground cover is a mosaic of aspen poplar groves and patches of mesic grass prairie. Excavation profiles indicate that this has been the situation since early precontact times, although as local climatic conditions change (primarily rainfall), the relative size of these areas and where they may have occurred also changed. The soil is aeolian sand sheet derived from delta outwash deposits along the western edge of glacial Lake Hind. The present topography is a variable dune landscape reworked by aeolian activity that creates a mosaic of microhabitats. These include forested patches in the lee of sand dunes grassland on the southern and western exposures and small damp lowlands that support balsam poplar, willows, red osier dogwood, high-bush cranberry and water birch. There is no permanent water source in the area although a small seasonal stream meanders through a damp lowland along the eastern margin of the Crepeele locale.
Excavations at the Graham site took place from 2004 to 2008. Analyses of the recoveries shows that, with two exceptions, all of the occupations that have been tested produced bison foetal bone. The presence of foetal bison is a strong indicator of wintering occupations...The absence of foetal in some area does not necessarily indicate warm season occupations since these excavation series are small and the absence could be due to sample error or perthotaxic factors, such as scavenging of the fragile bone by dogs or other carnivores.
From this evidence the Graham site has been interpreted as being primarily a wintering area. This is consistent with the lack of surface water (snow would serve as a substitute in winter) and the abundance of wood for fuel – a critical requirement for winter occupation. Cultural occupations date from Mortlach circa 250 B.P to woodland circa 580 B.P.
Scope and Content
Sub-series has been divided into sub sub series including: Graham 2004, Graham 2005, Graham 2006 and Graham 2008
The Atkinson site was named for the landowners Ken and Karen Atkinson who were very helpful to the archaeology and geoarchaeology crews that worked at the site. Their support made the project possible.
The Atkinson site story begins with the discovery of a charcoal lens eroding from the north bank of the Souris River in the summer of 2002. Study of Cultural Adaptations on the Prairie Ecozone (SCAPE) project geoarchaeologist Dr. Garry Running was exploring the stratigraphic layering in the bank when he noted the lens and reported it to Dr. Bev Nicholson. Upon closer examination, a tiny pressure flake was observed on the lens exposure and it was decided to collect a charcoal sample for radiocarbon dating.
The resulting date of 5250B.P cal. 4225 B.C. placed the site in the early Archaic period. A second date on bone collagen of 5580B.P. cal. 4500 B.C. confirmed the earlier date and gave an averaged date of circa 4400 B.C or 6,500 years ago.
The Atkinson site is one of the oldest excavated sites in Manitoba. Based on the date of the site and the kind of lithics (stone tools) present it is considered a Gowen occupation. The Atkinson site is evidence that bison hunters were active on the northern plains at a very early date. Similar sites have also been found on the High Plains in the U.S. and are referred to as the Mummy Cave Complex.
The Atkinson Site is of great importance as it is the first undisturbed site of this type to be excavated in Manitoba and extends the range of these sites south and east from the type-sites in central Saskatchewan. Based on the date and sample evidence further excavations were conducted by Dr. Nicholson's team. in 2003, 2004 and 2006.
Scope and Content
Sub series has been divided into three sub sub series including: (1) Atkinson 2003, (2) Atkinson 2004; (3) Atkinson 2006
The Duthie site is the first site identified in the Makotchi-Ded Dontipi locale. It was reported to Dr. Bev Nicholson by Doug Jackson, a local collector who had observed archaeological materials that had been exposed during the construction of Maple Hill Road northwest of Lauder. The site is named after the landowner, Randy Duthie.
The initial inspection of the exposed materials indicated that the eastern half of the site had been severely impacted by raising a road grade using an elevating grader. However, an undetermined amount of the site remained to the west, flanked by a low sand dune. Testing and preliminary excavations were conducted in 1992-93. In 1994 a field school added to the excavated sample. The undisturbed portion of the site, west of Maple Hill Road was situated at the base of a low sand dune and had an aspen and willow forest cover. The water table was approximately one meter below surface at the time of excavation. A rising water table has since prevented further excavations.
Two dates on bone collagen were obtained during excavations. These were 880+/-80 B.P. (Beta 62705) and 970+/-40 B.P. cal. 1030 A.D. (TO 13366). These dates are consistent with an Initial Middle Missouri cultural assignment. The site occupation is identified by the distinctive ceramics found there. Ceramics at the Duthie Site are tool impressed with incising and lip modeling with fabric impressions on most vessels. Jill Taylor analysed the ceramics from the site for a Specialist thesis, Brandon University (1994) and a Masters of Arts degree from the University of Saskatchewan. (Taylor 1995).
Analysis of residue from Duthie site pottery by Matthew Boyd recovered corn (Zea mays) phytoliths and bean (Phaseolus sp.) starch grains indicating consumption of these domesticates at the Duthie site. (Boyd 2006)
The occupation of this site indicates a migration of people from the south who were well acquainted with horticultural farming. These people had previously migrated to South Dakota following river valleys into the central plains from the eastern woodlands during late Hopewell times. It appears that they later migrated well to the north into southern Manitoba but there is no evidence that they remained there for more than a single year.
Boyd, M., C. Surette and B.A. Nicholson. 2006 Archaeobotanical Evidence of Prehistoric Maize (Zea mays) Consumption at the Northern Edge of the Great Plains. Journal of Archaeological Science 33: 1129-1140.
Taylor, J. 1994 An analysis of the ceramics recovered during 1992 and 1993 at the Precontact Duthie Site (DiMe-16). Specialist thesis, Brandon University.
Scope and Content
The Series has been divided into seven sub-series, including (1) Duthie site (2) Jackson site (3) Twin Fawns site (4) Vera site (5) Schuddemat site (6) Bradshaw site (7) Hollow B site.
See RG 6 Brandon University fonds, 7.4.1 Dean of Music for biographical information.
Custodial History
The records were collected during the course of Jones' career as a member of the School of Music and as Dean of the School of Music. They remained in his possession until their donation to the McKee Archives on June 29, 2011.
Scope and Content
Collection consists of records created and collected during the course of Lawrence Jones' teaching career in the School of Music and during his tenure as Dean of the School of Music at Brandon University.
Records include: dean's log books; recital programs and related materials; personal documents; academic papers; planning documents; contracts; administration documents; workshop documents; teaching documents; proposals; reviews; evaluations; violin concerto by S.C. Eckhardt-Gramatte, piano score, edited by Lawrence Jones. Topics include: planning for the School of Music; Master's degree program; award winners; the music building expansion; adjudicating; the New Brandon University Trio; and the National Music Festival.
The high biodiversity and evidence of pre-Europeon contact prompted the decision to test the Crepeele locale. The survey was named in recognition of the Casselman family, the original landowners.
Archaeological testing began in the Crepeele locale in May 2003 on property now owned by the Crepeele family. The locale covers over 6 sections or approximately 3,800 acres of land in an area of stabilized sand dunes and wetlands covered with mixed forest and prairie grass. Given the terrain, the size of the crew and time constrains, an area of approximately 60 acres was chosen for the survey. The survey used the established archaeological methodology of walking the selected area and using a shovel test surveyed grid. The use of GIS technology to locate the exact test spot and record the information into a GIS database was a significant advance and was one of the advantages of the integration of multi-disciplinary techniques encouraged by the SCAPE project. Over one half of the test pits resulted in the recovery of cultural materials. The results of the Casselman survey indicated several areas for further examination including areas that became the Crepeele, Sarah and Graham sites.
Scope and Content
Sub sub series has been divided into five sub sub sub series including: (1) Summary information; (2) Field journals; (3) Site records; (4) Artifact catalogues; and (5) Photographs.
Flintstone Hill is located on the north bank of the Souris River. It is a deeply stratified lacustrine, fluvial and aeolian soil profile that has been exposed by the river through stream-bank erosion. This section is thought to be the most complete middle to late Holocene exposure on the northeastern plains. While the value of the site is primarily for paleo-environmental research and reconstruction, cultural deposits have been identified at the site. Local collectors have picked up lithic materials as they eroded out of the bank for the past several decades and it was they who had named the site. Mr. Bruce Timms from Lauder first drew the Flintstone Hill site to the attention of Dr. Nicholson of Brandon University.
During the mid 1990’s to the early 2000’s archaeological testing took place on Flintstone Hill. In 1998, an archaeological field crew dug a series of overlapping trenches down the slope of the profile and produced a schematic drawing. A peat layer at the bottom of this profile, dated from the top at 9,400 RCY and at the bottom to 10,400 RCY, has provided details of marsh plant and insect communities at this time.
Subsequent archaeological investigations at the site recovered several cultural deposits including: a hearth dating to 3250+/-70 R.C.Y. (BETA 109529); a butchered atlas bone 4090+/-70 R.C.Y. (BETA 109990); and bone fragments accompanied by Swan River Chert and Knife River Flint lithic flakes 5350+/-50 (BETA 109530). While no diagnostic tools were recovered, these dates suggest that this occupation, which is contemporary with the Atkinson site, may be a Gowen occupation.
Extensive paleo-environmental research has been conducted at the site. Dr. Running, a geomorphologist from the University of Wisconsin – Eau Claire, participated in the Study of Cultural Adaptations in the Prairie Ecozone (SCAPE) Project and he and his students tested the site for several years. He was joined in this effort by Dr. Havholm, Dr. Boyd, Dr. Wiseman, Dr. Beaudoin, and other SCAPE researchers in the interpretation of the paleo-environment of the Glacial Lake Hind basin. The following article is recommended reading.
Running, Garry L., Karen G. Havholm, Matt Boyd and Dion J. Wiseman
2002 Holocene Stratigraphy and Geomorphology of Flintstone Hill, Lauder Sandhills, Glacial Lake Hind Basin, Southwestern Manitoba. Geographie Physique et Quaternaire
56(2-3):291-303.
Scope and Content
Sub series has been divided into two sub sub series including: (1) Flintstone Hill 1997 (2) Flintstone Hill 1998-2000
Sinclair Co-operative Elevator Association Limited Organizational papers: 1928 - 1961 Memorandum of Association and General By-laws, 2 February 1928 Minutes of Provisional Directors meeting, 28 February 1928 First shareholders meeting, 28 February 1928 By-law nos. 1-7, 28 February 1928 Lease, 1 August 1928 Memorandum of agreement, 12 November 1929 Agreement between Sinclair CEA and MPE, 15 October 1936 By-law nos. 19, 20 and General By-laws, 18 June 1941 Letter re: agreement, 19 June 1944 Agreement between Sinclair CEA and MPE, 1 August 1951 By-law no. 23, 21 November 1951 Memo re: agreement, 4 July 1952 General By-laws (last passed 27 October 1952), no date Directors' Resolution, 18 October 1961 Minutes of Executive Board meetings, volume 1, 28 February 1928 - volume 8, 25 Novmeber 1971 Minutes of Shareholders Annual meetings, 1929 - 1947 (7 reports) Financial records and statistics Detail of grain earnings, 1964 - 1968 (3 reports) Statement and demand for taxes, 1974 Auditors' reports, 1929 - 1974 (13 reports) Statement demand for taxes, 1975 Review of Operating Results, 1966 - 1967 Correspondence, 1928 - 1973 Membership list, 1947 - 1968 Miscellaneous Directors' attendance lists, 1964 - 1974 (7 reports) Corporate Name: Rural Municipality of Pipestone
The Lovstrom surface collection came from small fields cleared within, and adjacent to, the major portions of the site which were excavated. The Lovstroms initial collection has since been added to by field personnel from Brandon University. The initial collections consisted of lithics and ceramics. A collection of faunal remains from the cultivated area was made by a Brandon University zooarchaeology class in 1986 which yielded specimens of elk, canid, mussels, and sucker, in addition to an expected abundance of bison. Since these materials were in a surface context, it may be that some of the faunal remains were historic.
The high biodiversity and evidence of pre-Europeon contact prompted the decision to test the Lovstrom locale. Nine 1m2 units were excavated in 1985 and, in 1986, an additional 15 1m2 units were excavated for a total of 24 test units. This testing indicated the presence of a large precontact locale with lithics, woodland ceramics and large amounts of reasonably well-preserved faunal materials.
The lithics indicated a late Prehistoric occupation (Nicholson 1986:35). However, the ceramics were more useful in that they identified the presence of Late Woodland cultures (Blackduck and Duckbay) and a single Middle Missouri vessel. It is believed that the Middle Missouri vessel was imported since the paste and construction/decorative technology differ distinctively from that of all other vessels recovered from the site. It was on the basis of an examination of these surface finds that the decision to test the Lovstrom site was made. These test excavations were conducted during the summers of 1985 and 1986.
Field investigations through shovel tests, excavation units, and examination of rodent mounds, indicated that the cultural deposits at the Lovstrom locale extend approximately 500m north from the edge of the Souris channel and eastward for over two hundred meters from the escarpment along Jock’s Creek. The presence of dense forest vegetation covering much of the locale, and the subsurface nature of the archaeological deposits obscured surface indications.
Radiocarbon dates: Test Unit 4: 1215/320 BP and Test Unit 8 1280/190 BP
Scope and Content
Sub-series has been divided into sub sub series including: Lovstrom survey 1985 and Lovstrom survey 1986
Block A was the most southern site in the locale. The excavation block consisted of 12 contiguous 1m2 units dug in a 3m x 4m rectangle. The block was the least productive of cultural materials, and bone preservation was the poorest. Under the sod, the black loam layer appeared at 5 cm below surface, and the glacial clay at 25 cm below surface. Excavators described the soil matrix as gritty and silty, and it became concrete hard when dried.
The occupation or bone layer extended from 10 to 25 cm below surface and consisted of a contiguous scatter of FCR and unidentifiable large ungulate bone which was heavily processed and intensively scavenged by carnivores. Most cultural materials were recovered within this layer. Fire cracked rock (FCR) and small burnt bone fragments were present but no intact hearths or processing features were evident.
Non-cultural materials included limestone and other natural pebbles derived from the parent till. (These small limestone pebbles were apparent in the occupation layers in other blocks as well). Root and rodent disturbance was extensive throughout Block A. Most units were excavated to gravelly clay till. Nine of the twelve units were dug to level 4b, which ended at 40 cm b.s.
No further excavations were done at this site. No C14 dates were taken.
Scope and Content
Sub-sub-sub series contains: Summary information of field methology, number and co-ordinates of excavations, personnel and their staff position; Field journals are daily records of recoveries, features and activities at the site; Site records include excavation level and unit summaries, feature sheets, profiles; sample records and maps; Artifact catalogues are lists and identifications of all artifacts recovered; Photographs are of excavation units, features, the landscape and personnel.
Radiocarbon date reports have been scanned in multi-page PDF files.
History / Biographical
The North Lauder locale has a long archaeological and geological history that is important for understanding the forces that shaped the region. Archaeological research in the locale shows that the area has been occupied by humans for at least the past 6,500 years. Environmental forces provided an area of diverse resources that attracted early peoples.
Archaeologists from Brandon University have been conducting research in the North Lauder locale that has focused on the Atkinson site, a 6,500 year old hunter-gatherer site and Flintstone Hill.
The geomorphology of the glacial Lake Hind Basin over the past 11,000 years is known primarily through the study of a cut bank along the Souris River. Flintstone Hill contains the most complete stratigraphic record for the post-glacial period on the northern plains. The site has been extensively studied by geoarchaeologists, geologists and paleoenvironmentalists over many years and their findings have contributed to our understanding of the region.
Radiocarbon dates were obtained from the Atkinson site and Flintstone Hill.
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: the Atkinson site and Flintstone Hill.
Block C was situated in sparse oak forest with an understory of saskatoon, hazelnut and a thick ground cover of poison ivy and sarsaparilla. The block measured 3m and 3m and contained nine excavation units. All units were excavated to 35cm below surface. The soil horizons were much like the other blocks, except for a rusty brown stain in the first level, giving the upper black loam a mottled appearance. The brown patches were clay mixed with loam and were harder than the surrounding matrix. No definitive interpretation of these phenomena was attempted but this effect may be the result of natural brush or forest fires. Under the 5cm so d/humus (Ah) layer, the loam horizon extended approximately 5cm – 25 cm below surface, and averaged 20 cm thick. Bone was concentrated within this horizon between 10 cm – 20 cm below surface.
Block C was notable for its concentrations of articulated bison bone. Most noteworthy was an articulated unit composed of lumbar vertebrae, pelvis, and sacrum. Several thoracic vertebra/proximal rib end concentrations were also recovered. There were more vertebrae and rib sections recovered in the units in proportion to other bones. A few sherds, some debitage and a single Prairie Side-Notched point fragment were among the recoveries. Based on the quantity of bone, the density of the bone layer, and the articulated butchering units the area has been interpreted as a bone midden.
Faunal material was analysed by Jessica MacKenzie for her Honours Thesis: "A reconstruction of butchering processes in Block C from the Lovstrom site DjLx-1 in Southwestern Manitoba."
Radiocarbon date: 850/115BP XU 79.
Scope and Content
Sub-sub-sub series contains: Summary information of field methology, number and co-ordinates of excavations, personnel and their staff position; Field journals are daily records of recoveries, features and activities at the site; Site records include excavation level and unit summaries, feature sheets, profiles; sample records and maps; Artifact catalogues are lists and identifications of all artifacts recovered; Photographs are of excavation units, features, the landscape and personnel.
Block D was wooded with oak and an understory of saskatoon and hazelnut with a thick ground cover of poison ivy and sarsaparilla. Root and rodent disturbance was extensive.
Based on the recoveries from Test Unit 22 during the survey, further excavations were carried out. Two units 87 and 93 were excavated in 1987. A further four units were excavated in 1988. There appears to be a pre contact occupation and a protohistoric feature within the block.
Diagnostic lithics included a chert Plains Side-notch projectile point, and a large Woodland side-notched point. The lithic materials from Block D are primarily local cherts followed in abundance by Knife River Flint and Tongue River Silicified Sediment – both of which are exotics imported from the southwest. Faunal remains were primarily bison.
Thin-walled obliterated fabric impressed pottery with grit temper was recovered in all units. Diagnostic ceramics included two rims, one with a fabric impressed exterior and the lip notched with dowel impressions, and a second thick walled rim was fabric impressed to the lip. The ceramic wares appear to be essentially a Woodland complex with overtones of Plains influence.
RC date: 230/90 BP.
Scope and Content
Sub-series has been divided into sub sub series including: Lovstrom Block D 1987 and Lovstrom Block D 1988.
This site is situated in a naturally sheltered area with a low rise to the east and south partly encircling a flat area open to the west. Present natural vegetation is an open oak forest with a light understory of saskatoon, hazelnut, poison ivy and sarsaparilla. It is situated on the till plain at the upper end of a ravine leading to Jock’s Creek.
Two test units six meters apart were excavated in 1987 and produced cultural materials which warranted a block excavation, so seven contiguous 1m2 units were then opened. These units proved to be very productive of cultural remains. Subsequent excavations in 1988 increased the number of excavated units to 21. In 1991 a further eight units were excavated for a total of 29 excavations and two test units. Excavations went deeper in this block than in Blocks C or B. Remains from the block included bison bone, bone tools, fire-cracked rock, ceramics, lithics including tools and debitage and a hearth. Another occupation was recovered in 1991 containing a hearth and living floor.
Radiocarbon samples have produced two distinct sets of radiocarbon dates from 1987 and 1988 excavations. There appears to be two or possibly three cultural horizons definable within this block.
An upper cultural horizon, located between 14-21 cm below surface, contains large bison bone and fire-cracked rock dating to 465/100B.P from XU 128.
A lower horizon in the 20-25 cm level contained FCR, bison bone and lithic scatter that was dated to 675/70 B.P. from XU 122 and 715/110 from XU 114.
Scope and Content
Sub-series has been divided into sub sub series including: Lovstrom Block E 1987, Lovstrom Block E 1988 and Lovstrom Block E 1991.
Block B consisted of 20 contiguous 1m2 units excavated to 30 cm below surface. (except unit 58 which was excavated to 35 cm bs to obtain extended soil profile). The block is situated in recent oak and poplar forest at the head of a ravine leading to Jock’s Creek, adjacent to an area cleared for market gardening. As was the case with Block A, the understory is heavily overgrown with hazelnut, chokecherry, saskatoon, and a poison ivy/sarsaparilla ground cover.
The soil levels below the sod in Block B consisted of a black, silty, and gritty loam layer from 5 cm to 23 cm below surface, a yellow and sandy clay from 23 cm to 30 cm below surface, and glacial till at 30 cm below surface. As in Block A, limestone cobbles were found throughout the occupation level around the bone. It is evident that bioturbation – primarily tree roots and rodent burrowing – have significantly altered patterns of original deposition of lithics, ceramics and small bone.
The faunal layer lay close to the surface, situated entirely in the black loam 5 cm – 23 cm below surface. The 23 cm depth also marked the end of the dark silty loam. At 10 cm below surface, a discernible patterning of the bone appeared. Concentrations of bone in narrow rows ran in an irregular pattern from the northwest to the southeast part of the block. This pattern was most apparent in the north end of the block which is the highest point in the block. In the same 1m2 unit, patches of weathered, very poorly preserved bone would be found lying close to patches of well preserved bone. It is believed that this variability in preservation results from uneven rates of burial due to taphic activities of pocket gophers or other agents of bioturbation. The same pattern of uneven preservation occurs over much of the locale but is most evident in Block B.
Diagnostic lithics included eleven projectile points that were predominantly Plains or Prairie Side-notch types, but included two unnotched triangular points. Cord-wrapped impressed rim sherds and body sherds were recovered. The ceramics are variants of the Woodland Blackduck horizon.
RC dates: XU49 – 675/80 BP XU 59 – 705/75BP.
Scope and Content
Sub-sub-sub series contains: Summary information of field methology, number and co-ordinates of excavations, personnel and their staff position; Field journals are daily records of recoveries, features and activities at the site; Site records include excavation level and unit summaries, feature sheets, profiles; sample records and maps; Artifact catalogues are lists and identifications of all artifacts recovered; Photographs are of excavation units, features, the landscape and personnel.
In 1988 four 1m2 units were excavated in this Block F. The forest cover is identical to that of Block E, with an open oak forest with a light understory of saskatoon, hazelnut, poison ivy and sarsaparilla.
Underneath the litter mat (Ah) is a shallow, 15-20 cm “A” horizon of dark grey/brown silty loam with a high representation of pebble size clasts. The glacial clays, encountered at 20 cm below surface, consist of a matrix of light tan sandy clays containing rounded pebble to cobble size rocks.
The recoveries from this block consisted of a few ceramics, including Vickers Focus rim sherds, four lithic tools and a number of small bison bone fragments. There was no discernible cultural stratigraphy in the four 1m2 units and the limited deposits of bone, ceramics and lithics were dispersed randomly throughout the 25 cm of cultural matrix. The lithic materials frequencies were similar to those in Block E with local cherts and KRF being the most abundant categories. A small amount of fire-cracked rock and a few large identifiable bison bones were recovered – all distributed randomly with little evidence for any pattern of clustering.
No RC dates.
Scope and Content
Sub-sub-sub series contains: Summary information of field methology, number and co-ordinates of excavations, personnel and their staff position; Field journals are daily records of recoveries, features and activities at the site; Site records include excavation level and unit summaries, feature sheets, profiles; sample records and maps; Artifact catalogues are lists and identifications of all artifacts recovered; Photographs are of excavation units, features, the landscape and personnel.
In 1988 four units were excavated in Block G. The vegetation is similar to other areas in the locale with an open oak forest with a light understory of saskatoon, hazelnut, poison ivy and sarsaparilla.
Excavations recovered artifacts between 0 cm – 15 cm b.s. The cultural deposits are very shallow and it is quite possible that what appears to be a single occupation may in fact represent multiple occupation compressed deposits as a result of deflation or the lack of sedimentation in this raised area. This latter view is supported by the ceramics which appear to be a mixture of Blackduck and Vickers Focus wares.
The frequency and distribution of cultural material from block G contrasts with that of other sites in the locale. While the diagnostic materials are similar, the nature of the background debris and the associated lithic assemblage suggests that this area was utilized for a different set of activities.
Unlike Blocks E and H, there is very little in the way of ceramics, fire-cracked rock or bison bone, yet a significant amount of lithic debitage and six Plains/Prairie Side-notched projectile points were recovered. No unifaces or scrapers were recovered. This may be an area where activities such as manufacture and hafting of projectile points; hunting activities, butchering and refuse disposal took place.
No RC dates were taken.
Scope and Content
Sub-sub-sub series contains: Summary information of field methology, number and co-ordinates of excavations, personnel and their staff position; Field journals are daily records of recoveries, features and activities at the site; Site records include excavation level and unit summaries, feature sheets, profiles; sample records and maps; Artifact catalogues are lists and identifications of all artifacts recovered; Photographs are of excavation units, features, the landscape and personnel.
The vegetation in block H is similar to other areas in the locale with an open oak forest with a light understory of saskatoon, hazelnut, poison ivy and sarsaparilla.
The excavations of the eight 1m2 units in 1988 resulted in the recovery of over 650 ceramic fragments including 20 rim sherds from at least four vessels, a grooved maul, fire-cracked rock, lithic debitage and a reworked Avonlea projectile point. A large amount of bison bone, including a number of axial elements and a fragmented skull were also recovered.
Based on the 1988 recoveries at the site further excavations took place in 1991. Nine excavation units were opened next to the previous excavations. Another 250 ceramic sherds were recovered in 1991. Nine vessels have been identified based on rim sherds. Vickers Focus and Woodland vessels have been identified and two vessels similar to Scattered Village Complex were recovered.
The lithic material assemblage is intermediate between Blocks G and E with KRF being the most frequent material category followed by local cherts.
Two features, a hearth and a curvilinear arrangement of rock were recovered. The high numbers of ceramic fragments suggests a habitation area, rather than hunting or butchering behavior. However, the separation of occupations at the site is difficult to establish and there may be different uses of the site by successive occupations.
Radiocarbon dates from this block indicate two occupations separated in time by some 300 years. XU 181 – 405/110 BP and XU 184 – 780/110 BP.
Scope and Content
Sub-series has been divided into sub sub series including: Lovstrom Block H 1988 and Lovstrom Block H 1991.
The A.E. McKenzie Seed Co. Ltd. originated with the McKenzie family Flour, Grain and Seed business, started by F. B. McKenzie in the early 1880's. When F. B. McKenzie passed away in 1896, his son, Albert Edward McKenzie, assumed control of the company, and renamed it The Brandon Seed House. With its main office and plant in Brandon, Manitoba, the company specialized in the production and sale of field seeds and service exclusively to seed buyers in the prairie provinces and British Columbia. In later years, a complete line of products including garden seeds, lawn grass, and other allied lines was developed for sale across Canada.
In 1906, the company underwent a change of name when A. E. delete determined that the growth of the country demanded a larger seed institute than could be managed by one man. As a result, the company was incorporated under provincial statutes and the federal Joint Stock Companies Act as A. E. McKenzie Seed Co. Ltd., and new personnel were hired.
Under the Joint Stock Companies Act, A.E. McKenzie Seed Co. Ltd. was required to elect a Board of Directors of not less than three, and not more than nine individuals. Only shareholders of the company were eligible for election, and election was to take place yearly with each shareholder entitled to as many votes as shares owned in the company. The Act also dictated that the directors were, from time to time, to elect from among themselves, a president of the company. They were also able to appoint and remove all other officers of the company and to create company by-laws. The directors were not obliged to pay any dividend on shares if the company should became insolvent. Under the Act, the stock of the company was deemed a personal estate and was only transferable as such. In addition, the company could acquire, hold, and transfer real estate, and was required to submit annual statements.
A. E. McKenzie was elected President of the newly constituted company. For the memaninder of his natural life he remained in this position and supervised the operation of the company. S. A. Bradford, who was given responsibility for various company departments, filled the position of General Manager. H. L. Patmore became the Vice-President, overseeing the nursery business, while W. A. McCracken was put in charge of the warehouse stock, and shipping department. McCracken also supervised the mail order department.
The Company was intially comprised of three divisions: The Brandon Seed House, Brandon Nurseries, and Brandon Greenhouses. Each division was registered under Dominion Patents. Later, the company was divided into Retail Mail Order, Wholesale and Commission Packet Trade divisions. It also undertook some export business.
By registering the divisions of the company under under federal legislation affecting trademarks and industrial designs, McKenzie and the Board,were able to register both the company’s trademarks and to protect the company’s industrial techniques. Thet company could thus patent the methods and processes of its operations so that no other individual or business could duplicate them.
Located at 30 9th Street, the head office and plant of A.E. McKenzie Seed Co. Ltd. housed all the facilities and staff of the company, with the exception of the regional sales offices and warehouses. The business of the A. E. McKenzie Co. Ltd. was conducted from a frame warehouse until the current McKenzie building was constructed on the same site after a fire destroyed the original premises. Designed by architect Thomas Sinclair, and built by the Brandon Construction Company, the new building opened in 1911. In time, The A. E. McKenzie Co. Ltd. came to be known as Western Canada's Greatest Seed House.
During the 1930's, before a new building was erected in 1945, the A. E. McKenzie Co. occupied space at five different locations in Brandon, including the Massey Harris Building, the International Harvester Building and the Security Building. The last of these premises was destroyed by fire in 1972. As a result of its proximity to the Security Building, the main McKenzie Building also suffered heavy fire and water damage. A. E.
McKenzie Co. Ltd. also utilized a warehouse on the north side of Pacific Avenue alongside the Canadian Pacific Railway tracks between 5th and 6th streets. This building and its contents were destroyed by fire (1946). In May of 1949, the company purchased and erected a Quonset structure on the west side of 15th Street between Rosser and Pacific Avenues.
In 1908, the first branch of the A. E. McKenzie Seed Co. Ltd. was established at Calgary. In the following sixteen years, additional branches were established in Edmonton and Saskatoon (1923), Moose Jaw, Toronto (1934) and Winnipeg (1935). Both the Edmonton and Saskatoon branches were seasonal, operating for a four-month period, March to June inclusive. Business in the Maritime Provinces of Prince Edward Island, Nova Scotia and New Brunswick further extended the company's operations by the mid 1940's. In 1946, the company purchased property in Gilbert Plains, Manitoba, 120 miles north of Brandon. This purchase enabled the company to handle larger quantities of Sweet Clover, a popular crop that was grown in the surrounding area. Additional offices were opened in Vancouver and Quebec City in rented premises by the early 1960's.
In the years 1944-1945, the McKenzie Foundation was created. Through the Foundation, arrangements were put in place to transfer shares of the company to the Manitoba Government for the benefit of higher education, specifically Brandon College. In return for this gift, which included 90% of all capital resources of the company together with all of the income earned each year, except for the amount retained annually to ensure sufficient operating capital, the A.E. McKenzie Co. Ltd. received exemption from paying Corporate Tax.
Prior to the establishment of the McKenzie Foundation, in 1945, the National Trust for the benefit of the College held the shares of McKenzie Seeds. On April 7, 1945 the Manitoba Legislature passed legislation whereby A. E. McKenzie retained effective management control of his company, but 1031 shares out of 1145 issued shares were gifted to the Provincial Government. In return, the government agreed that all financial benefits from the shares would go to Brandon College through the A. E. McKenzie Foundation. When Mr. McKenzie passed away in 1964, the primary responsibility of appointing the Board of Directors for McKenzie Seeds passed to the Provincial government.
The remaining 114 shares of the Company were turned over to the Crown on July 16, 1975 in accordance with an agreement between Brandon University, A. E. McKenzie Co. Ltd. and the Manitoba government. The same agreement also turned the McKenzie Foundation over to Brandon University. Therefore, since 1975 the crown has held all shares of the McKenzie Co. through the Province of Manitoba.
A.E. McKenzie died on September 25, 1964 at the age of 94 and was succeeded as President of the company by J. Lasby Lowes. When Mr. Lowes retired in 1968, A. R. Swanson was appointed by the government to fill the position and was responsible for all operations of the company under a Board of Directors comprised mainly of appointees of the government. It has proven impossible to establish a complete list of those individuals who held the positions of President/General Manager of McKenzie Seeds after 1964. A partial account is as follows: Anthony J. Maruca became President of A. E. McKenzie Co. Ltd. in 1972. In 1975, the Board of Directors appointed William Moore General Manager, creating a new position to relieve the President of the company from management of plant operations. At the same time, Pat Kelleher was named new interim President. Following the resignation of Kelleher, William Moore assumed the role of President as well. Moore left the company in the early 1980s. He was later convicted of criminal misconduct as President of the company. Keith Guelpa became President/General Manager in the mid 1980's; Raymond West was his successor.
Beginning in 1969, the A. E. McKenzie Seed Co. Ltd. began phasing out the Field Seed division of their company, including business related to forage crops and cereals. Seed cleaning equipment located in Brandon and and the company’s Calgary and Toronto cleaning plants was sold. The Company concentration its resources on the production and sale of vegetable and flower seeds, and lawn and turf grasses. It acted as a wholesaler and conducted business through chain stores, grocery, hardware and general stores.
Late in 1971, A. E. McKenzie Co. Ltd. purchased its largest competition in packaged seeds - Steele Briggs Seed Co. from Maple Leaf Mills Inc. for two million dollars. At the time of the acquisition the company changed its name to A. E. McKenzie Co. - Steele Briggs Seeds, in order to benefit from the favorable reputation held by Steele Briggs Seeds across Canada. In the early 1970s, the acquisition of Brett-Young Seeds Ltd., a Winnipeg company that dealt exclusively in the production and sale of field seed, brought the A. E. McKenzie Co. back into the field seed market.
In 1994 the Manitoba Government sold the A.E. McKenzie Seed Co. Ltd. to Regal Greetings and Gifts, Canada's largest non-retail mail-order catalogue company, which is owned by MDC Corporation of Toronto.
In 2001, McKenzie Seeds is Canada's leading supplier of packaged seeds and related gardening products. It is divided into a Retail Consumer Products division which features well known seed brands including McKenzie Seeds, Pike Seeds and Thompson & Morgan Seeds from England. As well, this division also carries a complete range of lawn seeds and perishables. It also continues to ship the seed racks invented by A.E. McKenzie to numerous retail stores. The second division, Direct Mail, consists of the McFayden and McConnell catalogues which reach over 500,000 Canadian homes each year.
Custodial History
Following the sale of the A.E. McKenzie Seed Co. Ltd. to Regal Greetings and Gifts, the records of McKenzie Seeds and its subsidiaries were retained in the McKenzie Plant on 9th Street. In April of 1997, the records were transferred to the McKee Archives at Brandon University. Because the company was a crown corporation, the records of McKenzie Seeds belonged to the Province of Manitoba and might have been placed in the Provincial Archives. However, Provincial Archivist Gordon Dodds permitted the retention of the records in Brandon at the S. J. McKee Archives. The minutes of the Board of Directors, previously transferred to the Provincial Archives, remain in Winnipeg. Until 1960 these minutes, by-laws of the Company, and the letters patent of incorporation (April 7, 1906) were in the possession of the Company's lawyers, Johnson, Garson, Forrester, Davidson, & Steen.
Scope and Content
The fonds consists of textual records, photographs and artifacts from A.E. McKenzie Seed Co. Ltd. The textual records include minutes, documents, financial records, administrative records, by-laws, legal records, catalogues, sales literature, seed packets, newspaper clippings, appraisals, publications, scrapbooks and miscellaneous sections.
In addition, some of the records within the fonds relate to the operations of McKenzie subsidiaries -- Brett-Young Seeds, Steele-Briggs Seeds, Pike & Co. and McFayden Seeds -- and various properties owned by McKenzie Seeds.
Fonds contains approximately 500 photographs. These depict the operations and employees of McKenzie Seeds and the seed industry in general. Artifacts contained in the fonds include blueprints, newspaper clippings, copper printing plates, seed bags and plaques.
Fonds also includes an artificially created series of records dealing with Brandon College Inc., the A.E. McKenzie Foundation, the Brandon Allied Arts Council and the Brandon Board of Trade. These records stand outside the provenance of the McKenzie Seed Co.
Of particular interest within the textual records are the transcripts of various features of the company's history as dictated, researched and recalled by its second President/General Manager, J. Lasby Lowes. The fonds also contains a collection of company catalogue which is almost complete. Outside of the seed industry, the records dealing with both Brandon College Inc. and the McKenzie Foundation are significant records relating to the history of Brandon College/University and the City of Brandon.
Because the A.E. McKenzie Seed Co. Ltd. was a crown corporation, the records in the fonds are subject to the Freedom of Information and Protection of Privacy Act (FIPPA).
Storage Location
RG 3 A.E. McKenzie Company fonds
Related Material
Additional records regarding A.E. McKenzie Seed Co. Ltd. are housed at the Provincial Archives of Manitoba. In order to gain access to these records it is necessary to contact the Archives of Manitoba.
Arrangement
RG 3 A.E. McKenzie Seed Co. Ltd. Fonds
McS 1 Board of Directors
1.1 Documents
1.2 Minutes/Meetings
1.3 Management Consultant Reports
1.4 Miscellaneous
1.5 Financial Records
McS 2 Office of the President/General Manager
2.1 A.E. McKenzie
2.2 J. Lasby Lowes
2.3 Comptroller
2.4 Properties
2.5 Marketing
2.6 Reference Library
2.7 Miscellaneous Publications/Correspondence
McS 3 Acquisitions
3.1 Brett-Young Seeds/Sabetha
3.2 Steele-Briggs Seed Co.
3.3 Pike & Co.
3.4 McFayden Seeds
McS 4 Seed Marketing Co.
McS 5 Photographs
5.1 McKenzie Seed Co. Ltd. Executives
5.2 Construction at McKenzie Seed Co. Brandon (two files)
5.3 Exterior Photographs of the A. E. McKenzie Co. Building
5.4 McKenzie Seed Co. Plant Operations and Workers (2 files)
5.5 McKenzie Seed Co. Equipment and Plant - Head Office 1983
5.6 McKenzie Seed Co. Field Operations and Workers
5.7 McKenzie Seed Co. Strike 1944
5.8 Fires at McKenzie Seed Co. 1910, 1945, 1972
5.9 McKenzie Seed Co. Centennial Exhibition 1996
5.10 Miscellaneous McKenzie Seed Co. Photographs
5.11 People Connected to McKenzie Seed Co.
5.12 Princess Anne's Visit to McKenzie Seed Co. 1982
5.13 Onion Set Production Book
5.14 Irene Cullen Photographs - McKenzie Seeds Employee Photos
5.15 Josiph Airey Photographs - McKenzie Product Photos
5.16 Alan R. Mundie Seed Production Photographs
5.17 Steele Robertson/Steele Briggs Seeds Photographs
5.18 Seed Packet Display Units Photographs
5.19 Product Photographs
5.20 Parade Photographs
5.21 Oversized Photographs
5.21.1 Drawer #1: Executive Photographs
5.21.2 Drawer #2: Office and Equipment/Plant Photographs
5.21.3 Drawer #3: Miscellaneous Oversized Photographs
5.21.4 Drawer #4: Artifacts
McS 6 Miscellaneous
6.1 Centennial Exhibition
6.2 Miscellaneous Publications
6.3 Scrapbooks
MG 1 A.E. McKenzie Fonds
1.1 Brandon College Inc.
1.2 McKenzie Foundation
1.3 Brandon Allied Arts Council
1.4 Brandon Board of Trade
1.5 Miscellaneous
