Wetlands and Emergent Horticultural Economies in the Upper Great Lakes: A New Perspective from the Schultz Site

2001 ◽  
Vol 66 (4) ◽  
pp. 615-632 ◽  
Author(s):  
William A. Lovis ◽  
Kathryn C. Egan-Bruhy ◽  
Beverley A. Smith ◽  
G. William Monaghan

The Schultz site (20SA2) is a benchmark site for understanding the Woodland adaptations of the Upper Great Lakes, although its older excavation data is not comparable with recent Eastern Woodlands research, which consistently uses fine-grained recovery techniques. The 1991 Schultz-site research collected supplementary and upgraded subsistence and environmental data to address questions about regional transformations from hunting and gathering to horticulture. In addition, questions regarding the role of aquatic and wetland resources, and how environmental change affected the availability and productivity of these alternative resources, were addressed. Results of faunal, floral, and geoarchaeological research reveal that Woodland economies in the Saginaw region of the Upper Great Lakes were keyed to environmental changes affecting wetland availability and productivity. The Early Woodland presence of cucurbits does not appear economically important until later when it is combined with more reliable supplementary food sources. Although chenopod is present during the Middle Woodland and early Late Woodland, wetland plant and animal resources act as surrogates for other starchy and oily seeded annuals common in other portions of the Midwest and in the Mid-South. Maize apparently does not achieve economic significance until the Late Woodland period. A model of this combined northern and southern strategy is developed.

2018 ◽  
Vol 55 (7) ◽  
pp. 863-885 ◽  
Author(s):  
Riley P.M. Mulligan ◽  
Carolyn H. Eyles ◽  
Andy F. Bajc

Analysis of 56 outcrop exposures in cut banks along the Nottawasaga River in southern Simcoe County, Ontario, Canada, has led to the identification of eight stratigraphic units (SU1–SU8) that represent a record of changing environmental conditions during deglaciation and exhibit strong controls on shallow groundwater flow in the region. The stratigraphic succession is floored by the Late Wisconsin Newmarket Till (SU1), which is locally overlain by ice-proximal debris flow deposits (SU2). These glacial sediments are overlain by glaciolacustrine silt rhythmites (SU3) that pass upwards into deltaic sand (SU4) and channelized fluviodeltaic sand and gravel (SU5). Lying above the fluvial deposits are widespread interbedded glaciolacustrine sands and silt (SU6), which coarsen up-section toward the ground surface. The succession is locally capped by fluviodeltaic (SU7) and younger fluvial (SU8) deposits. These SUs record sedimentary environments that existed during deglaciation of the region and provide insight into the evolution of glacial lakes Schomberg and Algonquin and the Nipissing phase of the upper Great Lakes. The environmental changes described from sediments along the Nottawasaga River provide insights into basin-scale events that occurred throughout the upper Great Lakes during deglaciation. Qualitative observations of groundwater discharge from sediments at outcrop faces are used to characterize the hydraulic function of the stratigraphic units as well as possible preferential groundwater flow pathways in the shallow subsurface.


1994 ◽  
Vol 14 (3) ◽  
pp. 245-285
Author(s):  
Paul A. Raber

Investigations at 36Ch161, a site in the Piedmont Uplands of Chester County, Pennsylvania, have revealed a series of early Late Woodland Period camps associated with the Minguannan Complex. The use of local quartz seems to have been a primary focus of settlement at the site. Quartz, which formed an overwhelming majority of the assemblage, was used in ways that contrast strongly with that of non-local materials like jasper, a minority component of the assemblage obtained from quarries in the Hardyston Formation. The selection of raw materials suggests restrictions on access to certain materials perhaps imposed by territorial constraints. The combined evidence of artifact assemblage and cultural features indicates that 36Ch161 was inhabited seasonally by small, mobile groups of non-horticulturalists, a reconstruction consistent with that of Custer and others regarding the economy of the Minguannan Complex and related cultures of the Piedmont Uplands.


2020 ◽  
Author(s):  
J. Elmo Rawling ◽  
◽  
Lucas Zoet ◽  
Ethan J. Theuerkauf ◽  
Paul Hanson ◽  
...  

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