@Book Reviews/Comptes-rendus {9060,
	title = {{\textquoteright}Keeping the Lakes{\textquoteright} Way{\textquoteright}: Reburial and the Re-creation of a Moral World Among an Invisible People},
	volume = {27},
	year = {2003},
	pages = {112-116}
}
@Symposium Papers {10964,
	title = {The Early Component at Bear Cove},
	volume = {3},
	year = {1979},
	pages = {177-194}
}
@Conference Paper {10344,
	title = {The Nineteenth Century Archaeology of Harlan I. Smith in Southern British Columbia},
	year = {2000},
	address = {Ottawa},
	abstract = {Field letters and notes, photo scrapbooks, publications, and artifact collections of Harlan I. Smith from the American Museum of Natural History document the earliest archaeological expeditions to British Columbia. From a study of these records, the motivations, research questions, accomplishments, and relations with aboriginal peoples are revealed. Franz Boas largely dictated a biological approach to Smith{\textquoteright}s fieldwork, one that involved the collection of photographic portraitures and human skeletal remains; however Smith{\textquoteright}s published monographs from his expeditions focus on an analysis of the material culture of the Interior Salish peoples.}
}
@Conference Paper {10342,
	title = {A Place Where Chitons are Cooked: The Bear Cove Fauna in the Context of the Origins of Northwest Coast Maritime Culture},
	year = {1999},
	address = {Whitehorse, Yukon},
	abstract = {The Bear Cove site (EeSu 8) was excavated in 1978 on the northern end of Vancouver Island, British Columbia. The 8,200 B.P. stratigraphic sequence included shell midden and non-shell deposits, an early Pebble Tool Tradition artifact assemblage and later Developmental Northwest Coast artifact assemblages, radio-carbon dated samples (uncalibrated), and extensive faunal remains. This paper will present an overview of the hitherto unreported complete faunal assemblage from the early 8,020 B.P component to the later post-4,000 B.P. shell midden components of the site. The faunal data indicate a record of a fully marine-adapted culture that has focused on the sea for subsistence since early occupation.}
}
@Conference Paper {10340,
	title = {Glacial Lakes and Salmonids in the Southern Interior of British Columbia},
	year = {2001},
	address = {Banff},
	abstract = {Bony skeletons of salmon encased in clay nodules eroding from glacial lake sediments along Kamloops Lake, in the southern interior of British Columbia, have been AMS radiocarbon dated to 18,110+90 and 15,480+60 BP. These are the only known salmonid remains of Late Wisconsin age in the Pacific Northwest, and are significant in demonstrating the presence of salmon in the river drainages during the late glacial maximum. On the basis of morphological size of the specimens, and on measurement of the low delta C13 value in the bone (-22.2 o/oo and -23.8 o/oo), it is argued that these were probably landlocked Oncorhynchus nerka (the Kokanee form of sockeye salmon). An experimental study of the ancient salmon DNA on these specimens is presently underway and has promise for resolving the species determination issue. This paper will discuss the salmon specimens and their geological source with the purpose of reconstructing the paleozoogeography of salmon in the Pacific Northwest including the implications for early human subsistence and migration patterns. Also addressed are the questions of the extent and timing of glacial lakes and ice retreat, and drainage patterns, in the southern interior of British Columbia in the Late Wisconsin.}
}
