@article {12542,
	title = {Framing Questions that Count in African Canadian Archaeology},
	journal = {Canadian Journal of Archaeology/Journal canadien d{\textquoteright}arch{\'e}ologie},
	volume = {43},
	year = {2019},
	pages = {217-241},
	abstract = {<p>The archaeological investigation of African life in Europe{\textquoteright}s New World has been a major focus of much historical archaeology for decades. Canadian historical archaeologists, except for a number in Nova Scotia, generally have not pursued this line of research. This paper offers a brief history of African Diaspora archaeology, provides an overview of the research in Nova Scotia, and presents three topics amenable to further research in African Canada.</p>},
	author = {Charles E. Orser, Jr.}
}
@article {11244,
	title = {Geochemistry of Pre-Contact Potsherds from Southern Mainland Nova Scotia: Constraints on Pottery Pathways},
	journal = {Canadian Journal of Archaeology/Journal canadien d{\textquoteright}arch{\'e}ologie},
	volume = {40},
	year = {2016},
	pages = {231-267},
	abstract = {<p>The mineralogy and bulk chemical compositions of 33 potsherds (14 shell-tempered, 19 grit-tempered) and local sediments (sand and clay, where present) from six pre-contact Mi{\textquoteright}kmaw sites across southern mainland Nova Scotia were determined, and are compared to samples from a long-used aboriginal site (BdDk-1) near the mouth of Bear River, in the Annapolis Basin. The immediate area around four of these sites (at Brighton, Port Joli, Wynacht Cove and Frost Fish Cove), all coastal, lack surface clay deposits, but good-quality clay is abundant in areas once overlain by glacial lakes. These include the two inland localities (at Enfield and Melanson) and the Annapolis Basin. Grit temper is dominated by the mineralogical constituents of biotite granodiorite found near Bear River. Muscovite is virtually absent, precluding the use of two-mica monzogranite as temper. The mineralogical criteria linking grit-tempered sherds to the Bear River area are supported by statistical analysis of bulk compositional data for the sample suite. Shell-tempered samples lack granodiorite clasts, so are compositionally distinct except where calcium-poor (i.e., contain little shell material). Those from Bear River overlap the compositions of shell-tempered samples from the sites along the Atlantic coast, suggesting a common origin. We postulate that pottery from the Annapolis Basin was distributed to other sites in the province via navigable waterways.</p>},
	author = {J. Victor Owen and John D. Greenough and Megan Himmelman and Stephen T. Powell}
}
@Book Reviews/Comptes-rendus {11941,
	title = {Integrative Approaches in Ceramic Petrography},
	volume = {42},
	year = {2018},
	pages = {279-282},
	editor = {Stanley Klassen}
}
