M
Mary C. Stiner
Researcher at University of Arizona
Publications - 109
Citations - 9989
Mary C. Stiner is an academic researcher from University of Arizona. The author has contributed to research in topics: Upper Paleolithic & Cave. The author has an hindex of 48, co-authored 105 publications receiving 9185 citations. Previous affiliations of Mary C. Stiner include Loyola University Chicago & Hebrew University of Jerusalem.
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Differential Burning, Recrystallization, and Fragmentation of Archaeological Bone
TL;DR: In this paper, the conditions under which progressive levels of burning may occur to archaeological bone, and how burning damage changes bones' crystal structure and susceptibility to fragmentation (a.k.a. friability).
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The Tortoise and the Hare. Small-Game Use, the Broad-Spectrum Revolution, and Paleolithic Demography.
TL;DR: Ranking small prey in terms of work of capture (in the absence of special harvesting tools) proved far more effective in this investigation of human diet breadth than have the taxonomic-diversity analyses published previously.
Book
Honor among thieves : a zooarchaeological study of Neandertal ecology
TL;DR: In this article, the authors used ecological niche theory to analyze and interpret several Middle Palaeolithic archaeological and palaeontological sites in southern Europe and found that Neandertals were in direct and successful competition with lions, hyenas and wolves, but ended the period in unsuccessful struggle for the ecological niche.
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Paleolithic population growth pulses evidenced by small animal exploitation
TL;DR: Variations in small game hunting along the northern and eastern rims of the Mediterranean Sea and results from predator-prey simulation modeling indicate that human population densities increased abruptly during the late Middle Paleolithic and again during the Upper and Epi-Paleolithic periods.
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Thirty years on the "broad spectrum revolution" and paleolithic demography.
TL;DR: It is argued that subsistence diversification, mainly by adding new species to the diet, raised the carrying capacity of an environment increasingly constrained by climate instability at the end of the Pleistocene.