Life and death at Paloma: society and mortuary practices in by Jeffrey Quilter

By Jeffrey Quilter

Lifestyles and loss of life at Paloma, whilst released in 1989, used to be the 1st in-depth therapy of burials from a preagricultural South American village. It is still a important source utilized by scholars and students of Andean archaeology. Jeffrey Quilter analyzes the lifetime of Paloma's humans throughout the transition from a hunting-gathering-fishing lifestyle to a extra sedentary horticultural society and gives a learn of preceramic Peruvian existence via his research of this site's graves and their contents.

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Extra resources for Life and death at Paloma: society and mortuary practices in a preceramic Peruvian village

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The walking habits of the people of Paloma are, of course, unknown. Page 11 Midden deposits vary in thickness across the site. More than a dozen surface shell concentrations appear slightly to overlap the clusters of houses and burials, which are often under relatively light deposits of shell, although subsurface materials are fairly continuous throughout the area. The largest of the shell concentrations is Unit I, occupying approximately 6500 square meters. The thickness of its midden deposits ranges from a few centimeters at its southern limits to over a meter slightly north of its center.

Benfer (NSF BNS-76-12316, NSF BNS-78-07727a/b, and NSF BNS-81053940). Page xiii Preface One of the hallmarks of Precolumbian Peru is its many well-preserved and elaborate burials. In the postconquest period, the mummies of the Inca attracted the attention of the Spanish because of the reverence and wealth accorded the dead rulers. , Donnan and Mackey 1978). ) have been conducted. , when pottery was already used in some parts of Peru. Although detailed studies have recently been made on early burials in northern Chile (Allison and Gerszten 1982; Allison 1985; cf.

Every year, at the beginning of the austral summer, the warmer northern current overrides the Peru Current and pushes southward, but usually not very far. Sometimes the warm waters displace the Peru Current much further south than normal, down to the central coast. This disrupts the food chain. Phytoplankton are not available, so fish and seabirds migrate if they can; others die in droves, as do sea lions and mollusks. Sometimes torrential rains crash onto the central and north coasts, while drought occurs in the southern highlands due to the deprivation of the moisture normally brought to the area by the sea breezes.

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