North Pacific Prehistory 2

 

Abstract

 

Late Pleistocene and Early Holocene Cultural Connections

between Asia and America

AIKENS, C. Melvin

ZHUSHCHIHOVSKAYA, Irina S.

 

 

North Pacific coastal environments from the Sea of Japan to Northern California were occupied in ethnographic times by cultures that were clearly linked all along the way through an array of technological and architectural similarities, as well as social practices and spiritual beliefs. Their communities were generally of considerable size and sociocultural complexity, the region as a whole being long noted by anthropologists as one where hunter-fisher-gatherers, so-called “Affluent Foragers,” achieved levels of sociocultural elaboration elsewhere reached only by agricultural peoples.  Initial connections along this coastal zone through migration and diffusion, first established in terminal Pleistocene times, continued through much of the Holocene.  These are documented most clearly in archaeological assemblages by distinctive prepared core-blade/microblade and biface technologies, but there are other shared elements as well.  Socioeconomic similarities and variations that owe much to habitat similarities and variations along the 6000 miles of North Pacific coastline are also clearly marked. Waterside adaptations seen along the central and southern California coasts reached comparable levels of cultural elaboration and complexity, but did not participate in the North Pacific coastal diffusion sphere that existed throughout most of Holocene times.  Rather, they arose convergently from an indigenous North American Archaic cultural base that was widespread in the western continental interior and dates back to earliest Holocene times. This review proceeds from the present to the past, beginning with the ethnographic picture and then working back through broad slices of time: 3000 to 6000 years ago, 6000 to 10,000 years ago, and before 10,000 years ago. It is suggested that the first people to enter North America were northeast Asians culturally adapted to the North Pacific coast and adjacent interior regions, who came during the waning phases of the last glaciation, probably around 14,000 years ago.

 

 

 

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