摘要：Este artigo é um resumo expandido da Dissertação de Mestrado, defendida por nós, em Março de 2007, na Universidade do vale do Rio dos Sinos – Unisinos. A posição geográfica da Planície Costeira Central é dos 30º 15’ aos 32º 15’ e 50º 15’ a 52º 05’. É uma área de formação geológica Quaternária com solo arenoso, vegetação rasteira sobre dunas e matas litorâneas, hidrografia composta de lagoas, laguna e arroios. Os sítios arqueológicos da tradição cerâmica Tupiguarani encontram-se, na sua maioria, erodidos sobre dunas (31), bem como nos “cerritos” (01), sambaquis marinhos (03) e lacustres (04), além dos de campo aberto (09) (Mentz Ribeiro, 1994-1998). Ao estabelecermos um quadro comparativo, obtivemos os seguintes resultados: O material encontrado na planície costeira central assemelha-se nas técnicas de confecção ao material encontrado no restante do Estado do Rio Grande do Sul, o material cerâmico tem como características principais a decoração predominante do corrugado. Abstract: This paper is an expanded abstract of our dissertation, concluded in March 2007; at the University of Vale do Rio dos Sinos – Unisinos. The geographical position of the central coastal plain is 30°15’ to 32°15’S and 50°15’ to 52°05’. It is an area of a Quaternary geological formation with sandy ground, underbrush, coastal forests; hydrography composed by lagoons, lakes and streams. The archaeological sites of the Tupiguarani pottery tradition are located, the most of then, eroded over dunes (31), as well the mounds called “cerritos” (01), marine shell mounds (03) and lagoon shell mounds (04) and open-field sites (09). To establish an analog framework, the results obtained were: The material found in the central coastal plain is similar in manufacture techniques to the material around the Rio Grande do Sul State. The main aspects of pottery are, predominantly, corrugated decoration.
其他摘要：This paper is an expanded abstract of our dissertation, concluded in March 2007; at the University of Vale do Rio dos Sinos – Unisinos. The geographical position of the central coastal plain is 30°15’ to 32°15’S and 50°15’ to 52°05’. It is an area of a Quaternary geological formation with sandy ground, underbrush, coastal forests; hydrography composed by lagoons, lakes and streams. The archaeological sites of the Tupiguarani pottery tradition are located, the most of then, eroded over dunes (31), as well the mounds called “cerritos” (01), marine shell mounds (03) and lagoon shell mounds (04) and open-field sites (09). To establish ananalog framework, the results obtained were: The material found in the central coastal plain is similar in manufacture techniques to the material around the Rio Grande do Sul State. The mainly aspects of pottery are, predominantly, corrugated decoration.
关键词：Arqueologia;Tradição Tupiguarani;Povoamento;Planície costeira central
