The Abrigo Pozo Cavado site, Puna of Salta. New archaeological and chronological contributions to the study of processes of change from the end of the Middle Holocene (ca. 5600-4600 years BP)
This paper analyzes and discusses new archaeological and chronological data at the end of the Middle Holocene (ca. 5600-4600 years BP) from the Abrigo Pozo Cavado site. This site is located in the Salar de Pocitos, Puna of Salta, at an altitude of 3700 masl. The archaeofaunal record presents an abso...
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Facultad de Filosofía y Humanidades. Museo de Antropología
2017
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Acceso en línea: | https://revistas.unc.edu.ar/index.php/antropologia/article/view/12735 |
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I10-R372-article-127352024-11-04T18:45:52Z The Abrigo Pozo Cavado site, Puna of Salta. New archaeological and chronological contributions to the study of processes of change from the end of the Middle Holocene (ca. 5600-4600 years BP) El sitio Abrigo Pozo Cavado, Puna de Salta. Nuevo aporte arqueológico y cronológico para el estudio de procesos de cambio hacia finales del Holoceno medio (ca. 5600-4600 años AP) López, Gabriel E. J. Orsi, Juan Pablo Holoceno medio procesos de cambio Puna de Salta Middle Holocene processes of change Puna of Salta This paper analyzes and discusses new archaeological and chronological data at the end of the Middle Holocene (ca. 5600-4600 years BP) from the Abrigo Pozo Cavado site. This site is located in the Salar de Pocitos, Puna of Salta, at an altitude of 3700 masl. The archaeofaunal record presents an absolute predominance of Camelidae, yet variability in osteometric data indicates different species of this family. The lithic material has diverse morphologies of projectile points and raw materials, including allochthonous obsidian. Finally, the presence of shell beads is also reported. Este trabajo analiza y discute nueva información arqueológica y cronológica del sitio Abrigo Pozo Cavado correspondiente a finales del Holoceno medio (ca. 5600-4600 años AP). Este sitio se ubica en el Salar de Pocitos, Puna de Salta, a una altura de 3700 msnm. El registro arqueofaunístico indica una predominancia absoluta de los Camelidae pero con variabilidad osteométrica relacionada con la presencia de distintas especies de esta familia. El material lítico registra distintas morfologías de puntas de proyectil y materias primas, entre ellas, obsidianas alóctonas. Por último, se destaca la presencia de cuentas de valva. Facultad de Filosofía y Humanidades. Museo de Antropología 2017-06-30 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer reviewed article Artículo revisado por pares investigación básica Artigo revisado por pares application/pdf https://revistas.unc.edu.ar/index.php/antropologia/article/view/12735 10.31048/1852.4826.v10.n1.12735 Revista del Museo de Antropología; Vol. 10 No. 1 (2017); 43-48 Revista del Museo de Antropología; Vol. 10 Núm. 1 (2017); 43-48 Revista del Museo de Antropología; v. 10 n. 1 (2017); 43-48 1852-4826 1852-060X 10.31048/1852.4826.v10.n1 spa https://revistas.unc.edu.ar/index.php/antropologia/article/view/12735/17216 Derechos de autor 2017 Gabriel E. J. López, Juan Pablo Orsi |
institution |
Universidad Nacional de Córdoba |
institution_str |
I-10 |
repository_str |
R-372 |
container_title_str |
Revista del Museo de Antropología |
language |
Español |
format |
Artículo revista |
topic |
Holoceno medio procesos de cambio Puna de Salta Middle Holocene processes of change Puna of Salta |
spellingShingle |
Holoceno medio procesos de cambio Puna de Salta Middle Holocene processes of change Puna of Salta López, Gabriel E. J. Orsi, Juan Pablo The Abrigo Pozo Cavado site, Puna of Salta. New archaeological and chronological contributions to the study of processes of change from the end of the Middle Holocene (ca. 5600-4600 years BP) |
topic_facet |
Holoceno medio procesos de cambio Puna de Salta Middle Holocene processes of change Puna of Salta |
author |
López, Gabriel E. J. Orsi, Juan Pablo |
author_facet |
López, Gabriel E. J. Orsi, Juan Pablo |
author_sort |
López, Gabriel E. J. |
title |
The Abrigo Pozo Cavado site, Puna of Salta. New archaeological and chronological contributions to the study of processes of change from the end of the Middle Holocene (ca. 5600-4600 years BP) |
title_short |
The Abrigo Pozo Cavado site, Puna of Salta. New archaeological and chronological contributions to the study of processes of change from the end of the Middle Holocene (ca. 5600-4600 years BP) |
title_full |
The Abrigo Pozo Cavado site, Puna of Salta. New archaeological and chronological contributions to the study of processes of change from the end of the Middle Holocene (ca. 5600-4600 years BP) |
title_fullStr |
The Abrigo Pozo Cavado site, Puna of Salta. New archaeological and chronological contributions to the study of processes of change from the end of the Middle Holocene (ca. 5600-4600 years BP) |
title_full_unstemmed |
The Abrigo Pozo Cavado site, Puna of Salta. New archaeological and chronological contributions to the study of processes of change from the end of the Middle Holocene (ca. 5600-4600 years BP) |
title_sort |
abrigo pozo cavado site, puna of salta. new archaeological and chronological contributions to the study of processes of change from the end of the middle holocene (ca. 5600-4600 years bp) |
description |
This paper analyzes and discusses new archaeological and chronological data at the end of the Middle Holocene (ca. 5600-4600 years BP) from the Abrigo Pozo Cavado site. This site is located in the Salar de Pocitos, Puna of Salta, at an altitude of 3700 masl. The archaeofaunal record presents an absolute predominance of Camelidae, yet variability in osteometric data indicates different species of this family. The lithic material has diverse morphologies of projectile points and raw materials, including allochthonous obsidian. Finally, the presence of shell beads is also reported. |
publisher |
Facultad de Filosofía y Humanidades. Museo de Antropología |
publishDate |
2017 |
url |
https://revistas.unc.edu.ar/index.php/antropologia/article/view/12735 |
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first_indexed |
2024-09-03T20:00:53Z |
last_indexed |
2025-03-27T05:32:17Z |
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