Contributors: Universidad Nacional Autónoma de México = National Autonomous University of Mexico (UNAM); Instituto Nacional de Antropologia e Historia Mexico (INAH-Mexico); Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE); Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)); Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA); Climat et Magnétisme (CLIMAG); Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)); Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE); Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE); Assiut University; 273564 Universidad Nacional Autónoma de México, UNAM; We thank the financial support for the research project DGAPA-PAPIIT-UNAM IN113117 to LA. We also thank the ANR-CONACyT 273564 to MP and LA (France-Mexico). AN Mahgoub and A Rodríguez-Trejo acknowledged the financial support of the Universidad Nacional Autónoma de México-postdoctoral fellowship at Geophysics Institute-UNAM, CDMX and Centro de Geociencias-UNAM, Querétaro, México, respectively. We thank the staff of the BCCT-UNAM (head, Saúl Armendariz) for their technical assistance.; We thank the financial support for the research project DGAPA-PAPIIT-UNAM IN113117 to LA. We also thank the ANR-CONACyT 273564 to MP and LA (France-Mexico). AN Mahgoub and A Rodr?guez-Trejo acknowledged the financial support of the Universidad Nacional Aut?noma de M?xico-postdoctoral fellowship at Geophysics Institute-UNAM, CDMX and Centro de Geociencias-UNAM, Quer?taro, M?xico, respectively. We thank the staff of the BCCT-UNAM (head, Sa?l Armendariz) for their technical assistance.
Abstract: International audience ; Casas Grandes is a prehistoric culture area located between Chihuahua, northern Mexico, and New Mexico, southwest of United States of America. It had an intense occupation with large buildings during the ceramic period, from 0 to 1450 CE, developing very particular painted potteries. In this study, magnetic properties and archaeointensity experiments were investigated on two special ceramic types called Mimbres and polychrome Ramos. They come from four archaeological sites from Casas Grandes region in northern Chihuahua: Paquimé, Villa Ahumada, Galeana, and Samalayuca. Archaeological timing and typology assign Mimbres and Ramos to an age period between 900 and 1450 CE, but no absolute ages are available. Magnetic properties show that Mimbres and Ramos have different magnetomineralogical properties, suggesting that pottery making materials were different. Mean archaeointensity results were obtained from nine different pottery sherds, five from Mimbres and four from Ramos polychrome, for a total of 35 specimens. Intensity value range from 49 to 59 µT for Mimbres type and from 41 to 49 µT for Ramos type. Archaeomagnetic dating was performed using the SHAWQ2k global model and the Maghoub regional paleosecular variation curve. Archaeomagnetic dating give an absolute age range of 960–1100 CE for Mimbres type, and of 1300–1600 CE for Ramos samples, confirming that both ceramic types were manufactured at different times. These results highlight the potential of archaeomagnetism to precise the chronological framework of Casas Grandes culture.
No Comments.