scholarly journals Radiocarbon Dating of Underwater Archaeological Objects from the Nevado de Toluca, Mexico

Radiocarbon ◽  
2017 ◽  
Vol 59 (6) ◽  
pp. 1705-1712 ◽  
Author(s):  
M A Martínez-Carrillo ◽  
C Solís ◽  
I Hernández Bautista ◽  
R Junco Sánchez ◽  
M Rodríguez-Ceja ◽  
...  

ABSTRACTThe Nevado de Toluca is a stratovolcano located in the southwest of the Toluca Valley in central Mexico. At a height of around 4200 m there are two crater lakes: El Sol and La Luna. Since Precolumbian times, people in the surrounding valleys carried out rituals and deposited offerings into the lakes. After the Spanish conquest, these rituals were kept alive clandestinely. Currently, reminiscent of Mesoamerican rituals subsist. Due to the long duration of the ritual at the Nevado de Toluca, it is important to date the materials recovered in the underwater and terrestrial archaeological explorations. This article proposes a chronology of Prehispanic ritual activities performed in the Nevado de Toluca based on the characterization and radiocarbon (14C) dating performed to materials from the volcano’s lakes.

Ethnohistory ◽  
2020 ◽  
Vol 67 (2) ◽  
pp. 289-315
Author(s):  
Amos Megged

Abstract While earlier census studies yielded population data mainly for the Tepetlaoztoc and Morelos regions of central Mexico during the 1530s and 1540s, this ethnohistoric study, based on a newly discovered manuscript, sheds light on household types and population density in the town of Zinacantepec by 1574. By comparing population figures, household types, and migration patterns, this article reconsiders how Aztec invasion, and thereafter the Spanish conquest, affected population movements and stability in the Valley of Toluca, a former Aztec stronghold in central Mexico. Furthermore, the nature of Toluca Valley habitats may prompt us to rethink about how we interpret the nature of indigenous demographic layouts before and after the Spanish conquest, whether its features be urban or rural.


2015 ◽  
Vol 32 (2) ◽  
pp. 109-116 ◽  
Author(s):  
Krystyna Szeroczyńska ◽  
Edyta Zawisza ◽  
Marta Wojewódka

Abstract The objective of this study was the recognition and reconstruction of the origin of two high altitude lakes and the ecological conditions of their early existence based on subfossil Cladocera and chemical analyses. The study focused on the oldest lacustrine sediments from Lake Sol and Lake Luna, located in the crater of Volcano Nevado de Toluca (Central Mexico). The Nevado de Toluca crater developed approximately 12 ka yr BP. According to the literature, the volcano was last active approximately 3.3 ka yr BP, and the lakes developed after that eruption. The remains of nine Cladocera species were found in the bottom sediments of both lakes. The most dominant taxa were two endemic littoral species: Alona manueli and Iliocryptus nevadensis. The total frequency of Cladocera specimens in both of the sediment cores was very low. No Cladocera remains were recorded in the sediment layer at depths between 123–103 m from Lake Luna. The results of the lithological and geochemical analyses showed that this sediment layer was composed of allochthonous material, probably originating from slid down from the volcanic cone. This was suggested by the content of silica (up to 13%), iron (up to 12%), and titanium (up to 4%). The Cladocera remains recorded in the bottom sediments suggested that both reservoirs developed as freshwater lakes at the beginning of the sedimentation. The calibrated radiocarbon dates obtained for the bottom samples were 4040 to 3990 yr BP for Lake Luna (129 cm) and 4485 to 4485 yr BP for Lake Sol (89 cm). The obtained ages were older than the dates of the last eruption, which occurred approximately 3300 yr BP. This result was likely related to the type of radiocarbon dated materials (charcoals).


Diversity ◽  
2022 ◽  
Vol 14 (1) ◽  
pp. 42
Author(s):  
Estela Cuna ◽  
Javier Alcocer ◽  
Martha Gaytán ◽  
Margarita Caballero

Lakes El Sol and La Luna, inside the crater of the Nevado de Toluca volcano, Central Mexico, are the only two perennial high mountain lakes [HML] in the country. HML are considered among the most comparable ecosystems worldwide. These lakes are “extreme” environments with diluted, oligotrophic, and cold waters exposed to high UV radiation doses. In this paper, we document the phytoplankton species inhabiting these two extreme tropical ecosystems. The phytoplankton diversity of Lakes El Sol and La Luna is low compared to the global phytoplankton diversity from other Mexican inland waters. Nonetheless, the phytoplankton diversity turned out to be high compared to other HML worldwide, both temperate and tropical. The phytoplankton community in Lake El Sol was formed by 92 morphospecies and in Lake La Luna by 63; in both, the most diverse groups were Bacillariophyceae and Chlorophyceae. All species found in Lake La Luna were present in Lake El Sol, but 29 species present in Lake El Sol were absent in Lake La Luna. Nevertheless, 57% of the most frequent and abundant taxa in Lake El Sol were rare in La Luna, and 47% of the most frequent and abundant taxa in Lake La Luna were rare in Lake El Sol. Associated with their shallowness and polymictic thermal pattern, 87.5% of the Bacillariophyceae morphospecies are tychoplantonic, while the remaining 12.5% are truly planktonic. Dominant taxa were Chlorophyceae in Lake El Sol and Cyanobacteria in Lake La Luna. The most extreme conditions of Lake La Luna (ultraoligotrophy, very low pH, high ultraviolet radiation) most likely explained the differences in the dominant species composition and lower species richness compared to Lake El Sol. Herein, we provide for the first time a taxonomic list of the phytoplankton community of Lakes El Sol and La Luna. This information constitutes a baseline needed to use these HML as sentinels of global and climate change.


2002 ◽  
Vol 106 (7) ◽  
pp. 848-856 ◽  
Author(s):  
Wilbert G. Flier ◽  
Niklaus J. Grünwald ◽  
Laurens P.N.M. Kroon ◽  
Trudy B.M. Van Den Bosch ◽  
Edith Garay-Serrano ◽  
...  

2000 ◽  
Vol 318 (1-4) ◽  
pp. 281-302 ◽  
Author(s):  
A. Garcı́a-Palomo ◽  
J.L. Macı́as ◽  
V.H. Garduño

2012 ◽  
Vol 57 (4) ◽  
pp. 728-740 ◽  
Author(s):  
JOSÉ ARTURO ALCÁNTARA-RODRÍGUEZ ◽  
JORGE CIROS-PÉREZ ◽  
ELIZABETH ORTEGA-MAYAGOITIA ◽  
CARMEN R. SERRANIA-SOTO ◽  
ELÍAS PIEDRA-IBARRA

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