Holocene Paleoenvironment and Prehispanic Landscape Evolution in the Basin of Mexico
Dados Bibliográficos
| ID | 6034343 |
|---|---|
| Autores | E Mcclung De Tapia (0000-0003-1684-1069, Universidad Nacional Autonoma de Mexico, autor correspondente) |
| Ano | 2015 |
| Volume | 26 |
| Fascículo | 2 |
| Páginas | 375-389 |
| Data de publicação | 2015-01-01 |
| Peer Reviewed | Sim |
| Open Access | Sim |
| Tipo | ARTICLE |
| Periódico | Ancient Mesoamerica (JOURNAL) |
| Identificadores do periódico | ISSN: 0956-5361 • E-ISSN: 1469-1787 |
| Editora | Cambridge University Press (CUP) (PUBLISHER) |
| DOI | 10.1017/s0956536115000243 |
| OpenAlex | W2284834995 |
| Idioma | EN |
| Citações recebidas | 3 |
| Referências citadas | 55 |
Paleoenvironmental and geoarchaeological data generated over the past three decades for parts of the Basin of Mexico are little known among archaeologists working in the region. This paper summarizes and evaluates what is currently known about the prehistoric environment, landscape development, and human impact in the region. Archaeological evidence indicates that human activity became important in ecosystem evolution in the basin during the Middle-Late Holocene. Most traditional paleoenvironmental studies based on lake sediments, however, generalize results corresponding to this period simply asevidence for human impact. Essentially the same vegetation communities extant in the basin today appear to have been present during most of the Holocene, albeit with broader distributions and variability in secondary taxa. Recognizing potential contributions of archaeology to understanding human adaptation to climatic and ecosystemic change, past and present, should stimulate future research on paleoenvironment in the region
Archaeology · Geography · Holocene · Physical geography · Prehistory · Structural basin · Archaeology and ancient environmental studies · Geology and Paleoclimatology Research · Pleistocene-Era Hominins and Archaeology · Geology · Paleontology
Lake Levels since about 40,000 Years Ago at Lake Chalco, near Mexico City
Yr of vegetation history of the Upper Lerma, a tropical high-altitude basin in Central Mexico
High-resolution chronology for the Mesoamerican urban center of Teotihuacan derived from Bayesian statistics of radiocarbon and archaeological data
Geochemical Characterization of Late Pleistocene and Holocene Tephra Layers from the Basin of Mexico, Central Mexico
Paleoecological Studies at Lake Patzcuaro on the West-Central Mexican Plateau and at Chalco in the Basin of Mexico
Late Pleistocene and Holocene Paleoenvironments of Chalco Lake, Central Mexico
Ancient Teotihuacan
Mid- to Late Holocene climate change
Años de la cuenca de Zacapu. Evolución de los paisajes y primeros desmontes
The Basin of Mexico
Prosperity, power, and change
Social and cultural consequences of a late Holocene eruption of Popocatépetl in central Mexico
Spatial variability of environment change in the Teotihuacan Valley during the Late Quaternary
Some problems in the late Quaternary pollen records of Central Mexico
Fluvial processes and paleopedogenesis in the Teotihuacan Valley, México
Late holocene human impact on lake basins in central mexico
The Black San Pablo Paleosol of the Teotihuacan Valley, Mexico
Geoarchaeology of an Aztec dispersed village on the Texcoco piedmont of Central Mexico
Trees and shrubs
Bayesian Analysis of Radiocarbon Dates
Radiocarbon Dates from Soil Profiles in the Teotihuacán Valley, Mexico
Prehispanic Settlement Patterns in the Southern Valley of Mexico
Situaciones climáticas durante el auge y la caida de la cultura teotihuacana
Vegetation and Plant Use in Postclassic Otumba
Watering the Fields of Teotihuacan
Climatic Change and Lacustrine Resources at the Period of Initial Aztec Development
Climatic change, culture, and civilization in North America
Pollen Analysis and Mexican Archaeology
| Obras citantes distintas | 3 |
|---|---|
| Citações por ano | 0,43 |
| Intervalo de citações | 2019 - 2019 (1) |
| Velocidade de citação | historical |
| Altamente citado | Não |
| Tipos de citação | Neutras: 3 |