Late Pleistocene to Holocene environmental changes from δ 13C determinations in soils at Teotihuacan, Mexico
Stable carbon isotopic signature (δ13C) of soil organic matter (SOM) is used as a high–spatial resolution tool to infer environmental changes during late Pleistocene to Present in the Teotihuacan valley, Mexico. Interpretation was based on climatic preferences of C3, CAM and C4 plant groups. δ13Cval...
| Autores: | , , , , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2006 |
| País: | México |
| Institución: | UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO |
| Repositorio: | Geofísica Internacional |
| Idioma: | español inglés |
| OAI Identifier: | oai:revistagi.geofisica.unam.mx:article/332 |
| Acceso en línea: | http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/332 |
| Access Level: | acceso abierto |
| Palabra clave: | Teotihuacan isótopos estables del carbono paleosuelos cambios climáticos de Cuaternario México Central registros arqueológicos carbon stable isotope paleosols Quaternary climatic changes Central Mexico archeological records |
| Sumario: | Stable carbon isotopic signature (δ13C) of soil organic matter (SOM) is used as a high–spatial resolution tool to infer environmental changes during late Pleistocene to Present in the Teotihuacan valley, Mexico. Interpretation was based on climatic preferences of C3, CAM and C4 plant groups. δ13Cvalues of modern plant types are clearly distinguished. C3 plants display values around –27%o, while C4 and CAM plants have values around—13%o. Data from soil profiles range from –25.7 to –15.5 %o. Cerro Gordo site δ13Cvaryies around –20%o, indicating long–term, time–stable co–existence between C3 and C4 or CAM plants. The more depleted signatures (–23 ± 2 %o) are, dominated by carbon from C3 vegetation of late Pleistocene swamp paleosols in the Tepexpan profile of the Lake Texcoco. Younger paleosols from lower valley sites, have less depleted values (–17 ± 1) %o, dominated by C4 and CAM carbon. Late Holocene and modern soils present slightly more negative values (1–2 %o) with respect to δ13Cof underlying soils. Our results show 1) an increase of 10–70 % depending on the site, during the transition from the late Pleistocene to early Holocene, and 2) a dominance of C4 vegetation, up to 84%, in valley environment during the middle Holocene. These data support a climatic change from cold and wet conditions in the Last Glacial Maximum and late Pleistocene, to warm and dry conditions in middle Holocene. A slight rise in moisture availability during late Holocene is inferred based on the 4–10% increase in C3 plant carbon in soils from the valley. Conditions remained generally warm and dry, much as they are at present, favouring the development of agriculture in the valley. Our interpretation agrees with results of paleoenvironmental studies at Texcoco Lake based on diatom and pollen analyses in lake. |
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