Late Pleistocene to Holocene environmental changes from ¿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 inferenvironmental changes during late Pleistocene to Present in the Teotihuacan valley, Mexico. Interpretation was based on climaticpreferences of C3, CAM and C4 plant groups. ^...
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| Gepubliceerd in: | Geofísica Internacional |
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| Hoofdauteurs: | , , , , , , |
| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
Universidad Nacional Autónoma de México
2006
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| Onderwerpen: | |
| Online toegang: | https://www.redalyc.org/articulo.oa?id=56845201 |
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