Contribution to the paleo-environmental studies of Ambato Valley (Catamarca) from the Paleo-NDVI (442-1998 AD) reconstruction
In order to reconstruct the Late Holocene vegetation history we used a module from of HEMO (Hindcasting Ecosystems Model), an ecosystem-process model. This reconstruction of the environmental past in terms of the normalized difference vegetation index (NDVI) is related to plant’s absorption of the p...
Guardado en:
| Autores principales: | , , , , , , |
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| Formato: | Artículo publishedVersion Peer-reviewed papers Artículo evaluado por pares |
| Lenguaje: | Español |
| Publicado: |
Instituto de Arqueología y Museo, Facultad de Ciencias Naturales e IML, Universidad Nacional de Tucumán
2016
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| Materias: | |
| Acceso en línea: | http://publicaciones.csnat.unt.edu.ar/index.php/mundodeantes/article/view/174 http://suquia.ffyh.unc.edu.ar/handle/suquia/10123 |
| Aporte de: |
| Sumario: | In order to reconstruct the Late Holocene vegetation history we used a module from of HEMO (Hindcasting Ecosystems Model), an ecosystem-process model. This reconstruction of the environmental past in terms of the normalized difference vegetation index (NDVI) is related to plant’s absorption of the photosynthetically active radiation (APAR), with the canopy geometry of woody plants, soil cover and humidity. This work presents the Paleo-NDVI reconstruction from 442 AD to the present. Positive and negative anomalies are discussed here, which are linked to different Aguada´s occupational sequences, together with the model sensibility to global phenomena. |
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