8000 years of vegetation history in the northern Iberian Peninsula inferred from the palaeoenvironmental study of the Zalama ombrotrophic bog (Basque‐Cantabrian Mountains,Spain) |
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| Authors: | Sebastián Pérez‐Díaz José Antonio López‐Sáez Xabier Pontevedra‐Pombal Martín Souto‐Souto Didier Galop |
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| Affiliation: | 1. Dpto. de Geografía, Prehistoria y Arqueología, Facultad de Letras, Universidad del País Vasco Francisco Tomás y Valiente, Vitoria‐Gasteiz, Spain;2. Grupo de Investigación Arqueobiología, Instituto de Historia, Centro de Ciencias Humanas y Sociales, Consejo Superior de Investigaciones Científicas (CSIC), Madrid, Spain;3. Dpto. de Edafología y Química Agrícola, Universidad de Santiago de Compostela, Santiago de Compostela, Spain;4. Dpto. De Botánica, Universidad de Santiago de Compostela, Santiago de Compostela, Spain;5. Didier Galop, GEODE, UMR 5602 CNRS, Université Toulouse 2 Jean Jaurès 5, Toulouse Cedex 9, France |
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| Abstract: | This paper focuses on pollen, spores, non‐pollen palynomorphs (NPPs) and certain geochemical elements from the ombrotrophic blanket bog of Zalama (Basque‐Cantabrian Mountains, northern Iberian Peninsula), with the support of a robust chronology based on 17 AMS 14C dates. The main results related to the last 8000 years show that, during the early middle Holocene, pines and deciduous forests were the most extensive tree formations. At the beginning of the succession, pines reach 44%, showing regional presence, whereas after 7600 cal. a BP, deciduous forests were particularly abundant. From c. 6500 cal. a BP the pollen diagram constructed from our samples shows the first anthropogenic evidence, linked with the new economic practices related to the Neolithic of the Basque‐Cantabrian Mountains. From 3300 cal. a BP the expansion of Fagus sylvatica is particularly clear, and has since then become one of the dominant forest species in this region. We also discuss the Holocene evolution of other noteworthy plant communities in southwestern Europe, such as Taxus baccata, Juglans and shrublands. |
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