4.6 Article

Environmental Changes and Cultural Transitions in SW Iberia during the Early-Mid Holocene

期刊

APPLIED SCIENCES-BASEL
卷 11, 期 8, 页码 -

出版社

MDPI
DOI: 10.3390/app11083580

关键词

palaeoenvironment; mesolithic; neolithic; palynology; geochemistry; SW Iberian Coast

资金

  1. Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) [57444011, SFB 806]
  2. Fundacao para a Ciencia e Tecnologia (FCT)-Project OnOff [PTDC/CTAGEO/28941/2017]

向作者/读者索取更多资源

The study fills a gap in the lack of palaeoenvironmental and archaeological data on the SW coast of the Iberian Peninsula through a new palynological and geochemical dataset. It reveals warm vegetation conditions at the start of the Holocene followed by increased moisture and forest development, with peaks of aridity at 8.2 and 7.5 ka BP. Archaeological data suggest human groups in the Mesolithic and Early Neolithic periods adapted through seasonal camps and permanent settlements near rivers.
The SW coast of the Iberian Peninsula experiences a lack of palaeoenvironmental and archaeological data. With the aim to fill this gap, we contribute with a new palynological and geochemical dataset obtained from a sediment core drilled in the continental shelf of the Algarve coast. Archaeological data have been correlated with our multi-proxy dataset to understand how human groups adapted to environmental changes during the Early-Mid Holocene, with special focus on the Mesolithic to Neolithic transition. Vegetation trends indicate warm conditions at the onset of the Holocene followed by increased moisture and forest development ca. 10-7 ka BP, after which woodlands are progressively replaced by heaths. Peaks of aridity were identified at 8.2 and 7. 5 ka BP. Compositional, textural, redox state, and weathering of source area geochemical proxies indicates abrupt palaeoceanographic modifications and gradual terrestrial changes at 8.2 ka BP, while the 7.5 ka BP event mirrors a decrease in land moisture availability. Mesolithic sites are mainly composed of seasonal camps with direct access to the coast for the exploitation of local resources. This pattern extends into the Early Neolithic, when these sites coexist with seasonal and permanent occupations located in inland areas near rivers. Changes in settlement patterns and dietary habits may be influenced by changes in coastal environments caused by the sea-level rise and the impact of the 8.2 and 7.5 ka BP climate events.

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