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

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 d...

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Published in:Applied Sciences
Main Authors: Cristina Val-Peón, Juan I. Santisteban, José A. López-Sáez, Gerd-Christian Weniger, Klaus Reicherter
Format: Article
Language:English
Published: MDPI AG 2021-04-01
Subjects:
Online Access:https://www.mdpi.com/2076-3417/11/8/3580
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author Cristina Val-Peón
Juan I. Santisteban
José A. López-Sáez
Gerd-Christian Weniger
Klaus Reicherter
author_facet Cristina Val-Peón
Juan I. Santisteban
José A. López-Sáez
Gerd-Christian Weniger
Klaus Reicherter
author_sort Cristina Val-Peón
collection DOAJ
container_title Applied Sciences
description 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 <i>ca</i>. 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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spelling doaj-art-e7b13a15e63e45ecb37007fdf42e74852025-08-19T23:27:34ZengMDPI AGApplied Sciences2076-34172021-04-01118358010.3390/app11083580Environmental Changes and Cultural Transitions in SW Iberia during the Early-Mid HoloceneCristina Val-Peón0Juan I. Santisteban1José A. López-Sáez2Gerd-Christian Weniger3Klaus Reicherter4Institute of Neotectonics and Natural Hazards, RWTH Aachen University, 52062 Aachen, GermanyDepartment of Geodynamics, Stratigraphy and Paleontology, Fac. Geological Sciences, Complutense University of Madrid, 28040 Madrid, SpainEnvironmental Archaeology Research Group, Institute of History (CCHS), C.S.I.C., 28037 Madrid, SpainInstitute for Prehistoric Archaeology, Cologne University, 50923 Köln, GermanyInstitute of Neotectonics and Natural Hazards, RWTH Aachen University, 52062 Aachen, GermanyThe 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 <i>ca</i>. 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.https://www.mdpi.com/2076-3417/11/8/3580palaeoenvironmentmesolithicneolithicpalynologygeochemistrySW Iberian Coast
spellingShingle Cristina Val-Peón
Juan I. Santisteban
José A. López-Sáez
Gerd-Christian Weniger
Klaus Reicherter
Environmental Changes and Cultural Transitions in SW Iberia during the Early-Mid Holocene
palaeoenvironment
mesolithic
neolithic
palynology
geochemistry
SW Iberian Coast
title Environmental Changes and Cultural Transitions in SW Iberia during the Early-Mid Holocene
title_full Environmental Changes and Cultural Transitions in SW Iberia during the Early-Mid Holocene
title_fullStr Environmental Changes and Cultural Transitions in SW Iberia during the Early-Mid Holocene
title_full_unstemmed Environmental Changes and Cultural Transitions in SW Iberia during the Early-Mid Holocene
title_short Environmental Changes and Cultural Transitions in SW Iberia during the Early-Mid Holocene
title_sort environmental changes and cultural transitions in sw iberia during the early mid holocene
topic palaeoenvironment
mesolithic
neolithic
palynology
geochemistry
SW Iberian Coast
url https://www.mdpi.com/2076-3417/11/8/3580
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AT gerdchristianweniger environmentalchangesandculturaltransitionsinswiberiaduringtheearlymidholocene
AT klausreicherter environmentalchangesandculturaltransitionsinswiberiaduringtheearlymidholocene