Mots-clés
Analyse pollinique ; Charbon de bois ; Diatomée ; Epoque romaine ; Espagne ; Espagne centrale ; Paléo-environnement ; Relation société-environnement ; Sédiment lacustre ; Sédimentologie ; Utilisation du sol ; Variabilité climatiqueCentral Spain ; Charcoal ; Climatic variability ; Diatom ; Lacustrine sediment ; Land use ; Palaeo-environment ; Pollen analysis ; Roman era ; Sedimentology ; Society-environment relationship ; SpainAnálisis polínico ; Aprovechamiento del suelo ; Carbón vegetal ; Diatomea ; España ; Paleoambiente ; Relación sociedad-medio ambiente ; Sedimento lacustre ; Sedimentología ; Variabilidad climática ; Época romanaClimate change and human impact in central Spain during Roman times : High-resolution multi-proxy analysis of a tufa lake record (Somolinos, 1280 m asl)
Auteur(s) et Affiliation(s)
CURRÁS, A.
Dep. of Prehistory, Ancient History and Archaeology Univ., Barcelona, Espagne
ZAMORA, L.
Dep. of Microbiology and Ecology, Univ. of Valencia, Burjassot, Espagne
REED, J.M.
Dept. of Geography, Univ., Hull, Royaume-Uni
GARCÍA-SOTO, E.
Los Casares archaeological group, Sigüenza, Espagne
FERRERO, S.
Los Casares archaeological group, Sigüenza, Espagne
ARMENGOL, X.
Dep. of Microbiology and Ecology, Univ. of Valencia, Burjassot, Espagne
MEZQUITA-JOANES, F.
Dep. of Microbiology and Ecology, Univ. of Valencia, Burjassot, Espagne
MARQUÉS, M.A.
Dep. of Geodynamics and Geophysics, Univ., Barcelona, Espagne
RIERA, S.
Dep. of Prehistory, Ancient History and Archaeology Univ., Barcelona, Espagne
JULIÀ, R.
Inst. of Earth Sciences Jaume Almera, CSIC, Barcelona, Espagne
Description :
In order to improve the understanding of the synergies between societal and environmental change during the Roman Period in central Spain, the AA. present a case study based on the integration of multi-proxy palaeoenvironmental, archaeological and historical data. The Somolinos sequence extends from the 9th century cal BC (Pre-Roman) to the 8th century AD (Early Medieval). The analyses include pollen, non-pollen palynomorphs (NPPs), macrocharcoal, ostracods, diatoms, other biotic remains and sedimentology. The multi-proxy data reveal dry conditions during Roman and Visigothic times and moister phases during Iron Age and Late Roman. Wide human impact started at 80 yr BC, one century after the climate change towards drier conditions. The Somolinos record indicates that Roman humid period is not a simple phase as some suggest. The observed environmental changes resulted from the interaction of different driving factors.
Type de document :
Article de périodique
Source :
Catena (Giessen), issn : 0341-8162, 2012, vol. 89, n°. 1, p. 31-53, nombre de pages : 23, Références bibliographiques : 3 p.
Date :
2012
Editeur :
Pays édition : Allemagne, Cremlingen-Destedt, Catena
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)