Cambios ambientales en el noroeste peninsular durante el Campaniforme (2800-1400 cal BC)

descriptionPublicationkeyboard_double_arrow_right Conference object , Part of book or chapter of book , Other ORP type 01 Jan 2011 Spain English Publisher:Diputación Provincial de Pontevedra

Authors: López Sáez, José Antonio; Carrión Marco, Yolanda; López Merino, Lourdes; Kaal, Joeri; Costa-Casais, Manuela; Martínez Cortizas, Antonio;

handle: 10261/93981 , 10261/140051

Cambios ambientales en el noroeste peninsular durante el Campaniforme (2800-1400 cal BC)

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Abstract

In this presentation we will summarize the available knowledge on environmental changes during the Bell Beaker period (ca. 2800-1400 cal BC) in NW Iberia. The main drivers of environmental change were climate changes and human transfomations, as welll as the couplings between them. It is quite signficant that the Bell Beaker occurred during the second half of the Neoglaciation, one of the coldest phases of the Holocene in NW Iberia. The interaction between the climatic deterioration and an increasing human pressure on forests lead to a reconfiguration of the vegetation cover, the elimination of the soil resources in some areas (due to enhanced soil erosion ) and its concentration in more localized, control-demanding sectors. At the same time, denudation of 15TH BELL BEAKER INTERNATIONAL CONGRESS "FROM ATLANTIC TO URAL" the landscape resulted in the exhumation of rock outcrops and a higher availability of rock surfaces for rock carving.

Ponencia presentada en el 15th Bell Beaker International Conference: From Atlantic to Ural, celebrado en Poio (Pontevedra) del 5 al 9 de mayo de 2011.

Peer Reviewed

Country

Spain

Related Organizations

Spanish National Research Council
Spain

Keywords

Geomorfología, Reconstrucción paleoambiental, Antracología, Registro polínico, Edafología, Clima

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