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Quaternary palaeoenvironmental changes in South Spain

dc.book.titleQuaternary climatic changes and environmental crises in the Mediterranean Region / Editors, M. Blanca Ruiz Zapata... [et al.].
dc.contributor.authorYll, R.
dc.contributor.authorZazo Cardeña , Caridad
dc.contributor.authorGoy Goy, José Luis
dc.contributor.authorPerez Obiol, R.
dc.contributor.authorPantaleón Cano, J.
dc.contributor.authorCivis Llovera, Jorge
dc.contributor.authorDabrio González, Cristino José
dc.contributor.authorGonzález , A.
dc.contributor.authorBorja, Francisco
dc.contributor.authorSoler Javaloyes, Vicente
dc.contributor.authorLario, Javier
dc.contributor.authorLuque, Luis de
dc.contributor.authorSierro, Francisco Javier
dc.contributor.authorGonzález Hernández, F.M.
dc.contributor.authorLezine, Anne Marie
dc.contributor.authorDenefle, Michael
dc.contributor.authorRoure, Joan Maria
dc.contributor.editorRuiz Zapata, María Blanca
dc.date.accessioned2023-06-20T21:01:54Z
dc.date.available2023-06-20T21:01:54Z
dc.date.issued2003
dc.description.abstractThis paper presents the existing differences between the evolution of the Holocene landscape of the Southeastern and Southwestern areas of the Iberian Peninsula. Moreover, some palaeoenvironmental characteristics of OIS 4 and OIS 3 of the western Andalusia appear. The five presented sequences have been analyzed from palynological and geomorphological point of view. The obtained results show that during the Holocene no significant forest cover existed in the eastern area and that the different phases identified mainly show an alternation of shrub and steppe communities, taking place during the fifth millennium a radical transformation of the landscape and the definitive establishment of the semi-desert conditions that are registered at the present time. In the western area the evolution of the landscape is determined basically by the changes of geomorphological conditions of the coast and the marshland zones of the Guadalquivir and the Tinto-Odiel systems, registering diverse moments of increase of the aridity conditions, without remarkable changes in the vegetal landscape. Sequences obtained do not provide evidence of indicators of human intervention that might be clearly attributable to the pattern of human activities established in the area until a the two millennium ago.
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/11371
dc.identifier.isbnISBN: 84-699-8798-4.
dc.identifier.urihttps://hdl.handle.net/20.500.14352/60504
dc.language.isoeng
dc.page.final213
dc.page.initial201
dc.page.total291
dc.publication.placeAlcalá de Henares (Madrid)
dc.publisherUniversidad de Alcalá
dc.rights.accessRightsopen access
dc.subject.cdu504.53(262)
dc.subject.cdu551.585(262)
dc.subject.keywordPleistocene
dc.subject.keywordHolocene
dc.subject.keywordClimatic Change
dc.subject.keywordPollen
dc.subject.keywordSouth Spain
dc.subject.ucmGeología estratigráfica
dc.subject.unesco2506.19 Estratigrafía
dc.titleQuaternary palaeoenvironmental changes in South Spain
dc.typebook part
dspace.entity.typePublication
relation.isAuthorOfPublication1556fc8c-dd30-40b0-a180-d00679f99678
relation.isAuthorOfPublication55faa814-a938-4b9e-9840-d51419e44f20
relation.isAuthorOfPublication.latestForDiscovery1556fc8c-dd30-40b0-a180-d00679f99678

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