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Impact of late-Holocene aridification trend, climate variability and geodynamic control on the environment from a coastal area in SW Spain

Bibliographic Data

ID12267607
AuthorsGonzalo Jiménez‐moreno (0000-0001-7185-8686, Universidad de Granada, corresponding author), Gonzalo Jiménez-Moreno (Universidad de Granada), Antonio Rodríguez Ramírez (0000-0001-8437-6811, Universidad de Huelva), Antonio Rodríguez-Ramírez (Universidad de Huelva), José N Pérez‐Asensio (0000-0002-1393-7412, University of Geneva), José N Pérez-Asensio (University of Geneva), José S Carrión (0000-0002-6949-4382, Universidad de Murcia), José Antonio López-Sáez (0000-0002-3122-2744, Instituto de Historia), Juan J R Villarias Robles (0000-0002-5664-9795, Instituto de Lengua Literatura y Antropología), Juan JR Villarías-Robles (Instituto de Lengua, Literatura y Antropología, Centro de Ciencias Humanas y Sociales (CCHS), Consejo Superior de Investigaciones Científicas (CSIC), Spain), Sebastián Celestino-Pérez (Instituto de Arqueología de Mérida, Consejo Superior de Investigaciones Científicas (CSIC), Spain), Enrique Cerrillo-Cuenca (0000-0002-2476-0472, Instituto de Arqueología de Mérida, Consejo Superior de Investigaciones Científicas (CSIC), Spain), Ángel León (0000-0001-5616-5689, Fundación del Hogar del Empleado (FUHEM), Spain), Carmen Contreras (0000-0001-6184-3819, Universidad de Huelva)
Year2015
Volume25
Issue4
Pages607-617
Publication date2015-01-06
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1177/0959683614565955
OpenAlexW2170975074
LanguageEN
Citations received14
References cited66

A detailed pollen analysis has been carried out on two sediment cores taken from a marsh area located in the Doñana National Park, southwestern Spain. The studied sedimentary sequences contain a similar late Holocene record of vegetation and climate and show a progressive aridification trend since at least 5000 cal. yr BP, through a decrease in forest cover in this area. Long-term vegetation changes shown here (semi-desert expansion and Mediterranean forest decline) paralleled declining summer insolation. Decreasing summer insolation most likely impacted negatively on tree growing season as well as on winter precipitation in the area. Superimposed on the long-term aridification trend were multi-centennial scale periods characterized by forest reductions or increases in arid and halophytic plants that can be interpreted as produced by enhanced droughts and/or by local geodynamic processes. These are centered at ca. 4000, 3000–2500, and 1000 cal. yr BP, coinciding in timing and duration with well-known dry events in the western Mediterranean and other areas but could have also been generated by local sedimentary or geodynamic processes such as a marine transgression in a subsidence context and extreme wave events (EWEs). The alternation of persistent North Atlantic Oscillation modes probably played an important role in controlling these relatively humid–arid cycles

Arid · Aridification · Climate change · Climatology · Context (archaeology · Geography · Holocene · Mediterranean climate · Physical geography · Pluvial · Vegetation (pathology · Aeolian processes and effects · Geology and Paleoclimatology Research · Maritime and Coastal Archaeology · Geology · Oceanography · Paleontology

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Unique citing works14
Citations per year1,27
Citation span2015 - 2026 (12)
Citation velocitycurrent
Highly citedNo
Citation typesNeutral: 14
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