Saharan aeolian input and effective humidity variations over western Europe during the Holocene from a high altitude record

F. J. Jiménez-Espejo, A. García-Alix, G. Jiménez-Moreno, M. Rodrigo-Gámiz, Scott R Anderson, F. J. Rodríguez-Tovar, F. Martínez-Ruiz, Santiago Giralt, A. Delgado Huertas, E. Pardo-Igúzquiza

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30 Citations (Scopus)

Abstract

Saharan dust inputs affect present day ecosystems and biogeochemical cycles at a global scale. Previous Saharan dust input reconstructions have been mainly based on marine records from the African margin, nevertheless dust reaching western-central Europe is mainly transported by high-altitude atmospheric currents and requires high altitude records for its reconstruction. The organic and inorganic geochemical study of sediments from a southern Iberia alpine lacustrine record has provided an exceptional reconstruction of Saharan dust impact and regional climatic variations during the Holocene. After the last deglaciation, results indicate that Saharan dust reached Western Europe in a stepwise fashion from 7.0 to 6.0. cal.kyr. BP and increased since then until present, promoting major geochemical changes in the lacustrine system. Effective humidity reconstruction indicates wetter conditions during the early Holocene and progressive aridification during middle-late Holocene time, boosting abrupt changes in the lacustrine system. Cyclostratigraphic analyses and transport mechanisms both point to solar irradiance and aridity as major triggering factors for dust supply over Western Europe during the Holocene.

Original languageEnglish (US)
Pages (from-to)1-12
Number of pages12
JournalChemical Geology
Volume374-375
DOIs
StatePublished - May 26 2014

Fingerprint

Dust
Atmospheric humidity
humidity
Holocene
dust
aridification
marine record
last deglaciation
biogeochemical cycle
aridity
Ecosystems
irradiance
Western Europe
Sediments
ecosystem
sediment

Keywords

  • Holocene
  • Lacustrine record
  • Saharan dust
  • South Iberia

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geology

Cite this

Jiménez-Espejo, F. J., García-Alix, A., Jiménez-Moreno, G., Rodrigo-Gámiz, M., Anderson, S. R., Rodríguez-Tovar, F. J., ... Pardo-Igúzquiza, E. (2014). Saharan aeolian input and effective humidity variations over western Europe during the Holocene from a high altitude record. Chemical Geology, 374-375, 1-12. https://doi.org/10.1016/j.chemgeo.2014.03.001

Saharan aeolian input and effective humidity variations over western Europe during the Holocene from a high altitude record. / Jiménez-Espejo, F. J.; García-Alix, A.; Jiménez-Moreno, G.; Rodrigo-Gámiz, M.; Anderson, Scott R; Rodríguez-Tovar, F. J.; Martínez-Ruiz, F.; Giralt, Santiago; Delgado Huertas, A.; Pardo-Igúzquiza, E.

In: Chemical Geology, Vol. 374-375, 26.05.2014, p. 1-12.

Research output: Contribution to journalArticle

Jiménez-Espejo, FJ, García-Alix, A, Jiménez-Moreno, G, Rodrigo-Gámiz, M, Anderson, SR, Rodríguez-Tovar, FJ, Martínez-Ruiz, F, Giralt, S, Delgado Huertas, A & Pardo-Igúzquiza, E 2014, 'Saharan aeolian input and effective humidity variations over western Europe during the Holocene from a high altitude record', Chemical Geology, vol. 374-375, pp. 1-12. https://doi.org/10.1016/j.chemgeo.2014.03.001
Jiménez-Espejo, F. J. ; García-Alix, A. ; Jiménez-Moreno, G. ; Rodrigo-Gámiz, M. ; Anderson, Scott R ; Rodríguez-Tovar, F. J. ; Martínez-Ruiz, F. ; Giralt, Santiago ; Delgado Huertas, A. ; Pardo-Igúzquiza, E. / Saharan aeolian input and effective humidity variations over western Europe during the Holocene from a high altitude record. In: Chemical Geology. 2014 ; Vol. 374-375. pp. 1-12.
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