Atlantic forcing of Western Mediterranean winter rain minima during the last 12,000 years

Christoph Zielhofer, William J. Fletcher, Steffen Mischke, Marc De Batist, Jennifer F.E. Campbell, Sebastien Joannin, Rik Tjallingii, Najib El Hamouti, Annett Junginger, Andreas Stele, Jens Bussmann, Birgit Schneider, Tobias Lauer, Katrin Spitzer, Michael Strupler, Thomas Brachert, Abdeslam Mikdad

Rannsóknarafurð: Framlag til fræðitímaritsGreinritrýni

64 Tilvitnanir (Scopus)

Útdráttur

The limited availability of high-resolution continuous archives, insufficient chronological control, and complex hydro-climatic forcing mechanisms lead to many uncertainties in palaeo-hydrological reconstructions for the Western Mediterranean. In this study we present a newly recovered 19.63 m long core from Lake Sidi Ali in the North African Middle Atlas, a transition zone of Atlantic, Western Mediterranean and Saharan air mass trajectories. With a multi-proxy approach based on magnetic susceptibility, carbonate and total organic C content, core-scanning and quantitative XRF, stable isotopes of ostracod shells, charcoal counts, Cedrus pollen abundance, and a first set of diatom data, we reconstruct Western Mediterranean hydro-climatic variability, seasonality and forcing mechanisms during the last 12,000 yr. A robust chronological model based on AMS 14C dated pollen concentrates supports our high-resolution multi-proxy study. Long-term trends reveal low lake levels at the end of the Younger Dryas, during the mid-Holocene interval 6.6 to 5.4 cal ka BP, and during the last 3000 years. In contrast, lake levels are mostly high during the Early and Mid-Holocene. The record also shows sub-millennial- to centennial-scale decreases in Western Mediterranean winter rain at 11.4, 10.3, 9.2, 8.2, 7.2, 6.6, 6.0, 5.4, 5.0, 4.4, 3.5, 2.9, 2.2, 1.9, 1.7, 1.5, 1.0, 0.7, and 0.2 cal ka BP. Early Holocene winter rain minima are in phase with cooling events and millennial-scale meltwater discharges in the sub-polar North Atlantic. Our proxy parameters do not show so far a clear impact of Saharan air masses on Mediterranean hydro-climate in North Africa. However, a significant hydro-climatic shift at the end of the African Humid Period (∼5 ka) indicates a change in climate forcing mechanisms. The Late Holocene climate variability in the Middle Atlas features a multi-centennial-scale NAO-type pattern, with Atlantic cooling and Western Mediterranean winter rain maxima generally associated with solar minima.

Upprunalegt tungumálEnska
Síður (frá-til)29-51
Síðufjöldi23
FræðitímaritQuaternary Science Reviews
Bindi157
DOI
ÚtgáfustaðaÚtgefið - 1 feb. 2017

Athugasemd

Funding Information:
Christoph Zielhofer, Steffen Mischke and William Fletcher as principal investigators thank the German Research Foundation (DFG, ZI 721/9-1) and the Natural Environment Research Council (New Investigator Award to W Fletcher, NE/K000608/1, and NERC RCF dating awards, 1765.1013 and 1809.0414) for generous funding of the fieldwork and lab analyses. The authors are grateful to the Institut National des Sciences de l'Arch?ologie et du Patrimoine (INSAP, Rabat), the Centre National d'Hydrobiologie et de Pisciculture (CNHP, Azrou) and to the Caidad d'Azrou for helpful support in field and in preparing the expedition in autumn 2012. Acknowledgements to Mustapha Rhanem for assistance in obtaining the Sidi Ali meteorological data. Hanno Meyer of the stable isotope laboratory at AWI Potsdam is highly acknowledged for providing the stable water isotope data. Finally, the authors are grateful to two anonymous reviewers for helpful comments and suggestions.

Publisher Copyright:
© 2016 The Author(s)

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