Dynamics and sources of last glacial aeolian deposition in southwest France derived from dune patterns, grain-size gradients and geochemistry, and reconstruction of efficient wind directions
We acknowledge Christophe Tuffery (Inrap) for his help in the GIS. This work was funded by Inrap, the University of Bordeaux and Lascarbx (Universités de Bordeaux, program of the Agence Nationale de la Recherche ANR-10-LABX-52). The Labex L-IPSL, which is funded by the ANR (grant #ANR-10-LABX-0018), is also acknowledged. This is LDEO #8118. The two anonymous reviewers are also thanked for their remarks, which contributed to greatly improve the manuscript. The simulations used here have been run on the HPC facilities of the Commissariat à l'Energie Atomique.
Universidad de Tarapacá, Instituto de Alta Investigación, Laboratorio de Análisis e Investigaciones Arqueométricas, Antofagasta 1520, Arica, Chile; INRAP, 140 Avenue Leclerc, Bègles, France; PACEA, Université de Bordeaux – CNRS, bâtiment B18, allée Geoffroy-Saint-Hilaire, Pessac Cedex, France; Laboratoire de Météorologie Dynamique/IPSL, Sorbonne Universités, UPMC Université Paris 06, ENS, PSL Research University, École Polytechnique, Université Paris Saclay, CNRS, Paris, France; Bordeaux Sciences Agro, 1 cours du Général de Gaulle, CS 40201, Gradignan, France; Laboratoire de Météorologie Dynamique/IPSL, Département de géosciences, ENS, PSL Research University, École Polytechnique, Université Paris Saclay, Sorbonne Universités, UPMC Université Paris 06, CNRS, Paris, France; Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, United States
Recommended Citation:
Sitzia L.,Bertran P.,Sima A.,et al. Dynamics and sources of last glacial aeolian deposition in southwest France derived from dune patterns, grain-size gradients and geochemistry, and reconstruction of efficient wind directions[J]. Quaternary Science Reviews,2017-01-01,170