Chapter 16 Loess Records Daniel R. Muhs, Stephen R. Cattle, Onn Crouvi, Denis-Didier Rousseau, Jimin Sun, and Marcelo A. Zárate Abstract Loess is aeolian sediment, dominated by silt-sized particles, that is identifiable in the field as a distinct sedimentary body. It covers a significant portion of the land surface of the Earth and as such constitutes one of the most important archives of long-term dust deposition. Large tracts of loess cover Europe, Asia, South America, and North America, and smaller loess bodies are found covering parts of Africa, the Middle East, New Zealand, and Australia. Loess thickness, particle size, and carbonate content decrease downwind from sources, trends that are powerful tools for reconstructing paleowinds. Many loess sections consist of D.R. Muhs () U.S. Geological Survey, Federal Center, MS 980, Box 25046, Denver, CO 80225, USA e-mail:
[email protected] S.R. Cattle Faculty of Agriculture and Environment, The University of Sydney, Sydney, NSW 2006, Australia e-mail:
[email protected] O. Crouvi Geological Survey of Israel, 30 Malkhe Israel St., Jerusalem 95501, Israel e-mail:
[email protected] D.-D. Rousseau Ecole Normale Supérieure, Laboratoire de Météorologie Dynamique, UMR CNRS-ENS 8539 & CERES-ERTI, 24 rue Lhomond, 75231 Paris Cedex 5, France Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA e-mail:
[email protected] J. Sun Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China e-mail:
[email protected] M.A. Zárate Instituto de Ciencias de la Tierra y Ambientales de la Pampa (INCITAP), Avenida Uruguay 151, 6300 Santa Rosa La Pampa, Argentina e-mail:
[email protected] P.