Sc. Porter, High-resolution paleoclimatic information from Chinese eolian sediments based on grayscale intensity profiles, QUATERN RES, 53(1), 2000, pp. 70-77
Grayscale intensity profiles from photographic images offer a rapid means o
f obtaining paleoclimate proxy records from Chinese loess, dune sand, and p
aleosols. Although the data can be obtained using conventional 35-mm film i
mages, a digital camera and laptop computer will produce a high-resolution
grayscale profile at a field site within minutes. Comparison of grayscale p
rofiles with profiles of magnetic susceptibility measured down loess and du
nesand sections at sites on the Loess Plateau and Tibetan Plateau in a rang
e of altitudes and climatic regimes shows that the two parameters are highl
y correlated. Therefore, grayscale intensity is a convenient alternative to
magnetic susceptibility for generating paleoclimatic data in the loess and
desert-margin regions of China. The resolution of both grayscale and susce
ptibility profiles ultimately is limited by bioturbation, which is most pro
nounced in paleosols. (C) 2000 University of Washington.