An Active East Asian Monsoon at the Oligocene-Miocene Boundary: Evidence from the Sikouzi Section, Northern China

Abstract

AbstractThe East Asian monsoon forms a significant element of the global climatic system. We here present detailed sedimentologic investigations of the Oligocene to early Miocene succession in the Sikouzi section, northern China, to determine monsoon evolution during this time. The particle-size characteristics and grain surface structures, in combination with the large-scale cross-bedding arrangements, graded bedding laminations, and small-scale deformation structures, type the Oligocene red beds in association I as eolian, attributable to large dune forms. Rare earth element results imply that the Oligocene sediments are possibly sourced from a local provenance in the West Qinling Mountains, excluding a more regional wind system during this time. Packages of thick-bedded dark-red mudstone/silty mudstone as well as subordinate medium-bedded pale-gray fine- to medium-grained sandstone and thin-bedded gypsum, with the massive mudstone/silty mudstone taking dominance, point to a lacustrine deposition with d...