Chemical weathering over the last 1200 years recorded in the sediments ofGonghaiLake,LvliangMountains,NorthChina: a high‐resolution proxy of past climate

Abstract

Increasing interest in global climate change has led to attempts to understand and quantify the relationship between chemical weathering processes and environmental conditions, especially climate. This interest necessitates the identification of new climate proxies for the reconstruction of two importantEarth surface processes: physical erosion and chemical weathering. In this study, anAMS14C‐dated 2.8‐m‐long sediment core,GH09B1, fromLakeGonghai in north‐centralChina was subjected to detailed geochemical analyses to evaluate the intensity of chemical weathering conditions in the catchment. Multivariate statistical analysis of major and trace elemental data of 139 subsamples revealed that the first principal component axisPCA1explained ∼53% of the variance in the assemblage of elements/oxides with significant positive correlations betweenPCA1 scores and the separation of mobile and soluble elements/oxides from the immobile and resistant elements/oxides, which is thus able to indicate the chemical weathering in the catchment. These results are supported by the down‐core trends of other major and trace elemental ratios of chemical weathering intensity as well as by pollen data from the same core. Variations inPCA1, chemical index of alteration (CIA),Rb/Sr ratio and other oxides ratios indicate stronger chemical weathering due to a wet climate during the Medieval Warm Period (MWP). However, theMWPwas interrupted by an interval of relatively weaker chemical weathering conditions fromAD940–1070. Weak chemical weathering under a dry climate occurred during theLittleIceAge (LIA), and increased chemical weathering intensity during the Current Warm Period (CWP). Our proxy records of chemical weathering over the last millennium correlate well with the available proxy records of precipitation fromGonghaiLake as well as with the speleothem oxygen isotope record fromWanxiangCave, but do not show a significant correlation with the temperature record inN China, suggesting that the chemical weathering intensity in the study area was mainly controlled by the amount of rainfall rather than by temperature. We conclude that high resolution lacustrine sediment geochemical parameters can be used as reliable proxies for climate variations at centennial‐decadal time scales.