Chemical weathering over the last 1200 years recorded in the sediments of G onghai L ake, L vliang M ountains, N orth C hina: a high‐resolution proxy of past climate

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 important E arth surface processes: physical erosion and chemical weathering. In this study, an AMS 14 C ‐dated 2.8‐m‐long sediment core, GH 09 B 1, from L ake G onghai in north‐central C hina 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 axis PCA1 explained ∼53% of the variance in the assemblage of elements/oxides with significant positive correlations between PCA 1 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 in PCA 1, chemical index of alteration ( CIA ), R b/ S r ratio and other oxides ratios indicate stronger chemical weathering due to a wet climate during the Medieval Warm Period ( MWP ). However, the MWP was interrupted by an interval of relatively weaker chemical weathering conditions from AD 940–1070. Weak chemical weathering under a dry climate occurred during the L ittle I ce A ge ( 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 from G onghai L ake as well as with the speleothem oxygen isotope record from W anxiang C ave, but do not show a significant correlation with the temperature record in N C hina, 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.