Pedogenic carbonates document abundant paleoenvironmental information. However, the
seasonality of pedogenic carbonate formation varies under different climate regimes …

The mechanisms and processes of precipitation change during warm climatic periods, such
as the Holocene, may provide critical insights into future regional precipitation trends in the …

Goethite/hematite ratios in soils are widely used to reconstruct past climatic changes, but
their accurate measurements have remained challenging due to the matrix effect. Here we …

Magnetism, redness, and Fe oxides are indicators of pedoclimatic conditions. However,
uncertainties with observing how Fe oxides form within soils has led to debates about …

Assessing the impact of precipitation and temperature on soil moisture changes during the
Holocene is essential to understanding the regional ecological environment change in the …

卢红选, 王欢业, 刘旭, 盛维娟, 刘卫国. 2024. 支链GDGTs 与黄土古温度重建: 机遇与挑战.
第四纪研究, 44 (5): 1296-1307. doi: 10.11928/j. issn. 1001-7410.2024. 05.17引用本文 …

The rare earth elements (REEs) in loess sediments may preserve key information of
paleoenvironmental changes in East Asia but remain poorly explored. Here we present the …

Currently, our understanding of global paleotemperatures is primarily based on marine
records. Due to the lack of reliable terrestrial paleotemperature indicators, our knowledge of …

Soil organic matter (SOM) is a critical player in the global carbon cycle and a common
paleoclimate archive, yet the mechanisms governing its evolution, particularly in subsoil (> …

Iron oxides and associated magnetic properties are considered good indicators of the
pedogenic environment and regional climate. However, these indicators are under debate …