The Asian monsoons are triggered by complex interactions between the atmosphere, Asian
and African orography, and the surrounding oceans, resulting in highly seasonal climate …

Intensification of northern hemisphere glaciation (iNHG),~ 2.7 million years ago (Ma), led to
establishment of the Pleistocene to present-day bipolar icehouse state. Here we document …

The modern pattern of the Asian monsoon is thought to have formed around the
Oligocene/Miocene transition and is generally attributed to Himalaya–Tibetan Plateau (H …

In parallel with pronounced cooling in the oceans, vast areas of the continents experienced
enhanced aridification and restructuring of vegetation and animal communities during the …

Considerable debate exists regarding how the East Asian summer monsoon (EASM) varied
over the late Miocene, limiting our ability to understand the long-term evolution and forcing …

Continental-scale drainage reorganization is generally understood to result from landform
evolution forced by the coupling between tectonic activity and climate change, attracting …

Asian monsoon systems influence billions of people and understanding past monsoon
variability and dynamics is instructive in predicting future trajectories. Recent studies have …

Aeolian accumulation in the Chinese Loess Plateau (CLP) including Quaternary loess and
Miocene-Pliocene red clay has documented the evolution of Eastern Asian Monsoon, history …

The middle to late Eocene marked a key transition from greenhouse to coolhouse. However,
a lack of high-resolution and temporally well-constrained continental records hinders our …

毛学刚, 刘秀铭, 赵景波, 王练. 黄土高原西部上新统风成红粘土的微形态特征及其古环境意义[J].
第四纪研究, 2023, 43 (5): 1172-1185. doi: 10.11928/j. issn. 1001-7410.2023. 05.02引用本文 …